S M I T H S O X I A 4 N C O N T R I B U T I O N S T O B O T A K Y N U h l B E R 1 9 The Genus Thrinax (Falmae: Coryphoideae) Robert W. Read SMITHSONIXN INSTITUTION PRESS City of IYashington 1975 A B S T R A C T Read, Robert W. The Genus Thrinax (Palmae: Coryphoideae). Smithsonian ContriOutions to Botany, number 19, 98 pages, frontispiece, 57 figures, 1975.-The history, distribution, ecology, morphology, cytology, anatomy, and taxonolny of the four species of Thrinax are presented. The objective is to demonstrate that quantitative characters, formerly believed to be important in distinguishing species, merely represent random selections from clinal patterns and are therefore of little value in distinguishing taxa. Certain characters described for the first time-leaf sheath, blade, color and puberulence of the inflorescence-have proved to be of great taxonomic value. Particular attention is given to tlie variability of Thrinax parvifiora Sw. over a wide range of climatic conditions and to its unusual phenotypic behavior, in special situations, in the Cockpit Country and on the slopes of Mt. Diablo in Jamaica. The haploid chromosome number (determined at pollen-tube mitosis) of all four species is 18. Little difference in size or morphology of the chromosomes exists among these taxa. Anatomically all four species can be distinguished by comparison of leaf segment sections. The taxonomic portion is a thorough revision of the genus. It includes literature references, synonymy, complete descriptions, and specimens examined. Thrinax parvipora Sw. and T. excelsa Lodd. ex Griseb. are endemic to Jamaica while T. mdinta Lodd. ex J. A. & J. H. Schult. occurs in the littoral of the Greater Antilles (except Puerto Rico), tlie Bahamas, Florida, and Mexico. Th1-inax morrisii H. Wendl. occurs on most of the islands from Anegada (east of the Virgin Islands) to the islands off the coast of British Honduras, and Florida, but not in Jamaica. OFFICIAL PUBLICATION DATE is handstamped in a limited number of initial copies and is recorded in the Institutions annual report, Smithsonian Year. SI PRESS NUMHFR 5125. SI.RIES COWR n m m : Leaf clearing from the Katsura tree Cercidiphyllurn jnponicunz Siebold and Znccarini. Library of Congress Cataloging in Publication Data Read, Robert L$’., 1931- The genus Thrinax (Palmae: Coryphoideae) (Smithsonian contributions to botany, no. 19) 1. Thrinax , I. Title. 11. Series: Smithsonian Institution. Smithsonian contributions to botany, QKl .S274’i no. 19 [QK495.P17] 581’.08s [584‘5] 74-6489 no. 19. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Price $2.40 (paper coler) Contents Page Introduction 1 Acknowledgments . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2 History of the Genus . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 Distribution and Ecology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 Thyinax radiata . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 Thrinax excelsa . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 Thyinax mowisii . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Thrinax parviflora . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 Morphology 17 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Selection of Samples for Measurement . . . . . . . . . . . . . . . . . . . . . . . . . . 17 Caudex . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 Leaf . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 Inflorescence . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 28 Germination of Seeds . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38 Pollen . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38 Anatomy . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39 Anatomical Key to the Species of Thyinax Using Laminar Characters . . . 41 Material and Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 Lamina . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 Material and Methods . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 44 48 52 59 Cytology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 44 Phytomorphosis and Zoomorphosis in Thrinax parviflora . . . . . . . . . . . . . . . Breeding System . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48 Variation of Thrinax pai-viflo~.n., . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Transect from Portland Ridge to Hollymount, Jamaica . . . . . . . . . . . . . Donkey Trail Transect . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 63 Thyinax Swartz . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 66 Key to the Species of Thl-inax . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Typification of Thrinax ParuifEora . . . . . . . . . . . . . . . . . . . . . . . . . . . . Diagnostic Key to the Subspecies of Thrinax parvipora . . . . . . . . . . . . 68 1 Thyinax paruiflora 69 70 74 75 76 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Thrinax parvifiora Swartz subsp . parvipom . . . . . . . . . . . . . . . . . . . . . Th?~inax pat-uiflora Swartz pziberula, new subspecies . . . . . . . . . . . . . . . . 2 . Thrinax radiata . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 77 3 . Thrinax excelsa 84 4 . Thrinax monisii . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 88 Appendix 11: Nomina Incerta et Dubia . . . . . . . . . . . . . . . . . . . . . . . . . 95 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Appendix I: Binomials Published in the Genus Thrinax . . . . . . . . . . . . . . 94 Literature Cited . . . . . . . . . . . . . . . . . . . . . . , . . . . . . . . . . . . . . . . . . . . . . . . . 96 ... 111 The Genus Thrinax (Palmae: Coryphoideae) Robert W. Read Introduction Thrinax is a genus of true palmate-leaved palms in the subfamily Coryphoideae. The genus occurs only on the islands of the northern Caribbean and the nearby continental coastal areas bordering on the Gulf Stream. Its nearest allies are Hemitlzrinax and Coccothrinax, which share the same general range of distribution. The genus Thrinax may be recognized by the unarmed split leaf-petioles, flowers with a single whorl of perianth, and nonruininate seeds which have the center partially or completely intruded by the testa. Stamen number varies from 5 to 15 (rarely more) and the abaxial surface of the leaf may or may not be white or silvery. Fully mature fruits are always white or ivory colored. At the beginning of this study five species of Thrinax were attributed to Jamaica with an additional seven or eight distributed throughout the Caribbean region apart from Jamaica. With the exception of a few quantitative Characters of dubious value, no convincing differences could be found between Beccari’s T. parviflora, T. tessellata, and T. harrisiana. This was also true concerning T. mowisii of FVendland, T. ponceana and T. psaeceps of Cook, T. drtidei and T. puncttilata of Beccari, and T. miclocarpa ol‘ Sargent. Similarly, Bailey’s T. parvifloi.a and T. excelsa were separated in a key based solely on the size of the fruit and leaf segments. During the present study it has been found that, with the exception of Beccari’s T. parviflora (in part), none of the names in common use Robert Tt’. Read, Department of Botany, Smithsonia?~ I t i s t i - tution, Washington, D.C. 20560. 1 have been applied correctly, and all of the names of the species not occurring in Jamaica are to be relegated to synonymy or to subspecific status of the least commonly used specific epithet. The reasons for the previous confusion are inadequate herbarium material and a lack of understanding of the variability of Thrinax species in natural populations. My interest in Thrinax developed as a result of an attempt to understand the palms of southern Florida, and the necessity of clearing up nomenclatural problems of the plants used in my cytological studies. After several trips to the islands of the Caribbean, and to Jamaica in particular, it was soon obvious that the same taxon known in Florida as T. parviflora was known under a different specific epithet on each of the various islands. In Jamaica, the type locality of T. parzri%ora Sw., the Florida taxon was known as T. excelsa and the epithet T. parviflora was applied to an entirely distinct but very poorly understood local taxon. It was clear that a study of the Jamaican taxa of Thrinax was essential before an understanding of the taxa elsewhere was possible. Before revisionary work in palms could be accomplished at the species level, it was essential to understand the range and type of variation possible within each taxon and to have some understanding of the effects of environment on the variation. It was also important to determine the kinds of characters (key characters) which unquestionably distinguish taxa and which remain recognizable regardless of environment. Far too often descriptions of palms drawn from incomplete and and inadequate collections have been relied upon 2 for identification. The situation clearly stated by Joseph D. Hooker and Thomas Tlionison (1855) has been found true today in the study ol‘ palms. They wrote that “the niore specimens we examined, and especially if taken from different indivicluals, the greater the difficulty in framing diagnosis. . . . iVe are firmly convinced that no species can be properly defined, until it has been examined in all the variations induced by those differences in climate, locality, and soil.’’ It seems superfluous to restate these well-knoTvn facts, but this basic information lias yet to be acquired in most tropical families, particularly those with large cumbersome plants such as the Palmae. No amount of statistical analysis, numerical taxonomy, or classical taxonomy for that matter, Trill solve the problems of species definition when based on inadequate collections, incomplete herbarium specimens, and insufficient knowledge of ecological tolerances. A study of tlie scope undertaken here is too laborious and time-consuming to be applied Fvithin the foreseeable future to niore than a fraction of the palm species described. Proof of conclusions regarding genetic differences is not possible without transplant experiments; but the obstacles to long-term experiments ivitli such slolvly developing plants as paliiis preclude this approach. Proper study of palms lias until recently also been hampered because ol their size, complexity, general unuielcliness, and inaccessibility in tropical regions. In addition, portions of the plants \vliicli did not conl‘orni to the limits set by the standard herbarium sheet or “pigeonholes” were often tlisregarded by collectors. The opportunity ~ v a 5 taken during this study to make intensive observations of Tkiirznx in tlie field and to analyze antl present the data in a comparative Tvay for taxonomic purposes. This has led to detailed examination of the development and mature condition 01 all organs Tvliose nature could in any Tray assist the accurate antl complete definition of the genus Tlzrinnx antl its species in Jamaica. The result is a statement of tlie natural variability of Tlz~iiznx against the background ol the pliysical factors 01 tlie environment, leading to a complete taxonomic revision of the genus. . C K ~ . O ~ ~ L E L ) G ~ l T ~ T s . - T h e basis of the present monograph is a thesis for the P1i.D. degree. The author rrishes to express his sincere appreciation to 5hlITHSO\I4\ COATRIBLTIOXS TO ZOTANY Dr. C. Dennis Adams of the Botany Department of tlie University of the ’1Vest Indies for his valuable advice, guidance, and patience during the investigations and preparation of tlie original manuscript; and to Dr. Harold E. Moore of the Liberty Hytle Bailey Hortorium, Cornell University, who has contributed immeasurably by providing information, suggestions, and reading tlie manuscript. Very special thanks are extended to the Botany Department of tlie University of the West Indies, and to George R. Proctor of the Institute of Jamaica, for providing transportation, assistance, and facilities during the studies in Jamaica; and especially to Dr. and Nrs. Ivor Cornman for their contribution to the success of many trips into the “bush.” Sincere appreciation is also extended to tlie directors and staff of numerous herbaria and libraries for photographs, loan or use of herbarium material and freely given information, assistance, and encouragement; especially Dr. William Dress of Corriel1 University; Dr. George Bunting, formerly at Cornell University; Dr. Richard A. Howard, Director of tlie Arnold Arboretum; Drs. Lyman B. Smith and Velva Rudd of the National hluseuni of Natural History, Smithsonian Institution; Dr. Howard Irwin of the New York Botanical Garden; Mr. George W. Rosner, Richter Library, University of Miami, Florida; Dr. T.V. T. Stearn of the British hIuseuiii (Natural History); hlr. ’Iy. hlilne-Redhead of Kew Royal Botanic Gardens; Dr. C. E. B. Bonner of the Conservatoire et Jardiii botaniques, Geneve; Prof. Tycho Norlindh and Barron Sparre of the Naturhistoriska Riksniuseum, Stockholm; Drs. H. AIerxmuller and A%. Schreiber of the Botanische Staatssammlung, hlunich; antl to hlr. Harold Loomis, former director of the United States Plant Introduction Station in Xliami, Florida, lor his early encouragement and knowledge of the palms at the time I was starting to get interested in the family. Additional research ~ v a s made possible for me as a National Research Council Visiting Research Associate in the Department of Botany, Smithsonian Institution, later as a Research Associate of tlie Department, and now as an Associate Curator in the same Institution. This has made it possible to change “A Study of the Genus Thiinnx in Jamaica” into a monograph of the genus as a whole. AUXIBER 19 3 History of the Genus Although Linnaeus did not include any palms of the Caribbean islands in his Species Planlarum, their existence had been recorded by various authors during the century prior to 1753. In tact Sir Hans Sloane (1696) described ten true palms in his Catalogiis Plantarurn, of which one has been determined to be a member of the genus Thrinax. It is important to understand that while Sloane ~ v a s writing specifically of palms he observed in Jamaica, he also attempted to identify them with descriptions already in the literature. This association of earlier accounts Tvith the Jamaican palms n’as often incorrect; therefore in order to understand the application of Sloane’s descriptions, it is essential to ignore these misleading synonymies. Nor did that practice end with Sloane for it has continued to plague the study of palms to the present. The palm to be discussed most fully in the present paper appeared for the first time in the literature as the last true palm mentioned by Sloane (1696: 178, 179). Sloane unfortunately associated the Jamaican “thatch” with Ray’s “4. Palnin Biasiliensis p ~ z i n i f e ~ n ” (1688: 1368 ) because of the similarity of the leaf form. Ray’s palm, liolvever, is Brazilian antl has been determined to belong to the genus Copemicia (Noore, 1963). Since no Cofiernick has been found in Jamaica, the plicate-leaved palm growing “In sylvis saxosis k collibus sterilioribus Jamaicae Insulae ubiyue reperitur” (Sloane 1696: 179) can only be one of those presently knoivn as Thi.innx or Coccotkiinox. In 1525, Sloane again cited “Palma Bmsiliensis” as the “thatch” (1). 121) of Jamaica and again the sole indication of its identity, in the text, is that, “This grows on all tlie Honey-comb Rocks of this island” (p. 122). Sloane’s pl. 213: fig. 2 of tlie same lvork, holvever, unquestionably illustrates a Thrinax-like palm leaf. The lack of teeth on the petiole, the nonacuminate hastula, and the irregular fusion of the segments, it‘ this xvas intended to be diagnostic, clearly intlicate that this illustration depicts the plant no~v determined to be Thrinax pawij7oi.a Sw. The first complete account of a palm readily identifiable as Th~inax parvij7orn Sw. in the literature appeared in Patrick Browne’s Civil ai7d X n t - ziral Histoyy of Jamaica, published in 1756. The Latin diagnosis of “Coryphn I. Palniacen” 1 is accurate, but the association of Kay’s Brazilian palm again apparently contributed to Grisebacli’s (1 864) belief that a Copemicia was to be found in Jamaica. In 1‘784, Olof Swartz left Sweden at the age of 24 and spent tlie next two years traveling through the West Indies and Jamaica. Follolving his trip through the Caribbean, Swartz \vent to England to study the Hans Sloane Jamaican collection and the herbarium of Sir Joseph Banks at the British Museum. Within two years of his return to Siveden he published (1788) the first of his major works 011 LVest Indian plants, Souti Genera et Species Plantal- unz sell Prodronzzis. In the Prodromus, as it is known, appeared the first published description of the palm Thi.inax parviflo~a. A diagnosis of the genus appeared on page 4, number 29, and tlie single species was described on page 57. It is possible that Swartz went to Jamaica with some foreknorvledge of the palm lie later described as Tlzrinax pawifiora. Although he gave no indication in the P?.odromiis of the source of the name or its meaning, he attempted to rectify his debt to Linnaeus the younger by inserting a note ol‘ acknowledgment in his Flo1.a (1797). That the younger Linnaeus was preparing to publish the binomial, before his death in 1783, is now an establishetl fact. =\ complete and accurate description of T h ~ i - nax, under the binomial T. pat~viflo~a, has been found in an unpublished manuscript belonging to the younger Linnaeus. The manuscript reproduced in part in Figure 2 is clearly the source ol the binomial, antl whether Sivartz saw the manuscript before he ivent to Jamaica or upon his return is not known. Linnaeus’ description is a composite of Browne’s Coqpha I., Sloane’s illustration (pl. 213) and a specimen of an inflorescence preserved in the Banksian herbarium at the British Museum. Since the Linnaean manuscript was never published, we must consider only Swartz’s speci- Correspondence between Dr. Bailey and the Linnean Society of London in 1937, in a lcttcr signed by 5. Savage, Assistant Secretary, revealed that “no specimen of the species of Corjl~ha described by Patrick Browne in Hist. Jni?!. p. 190 exists in the Linnaean Herbarium. In Linnaeus’ copy of Browne’s book there is no annotation by Linnaeus to show that a specimen of this plant was received by him with Browne’s herbarium.” ’ Proritled by the courtesy of the Linnean Society, London, through Dr. H. E. Moore of Cornell I*niversity (List no. 40, “ I h n. /i 1. Palmarti in De icript iones”). 4 SMITHSOSIAN COSTRIBUTIONS 10 BOTAKY FIGURE I.-Tlfrinas pnruipotn, cut and removed froin the forest for photographing, being examined 117 Dr. Itor Cornman. KUMBER 19 5 men and his descriptions based on personal experience in Jamaica in typifying Thrinax pawiflova. The finding of the Linnaean manuscript is, however, of historical significance and provides answers concerning the source of the binomial and its meaning. Thrinax according to the manuscript is derived from the Greek 6giva5, which can be translated as “trident” or as indicated by Linnaeus “ventilabrum” meaning, “winnowing fork.” Thrinax was the tenth genus described in the Palmae after the publication of Linnaeus’ Species Plantarum in 1753. It should not then be surprising that a number of dissimilar and unrelated palms have been included in the genus (see Appendix I). The original description by Swartz in the Prodromus (1788) clearly sets down characters that are still diagnostic for the genus. The six-lobed perianth cupule, unilocular ovary, and infundibuliform stigma apply exclusively to the Thrinnx alliance. Early in 1789, W. Aiton reported in his Hortits Kewensis that there was a palm growing at Kew under the name of Thyinax parvipoia, which was introduced by Dr. William Wright upon his return FIGURE P.-Facsimile of a portion of Linnaeus the younger’s unpitblished manuscript on Thrinax paruipora. 6 SMITHSOSIAK CONTRIBUTIONS TO BOTANY from Jamaica in 1777. The palm at Kew ~ i a s mentioned again by IV. T. Aiton in 1811, and again seventy-one years later by Hooker in the Kew Report for 1882. Thiinax was treated in the eighth edition of Linnaeus’ Genera Plantarum (edited by C. D. Schreber, 1791), and T. parviflora was treated later in the fourth edition of the Species Plantamm, edited by C. L. Willdenow (1799). In his magnum opus on West Indian plants, Swartz (1797:613-615) published a much amplified account of the genus and species in the Flora Indiae Occidentalis; flowers and fruit were illustrated on plate 13. The first mention of additional species in the genus Thrinax appeared in 1829 in Desfontaines’ Catalogus Plantariim (3rd ed.) where T. radiata and T. argenten appeared in a list without descriptions. The father and son team of J. A. and J. H. Schultes (1830) took up the Desfontaines names for which, with the addition of T. piimilio, they published diagnoses based on specimens sent by Loddiges, a nurseryman, to the botanical garden at Munich. hlartius (1838) elaborated on tlie clescriptions of T. parviflora, T. radiata, and T. al-gcntea and added two new species, T. miiltiffol-a and T. barbadensis. In 1845, nurseryman Loddiges, froiii whom Alartius also obtained several specific epithets, published a catalog of palms; there are no descriptions, thus the names that Tiere not already provided with diagnoses are nomina nuda. During the one hundred years between treatments by Rlartius and Bailey (1838 and 1938 respectively) forty additional epithets were attributed to the genus Thrinax. In 1866, A. H. Grisebach attempted to erect a new genus, Porothrinax, based on lh1inax piimilio of J. A. & J. H. Schultes. The lack of a separate diagnosis or description for a monotypic genus based on an old species does not satisfy the requirements of the present International Code of Botanical Nomenclature (see Appendix 11), so I am treating the genus as a nomen nudum. Charles S. Sargent (1899:88) made tlie first clear division of the genus when he recognized that specimens collected in Florida, and attributed to Thrinax, could be separated from that genus on the basis of the seeds being “vertically sulcate by the infolding of the testa into the ruminate albumin.” Thus he described Coccothrinax, a new genus based on C. jiiczinda Sargent. He also transferred Thrinux garberi Chapman into the genus to make a second species, C. garberi (Chap.) Sarg. He further suggested that Thrinax radiata and T. argentea both of Lodd. ex. J. A. & J. H. Schultes might also belong in the newly described genus, but it remained for K. Schuinann to make the formal transfers in 1901. Sargent (1899) divided the species remaining in Thrinax into two sections, the Peditellatae and Sessiliflol-ae, and described two new species, T. floridana and T. keyelzsis. In 1883, Bentham and Hooker included Thrinax along with their newly founded Hemit hl-inax in the tribe Corypheae, but Drude (1887) reduced Hemithrinax and Porothi.iizax along with Euthl-inax as subgenera of Thi.inax. Thus it remained until Beccari (1907) produced his work on American Coryphoid palms. Beccari raised Hemit hrinax to full generic status again and divided the Corypheae into two subtribes: Eucorypheae, characterized by the perianth having two whorls and the ovary being three-locular or with three carpels; and Thrinaceae, with a periantli of a single six-lobed whorl and the ovary consisting of a single uniovulate carpel. He divided the genus Thrinax into two subgenera based on the degree of intrusion of the testa into the seed: Ezithrinax, including the earlier Porothrinax of uncertain identity, and Typh10- thririnx. No mention was made of Sargent’s earlier division of the genus based on pedicels. The genus as outlined by Beccari (1907) contained ten species that he considered good, including four new names, plus three names of dubious application. Beccari (1912) published a series of articles on the palms of Cuba in which he treated three species of Thrinax. A supplement to his earlier work, in English, was included in a larger posthumously published xiork in 1933 [“1931”]. ’1 new genus, Sitnpsonia, based on Thyinax microcarpa Sarg., it-as published by Cook (1937); however, the requirements of Article 36 of the International Code of Botanical hTomenclatzil-e, 1966, were not satisfied and the genus was not validly published. Bailey (1938), in an attempt to clear up some identification problems among palms in horticulture, produced a comprehensive study on the genus Thrinax. He accepted ten species, which he arranged in two subgenera as suggested earlier b~ Sargent. In a review of Beccari’s work Britton wrote (1908:240) that, “This is probably the most SUhiBER 19 7 difficult of the American palm genera to untlerstand,” to which Ba.iley (1938: 133) replied thirty years later: Any subsequent student of the genus will be sympathetic with this estimate; but many of the difficulties banish if one knows the plants in the field, has really good herbarium material, and does not assume he must necessarily recognize all the species that have been described. Differences one draws diligently from poor herbarium sheets may disappear in the living plant. The present author must agree with this, antl with Bailey’s earlier statement (1938: 133) concerning Thyinax paixipoi,a Sw. and T. nzicrocai,pa Sarg. that, “If the student understands these two, all tlie other species fall readily into place.” Unfortunately Bailey did not have an adequate understantling of T. payvifloya in Jamaica, hence the species there did not fall so readily into their proper places. Distribution and Ecology Palms of the genus Thi,inax occur only on alkaline substrate, specifically coralline sands or limestone outcrops, from sea level to about 1200 meters elevation. They are distributed from areas of strong seasonal drought with rainfall averaging 100-1 12 cm per year (with no more than 6 months having rainfall less than 8 cm per month) to regions where the rainfall may reach 762 cm per year. Two species endemic to Jamaica-Thyinax pni-uipol-a antl T. excelsa-are restricted entirely to exceedingly welldrained sites far from the influence of salt spray. Thyinax radiata, in addition to Jamaica, is widely distributed in tlie littoral throughout the northern Caribbean and nearby shores of the Gulf Stream, and tolerates considerable exposure to salt-laden winds. The fourth species, T. mowisii, not found in Jamaica, is fairly tolerant of salt and, although usually at sites similar to tlie aforementioned, is commonly found farther inland beyond the worst effects of salt spray. Each of the three species in Jamaica is confined to one of three major environmental situations (see Asprey, 1959): e.g., Dry Evergreen TVoodlantl or Thicket, Lower Rlontane Rain Forest, and Littoral Woodlantl or Thicket. Species of Thyinax have not been found naturally in areas lacking limestone or alkaline sand, they are strict calciphils. -rHKINAX RADIhTA.-one Of the tWO most widely distributed species in the genus, T. ~ a d i a t n , is found only in coastal areas on limestone and alkaline sand, under tlie influence of salt-laden breezes, throughout the Greater Antilles (excluding Puerto Rico). It is also found on many of the smaller islands to the north and wesr such as the Cayman Islands and tlie cays off the coast of Cuba and British Honduras, the Yucatan Peninsula of Xlexico, the Bahama Islands, and southern Florida. In nature this palm is confined to saline conditions of the littoral but where there is adequate rainfall (127-254 cm per year) throughout the year. This is also the most commonly cultivated species and is grown under various conditions of soil and moisture far from the influence of salt. In Jamaica, Thyinax yadiclta may occur in dense stands but is more coinmon in small scattered populations along most of the coastline from extreme eastern Morant Point along the north coast west to Negril lighthouse and south to Little Bay. A small population also occurs at Long Acre Point, near Black River, and another is believed to be on Big Pelican Cay some distance off the southern coast of Jamaica. In 1958, G. F. Asprey and A. R. Loveless described a new addition to their list of Littoral Dry Evergreen formations in Jamaica based on a population of Thi inax 1-ndinta situated at Galina Point on tlie north-central coast in the parish of St. Mary. This formation, which they called “Littoral Palm thicket,” occurs on a raised coralline limestone shelf, 3.05 to 7.62 in (10 to 25 ft) above sea level. The shelf is relatively flat, devoid of soil, and is exposed to the full force of strong salt-laden trade winds. The sea is frequently rough and breaks over tlie low cliffs to produce a splash zone up to 12 meters broad. The species forms a characteristic feature of the littoral hedge, becoming increasingly plentiful on the landward side, “where it would appear to take the place of Littoral Evergreen bushland, but no explanation as to why this occurs can be offered” (p. 560). The authors further pointed out (p. 560) that Asprey and Loveless (1958) failed to distinguish between T. pnrzli/7orn Sic.., a conspicuous element in their studies on the Dry Evergreen thicket of Portland Ridge on the south coast, and the \ery different T. rndintn at Galina Point. SMITHSONIAN COSTRIBUTIOSS TO BOTANY The raised limestone beach is dominated by Thrinns pnrviflora [sic] to the exclusion of other plants. The trces grow out of fissures in the bare soilless rock and vary in height from 73-12! m (25-40 ft). The) are spaced, on the average, about 1.2 m (4 ft) apart and form a closed canopy. The palm reproduces actively since seedlings abound and thc plant is evidently in a most favourable environment. 4 somewhat similar situation occurs at Morant Point near the lighthouse where the palms form small stands in the thicket along the windward coast. Throughout the rest of its range in Jamaica, T. mdintn occurs as scattered individuals in coastal thickets within the range of salt spray. The dense stand at Galina Point is not unique, for of Florida’s upper Keys, J. K. Small (1925:53) wrote: “There the groLvth is phenomenal, or at least it was, before the lust for destroying every living thing reached these islands with the advent of civilized man. Thatch hammocks clothed large and small areas.” In some small low areas and on outlying ke)s the palms still dominate the landscape. In the paper by Xsprey and Loveless, a site at Fort Point on the eastern edge of Discovery Bay FIGURE 3.-The Cockpit County of western Jamaica, in the vicinity of Barbecue Bottom. NUMBER 19 9 (Dry Harbour) was also described. Fort Point is approximately 36 miles west from Galina Point. Meteorological data used for both localities were based on records for Richmond Llandovery Sugar Estate, which is nearer to Fort Point than to Galina Point. The rainfall figures quoted were 55 to 70 inches (139.7-177.8 cm) per year which, when compared with evaporation figures over the same period of seventy years, presents a condition where there are only 5 months in an average year when precipitation exceeds evaporation. It must be realized, however, that the utilization of such figures is indeed tenuous in a region where abrupt changes can occur in very short distances depending on the exposure and topography. According to the most recent rainfall figures, Galina Point, at the western edge of one of the wettest regions of the Island, has between 60 and 80 inches (152.4 and 203.2 cm) of rain per year, while Fort Point is in a region of considerably lower rainfall not exceeding 50 inches (127 cm) per year. The preceding observations are brought out be- FIGURE 4.-Thrinax radiata, base of the caudex and low mound of surface roots, growing on exposed and eroded limestone in the Florida Keys. 10 SAlITHSONIz4N CONTRIBUTIOSS TO BOTANY cause even as Asprey and Loveless noted (1958: 561): “The only major anomaly in the data is brought about by the megapliyllous palm Thiinax parviporu Sw. [sic].” Had they recognized that the palm from Galina Point was distinct from the palm in their Portland Ridge studies, a very important fact would have been realized and quite different conclusions might have been reached. Characters for separating the two species are in the key to the species in the taxonomic section: however, a very important characteristic, not in the key, is the fact that T. radiata is a true halophyte and T. parviflora is not. Further, T. mdiata occurs only where regular deposition of salt is accompanied by regular high rainfall. Thiinax paiviflora on the other hand occurs not at all where saline conditions prevail but can survive very dry environments. The present author agrees with the observation made by Asprey and Loveless (1958:562) “that the vegetation reflects the climate far more accurately than any meteorological data.” It seems appropriate here to point out a few very important differences between the two localities studied by Asprey and Loveless on the north coast of Jamaica, which bear on the ecology of Thrinux radiata. Galina Point is exposed directly to the full impact of strong trade winds and heavy seas. Ample rainfall is indicated by its proximity to the highrainfall zone of Portland and by the character of the vegetation in the immediate vicinity beyond the reach of the salt spray where herbaceous ground cover is plentiful. Asprey and Loveless noted (1958: 561) that, “The presence of Philodendron sp. [ Iacertim] among the fringing woodland plants indicates a moist habitat,” from which they concluded that “the relationship of Palm thicket to rainfall distribution might repay further investigation.” A further observation by the authors (1958: 562): In view of the fact that the rainfall along the stretch of coastline in which Fort Point and Galena Point are situated is more than twice as much as at Port Henderson, although the monthly distribution patterns are similar, it might at first sight seem surprising that Evergreen bushland is found at both centres. FIGURE 5.--Thrinax radiata in Jamaica: A, near the lighthouse at Morant Point; B, plants exposed along the limestone shelf at Galina Point. SUhIBER 19 11 This is not surprising, for they did not in fact find bushland at Galina Point, it was displaced by palm thicket, and the bushland described at Fort Point is in a much drier area than Richmond Llandovery, where the rainfall records were made. The authors relied too much on interpolation of rainfall data and included too extensive a stretch of north coast in their data. Furthermore the additional effects of strong constant winds in conjunction with salt would produce drought conditions in the spray zone more intense than might be indicated by rainfall figures, no matter how accurate. A short distance away, to the west of Discovery Bay in the vicinity of the Queen’s Highway, Thrinax radiata occurs under what appear to be pessimum conditions for the species. Several widely spaced individuals are growing on the seaward side of the highway on a flat limestone terrace where there is an accumulation of sand and decaying vegetation. Evidence of low rainfall can be seen in the abundant xerophytic vegetation containing plants such as Agave hart isii, Eztphot bin punicea, and Plitrneria jamnicensis, which become increasingly abundant on bare rock toward the east in a thicket of semideciduous trees and shrubs. Coccothrinax jamaicensis, a palm otherwise limited to the drier thicket vegetation along the south coast (Read, 1966), occurs in abundance along the eastern portion of the Queen’s Highway. To.ivarc1 the western end of the Highway, halfway between Discovery Bay and Bengal Bridge, the climate changes rapidly to a more moist environment containing none of the species mentioned as characterizing the dry thicket toward the east. A single plant of T. pat-viflora stands out conspicuously in the ecotone on the inland side of the highway. On tlie seaward side of the highway Coccothrinax persists farther west among the plants of T. 7aclintc2, .\\.here it appears to tolerate increased moisture under saline conditions. It has been the author’s experience with palms in cultivation that many species which occur naturally in a very dry climate also have a high tolerance for saline conditions; e.g., species of Waslzingtonia, Erythen, Hyphnene, Phocnix. That is not to say that the converse is also true, for it is not. At the westernmost end of Jamaica between Orange Bay and Negril there occurs a variety of habitats in a region of fairly regular, often high rainfall. On Orange Point, Thi inax radinta thrives on a limestone ridge a few feet removed from the weatherit orn, absolutely soilless, clinker-type dogtooth limestone. Farther south along the shores of Bloody Bay and inland from Kegril Beach the land is low, almost flat but slopes imperceptibly into the nearby Great Morass. The substrate is white sand, with a very high water table, and T h r ~ n n x tcidzata occurs as scattered individuals along tlie better chained rise, only a few feet above sea level. The species is fairly common along the high cliffs near the Kegril lighthouse and occurs as scattered individuals southeastward to Little Hay and Long Acre Point. THRINAX ExCELsA.-This is a Jamaican endemic which is iery restricted in its distribution, occurring only in the region of the John Crow Mountains 01 the easternmost parishes of Portland and St. Thomas, and on Uncommon Hill, a limestone outcrop on the lower slopes of the Blue Mountains above Fruitful Vale in Portland. Its environmental requirements are rather unusual in that it is limited to the driest, best drained, most exposed situations in the wettest part of Jamaica. According to Asprey and Robbins (1953), the John Crow Mountains are clothed with lower montane rain forest on the lower slopes, Mhere the rainfall may be as much as 762 cm per year. That the vegetation is very characteristic of the substrate and drainage is strikingly illustrated by the situation in the John Crow AIountains. In the vicinity of TVinchester Peak at the southern end of the range, the deep heavy soil on the lower slopes supports a tall forest with a dense canopy. In the relatively low illumination, epiphytes are rare and the undergrowth consists mainlj of seedlings, some ferns, and a few herbaceous plants. Higher on the steep slopes below the peak, the well-drainetl substrate consists of a mixture of soil, decajing matter, and loose broken rock. The forest here is lower and more open with smaller more slender trees but with occasional large emergent trees. Ferns and herbaceous plants are more common in the increased illumination and abundant mcisture. At elevations between 304 and 762 m on the slopes and ridges throughout the range the foundation rock is frequently exposed, particularly along water courses. It is peculiar that in such a wet environment the exposed rock is usually devoid of vegetation other than the palm Thrinax exrelsn, which dominates the forest on nearly all exposed 12 SMITHSOSIAN COSTRIBUTIONS TO BOTANY solid rock. Winchester Peak, at the southern end of the John Crows, receives less rain than elsewhere in the range. The southeast face of this peak is dominated by a palm brake of T. excelsa at between 457.2 and 533.4 m elevation. Throughout the rest of the range of the John Crow Mountains the forest is considerably more dense and more typical of lower montane rain forest, than that just described, because of the greater rainfall. On Uncommon Hill in the northeastern foothills of the Blue Mountains and in the John Crows, where the rainfall is consistently high, T. excelsa occurs only on rock outcrops at the higher elevations. An exception was more recently FIGURE 6.--Thrinax morrisii in the pinelands of New Providence in the Bahamas. This species is found in almost identical associations on Big Pine Key in Florida. KUXIBER 19 13 found on a rocky hill near the mouth of the Rio Grande. THRINAX MORRISII.-~~ith much the same range as Thrinax radiata, this species extends farther east to the Virgin Islands and Anguilla, but it is conspicuous by its absence on both Hispaniola and Jamaica; however, the tiny island of Navassa, situated immediately between tlie two much larger islands, supports a small population of T. mol-risii. In Puerto Rico and Cuba the species is common on limestone hills of the interior where it occupies habitats apparently paralleling those of T. parviflora in Jamaica. Occupying a niche which seems to be intermediate between T. pai.niflol-a and T. ~adiata, the Morris palm apparently cannot compete with either. Although somewhat tolerant of saline conditions, T. morrisii does not readily compete with T. radiata except on the smaller islands where annual rainfall probably falls below the minimum necessary for survival of the latter. Intermittent periods of rigorous drought may also restrict competition from T. mdiata. Thrinax morrisii exhibits a very wide range of tolerance for extremes of climatic conditions. As might be expected from a species that has two synonyms in Puerto Rico, two in Cuba, and two more in the Florida Keys, Thrinax mowisii is morphologically very variable; however, there does appear to be a pattern suggestive of more than a single genotype. Considerably more research is needed before anything more definite can be written concerning the delimitation of subspecies. One of the earliest reports of ecological consideration and competition between palms and other plants appeared in a discussion of T. ponceana by Cook (1901:536): Many of the palms are scattered among the taller shrubs and trees wherever there is sufficient soil and water to permit these to grow and yet not enough to give them exclusive possession, but on many of the drier and more sterile higher slopes the advantage is with the palms. THRINAX PARVIFLORA.-h the broadest sense this species occurs on nearly all exposed and eroded “Jamaican Hard White Limestone” throughout the western two-thirds of Jamaica. Along the southern part of its range Thl-inax pa?-viflom is a conspicuous element of the formation described by Loveless and Asprey (1957:813) as “Dry Evergreen Thicket,” typified by the vegetation of Portland Ridge in the parish of Clarendon. Thrinnx parviflorn ’isas described as “The commonest member,” of the shrub layer, “. . . which although capable of growing much taller, does not do so in this community except where there is a gap in the canopy.” These authors included the species as the principal representative of the Palmae among the five most important families of arborescent species in the Dry Evergreen Thicket. Apart from the presence of the “thatch,” the formation is characterized by the absence of herbaceous ground cover and terrestrial ferns. The substrate is generally deeply eroded bare rock with occasional pockets of shallow soil and very little humus. “Epiphytes are not well developed but are represented by tivo xerophytic species, the bromeliad Tillandsin fascicitlafa antl the orchid B1-oztghtonia sangitinen.” Dry Evergreen Thicket is a widespread formation on most of the hills and ridges of low to middle elevations from sea level to about 457.2 m (1500 ft) where the limestone is naturally exposed. Local variations in floristic composition result from local changes in topography and edaphic conditions. Areas of dry evergreen thickets on Dallas hlountain, Long Mountain, lower llolynes hIountain, antl Ferry Hill in St. Andrew represent the easternmost part of the range of T. pnwifloio. The Hellshire Hills of St. Catherine; Portland Ridge, Brazilleto hlountain, antl Round Hill in Clarendon; and the low irregular hills which rise along the northern edge of the St. Catherine and Clarendon plains, all support a dry evergreen thicket formation which continues northward past Juan de Bolas and llocho hlountains, hlende7 and Point Hills to the slopes of hlt. Diablo. This same formation containing T. painiflorn continues along the base of the May Day Mountains in Manchester froin the vicinity of Clarendon Park south past Round Hill and west toward Alligator Pond, then north along the southivestern escarpment of tlie Don Figuero lfountains in the vicinity of Gutters and Spur Tree. In St. Elizabeth a small area near Bull Savanna in the Santa Cru7 Mountains represents the only significant population in that parish. In a few places at low elevation such as Cane River Gorge, where cool moist air flows down from the Blue Mountains, the physical environment is modified by the lower temperatures and increased atmospheric moisture causing the formation of clew and fogs or increased rainfall. Somewhat similar conditions seem to exist along the Rio Cobre 14 ShfITHSONI.4S COKTRIBUTIONS TO BOTAKY in the gorge between Bogwalk and Spanish Toivn and on the eastern slopes of the mountains near Clarendon Park. In the extreme southwest of Jamaica lies Negril Hill, a long low ridge running parallel to the south coast in a region of moderate precipitation 127-190.5 cni (50-75 inches) per year. Thrinax parvifloiu occurs here at the westernmost limit of its range as scattered individuals between New Hope Estate and Rivival. Similar populations occur to the north along the eastern edge of the Great Morass near Silver Spring, Hanover. Areas of frequent drought, described as Dry Evergreen Busliland by Loveless and Asprey (1957, support only the more drought resistant palm Coccothrinax jamaicensis in the ecotone between the two vegetation formations where i t replaces FICURF 7.--Thrinax paruiflora growing in a siyal field near Palmer's Cross, Clarendon, Jamaica. Notc the heat) texture and coirupated armearance of the IeaFes. T. puivifloia. This is the situation east of Cane River in St. Andrew; south of May Pen, Clarendon; the western end of Portland Ridge; and between Gut River and Alligator Pond in Mancliester. Between Black River and Savanna-la-mar, an area with less than 88.9 cm (35 inches) of rain per year and subject to long drought, T. pa?vzflora is absent and Coccothrinax jamaicensis occurs only near the parish boundary shared by St. Elizabeth and Westmoreland. At Lances Bay in Hanover, an area of high rainfall with over 190.5 cm (75 inches) per year, a few individuals of T. pnrviflora have been found growing on the low rocky slopes overlooking the sea only a short distance from a population of T. 7adiata. While the cliffs supporting the latter face northeast and are exposed to frequent salt-laden winds, however, T. parvifloia occurs only on the lee side of the ridge facing west. Along the north coast, T. pnruiflora has been found at only two localities near the sea: at White Bay, Trelawny, and along the Queen's Highway near Bengal Bridge in St. Ann. The region around 'IVhite Bay apparently experiences occasional drought since the vegetation consists mainly of logwood and thorn scrub. Rainfall is normally under 127 cm (50 inches) per year. The solitary robust plant of T. pnrviflora growing along the Queen's Highway stands among T. radiata and Coccothrinax jamaicensis. Ddphin Head, south of Lucea in Hanover, is a somewhat isolated mass of limestone rising to about 548.64 m (1800 ft). Although dry evergreen thicket occurs on the lower cliffs, the upper ridge and peak are swept by clouds and support a dense woodland. Th?.inax paruifloru is a conspicuous element of the more exposed and higher levels of the mountain. A short distance to the east in the parish of St. James, T. parviflora has been collected at Bubby Hill under conditions similar to those on Dolphin Head. A single plant was seen near Hastings along the road to Maroon Town. It is curious that although conditions appear to be favorable for Thrinau, over the western Cockpit Country the species, with one exception, has not been collected or recorded anywhere between Deeside and Catadupa. The species no doubt occurs as widely scattered individuals, but the fairly evenly distributed and high rainfall of 190.5 to 508.0 cm (75 to 200 inches) per year seems to be the limiting factor " I I determining its exclusion. SUhIBER 19 15 In the vicinity of IVindsor Cave, Trelawny, sharply eroded limestone hills form both the northern edge of the Cockpit Country and the headwaters of the Martha Brae River. The annual rainfall in the area averages between 127 and 190.5 cm (50 to 75 inches) and appears to be fairly evenly distributed throughout the year. The ridges are heavily wooded and T. pal-vipora occurs as widel) spaced individuals; however, the palm reaches its best development on exposed cliffs. 4 short distance to the north where the rainfall is much less, about 127 cm (50 inches) per year, the hills and ridges support larger populations of the species near N t . Pantrepant and Sherirood Content nhere typical dry evergreen thicket again prevails. The eastern portion of the Cockpit Country is characterized by a region of jagged limestone pinnacles and interconnecting ridges 457.2 to 548.6 m (1500 to 1800 ft) in elevation which set off huge pits or “bottoms” often having vertical walls 60.96 to 152.4 m (200 to 500 f t ) high. Thi-znax pn?vlffo~n again assumes a conspicuous place on the top of each pinnacle, ridge, and cliff as at Mango Tree Hi1l.l Frequent rains permit a rather dense wootlland at all places where soil or humus can collect in the “bottoms” and on the slopes betTveen the pinnacles. A peculiar antl most interesting situation exists in the huge cockpit extending from Barbecue Bottom along the road to Burnt Hill. This is fully described elsewhere. East of the Cockpit Country is a region called the Dry Harbour Mountains which closely resembles the Cockpit Country but differs principally in the more extensive scrubby to thicket vegetation and higher elevations. This somewhat drier, rather inaccessible region supports a large population of Thrinax on the numerous ridges and pinnacles, particularly in the neighborhood of Albion Mountain. The lower elevation in the vicinity of Pedro and Grierfield supports a heavily wooded vegetation and relatively fewer Thl-inax. Scattered plants occur in the vicinity of Browns Town where limestone is exposed, but along the northern escarpment the annual rainfall increases steadily toward the east where 190.5 to 254 cm (75 to 100 inches) of rain per year may prevail. Thyinax p a ~ v i f l o ~ a is \$’hen questioned concerning a name for hlango Tree Hill, the local farmers gave the name “Carambi Hill”; however, “Mango Tree Hill” is the name coined b~ G. R. Ploctor of the Institute of Jamaica. found only occasionally near Bamboo and is rare on the cliffs of Fern Gdly. North and east of a line from Bamboo through Claremont, Moneague, Guys Hill, Glengoffe to Stony Hill, Thyinax does not occur except as individual outliers such as that at Fern Gdly, no doubt because of a lack of proper substrate antl the effects of increased rainfall. It is now clear, after comparing the distribution of T. parviflora with a rainfall distribution map, that the greatest concentration of plants of the species is to be found in the region classified as having 127 to 190.5 cm (50 to 75 inches) of rainfall per year with numbers decreasing rapidly as rainfall increases above 215.9 cm (85 inches) per year or decreases below 101.6 cm (40 inches) per year. Optimum rainfall for T. p a w i p o ~ a must then be 101.6 to 203.2 cm (40 to 80 inches) per year. In the center of the Island betlveen the fertile rolling cattle country of Claremont and the rich valley of St. Thomas in the Vale (Ewarton-Linstead) lies hlt. Diablo, a mass of limestone rising gratlually from the north to over 914 m (3000 ft) near the parish boundaries of St. A-inn antl St. Catherine. An extension running to the northeast forms a range of irregular limestone pinnacles (herein referred to as the Devils Backbone) about 762 ni (2500 ft) in elevation along the parish boundary. The principal mass of 5It. Diablo terminates in a very steep escarpment about 609 in (2000 f t ) high along the southeast and west, overlooking Ewarton and Worthy Park respectively. X spur projects to the south and connects with a system of hills, of which Point Hill and RIendez Hill are a part, and encircles the valley of St. Thomas in the Vale to the gorge of the Rio Cobre. Thrinax pn~viflorn occurs on almost all exposed limestone and great numbers cling to the walls of the gorge. The vegetation above 548.64 m (1800 ft) elevation on hlt. Diablo and associated slopes, which are frequently bathed throughout the year in morning clouds and mists, most closely conforms to the formation described by J. S. Beard (1955) as “Dry Evergreen Woodland.” Perhaps a new formation to be called Montane Dry Evergreen IVoodland would be preferred, since Beard’s formation applies primarily to the lower elevations and not to those influenced by clouds and mists. Thrinax parvipol-a occurs on the more exposed cliffs and nearly all of the higher peaks, e.g., Hollymount, Grier Mount, Blue AIountain, Devils Backbone. The environ16 SMITHSONIAS CONTRIBUTIONS TO BOTANY ment is perpetually moist and temperatures are normally in the 20s ("C) or often lower. Softleaved epiphytes are quite numerous on the tree trunks and rocks where a lush growth of moss, miniature orchids (Pleurothallis, Lepanthes), and delicate ferns often obscure the substrate. Hohen- Dergia polycephala and Vyiesea platynema, bromeliads requiring a somewhat drier environment, are restricted to the upper level of the canopy. Gzumania erythrolepis, G. lingzilata, and Vriesea ringens require cool moist conditions and are common on the rocks and lower parts of the tree trunks. The limestone outcrop upon which mature plants of T. parvipora are localized, occurs as ridges and small peaks with intervening valleys of deep heavy soil or scree slopes. Although Thl.inax FKXRK 8.--Thritinx parviflot-a growing at about 914 m elevation on Jlt. Diablo. Sote the open crown and peculiar form of the leaves. Thesc plants and those in Figure 7 probably represent the two greatest extremes of phenotypic variability of the species. KUhIBER 19 seedlings are plentiful on all types of soil, they are not known to reach maturity except on the stable rock outcrop where similar lithophilus species such as Euphorbia punicea and Plzimeiia marchii grow. Similar environmental conditions are met with on nearly all high limestone peaks and ridges such a5 Albion hlountain, Top Hill, Somerset, and Dolphin Head. The foregoing is a general account of the distribution and ecology of Th1inax paruzfloin in Janiaica. Further details of the behavior of this species in two series of habitats where special ecological features can be recognized are described elsewhere. Morphology The genus Thyinax, in common with Heirzitlri inax, Coccothrinax, Zombia, and Haitiella of tlie Thyinax alliance, is distinguished from all other palms by having bisexual floivers in ivliich the perianth consists of a single irregularly lobed cupule. The genus is further distinguished fro111 Corcothrinax, Zombia, and Hnitielln by the splitting of the base of the petiole in the region ol' the sheath (Figure 9c). From HemiLhi.innx it is zipparently separated solely on the character 01 the stamens. Hemithrinax with subsessile anthers, a broad connective, and extrorse dehiscence is in need of additional intensive study, but adequate material of the different species is lacking at present. During this study certain characters, mainly of a quantitative nature and formerly believed to be of diagnostic importance, were given particular emphasis in order to test their useiulness as diagnostic characters. The literature is full of descriptions in which the size of the various organs (usually l'roiii a single incomplete specimen) is all one has for comparison of taxa. Good qualitative characters were all but lacking. mature flowering size plants were considered in tlie data presented. Whenever possible, specimens were taken from all accessible plants in a particular locality (measurements and specimens were collected from every plant exhibiting an inflorescence at some stage from anthesis onward even if the fruit had fallen already). Local populations consisted of all the plants in a particular niche or environment, e.g., a rocky pinnacle, gully, cliff, or hillside. These are usually of limited si~e; how- SELECTION OF SAkZPLES FOR h~EASLJRE1\IEXT.-Onl). ever, if the population was extensive the collections consisted of all the material that could possibly be collected during the time available in one or more trips to the area. In order to study the species in every conceivable environmental situation at all elevations in Jamaica, a great deal of time was devoted to exploring the island in search of new localities. This was necessary in order to describe the range of distribution and the range of tolerance of each species. It was also necessary to collect representative specimens from as many different localities as possible in order to eliminate the bias caused by information from classical collecting areas. As much information as possible was obtained from herbarium specimens early in the study, but a concerted effort was made to re-collect in the localities represented by existing specimens in addition to the numerous new localities. It should be noted that herbarium specimens rarely if ever contain complete leaves or inflorescences. The most conimonly occurring materials on herbarium sheets usually comprise one or more of the lower primary branches of the inflorescence at some stage betneen anthesis and maturation ot the fruit but rarel) at either of these stages, and fragments of a single leaf, most commonly juvenile, Jvithout petiole or sheath. Most frequently if a petiole is present it and the hastula, and the blade, are split in two rendering them fairly useless for measurements. hIeasurements of the length antl diameter of the caudex were made at the time and on the plant froin which leaf and inflorescence specimens were taken. The specimens consisted of one complete inflorescence (usually cut at the sheath level, if the plant \51THSONIAN CON1 RIBUTIOSS TO HOTAUY FIGURE 30.-Scanning electron micrographs of Thritiax pollen magnified about 10,000 times. A, T. parviflora; B, T. radiata; c, T. excelsa; D, T. morrisii. Xote how different the surface pattern appears under the much greater magnification. SUMBER 19 41 ble.” But he states: “In many genera this is no disadvantage since interspecific differences are often only quantitative and are obscured by anatomical variation within a single species.” This statement may be true for other palms but in the genus Thrinax, once the taxonomy is worked out, certain anatomical characters follow the same pattern as the key morphological characters. It is now possible to identify accurately each species of the genus simply by comparing the anatomical characters of the lamina with the following key or the accompanying illustrations. Anatomical Key to the Species of Thrinax Using Laminar Characters I. Laminar cross section composed almost entirely of palisade cells: stomata deeply sunken: abaxial outer epidermal cell walls greatly thickened, surface very irregular . . T. morrisii 1. Laminar cross section composed of either distinct layers of palisade and mesophyll, or palisade cells few and scattered; stomata not sunken: abaxial epidermal cell walls not greatly thickened nor is the surface highly irregular. 2. Palisade and mesophyll layers quite distinct; hails when present large and cornplex with numerous surface cells in cross section. 3. Stomate guard cells in cross section, hooklike in appearance . . , , T. radiata T. excelsa 3. Stomate guard cells in cross section, not at all hooklike in appearance 2. Palisade cells absent or rather uncommon and widely scattered if present; hairs when present, small and with few surface cells; stomate guard cells, in cross section hooklike in appearance hIATERIAL AND h!fETHODS.-In most cases Samples of 2 sq cm each of dry herbarium material were selected and soaked overnight in aerosol (Ayensu, 196‘7). Thin sections were then made by hand using a sharp razor blade with the specimen supported by elderberry pith. The sections were then stained using a 0.05 percent solution of toluidine blue in 0.15 R/I phosphate buffer for a few seconds and mounted in ethylene glycol under glass cover slips. Neither soaking in sodium hypochlorite solution nor heating in hydrochloric acid seemed to make the material easier to section. The material to be sectioned was selected from the midportion of leaf segments, about halfway bet.rveen apex and hastula, between the major veins. The following account of the anatomy of the lamina of Thrinax is based in part on a treatment of the genus by P. B. Tomlinson (1961), but it has been modified significantly by more recent personal observations. Tomlinson’s treatment was unfortunately based on a mixture of both Coccothrinax and ThTinax, closely allied but distinct genera. He (p. 296) concluded that from the material . . . examined, although some of it has not had a reliable name and may have been confused Hith Coccothrinax, there appears to be considerable \ariation in the anatomy of the lamina, particulaily in the stiucture and distribution of the hairs and the disttibution of the ceins ~ T. pamiflora and fibrous strands, Since the taxonomy of Thrinax and related genera seems to be rather confused, little reliance can be placed on the anatomical information which has SO far been recorded until a detailed survey can be made upon a large number of species from accurately established sources. The elements that do not agree with observations on verified Thyinax materials have been removed, and in addition to my own new observations those that do apply to the genus Thyinax have been retained. LAMINA o.--Hnins frequent in abaxial costal regions, each with sunken, elliptical, sclerotic, multicellular bases. Ciilicle thick, Epidermis wholly cutinized, outer wall somewhat thickened. Adaxial epiderniis fairly uniform, costal regions tlifferentiated only above largest veins, cells rather variable, mostly more or less cubical or slightly longitudinally extended, walls not sinuous. Xbaxial epidermis differentiated into narrow costal and wider intercostal regions. Costal cells rectangular, longitudinally extended, narrow, shallow; intercostal cells less regular, shorter, wider, deeper, and slightly papillose. Stomata restricted to abaxial intercostal regions, those of both T. ra- ’ Grateful appreciation i? extended to Mrs. Li5a Keys, graduate Ttudent at the CniLersity of \faswchusetts, for her freelt \olunteered help in the preparation of materials and hand sections used in the laminar anatomy. 42 ShIITHSOSIAS CONTRIBLTIOSS TO BOTASY FICCRE 31.-Camera lucida drawings of Thriiznx leaf sections: A, T. parviflorn (Read 1736, Devils Backbone); B, T. escelsn (Read 193Gb, John Crow Mountains); c, T. radiata (Read 1862, Morant Point); D, T. morrisii (Read 798, Grassy Key, Fla.). KUMBER 19 43 diata and T. parvipora similar in cross section as in Figure 31~,c, while T. excelsa and T. morrisii share similar guard-cell types which differ from the other two species (Figure 31n,~). Hypodermis 1- to 2-layered below each surface but adaxial liypodermis mostly 2-layered; cellfiles often replaced by fibers. Adaxial cells rectangular, longitudinally extended. Abaxial cells more cubical, irregular in intercostal regions. Chlorenchymn with a fairly distinct 2- to 3-layered adaxial palisade (except T. parvipora which has only widely scattered infrequent palisade cells, the chlorencliyma being primarily composed of mesophyll). TIirinax morrisii is distinctive in having the chlorencliyma composed almost entirely of palisade cells. Xbaxial mesopliyll cells more or less isodiametric, compact. Fibers frequent, mostly in strands below each surface. Adaxial strands irregular, with 1-21 (rarely more) fibers per strand irregularly intruding the chlorenchyma, these adjacent to the epidermis or separated from the epidermis by a layer of small hypodermal cells. Abaxial strands with fewer fibers, sometimes cylindrical, mostly adjacent to adaxial epidermis. Veiny mostly in abaxial mesophyll or equidistant from either surface. Outer parenchymatous sheath complete around, or interrupted below small veins, always interrupted both above and below large veins; sheath-cells cubical, often containing chloroplasts. Inner sclerotic sheath completely fibrous around large veins, usually including sclerotic parenchyma adjacent xylem of small veins. Phloem of large veins not subdivided, rarely slightly sclerotic. Transverse com missures usually in abaxial mesophyll, rather infrequent, wide. Ribs most prominent adaxially in proximal part of lamina. Surface layers similar to those of lamina, with few small hypodermal fibrous strands. Central ground parenchyma containing several vascular bundles: those in adaxial ribs with well-developed, somewhat confluent, fibrous sheaths; those in abaxial ribs more or less surrounded by a common sclerotic cylinder. Expansion cells in bands, including fibrous strands, within each fold of the lamina. These studies have provided the only positive means of identifying Thrinax radiata with living taxa. Leaf Axis: Epidermis with more or less cubical cells; walls thickened, cutinized. Stomata occasional, slightly sunken. Hypodermis I-layered, inconspicuous, sometimes slightly lignified. Peripheral chlorenchyma indistinct. Fibrous bundles occasional in chlorenchyma. Vascular biindles uniformly scattered, not congested at the periphery; each with a complete fibrous sheath, usually including 2 wide metaxylem vessels and an undivided, not sclerotic, phloem strand. Cell Inclusions: Stegmata of leaf in short, often continuous, files mostly adjacent to vascular fibers. Silica bodies spherical, spinulose, diameter 12 microns; basal wall of silica cell slightly thickened. Enlarged cells filled with raphid bundles are fairly common between the smaller veins. T’ascular Elements: Vessels: elements of leaf with sclariform perforation plates on oblique end walls. Sieue tzibes: elements of leaf with compound sieve plates on more or less transverse end walls. It was noted by Partliasarathy (1968) that the Thrinax alliance and Licztala are exceptional among coryplioid palms in possessing more arecoid than typically coryphoid sieve plates. Furthermore, he stated that Thrinax in common with other closely allied genera is also set apart from most coryphoid palms by having but a single phloem strand, and sclerotic parenchyma cells in the metaphloem of many vascular bundles. Literntiire: The greatest criticism concerning studies by earlier workers is that most of the material was Lunreliablj identified, as mentioned by Tomlinson (1961). Furthermore the material was either obtained from botanical gardens which are questionably reliable, unless vouchered materials are available at the institution, or the materials were obtained from herbarium specimens Tvitliout citation of specimen numbers or collector. Thus the unvouchered materials used by past workers cannot now be identified with certainty. Tomlinson (1961:296) cited as his material, ‘IT. argenten Lodd. -Kew. Leaf,” which is probably a Coccothrinax; and “T. tessellata Becc. Jamaica. Leaf,” which name is now in synonymy of Thrinax parviflora Sw. Drabble (1904) treated T. excelsn Lodd. and T. pa?vipora Sw., the former name having been applied to T. radiata in Jamaica and the latter to T. radiata in Florida. Gillain (1900) treated T. argentea Lodd. and T. gTaminifolia IVendl., the first a Coccothrinax and the second a nomen incertum. Jost (1887) and Zawada (1890) simply cited “Tlirinax sp.” And of the nine taxa attributed to Thrinax in the study by Pfister (1892) only “T. exceZsn Lodd.” could be a Thrinax but certainly 44 SMITHSONIAN COK?'RIBUTIONS TO BOTANS not of that species. Rudolph (1911) and Solereder and Meyer (1928) worked only with species of Coccothrinax. Cytology 10 The species of Thiinax in Jamaica, in addition to many other similarities already mentioned, have a chromosome complement similar in number antl morphology to other members of the alliance. The results of the present study when compared with previous work (Read, 1963, 1964, 1965a, b) lead to the conclusion that, as far as can be determined, it is not pissible to distinguish between genera ot tlie Thrinax alliance by means of their chromosome karyotjpes. The relatively large size, 1-3.0 (-3.5) microns in length, of the cliromosomes places Thrinax, together with its closest allies, in a group of palm genera having chromosomes of a similar size but which differ primarily in having a 2- whorled perianth and a 1- to 3-carpellate ovary (i.e,, Sclzippia, Ciyosophila, T r i t h i n a x , and Chely- O C G ~ ~ I I S ) . Except for the genera just mentioned antl several genera of dioecious palms, which also have large chromosomes, all other coryphoid palms studied thus far have mostly very small chromosomes, 0.5 to 1.5 (-2.0) microns long. The karyotype for each species exhibits an almost complete gradation of sizes from smallest to largest with some recognizable differences in morphology. With such small chromosomes, however, and with the present technique it has proved unsatisfactory to attempt a classification of size or morphological groupings. Chromosome size may vary considerably among the preparations of a single species or individual depending on the timing of pretreatments or fixation and especially tlie degree of squashing. And although certain cliromosomes are recognizable as having subterminal, submedian or median constrictions, it is extremely difficult to differentiate between real and apparent differences. For example with such small cliromosomes, as so often happens, they do not allvays lie flat or parallel with the level of resolution. It is then possible to misinterpret a chromosome which 1°From work related to a project supported by National Science Foundation grants G-18770 and extension GB-13.54. IVhile in Jamaica the Botany Department of the I:.IV.I. acquired phase-contrast attachment5 especially for use by the author in his research on palm cytology. may have part of its arms bent down or under; thus a submedian or subterminal primary constriction may appear as a median or submedian respectively. An ideal preparation would require squashing to less than 0.5 micron in order to flatten the chromosomes sufficiently. This has not been possible because of the presence of the pollen grains in the preparation. MATERIAL AND METHODS.-A~~ material used in tlie present study was collected from wild plants in the field in Jamaica. 4 detailed description ot the technique has already been published (Read, 1965), therefore only a brief review need be given here. Portions of inflorescence were collected at antliesis or as soon before as possible. The pollen was collected by allowing it to shed on a piece of paper in a draft free room. It was then stored in gelatin capsules and placed in an airtight container with dry silica gel and a color indicator, at room temperature (about 26°C). It was necessary at times to dissect the unopened anthers from the flowers and permit them to dry in the gelatin capsules and silica gel. It was important not to store more pollen in a capsule than would effectively coat the walls when dry, otherwise the possibility of fungal and bacterial contamination became serious. Pollen was sown on a nutrient medium (100 ppm H,BO, in water; 0.02% colchicine in distilled water; 10% lactose or sucrose and 10% gelatin) for tlie study of pollen-tube mitosis. After heating medium slightly it was applied to cover glasses by means of a small cotton swab. Tlie pollen was dusted lightly over the surface of the dry medium and the cover glass then overturned onto a Van Tiegliem cell lined with moist absorbent paper. ,4n improved method was to place the rings that form tlie Van Tieghem cells directly on a layer of moist absorbent paper lining the bottom of a plastic tray. After the prepared cover glasses were in place the container was closed to prevent drying. Tlie tray was maintained at room temperature (about 26°C) and germination was usually found to have proceeded sufficiently within 8 to 10 hours. When examination of sample slides indicated that mitosis was in process, the cover glasses were stained with acetocarmine and made permanent by the vapor transfer method. All counts and drawings Tvere made on freshly prepared slides. The tapping and differential squashing necessary to produce the X'UJIBER 19 FIGURE 32.-Photomicrographs of the chromosomes of species of Thritiax at pollen tube mitosis: A, R, T. pnrviflora, Read 1657; c, T. pnrr?iporn, Read 1675~; D, T. excelsn, Read 1625. (X ca. 2500.) 45 46 SMITHSONIAS CONTRIBUTIONS TO BOTASY FIGURE 33.-Photomicrographs of the chromosomes of species of Thyinax at pollen tube mitosis: A, B, T. radiata, Read 1671; c, D, T. movjsii, Read 143ia. (X ca. 2500.) Note the chromosomes obviously stiH within the developing pollen tube in Figures B, C. KUJIBER 19 47 best figures was not possible after a few hours. Drawings were made with the aid of a camera lucida, and the photographs were made on 35 mm film either in black and white or color (Kodachrome 11). The use of phase-contrast aided immeasurably in distinguishing between closely situated chromosomes and also produced photographs of better quality. Before the present study was undertaken, reports of chromosome numbers in Thrinax were already in the literature; however, as a result of the present revision of the nomenclature among the Jamaican taxa, it is necessary to revise the names cited for the species for which chromosome numbers have been reported. Thrinax excelsa as reported by Venkatasubban (1945) and Read (1963) should be named T. iadiata. Thrinax parvifloia and T. floridana as reported by Read (1964, 1965a respectively) should likewise be named T. mdiata. Thrinax miciocarpa as reported by Read (1963, 1964, 1965a) should be named T. morrisii. Thrinax radiata has been reexamined using native material from its natural habitat. Authentic T. excelsa also lias been studied from material collected in the field. It was particularly interesting, early in the research, to compare the chromosomes of T. parviflora from plants growing in the extreme climates in which the two biotypes occurs. The chromosome number in each case lias been determined to be n=18, agreeing with all other Cory phoid palms studied to the present. Idiograms of each species in Jamaica are illustrated in Figure 34. Thrinax pnrviflora from a lowland habitat at Cockpit, Clarendon, is represented by a, b, and the high elevation phenotype from plants on the Devils Backbone is represented by c, d, e. Thrinax ?-adinfa is represented by idiograms f, g, and T. excelsa by idiograms h, i. FIGURE 34.-Idiograms of Thrinax showing their cornparati\ e karyot) pes. a, b, T. parvipora, Read 167%; c-e, T. patvzflota, Read 1736; f, g, T. radmta, Read 1671; h, 2, T. eucelsa, Read 1625. 48 SMITHSONIAS CONTRIBUTIONS TO BOTAKY Phytomorphosis and Zoomorphosis in Thrinax parviflora The specific epithet “tessellata” was applied by Beccari (1907:Zil) to a specimen from Hollymount at the upper elevations on Mt. Diablo. The name was given in allusion to the fruit which Beccari described as having the “epicarpio distincte suberosotessellato,” a condition common in the cool moist environments where a fungus infection radically alters the exocarp of the fruit producing the condition shown in Figure 2 6 ~ . The fruit can become infected at almost any stage of development. Figure 2 6 ~ shows two stages in the development of the fungiis on young fruits. The fruit on the right has a small area where the epidermis has only begun to erupt as a result of the fungal activity. The fruit on the left has no trace of epidermis remaining as in Figure 26c. Fruits exhibiting both partial and complete alteration of the epidermis are part of the isotype of T. tessellata, herein treated as synonymous with T. parviporcr. The fungus, although observed in situ, has not yet been isolated and identified. In the same environment where fungal damage is common on tlie fruit, the branches of tlie inflorescence also undergo a dramatic change. Extensive grazing by caterpillars causes considerable damage to the epidermis and outer tissues of the branches (Figure 35). So extensive is the damage in some areas, it is seldom possible to find healthy or uninutilated epidermal tissue anywhere on the inflorescence branches. The grazing creates a distinctive pattern of trenches, exposing the fibrovascular bundles, intersected with narrow ridges of ungrazed tissue in Figure 35B. At the lower elevations only occasional damage by larval grazing is encountered on specimens and this is usually of minor importance (Figure 35A). At the higher elevations, however, it is seldom possible to determine the nature of the epidermis (e.g., degree of puberulence), or for that matter even to find ungrazed epidermis at all on fruiting material. The apex of tlie petiole in the region of the abaxial hastula and infrequently even the adaxial hastula are often grazed extensively. Often the abaxial liastular region of the youngest leaf on a plant is completely grazed of epidermal tissue exposing a network of fibrovascular bundles. Breeding System The breeding system is very difficult to understand completely, primarily as a result of the difficulties of observing anthesis in the field. Individual plants may bear as many as 6 to 10 inflorescences each year and at one time. The most conspicuous feature of an inflorescence at anthesis is the predominance of anthers. Lacking conspicuous and enclosing perianth parts, tlie anthers are exposed immediately as the primary branches are extended beyond the primary bracts. The anthers in turn obscure the pistil. Each inflorescence may have between 7 and 21 primary branches. These decrease in size and the number of secondary branches successively toward the apex. Those at the apex may have only 6 to 10 secondary branches. The primary branches below the apex may possess from I7 to 47 secondary branches and each of these may possible for each plant to prOdLlce between 100,000 and 300,000 flowers over a 24-hour period. Consid- FIGURE 35-Grazing by caterpillars has pioduced vai)ing have fro111 about 40 to 115 flowers. Therefore it is amounts of damage to the infloiescence branches of Tflit?lax parzupoia. Vasculai bundles ale exposed in ’‘13.’’ SUXIBER 19 49 ering also that each flower may possess froin 5 to 15 stamens, each of which produces an abundance of light dry pollen, it can easily be seen that the production of pollen by a single plant is phenomenal indeed. The anthers dehisce almost immediately as the sun rises and atmospheric moisture decreases. Normally all parts of the inflorescence are covered with scattered pollen very shortly after anthesis. When an inflorescence was permitted to reach anthesis overnight in a closed office, all surhces, books, and objects in tlie room were visibly coated with pollen within an hour. The light, dry pollen of Thi-inax is conceivably carried over very long distances by the wind and has been determined to remain viable for periods up to 3 or 4 months at room temperature (about 26°C). Pollen of T. fiarvifloia collected on 12 January 1967 was maintained dry in gelatin capsules that were kept in containers of silica gel with a color indicator at room temperature. Samples of this pollen were sown and germinated on the medium used in the cytological studies at intervals over a 4-month period. Pollen viability was excellent at first (between 70 and 80 percent) on 15 January. It dropped to 41 percent by 9 February, and on 27 February had further dropped to 37 percent. On 1 April viability was only 1 percent. It is conceivable then, considering the great quantity of pollen produced by a single plant at one time, that crossing need not be a rare occurrence. 4 n attempt was made to test inhibition to selfing. Pollen froin two different plants was to be placed on the stigmas of emasculated flowers of one 01 the plants. A difference in the rate of pollen germination (determined by fixing and staining an hour or so after pollination) favoring the outcrossed flowers would indicate a resistance to selfing. If this were the case, pollen from nearby plants would conceivably be able to germinate and coinpete rvith the mass of pollen from tlie flower’s oivn anthers. Attempts at emasculation of flowers on fully developed inflorescences in the field proved futile. Within seconds following removal of the enclosing bracts the anthers clehisced and scattered pollen over the pistils. Further attempts were made on inflorescences removed and placed in containers of water in the laboratory. It was possible to remove the unopened anthers by spraying thein with water. It was observed, however, that pollination was effectively prevented by the lateral compression of the stigmatic surfaces. Before pollinaton could be achieved with certainty tlie flowers fell without having exposed their stigmatic surfaces. Other attempts were made using inflorescences still attached to the crown of a plant which was cut at the apex of the caudex and removed to the laboratory. hIost of the leaves were removed and the cut portion was placed in a container of water. Several fully developed inflorescences proceeded to reach anthesis during the following night in the laboratory, but again the flolvers fell without having exposed their stigmatic surfaces. Further observations on plants in the field confirmed that tlie stigmas are tightly compressed at anthesis and follow roughly the following schedule: FIGURE 3G.-Flower of Thrinnx pari1i//orn. Photographed with a Contaflex camera, hand held on a binocular-dissecting microscope and using Kodachrome I1 film exposed for 10 seconds. Kote the form of the stigmatic region. 50 S\fITHSOhIIAN COh 1 RIBUTIOUS TO BOTANY 21 Sept. 7:30 p.hi. 22 Sept. 8:OO A.M. A few rachillae and flowers exposed. All rachillae and flowers exposed; flowers creamy-white including ovary; anthers dehisced; stigmas tightly compressed. 22 Sept. 8:OO P.M. Pollen covering all infloyescence parts; stigmas still compressed. 23 Sept. 9:30 A.M. Ovary yellow, conspicuous; quantities of pollen still present; stigmas open, funnellike. That this is not always the situation is borne out by pickled material in which the anthers ale not fully tlehisced while the stigma is fully open and by the photograph (Figure 36) showing a flower at anthesis with its stigma fully open and apparently receptive. The fact that the stigmatic surtaces are often closed during anthesis, effectively preventing selfing, permits a period during lvhich pollen from surrounding plants can mix either in the air or on the inflorescence before receptivity of the stigma occurs. Thus although the chances for selfing are far greater, outcrossing is not ruled out altogether. Success of the species seems, however, to depend on the fact that, lacking pollen from another population or another plant, seed production is assured in quantity by selfing, as evidenced by the excellent fruit production of solitary individuals in the field or in cultivation. Flowering in Jamaica: In January 1966, several plants of T. parvifloi-a on Mango Tree Hill, in Trelawny, were observed to have inflorescences exposed in bud for about 20 cm. Subsequent and frequent trips to the area found the inflorescence unchanged until 14 May when the same inflorescences were at a stage one or two days past anthesis. At Cockpit and Palmers Cross in Clarendon the entire population was at full anthesis on 9 June, while all the plants on Long Mountain, St. Andrew, had flowered a month earlier on 8 May. It was observed, in 1966, that most inflorescences of a single plant reached anthesis within a 48-hour period. This is notable considering that the 4 to 6 or more inflorescences reaching anthesis at the same time had developed in the axils of successively produced leaves over a 12-month period two seasons earlier. Apparently each solitary inflorescence produced within each leaf axil remains at a particular stage until several reach the same stage. They then proceed development together and reach anthesis at the same time. Each plant presumably has 3 seasons of inflorescence production at any one time. The 3 or more older lea\es subtend 3 or more spent inflorescences; the 3 or more younger leaves subtend inflorescences at or past anthesis, or in fruit; and, apically, 3 or more youngest leaves subtend resting or developing immature inflorescences. Each season a select number reaches anthesis at once, during which time the next season’s inflorescences will be reaching a certain stage of equal development. In Table 1 the localities, within each subspecies grouping, are arranged in descending elevation from the top toward the bottom. It can be Seen that in any one year, widely separated populations flo~v- TABLF 1.-Flowering and fririting dates for Thrinax parviflora arranged by phenotypic expression (localities 27-30 represent subspecies parvipora; 33-29 represent subspecies pubertila) I.ocality nti m her 27 10 8 I 5 32 31 30 33 2 14b 38 34 3 36 17 40 26 42 21 4 22 24 29 An thesis Jan 1967 Mar 1967 Jan 1967 Jan 1967 Jan 1960 Jan 1967 Nov 1964 May 1966 Jul 1967 May 1966 Jul 1967 Apr 1963 May 1966 Jun 1967 Sep 1967 May 1966 May 1966 May 1966 Jun 1966 Jim 1966 Jun 1966 Jim 1967 Immature fruit Feb 1955 Mar 1967 Jan 1958 Jan 1956 Apr 1955 Mar 1960 Aug 1955 Jill 1966 Feb 1967 Aug 1966 Mature fruit Jun 1966 4pr 1966 May 1966 Nov 1966 Nov 1965 Nov 1955 Oct 1955 Aug 1955 Nov 1965 Nov 1955 Nov 1965 SUhIBER 19 51 ered several weeks to a month apart. This was especially true in 1966. A plant removed from a hill near Silver Spring, Hanover, and planted in the palm collection at hlona, produced an inflorescence, antl reached anthesis on 26 May, but the pollen was sterile. Additional plants were collected at Cliarlton, TVintlsor Cave, and Negril Hill on 4, 5, and 6 June respectively. These Jvere a week or more past anthesis, when collected, providing some overlap in flowering among widely spaced populations. Nearly all populations of tlie warm, dry, lower elevations leached anthesis between 8 hlay antl 9 June 1966. During the first half of 1966, no plants \\‘ere found at antliesis or even postanthesis anywhere in the higher elevations. The presence of mature fruit on 29 June at Hollymount Hill suggested that the plants may have bloomed during tlie winter. In 1967 several individuals from throughout the higher elevations were collected at or near antliesis between January and March. Flowering and seed production must be very irregular and rarely plentiful among tlie plants at the higher elevations, for after having collected tlie fev available inflorescences for herbarium specimens antl stud), no fruiting specimens have since been found among tlie thousands of plants observed. In January on tlie Devils Backbone one of the plants Tvitli fully developed inflorescences was cut below the crown and removed to the laboratory. At 9:00 P.M. on 12 January not one flower was exposed, but by 8:OO the following morning all piiinai) branches were fully exposed and all flou ers were shedding pollen. Although most of tlie lowland plants have been observed to flower during the summer months, a single plant of T. paivipoin near Portland Point was found at postanthesis in Febiuary 1967. It is not known if fruit set as a result, because no fruit was found later in the year. TVidespread drought and widely scattered, irregular, late, and below normal rainfall in 1967 no doubt had a strong effect on the flowering of Thyinax paiviporn, because the pattern of flowering at the lower elevations in 1967 was markedly different from that described for 1966. A trip to hfango Tree Hill in late May, where all plants hatl finished bloom by the same (late in 1966, yielded not a single inflorescence. Kone were exposed for more than a few centimeters. Two plants on Long hlountain, which flowered in early May in 1966, flowered on 22 and 23 June 1967. Several other plants on Long Mountain hatl inflorescences exposed, but they did not reach anthesis until late September, several weeks following a period of heavy rain which broke tlie 8-niontli drought. At Cockpit and Palmers Cross, Clarentlon, not one inflorescence was observed on 24 June 196i when nearly every plant in the Portland Ridge area, a few miles to the south, was at full antliesis. Genetic exchange between distant populations of T. pavuifloia by means ol pollen exchange is probably very low. Since nearly all plants in a popiilation shed their pollen during a 48-liour period, and since populations widely removed from one another may flower a week or more a p t , it is unlikely that pollen from one population can be cari ied through wind and rain and still be able to compete a -tveek later with the greater mass of pollen already available on an inflorescence in another population. Except for this unlikely but possible exchange of pollen, genetic exchange between local populations niost likely results from the indiscriminate distribution of seed by birds and the resulting plants crossing with their neighbors in tlie new locality. Plants of T. Iadiatn have been observed in flower or fruit tliroiighout the year. Most of the plants in a given population are usually at the same stage of bloom or fruit, but there seems to be no definite season. Thrinax excelsa has been observed in flower from .4pril to September, and fruit has been collected from July through September. Seed Divt~ibzctioiz: Doves and pigeons are common throughout the range of Thyinax in Tainaica, antl have been reported by the country people as niost plentiful when the “thatch” is in fruit. It was said of tlie hills near Silver Spring, Hanovel, that, “Bald Plates” [sic] are seen in flocks feeding on the thatch “peas.” At the time of my visit to tlie ‘ires, the palms were not in fruit and no “Bald Plates” were in evidence. There are eleven species of dokes or pigeons indigenous to Jamaica and the Baldpate or TYliite Crowned Pigeon is coinnion throughout the distribution range of T. Tadiota in the northern Caribbean. Several of the others are common to Jamaica and neighboring islands but the Baldpate is said to move freely among the islands (Bond, 1961). 52 SSIITHSOXIAN COSTRIBUTIONS TO BOT’ASY Variation of Thrinax parvijlora plants, the true extent of genetic differentiation Thyinax parviflora is a highly variable and polymorphic species and occurs over an equally variable and complex system of environments from near sea level to about 914 in (3000 f t ) elevation. Considerable effort has been expended in attempting to correlate variability of phenotype with environment. Lacking experimental evidence, holvever, of any genetic bases for the variation, it is not possible to do more than describe the range of variation in the various environmental zones. Until such a time as plants from the different areas are grown under identical conditions and/or with reciprocal transcannot be known. The extent of variability can be and has been measured by field studies on plants in 42 localities throughout the entire range of distribution of the species, and in nearly every ecological situation over a 2-year period. In the t\vo extremes of climatic conditions there are what appear to be two distinct biotypes which, although lacking really significant qualitative diflerences, look quite different as a result of the combined effect of a number of apparently minor quantitative differences. Two localities, each hav- FIGURE 37.-Tlirinux parviflora: A, Subspecies parvipora growing at “R”-ridge above Charlton, Mt. Diablo (the late Mr. L. XVynter assisted in the collection of palms while I I\ as i l l Jamaica); 13, subspecies finbe~rt2n growing near Beverly Hills, Long hlountain, Kingston. KIJlIBER 19 53 ing a large number of individuals in a nearly uniform environment and representing as nearly as possible (1) the hottest, driest, lowest elevation and ( 2 ) the coolest, wettest, highest elevation, were selected for intensive study of the widest range of variation in the species. Each population was selected primarily for its ecological situation and for having an adequate sample of individuals in a relatively accessible area. See the section on Morphology for an explanation of the method of selection of plants and parts for measurement and study. It will be demonstrated under the section on the typification of Thrinax parzrifZo~a that the characters of Thrinax, at the higher elevations of Mt. Diablo, most closely correspond with characters drawn from the type specimen and original diagnosis of the species. These plants, typified by a large sample taken at collection locality #lo on Hollymount Hill at 792.4 ni (2600 ft) elevation, represent one extreme in the overall variation of the species. Figure 37A illustrates the typical “pinwheel” form of the leaf and the open crown on tall slender trunks. In addition the very short, blunt or acutely pointed hastula and the relative absence of an abaxial hastula, glabrous to glabrate (Figure ~ O C , D , E ) inflorescence branches, generally short pedicellate flowers or fruits, and short anthers are characteristic of the plants in this locality. Inflorescences are shorter than the petioles, erect except in fruit, and the lowermost branches of the lower primary branches are occasionally branched more than once. Flowering is very irregular but occurs between December and March. Also characteristic of all plants at the higher elevations are certain biotic changes of the inflorescence and fruit (described under Phytomorphosis and Zoomorphosis in Thyinax paruiflom). These changes have led to considerable confusion and misinterpretation. In fact one specific epithet, now in synonymy, is descriptive of the change in the character of the fruit, and the plants to which it applied have been suggested as having some significance in evolutionary theory. In a discussion of the durian theory in relation to palms, Corner (1966: 180) wrote: “Perhaps in this durian complex, there should be added Thrinax tesselatus [sic] of Jamaica, the fruits of which appear to have small flattened warts as in Pholidocaipus.” In contrast with the Hollymount Hill “biotype” the plants of the lower elevations, below 365.76 m (1200 f t ) from the base of Mt. Diablo south to Portland Ridge, and typified by collection locality #22 at Cockpit, Clarendon, have quite a different aspect somewhat resembling the plant in Figure 3 7 ~ . The heavy crown, with relatively broad leaves . A F FIGURE 38.-~-c, Frequency distribution of anther lengths; D-F, range of pedicel lengths. A, D are Thrinnx pnruifiora from Devils Backbone; B, E are from the Swartz t)pe specimen; and c, F are from T. rndintn hlorant Point, Jamaica. (Histograms are based on 100 measurements; bar graphs are based on 29 measurements. Measurements in mm.) 54 SMITHSONIAN CONTRIBUTIONS TO BOTANY and slightly drooping segments, supported on a short trunk is typical. The adaxial hastula is prominent, long pointed, and often tubular when the leaf is fully expanded. The abaxial hastula is also conspicuous, frequently forming a triangular projection up to 1.6 cm long. The arching inflorescences equal or exceed the petiole in length, and all branching parts including the elongate pedicels are densely puberulous (Figure ~ O A , B ) . The length of the pedicels, in flower or fruit, and the length of the anthers have frequently been used as key characters for distinguishing between taxa. These characteristics have been given some emphasis in this study to test their usefulness and to emphasize the danger inherent in the use of small samples such as are available on herbarium specimens of palms. It can readily be seen in the histograms in Figures 19, 38 that pedicel length is certainly not a good character. Figure 38~,c illustrates the variability of anther length in Thrinux parviflora and T. m d i a t a . If only two localities are considered, the character might appear useful; however, plants with very short or very long anthers occur in the same population. This situation occurs in nearly all the characters tested. Given only two extreme localities, which were the basis of Beccari’s work, because the): represent classical collecting areas, two quite distinct taxa are the result. Additional collections however, lrom many localities over the entire range of the species throughout the island fill in the gaps and blend the overlapping measurements, resulting in a kind of clinal variation of nearly all characters. Accumulation of mutations expressed as certain of the extreme variations, with subsequent introgression, might be achieved as a result of the fact that the highland biotype flowers from November to March, while the lowland plants flowered from April through September. Throughout the range of T. pa~vif7o~-cr, definite trends in leaf form and trunk size exist which appear to follow certain gradual changes in climatic conditions. The most significant variations in the physical environment that appear to influence the phenotype are changes of moisture availability in the areas of different rainfall and of temperature with differences in elevation. Consistent east-west trends may also be due to combinations of these factors. Several features such as branching and puberulence of the inflorescence rachillae and hastula form, although different at the two principal environmental zones, seem to vary little throughout the range of the species and appear to be characteristic of particular ecotypes. Caudex: The caudex diameter and height of mature individuals are extremely variable even within a small local population, but the largest mean diameters and shortest trunks occur in the hot, dry, exposed areas of St. Andrew, St. Catherine, and Clarendon. Plants with trunks having smaller mean diameters are found in regions of greater rainfall toward the west and in the cool moist gorges (i.e., Cane River, Rio Cobre), or at the median elevations of the hills or Cockpit Country. The very tall plants of smallest trunk diameters are found only at the cool, moist, high elevations or in exceptional areas of unusual climatic FIGURE 39.-Polymorphic leaves of Thrinnx pnrviporo: G. R. Proctor, of the Institute of Jamaica, holds a leaf from a juvenile plant in hi5 right hand, and a leaf from a flowering sire plant in his left hand; near Ramgoat Cave, in the Cockpit country of Jamaica. SUhIBEK 19 55 conditions such as that described under Donkey Trail and “R”-ridge. Leaf Polymorphism: Among the plants of Thrinax pawifiora growing at the higher elevations, there is a striking change in leaf morphology from seedling to maturity and eventual exposure of the crown at tlie canopy. The seedling stages up to the formation of the trunk are typical for the genus. The change in leaf form, however, subsequent to the first appearance of a trunk is possibly unique among fanleaved palms (Figure 39). The leaves produced at tlie time of trunk formation are circular in outline and rather flat or slightly funnel shaped with tlie free part of the segments rigid. As the trunk elongates the leaves attain their greatest diameter, have a broad palman, and the segments arch slightly. With increased age oE the plant the palman is slightly smaller and the longer segments tend to droop. When the plant reaches maturity the leaves appear to be much smaller as a result of the much reduced palman and the fact that the drooping segments begin to curl. Fdly mature plants in tlie full dense shade below the canopy may have leaves with a fairly broad flat palman and drooping curled segments such as are illustrated in Figure Sin; however, when the plants are exposed either on a cliff face or above the canopy they assume a strikingly different form. The basal portion of the blade folds up and forward, the palman is very small and uneven, and the segments are twisted and tightly coiled (Figures 8, 39). At this latter stage the blade often appears as a “pinwheel” on an excessively long slender petiole. The petiole in fact is shorter on older plants, but the much contorted blade creates an illusion of a longer petiole. Vm-iabilify of the Leaf Elsewhew: The form of the leaf blade throughout the range of tlie species is the most highly variable characteristic of the entire complex of variation, reflecting in effect different phases of the polymorphism exhibited tluring the development of plants at the highest elevations. The change in shape or form is in fact simply the result of quantitative changes in the component parts of the leaf. The form ol the leaf, which must not be confused with outline, is three dimensional resulting from varying degrees of folding, twisting, and curling of the palman and segments. The overall trend appears to be a decrease in siLe of parts with maturity, aging, increased height and exposure and with change from hot and dry to wet and cooler climates. The change in leaf form during maturation of individuals, throughout the greater portion of the population, is simply the production of larger leaves accompanied by increases in the number, width, and length of segments, and the breadth of the palman. Mature plants, not yet having reached the canopy, produce larger, more heavily textured leaves, juvenile types showing a tendency for the lower portion of the blade to be folded upward. In the hot dry plains of Clarentlon near Palmers Cross the mature leaf blade (Figure 7) has a broad uneven palman and wide very leathery segments. Elsewhere in the dry evergreen thicket formations of St. Andrew, St. Catherine, and Clarendon, the leaf blade is not quite so leathery, tlie broad palman is relatively flatter but with the basal part of the blade folded up and forward (Figure 37n), and the segments arching or drooping. The leaves of plants exposed at the canopy or in a clearing exhibit a narrower palman and increasingly lax segments. Tall, very old plants have leakes in which the changes just described are even more strongly expressed. In certain areas of lower temperatures and/or higher moisture availability (i.e., Cane River Gorge, Rio Cobre Gorge, Fern Gully, and westward from Clarentlon) mature plants have leaves with proportionally smaller palman and narrower segments which twist or curl slightly (Figure 37A). In regions of higher rainfall in tlie west and northwest of the island such as at Negril Hill, Silver Spring, Lances Ray, Dolphin Head, and TYindsor Cave, the species exhibits a markedly reduced leaf with a narrow uneven palman, and narrow twisted segments. This form of leaf blade is expressed to different degrees depending on maturity or exposure but appears almost intermediate between the two extremes discussed earlier. During the early part of the study, plants having the latter leaf form were classified along with plants of the highest elevations until it was realized that the dense puberulence on the inflorescence branches placed the plants more consistently among those of the lower elevations. In Cockpit Country, plants of median elevations (hut on exposed drier locations) resemble the lowland forms most closely. In regions of still greater moisture availability and cooler temperature?, as on the upper levels of 56 SXIITHSONIAN CONTRIBUTIOSS TO BOTASY Dolphin Head, Somerset, Top Hill, Albion Mountain, and Mt. Diablo, the leaf blade of mature plants is smaller and more tightly curled and twisted in proportion to increased elevation and exposure at the canopy. The greatest extreme in reduction in size of leaf parts accompanied by a great amount of folding, twisting, and curling occurs on the highest levels of Mt. Diablo where the plants (Figure 8) exhibiting these characteristics are very tall and exposed above the canopy. Hastula: Although quite variable throughout the range of the species, at the higher elevations the hastula is generally short and blunt adaxially and lacking or vestigial on the abaxial surface. This is one of the few characters of which measurements do not appreciably overlap. With the exception of the plants at the highest elevations, the adaxial hastula is quite prominent, long pointed, and frequently tubular. The abaxial hastula is also conspicuous whether as a flap of tissue projecting from the apex of the petiole or as a well-defined triangular extension with a retuse apex. In the sample studied at Cockpit in Clarendon, a specimen was collected in which the abaxial hastula was developed into two slender processes projected up along the undersurface of the blade for 20 to 30 cm (Figure 13c,~). Although not noticed at the time the specimens were collected, two leaves taken from the same plant exhibited the same anomalous condition, suggesting perhaps that all leaves produced by the plant possessed similar processes. Inflorescence: The usually arching inflorescence equals or exceeds the petioles among the plants of lower elevations but varies considerably in length and aspect at the higher elevations where it may be erect and much shorter than the petiole. Of particular interest is the occurrence of p i - mary branches which are twice branched, a unique condition so far as is known among members of the Thrinax alliance. As a rule the individual primary branches are once branched. At the lower elevations the ultimate branches are commonly forked but never as elaborately branched as those at the highest elevations. Several specimens have been collected on Aft. Diablo in which the lowermost primary branches are twice branched producing a secondary condition resembling the primary branch from which it originates. These highly branched secondary branches, however, are subtended by the same triangular nonsheathing bracteoles as are the simple unbranched ultimate branches. Pedicels: One of the key characters used to distinguish between the “species” of the Thrinax pU7aifiol-U complex, and among species of other genera as well, is the length of the floral and fruit pedicels. As was mentioned earlier the importance given to the length of the pedicels by the various workers in the genus has necessitated particular attention to testing its reliability. The results presented in graph form in Figures 17 and 19 illustrate the uselessness of the character in Jamaica and emphasize the need for adequate samples irom throughout the entire range of the species complex. It also points out the danger of basing taxonomic conclusions on too few characters and in certain cases upon the wholly inadequate presently available herbarium specimens. Samples from 144 plants in 32 different localities totaling some 12,000 measurements are tabulated in Figures l i and 19. It can be seen readily that any attempt to correlate pedicel length with a particular phenotype or locality is futile. The frequency histograms (Figure 19), representing only three localities, alone show so much overlap at the higher frequencies that one can conclude the shortest pedicels (lo occur at Hollymount Hill and the longest occur at Cockpit, but these extreme areas share the identical lengths with such great frequency as to be of hardly any taxonomic significance. TVhen all 32 localities are considered together as in Figure l i the ranges and means of variation overlap considerably. They show a general tendency to increase gradually from high to low elevations. Pubel ulence: The entire population of Thi innx pawiflora is divided into two fairly distinct expressions of puberulence on inflorescence branches. This character, never having been mentioned in any study of the genus, provides the only fairly consistent means, apart from the hastula, for separating the species into two biotypes. Throughout the range of distribution of the species, with the exceptions to be mentioned below, all parts of the inflorescence branches are densely puberulous. This, as far as can be ascertained, is another unique character in the Thrinux alliance; certainly no other members of the genus have been reported to have puberulent rachillae. Although the presence of puberulence can sometimes be determined by the naked eye, it is usually necessary to use a lens of SUMBER 19 57 at least X 8. The degree of puberulence does not vary much at the lower elevations (Figure ~ O A , B ) . On the upper peaks and ridges where cool mists and clouds prevail (e.g., Hollymount Hill, Union Hill, Grier Mount, Devils Backbone, Dolphin Head, Somerset, Stirling Castle, Ramgoat Cave, etc.), there is a striking change in the puberulence. The plants here produce inflorescences with apparently glabrous (Figure 4 0 ~ ) or glabrate (Figure 4 0 ~ ) branches. Frequently the puberulence is limited to widely scattered hairs in lines or patches usually on the rachis or peduncle. It is doubtful that any plants produce inflorescences which have truly glabrous branches, but it is difficult to see the hairs at anthesis and pollen grains can easily be mistaken for puberulence. Occasionally inflores- FIGURE IO.-Different degrees of puberulence exhibited by inflorescences of Thrinax parvifiora, ultimate branches: A, Cockpit, Clarendon; 13, Spring Garden, St. Catherine; c, Devils Backbone; D, E, Hollymount Hill. 58 0 LOCALITY # 4 5.0 52 5k . 22 4 1 ,.A. .. i . . * = low 4 1 SMITHSONIAN CONTRIBUTIONS TO BOTANY 15 14 13 12109 8 7 5 . . . . . . . . . . . . . . . . . . . . . . * . . . . . . . . b . 1 . . . . . . . ' . . . . . . . . . . . . ' I I \ '%I.-()-, - 457 't ..... $. 304 - 914 - 762 - *. . *. .-it; 152 - \ir...-. Ir ........... * .. .and phenotype 0 = high elevation phenotype 1- . May Pen w p - 1 *.e- I n ' I 9 8 \ a W 3 :402,000 Suanish Town *- A* ST. ANN '. FIGURE 41.-Transect across central Jamaica, showing pedicel length and phenotype, from lowest to highest elevations where Thrinnx parviporn occurs. The large dot in the bar graphs represents the mean length of the pedicels, the solid line represents 90% of all measurements, and the broken line indicates 5% of the total taken off each end of the range, SUXIBER 19 cences of plants in exposed localities produce branches with considerable puberulence (Figure 40c). Insect grazing on the branches of plants at the higher elevations often entirely denudes the epidermis preventing accurate determination. In certain localities such as at Dolphin Head and Windsor Cave phenotypically similar plants growing in the same general area may produce inflorescences with dense puberulence or almost glabrous branches. Transplant experiments would be most helpful to test the effect of climate on the degree of puberulence. Transplant Expel iment: An attempt was made to transplant mature individuals from the highest elevations into a garden at the University of the West Indies Botany Department to be grown with individuals removed from low elevations. The elevation at Rlona is approximately 600 feet, and the area frequently suffers from prolonged dry periods. The primary purpose was to obtain flowering material for cytological studies dependent on the production of inflorescences within the year or two following transplanting. Only one plant produced inflorescences and this was very soon after having been transplanted. The flowers produced nonviable pollen. Another possible and valuable result of the experiment would have been the observation of the degree of puberulousness on the inflorescence branches of plants removed from the high elevations. It was strongly suspected that there would be an increase in puberulousness if the high-elevation plants formed inflorescences in the hot dry climate of Mona. Leaf form and pedicel lengths produced at Mona would also have provided valuable information about possible genetical differences between the two apparent biotypes. This experiment has been terminated as a result of an abnormally long drought and a severe water shortage from January to September of 1967. Most of the plants remained green and in fact produced new leaves during the growing season of 1966; however, lvatering was stopped in the spring of 1967, and during two weeks of particularly hot drying winds, without rain or water, nearly all leaves rapidly turned brown and the trunks began to Tvrinkle from slirinkage. All plants have since died due to the continued drought and lack of water. Seeds from many remote areas have been germinated and the resulting plants ivill be transplanted in a test garden. The comparative results of seedling transplants will take many years because of the extremely slow growth rate characteristic of palms in this genus. Seedling palms grown in containers will become established more easily if root damage is minimized and water is available. It is the earnest desire of the author to bring together in one test garden seedlings of all taxa in the genus for comparative studies at some future date. TRANSECT FROM PORTLAND RIDGE TO HOLLYMOUNT, JAMAICA.-A line drawn from Portland Ridge, in the south, to the northern slopes of Mt. Diablo (Figure 41) passes through regions of low to high elevations from sea level to about 914 m (3000 ft), and from hot, dry nearly xerophytic conditions to cool, moist mesophytic woodlands and high pinnacles frequently bathed with mist. The rainfall varies from less than 126 cm (50 inches) per year at Portland Ridge to more than I78 cm (70 inches) per year on the heights of Rlt. Diablo. Along the line, changes in temperature and moisture availability are mostly gradual up to the middle elevations on Mt. Diablo where, as a result of the combined effect of exposure, elevation, and the very steep escarpment, the changes are more abrupt. At the elevation where cloud formation most frequently occurs, noticeable differences in the climate and flora are evident over a very short distance. Thrinax parvipora grows on practically every natural outcrop of limestone along the transect line. During the present study numerous collections were made in nearly every accessible area along an irregular line froin south to north, and on Rlt. Diablo, in an attempt to obtain adequate material over a range of variable ecology. The collections were also part of an investigation to determine the distinctions for maintaining two taxa in the region, one in the lower elevations (T. parvifiola) and one at the highest elevations (T. tessellata). The principal means of distinguishing between these two species had been the supposed absence of pedicels and the appearance of the fruit in the latter. The tessellated appearance of the fruit at the higher elevations, resulting from fungal infection described earlier, and the length of the fruit pedicels are poor characters which were based on Tvholly inadequate material. The transect runs through two of the three intensive study areas. Samples of inflorescences were taken from every available plant at both Cockpit 60 SMITHSONIAK CONTRIBUTIONS TO BOTANY and Hollymount Hill. In addition pedicel measurements were taken from every collection locality along the route of the transect. These measurements are all compared in Figure 41, and it is obvious (as has already been shown) from the results that the length of the pedicels cannot be used for separating taxa. Although the high-elevation plants have a predominance of short pedicels, those of lower elevations exhibit an abundance of pedicels in the same length ranges, and there is considerable overlap at the 90 percent level. Only two apparently reliable characters can be used to characterize the high- and low-elevation phenotypes along the transect: the hastula and the degree of puberulence on the primary branches of the inflorescence. The designation in Figure 41 for lowland phenotype represents plants with long, pointed hastulas and densely puberulous primary branches, accompanied usually by large leaves and relatively short and stout caudices. The designation for high-elevation phenotype represents plants with short, acute or blunt hastulas and glabrate (Figure 4 0 ~ ) to lightly puberulent (Figure ~ O C , D ) primary branches. Additional measurements are included in Figure 18 comparing variability at the three intensive study areas. Bar graphs giving the range of variation and means for the various organs of plants along the transect route may be found in Read (1968). Blue Mountain Trail: Along the southern face of Mt. Diablo an exceedingly steep escarpment rises nearly 609 m (2000 f t ) above the valley. Along most of the escarpment, which faces south, climatic conditions up to about 502.92 m (1650 ft) elevation are very similar to those at lower elevations. Full exposure to the sun, particularly in the winter months, perfect drainage, and average rainfall permit a dry evergreen, thicket-type vegetation in which the palms are almost indistinguishable from plants growing near sea level on Portland Ridge. At approximately 609 m elevation the vegetation changes to open woodland in protected valleys and gorges, and tall, slender plants of the typical highelevation palm dominate the exposed ridges and rocky pinnacles. There does not appear to be a transition zone for the palms along the trail, because suitable rocky outcrop was not encountered between 502.92 and 762 m elevation. It is important to note that the point between 518.16 and 609 m (1700 and 2000 ft) elevation is the altitude at which clouds generally form and obscure the peaks and ridges, commonly throughout the year, but more frequently in the late summer and winter months. The clouds and mists common above 609 m elevation on Mt. Diablo result partly from and contribute to the higher moisture availability and cooler temperatures reflected in a different flora. The greatest extremes in phenotypic expression are coincidentally found growing on the southfacing escarpment of Mt. Diablo above an area known as Charlton. At locality #13, between 457.20 and 502.92 m (1500 and 1650 ft) elevation, several palms exhibit among themselves the largest trunk and leaf dimensions, and although two of the plants in the group had pedicel lengths averaging within the normal range of means for lowland lorms, the third plant exhibited exceptionally long pedicels which caused the mean for the group to be among the longest pedicel lengths (Figures 17, 41) of any population on the island. Near the upper limit of the escarpment, overlooking the group of exceptional plants just mentioned, typical high-elevation plants occur between 609 and 807.72 m (2000 and 2650 ft), in the cloud zone. The very tall, slender-stemmed palms with very small tightly folded and curled leaf blades grow among somewhat dwarfed thicket wherein occur numerous epiphytes, ferns, and herbaceous plants. “R”-)idge: ’4 short distance to the west of the Blue Mountain trail, a spur extends southward from Mt. Diablo and descends to 457.2 m (1500 ft) elevation at a pass over which the Ewarton-’IVorthy Park road crosses. Apparently the spur and ridge provide a barrier to moisture-laden prevailing winds from the east, for the appearance of the vegetation seems to indicate a rapid increase in moisture availability as one ascends a short distance along the road to the pass. At approximately 365.76 m (1200 f t ) the road passes from an area of exceedingly dry, nearly xerophytic rocky outcrop to an area of mesophytic woodland on an east-facing slope. Thiinnx parvif?ora exhibiting the lowland phenotype are common on the slope. X short distance uphill, but beyond a bend in the road, the vegetation changes to dense woodland where tall, slender palms of the high-elevation phenotype are found. Patches of mesoph) tic woodland alternate with xerophytic scrub between 396.24 and 457.20 m NUMBER 19 61 (1300 and 1500 ft) elevation along the road, and it is possible to observe both phenotypic expressions of T. parviflora growing a short distance apart but still apparently in different habitats. Near the pass at 457.2 m (1500 f t ) the vegetation mostly resembles moist woodland, which is usually limited to much higher elevations on Mt. Diablo. The whole of the ridge area is one of strong ecological contrasts. On a small limestone and marl ridge, at the highest elevation along the road, there is a strange mixture of both high mountain and lowland species of plants other than palms (e.g., Sloanea jamaicensis and Bursera simaruba) growing side by side. Here too was found the unique situation where both phenotypes of T. parviflora are growing very near one another. Retaining their peculiar individuality, the two phenotypes are distinguished by the tightly congested leaf blade with twisted segments and more slender trunk of the high-elevation form (Figure 42~,c) as compared with the larger, flat or simply folded leaf blade with straight or drooping segments and much heavier trunk of tlie lowland form (Figure 4 2 ~ ) . In attempting to verify these apparent differences it was found that the old inflorescences, taken from plants exhibiting the characteristics of the high-elevation phenotype, were so completely damaged by insect grazing that they were useless for comparison with the densely puberulous inflorescences taken (collected in young fruit in July) from plants exhibiting characteristics of the lowland phenotype. The occurrence of two different phenotypes (differing it must be stressed only in quantitative characters which overlap considerably with plants elsewhere on tlie island) in the same population, while proving nothing and raising numerous unanswerable questions, certainly suggests the existence of two genotypes, at least in that particular locality. Among a group of tall, slender plants growing on a steep slope in a depression behind the ridge, where even the lowland form attains considerable height (up to 9 or 10 m), two plants were observed which might represent intermediates between what may now be considered two genetic biotypes. Both FIGURE 42.-Phenotypes of Thrinax paruiflora found growing within a short distance of one another on “R”-ridge, at about 457 m ele\ation, along the Ewarton-\\’orthy Park road. The two plants at the left are tjpical of the two extreme forms; the plant on the far right could possibly be a hybrid between the two biotypes. 62 S.MITHSONIAN CONTRIBUTIONS TO BOTANY FIGLRE 43.-Region of the Cockpit country showing extent of deep continuous box canyon running from Barbecue Bottom to Burnt Hill. Adapted from the topographic maps of the Directorate of Colonial Surveys, D.C.S. 1st edition 1954. Jamaica l/50,000. Further explanation will be found in the text. SUXIBER 19 63 of the intermediates exhibited flatter leaf blades, intermediate in size, with rigid segments (Figure 4 1 ~ ) , and the trunks were intermediate between plants exhibiting the clearly recognizable phenotypes of high or low elevations. It should be mentioned that apart from the area just described it is almost impossible to be certain about the position of certain plants growing in exposed situations at middle altitudes without resort to examination of the puberulence on the inflorescence branches. In the population described above both forms appear most robust and the differences between them appear somewhat exaggerated. The area here in question was not found until very late in the study and, although of great significance, it is regretted that time and circumstances did not permit additional field xvork. It remains an exceedingly interesting area for future concentrated study when plants of both forms can be compared by study of inflorescences at anthesis and in fruit. DONKEY TRAIL TRAKSECT.-In the northeastern corner of the “Cockpit Country” in Jamaica, a series of large interconnected cockpits extends four miles southward along the road from Kinlosr to within half a mile of Burnt Hill intersection. The cockpits (indicated by solid shading in Figure 43), including the one at Barbecue Bottom, vary from nearly a mile wide in the vicinity of Campbells, to only 100 or 200 m wide at the southern end. The formation resembles a “box canyon” with walls 100 to 200 m high throughout its length and opens to the north where it is exposed to the prevailing northeasteily winds. Figure 43 illustrates the major topographic features of the region. In mountainous regions, increase in elevation is normally accompanied by a gradual decrease in temperature, and cloud formation is usually restricted to the higher peaks and ridges. An anomalous situation occurs in these cockpits where the usual climatic conditions are inverted. High ridges surrounding the southernmost cockpit (Figure 44), although rising above 548.64 m (1800 ft), support an open, dry evergreen thicket which resembles that on the lower slopes of hlt. Diablo. Likeivise, plants of Thyinax pawipoin growing on the ridge very closely resemble those of much loTver elevations elsewhere. As one descends into the cockpit the air temperature decreases noticeably in a very short distance and the vegetation changes from dry evergreen woodland on the upper slopes to wet forest on the lower slopes and in the bottom Thrinax pawipora growing inside the cockpit (Figure 44n) exhibits the phenotype usually associated with the highest and wettest elevations of Mt. Diablo. Because extremely different phenotypes were found growing a short distance from one another, a transect study was made in order to compile additional information in support of ecoclinal variation in Thrinax parviflora. During a 48-hour period from 25 to 27 May 1967, a climatological and morphological study was made along a transect projected through a population of T. paruiflora on the south side of the cockpit at “R” in Figure 44. FIGURIC 44.-Donkey Trail special area, enlatged from section indicated in Figurc 43: A, start of the donkey trail; B, C, points at which climatological readings were made, Further explanation in the text. 64 ShIITHSONIAX CONTRIBUTIONS TO BOTANY e l e v a t i o n i n f e e t 1825 LOW Elevation 1 1740 Phenotype May tF RH tF RtI High Elevation Phenotype \ 1707 1700 1695 1690 1685 RH "? 1500 1400 tF RH 25th P.M. o m 0 3 IA o> .. .. 83 7; 78 7C 87 9E 76 70 89 95 76 89 75 96 26th , . . . . . . . N cu m c - 4 81 79 77 76 72 82 80 74 76 89 75 74 91 91 27th A.M. I n 0 3 m L n c - .. .. 71 73 69 72 88 86 59 38 FIGURE 45.-Donkey Trail Cockpit profile (tF = temperature in degrees F; RH = the ielatiie humidity; o = matuie plants; u = juienile plants; Xertical scale, 1 cm = 10 ft; angle of slope 55-60 degrees). SUXIBER 19 I,ocnlity 65 T?mfieratzires i i i a y i - minimum muin Flowering season The transect originated on the highest ridge at 556.26 m (1825 f t ) elevation ("E" in Figure 44) and extended down into the cockpit for 47.24 ni (200 f t ) to 509.02 m (1670 f t j elevation along a belt 3.05 m on each side of a string stretched between the two points. The upper 15 'm of the transect consisted of nearly vertical exposed cliffs above the donkey trail. Below the pass a scree slope at an angle of 55" comprised the remaining 32 m. The donkey trail originates at point "A" in Figure 44, passes over the ridge at 539.49 m (1770 ft), and continues diagonally across the path of the transect providing access to tlie stations where climatological information was gathered (Figure ~ ~ B , c , D , E ) . A constant recording thermometer i ~ a s pIacet1 at the highest (most inaccessible) point at 556.26 m (1825 ft) elevation, near the base of a large palm. A rnaxiinum-minimum recording thermometer was placed at the 509.02 m (1670 f t j level. Periodic recordings of temperature and relative humidity were made using a sling psychrometer and the percentage relatiye humidity was computed with the aid of the Psychorometric Tables compiled by C. F. 1Iarvin.l' The information obtained is recorded in Figure 45 and is compared with the distribution of phenotypes on the side of the cockpit. Mango Tree Hill, one of the original areas of intensive study, is about a mile to the southwest of the Donkey Trail study area. The palms mostly exhibit the lowland phenotype antl closely resembIe those on the uppermost ridge at the Donkey Trail area. A maximum-minimum recorded thermometer was also maintained on Mango Tree Hill throughout the 48-hour period for comparison rvi th temperatures recorded on the Donkey Trail ridge (Table 2). Although the sample studied at the Donkey Trail site is small and the period covered by the climatological data is short, certain significant trends antl features are thought to be worth noting. A marked difference in climate between the ridge and slope of the cockpit is not only evident in the differences in temperature and percentage of relative humidity, but is also reflected in the distribution of species of certain plants. Hohenbeyio xmota, H. polycephalo, and Tillnndsin sp. aff. fnsciciilatn are plentiful on the ridge but entirely absent on the slope 'I I'uhlished by the C.S. TVeather Bureau, TVnFhington, D.C. (1V.n. No. 235, U.S. Department of Commerce, 1041). Vango Tree Hill Tiansect 1825' rianrect 1670' below. Gzizrnclnia lingulata, ferns, and herbaceous plants occur on the slopes but are entirely absent on the ridge. IYere it not for the fact that the sky was overcast during part of the study, the disparity in the temperature and relative humidity readings between the ridge and the slope might have been even greater. At all times a strong cool breeze blew through the Donkey Trail pass at 539.49 m (1770 f t ) elevation where the temperature was as much as 1.68"C lower on the northern side, a distance of only twenty feet. Dew and fog began to form in the bottom of tlie cockpit soon after 7:OO p.v. The fog persisted up to the 487.68 m (1600 f t j level until after 8:00 A.M., when the sun's ra)s reached tlie lower levels of the cockpit. During the Ivinter months when the angle of the siin would be to the south, longer periods of shade and fog, along with a greater difference in temperature between the ridge and the north-facing slope of the cockpit would be expected. The conditions just described for the inside of the cockpit resemble conditions pielailing above 609 m (2000 r t ) elevation on the >It. Diablo range of mountains. It can be seen from a study of Table 9 that in each organ studied size differences occur, but they are not great enough to be considered important; however, the more congested and twisted leaf hlatles and taller, more slender cautlices of the plants in the cockpit create a distinct impression of two distinct biotypes. In Table 3 each elevation recorded represents a single plant along the transect. Each mearurement, ivith the exception of caudex height antl diameter, represents the average of four measurements for each plant. ,411 characters . Little L* Af. L. Kuns 16528 (US). VIEQUES ISLAND. Feb. 1914, J. A . Shafer 2796 (US). TURKS AND C.4ICOS ISL.4NDS. FIVE CAYS. Prolidenciales: July 1954, G. R. Proctor 9181 (IJ). BAHAMA ISL.4NDS. GREAT BAHAMA. Apr.-May 1905, L. J. K. Brace 3709 (US). NEW PROVIDENCE. Nov. 1937, L. H. Bailey 1054 (BH); Nassau: hfar. 1903, A . H. Curtiss 101 (US): July 1903, IV. C. Coker 539 (US). HOG ISL.AND (Paradise Island). Freshwater Pond: Feb., 257 (? syntype of T. bahawensis); July 1962, R. W. Read 840 (US). ELEUTHERA. Feb.-Mar. 1907, E. G. Britton 6515 (US). ASDROS. Big Cabbage Creek: Dr. 6 Mrs. J. D. Nortlwop 668 (US, holotype of T. bahainensis). Margin of Fresh Creek Lagoon: Mar. 1966, E. Y. Dawson 26650 (US). Key near Mastic Key: Kov. 1937, L. H. Bailey 1046 (BH). Near Fresh Creek: J . K. Small 6 J . J . Carter 8757 (US). Deep Creek: Aug.-Sept. 1906, L. J . K. Brace 5183 (US). West Side, in Loggerhead Creek region: h’ov. 1937, - & C. A . Mosier “a” & “c” (BH). Lower Matecumbe Key: .4pr. 1932, 0. F. Cook 6 J . T. Presley (US). Long Key: Jan. 1963, R. TI’. Read 797 (US). Grassy Key: Jan. 1963, R. T V . Read 798 (US). Ram Rod Key: Apr. 1932, 0. F. Cook 6 .I. T. Presley (US). Saddle Bunch Key: Mar. 1898, C. I-. Pollard, G. A’. Collins &- E. L. Morris 23 (US). Big Pine Key: Apr. 1932, 0. F. Cook L* J. T. Presley (US); Aug. 1935, I.. H. nailey 42 (BH); Ang. 1929, J . K. Small & C. A . Mosier “b” (BH); Feb. 1937, E. P. Killip 32025 (US); Feb. 1935, E. P. Killip 31436 (US); Jan.-Feb. 1940, R. F. Martin, 1328 (US): Mar. 1936, E. P. Killil, 31717 (BH US); June 1963, R. W. Read 923 (US). No Name Key: June 1879, A . H. Cttrtiss 2679”** (NY, holotype of 7 . microcarpa, US); May 1891, J. H. Simpson 268 (US); 1881, A . H. Curtiss S o . H (NY, US); June 1895, A. H. Curtiss (US): July 1927, H. O’Seill (US); Nov. 1929, 0. F. Cook (US); Apr. 1932, 0. F. Cook 2 J . T. Presky (BH, 1;s). Marquesas Keys: north shore of the largest, 1898, C. ,S. Sargent (AAH, not seen, holotype of T. keyensis); Hotel, Miami: Feb. 1925, L. H. L* E. 2. Bailey 6350 (BH); hfar. 1925, L. H. Bailey 6174 (BH). C. T. Simpson’s place, Little River: Feb. 1925, L. H. Bailey 6342 (BH); .4pr. 1932, 0. F. Cook &,I. T. Presley (US); June 1928, 0. F. Cook (US). WD.4 Plant Introduction Station, Miami: Feb. 1952, H. E. Moore 6010 (RH); Sept. 1962, R. TT’. Read 782, 781, (US): R. I$’. Read 1437 (BH). Fairchild Tropical Garden, Coral Gables: June 1962, R. TV. Read 771 (US); Apr. 1965, R. TI’. Read I409 (BH, FTG, Voucher for chromosome nnmber); June 1969, DeArmand Hull H-41 (BH, Voucher for M Sc. Thesis). SOURCE UNKNO~VN. Florida 1913 (US). HAITI. NAvASS.4 ISLAND. Oct. 1928, E. L. Ekinnn H. I0839 ( S , holotype of T. ekmanii; US); June 1956, C. R. Proctor 15468 (IJ, US): Feb. 1960 S . Kiem (BH). CUBA, PRO\,. CAMAGUEY. Cayo Cruz: Oct. 1909, ,I. A. Shafer 2800 (US). Cay0 Romano: Pnnta Jncaro, Oct. 1909, J . A . Shafer 2602 (US). Cayo Ballenato Grande: Mar. 1909, J . A . Shafer 947 (US). PROV. MATASZAS. Curva de Gnerro between Caliso and San Miguel de 10s BaAos: Dec. 1931, Bro. Ledn 15328 (BH). San Miguel de 10s BaAos: Mar.-Apr. 1931, J . T. Roig (BH). PROV. HABANA. Lomas de Capasse: June 1930, Bro. Ledn 14583 (BH). Loma de la Janla, Capasse: Dec. 1929, Bro. Ledn 11723 (BH). Loma Peregrina, Capasse: May 1928, Bro. Ledn 13336 (BH). Sikrra de .4nafe: Dec. 1936, Ri-o. Ledn 16667 (BH, US). Sierra de Esper6n: Sov. 1932, L. H. Bailey 1088 (BH). PROV. PINAR DEL RIO. Xft. Guanajay: Dec. 1904, Baker L- Van Hermann 4245 (B, destroyed, F; XY, Lectotype of T. punctulata); 1859-1860, Wright 3965 (AAH; B, destroyed; F; GH, lectotype of T. dritdei; NY, US). Sierra de Esper6n (“0 Anafe,” Mt. Gnanajay of Van Herman): AUg. 1935, I . H. Bailey ff (BH). CULTIVATED. Royal Palm KUXIBER 19 91 Dec. 1936, Bro. Ledn 16667 (BH). Sierra de Anafe: Dec. 1911, P. Wilson 11504 (US). Vicinity of Sumidero: July 1912, J . A . Shafer 13414 (US). Sierra del Sumidero: Mar. 1932, L. Howell for Bro. Ledn 15563 (BH). La Guira: Aug. 1912, J . A . Shafer I3752 (US). Hills between Rio Cayaguateje and Sierra Guane: Nov. 1911, J . A. Shafer 10469 (US). Santa Cruz de 10s Pinos: Arroyo Piedras, July 1930, Bro. Ledn I4590 (BH, US). Vinales: Dec. 1930, E. P. KiZlip I3596 (US); Apr. 1930, Bro. Ledn 14369 (US). Sierra de la Guassa: Mar. 1932, L. Howell for Bro. Ledn 15562 (BH). Mogote de la Baudea: Dec. 1930, Bro. Ledn 14721 (BH). Cayos de San Filipe: Oct. 1932, Bro. Ledn 15860 (BH, CS). Arroyo Mamey-Pan de Quajaib6n: Aug. 1934, G. Sateson for Ledn 16142 (BH). Sierra del .41ic6n: Mar. 1932, L. Howell for Bro. Ledn I5561 (BH). Sierra del Rangel: ArroJ-o Aspiro, Dec. 1930, Bro. Ledn 14724 (BH). DIscussIoN.-Almost from its conception, Thrinax mol-l-isii has been treated as a distinct but poorly known species restricted to two tiny remote islands at the extreme northeastern margin of the Caribbean Sea. As a matter of fact it was the most thoroughly known of any Thl-inax described up to that time. It was the only one for which the description and illustrations had been drawn up from excellent material, including mature leaves, inflorescence, and mature fruit. Treated simply as a dwarf, narrowly endemic species on the islands of Anegada and Anguilla, the name Thrinax morrisii frequently appeared in the literature but never in synonymy. It wasn’t even associated with T. Pumilio, a name which means “small,” from which it was said to differ (Wendland, 1892: 104) “in the greater number of segments of the lamina and in the shortness of the lamina itself.” Thl-inax mon-isii was first discovered in December 1890 by D. Morris, then Assistant Director of Kew, near a place called Blowing Point on the southwestern part of the island of Anguilla. In a report published by Norris (June 1891:131) the palm (without a name) was described as “present in fairly large quantities, and the fan-shaped leaves were used for thatching native huts.” Morris explained that “the chief interest attached to this palm is connected with its dwarf habit. The largest and apparently most matured specimen did not measure more than about 30 to 35 inches in height.” He was unable to find fruit or flowers at the time, but “30 to 40 plants . . . were carried away . . . to be established at the Botanical Stations at Antigua and St. Lucia.” Figure 56 is an old photograph, possibly Antigua. It is not known if these are from the original Morris collection, but I suspect that they are, since the photograph dates from between 1902 and 1931. Sargent (1896) published a new species of Thrinax from the Florida Keys which he called T. microcal-pa in allusion to the small fruits (I/s inch in diam.). Instead of 30-35 inches, however, as in T. morl-isii, this new species measured 20-30 feet in height. He also described (p. 162) a palm growing on the Marquesas Keys (Florida), to which he erroneously attributed specimens of fruits with a “fleshy succulent pericarp.” For this, he later (1899) published the name T. keyensis. Thl-iizax micl-o- FIGURE 56.-Small plants of Thrinax morrisii, possibly from the oiigiiid collection, in the Botanic Garden, Antigua. (Photo b) M. XI. Joseph, Dominica, in the L. H. Bailey collection at the Bailm Hoitoiium. Cornell 19373 ~~ depicting a group of plants in a botanic garden, I - I 92 S\fITHSONIAN CONTRIBUTIONS TO BOTANY carpa was said to differ, from this species (p. 87) “in its taller and more slender trunk without a basal enlargement, in its shorter spadix and smaller fruit with darker colored seeds, and in its smaller and thinner leaves.” But characters such as “taller,” “more slender,” “shorter,” “smaller,” “darker,” and “thinner” are not considered adequate in the present treatment. Sargent (1902:80) separated the two species in a key only on the basis of seed and leaf size. Thrinax praeceps and T. ponceana appeared simultaneously in 0. F. Cook’s synopsis in 1901. FIGURE 57.-Thrinax morrisii growing naturally on Big Pine Key, Florida. (Photograph from the 0. F. Cook collection, now deposited in the Department of Botany, Smithsonian Institution.) Considering the results of studies on Thrinax parviflora in Jamaica, the following observations by Cook (1901:537) are certainly of interest: Several species of Thrinax, of which T. Morrisii Wendland may serve as an example, have been described chiefly with reference to the relative size of the leaf segments and the extent of their separation. If the palms under observation near Ponce belonged as was believed, all to one species, it is not only true that the individual Thrinax passes all the stages from the narrow and grass-like almost completely separated segments of the very young plant to the more than half united leaf of the large tree, but it also appears to be true that under unfavorable conditions a Thrinnx may not be able to attain full maturity of size and form but may at the same time produce flowers and seeds. In the narrow chinks and crevices of the bare rocks were very small, stunted trees, obviously of great age, while but a few feet distant a deeper fissure might hold vegetable debris and moisture sufficient to nourish vigorous specimens several times the size of their less fortunate companions. The stunted trees retain in proportion to their size, but apparently with little reference to their age, the small deeply divided leaves of young plants and have short few branched inflorescences, another difference of supposed systematic importance. Yet examination of the Cook types and his original diagnoses reveal little more than quantitative differences between his two new species, and no reference to T. mol-risii other than that quoted above. Unpublished notes in the Washington files left by Dr. Cook (in the Department of Botany, Smithsonian Institution) state that T. praeceps “differs from T. ponceana in longer and slightly more slender and more tomentose leaf sheaths; smaller, smoother leaves with longer petioles and smaller, more acute ligule.” These “diagnostic” characters are, as has been repeatedly stated, the real problem in palm taxonomy. The only sure way of separating them remains the admonition by Cook in the same paper (p. 526) where he stated that a locality definitely indicated would often go further toward establishing the identity of a species than much of the descriptive matter prepared for this purpose. For the present at least, the geographical idea should be kept uppermost in systematic studies of the palms, since it is generally much easier and far more logical to extend the limits of supposed species, than to cope with the confusion caused by the miscellaneous reporting of species far outside their natural ranges. The test of time has shown that good diagnostic qualitative characters, as in many other groups of plants, seem to be the easiest means of distinguishNUMBER 19 93 ing taxa in the Palmae; however, this has required a thorough understanding of ecological tolerances and phenotypic plasticity within the species. The following year (1902) Cook described yet another new species, this time from the Bahamas. Based on specimens collected by Northrop at Big Cabbage Creek, Andros Island, Thrinax bahamensis was said to compare favorably with Sargent’s T. keyensis “in view of the short pedicels, distinctly lobed calyx, broad filaments and short styles.” But “this species is evidently much smaller in all its parts than Thrinax Keyensis” (p. 20). And “in comparison with Thrinax Ponceana . , . the leaves of the present species are smaller with the petioles less flattened and more distinctly ribbed on the upper side near the apex.” In 1907, Beccari treated ten “good” species and three dubious species in the genus Thrinax. I now treat six of the ten good species as conspecific with T. morrisii. Two of these, T. drudei and T. punctulata, were described as new and apparently distinguished solely by the extent of the intrusion of the testa into the center of the seed, for they were placed in two subgenera separated by this character. While seemingly a good distinction betweeen T. radiata and T. morrisii, this character appears to be variable in T. parviflora subspecies parviflora in Jamaica and requires further investigation with more adequate material in T. morrisii in Cuba, especially since the fruits upon which the species in Cuba were based are immature. I find no other significant differences between the type of T. diudei (Wright no. 3965) and the type of T. punctulata (van Hermann no. 4245). Beccari (1913:407) felt the resemblance between the two species to be great enough to suggest that ‘I. . . it is necessary to obtain better specimens with flowers of both to establish these species on more sure diagnostic characters.” Descriptions of new species of palms, based on single incomplete specimens, have usually proved to be extremely questionable at best. When N. L. Britton and Percy Wilson (1923) presented their findings, they did not accept Cook’s two species but treated them under the earlier T. microcarpa of Sargent and distinguished this species from T. morrisii by the (p. 116) “mature leaves silvery beneath” for the former and “leaves green on both sides, or faintly glaucescent beneath” for the latter. Thrinax ekmanii was described by Max Burret (1929) based on collections made by E. L. Ekman on the island of Navassa. A limestone island with steep cliffs rising high out of the sea, Navassa lies just off the westernmost penisula of Haiti between Hispaniola and Jamaica. While Thrinax morrisii does not occur on either of the larger islands it does occur naturally, as presently circumscribed including T. ekmanii, on this tiny island. Interestingly Navassa supports another palm, Pseudophoenix sargentii. Although no really good diagnostic characters are known which can be used to maintain T. ekrnanii as a distinct species the most conspicuous thing, characterizing both palm taxa on Navassa, is the extremely silvery white condition of the abaxial surface of the leaves. Until further extensive observations of this character in the field are accomplished the nature of its variability throughout the entire range of the species must be treated as uncertain. COMMON NAxxEs.-Known variously in the literature as “brittle-thatch,” in Florida; “palmita” or “miraguano,” in Cuba; “buffalo-top,” in the Bahamas or “buffalo-thatch” in the Caicos Islands: the name “pimetta” was noted on specimens from Barbuda. Various herbarium specimens collected in Cuba bear the names, “miraguano de sierra,” “guano blanco de sierra,” and “guanita de sierra.” It is called “broom palm” in Anguilla. Appendix I Binomials Published in the Genus Thrinax (Arranged in chronological order) T. parvipora Sw., Prodr. 57. 1788. T. radiata Mart. ex Desf., Cat. PI. Hort. Reg. Paris, ed. 3, T. argentea Lodd. ex Desf. loc. cit. nom. nud. T. argentea Lodd. ex J. A. & J. H. Schult., Syst. Veg. 7 (2): 1300. 1830. = Coccothrinax argentea (Lodd. ex J. A. & J. H. Schult.) Sarg. ex. K. Schum. T. pumilio Lodd. ex J. A. & J. H. Schult. loc. cit. 1301. nom. incert. T. pumila Fulch.? ex J. -4. & J. H. Schult. loc. cit. nom. nud., in synon. T. radiasta Lodd. ex J. A. 8s J. H. Schult. loc. cit. T. gracilis Hort. ex J. A. & J. H. Schult. loc. cit. pro syn. T. elegans Hort. ex J. A. & J. H. Schult. lac. cit. pro syn. T. aurantia Fulch. ex J. A. & J. H. Schult. loc. cit. nom. nud. T. m,ultiflora Mart., Hist. Nat. Palm. 3:255. 1838. = Cocco- T. aurata Hort. ex Mart. ihid p. 257. pro syn. T. barbadensi.p Lodd. ex Mart, loc. cit. = Coccothrinax sp.? [not necessarily C. barbadensis Becc.]. T. inaritima Lodd., Cat. Palm. 1845. nom. nud. T. montana Lodd. loc. cit. nom. nud. T. stellata Lodd. loc. cit. nom. nud. T. ferrziginea Lodd. loc. cit. nom. nud. T. excelsa Lodd. loc. cit. nom. nnd. T. mexicana Lodd. loc. cit. nom. nud. T. rupestris Lodd. loc. cit. nom. nud. T. ? chitco Mart., Palm. Orhig. p. 45. 1846. = Chelyocarpus chuco (Mart.) H. E. Moore. T. yurnguana 4. Rich. ex Sagra, Hist. Fis. Pol. Nat. Cuba, pt. 2. 11:278. 1850. nom. illeg. = Coccothrinax niiragziama (H. B. K.) Le6n [as to type, not as to plant described, which = C. yuruguana Le6nI. T. miraguano Mart., Hist. Nat. Palm. 3:320. 1853. = Coccothrinax miraguanza (H. B. K.) Le6n. T. Imiragziaina (H. B. K.) T\'alp., Annal. Bot. Syst. 5:818. 1858. T. e x c e h Lodd. ex Griseh., F1. Brit. 1%'. Ind. p. 515. 1864. T. martii Griseh. et H. Wendl. ex Griseh., Cat. PI. Cub. p. 221. 1866. = T. radiamta Lodd. ex J. A. & J. H. Schult. T. rigida Griseh. et H. Tt'endl. ex Griseh. loc. cit. = Coccothrinax rigida (Griseb. & H. Tt'endl.) Becc. T. crinita Griseb. et H. TVendl. ex Sauv., Anal. Acad. Ci. Habana 7:563. 1871. = Coccothrinax crinita (Griseb. & H. Wendl.) Becc. 31. 1829. nom. nud. thrinax sp. T. acuniinata Griseh. et H. TVendl. ex Sauv. op. cit. = Coc- T. grandis Hort. ex Kerchove, Les Palm. 258. 1878. nom. nud. T. garberi Chap., Bot. Gaz. 3: 12. 1878. = Coccothrinax argeti- T. graniinifolia Hort. ex Kerchove, Illust. Hort. 31:187. 1884. T. arborea Hort. ex Kerchove, ibid. p. 187. nom. nud. T. tunicata Hort. ex Kerchove, loc. cit. nom. nud. T. elegantissima Hort. ex Hook., f. Kew Rept. 1882:66. 1884. T. inorrisii H. TVendl. ex Anonymous, Gard. Chron. ser. 3, T. morrisii H. TVendl., Gard. Chron. ser. 3, 11:104. 1892. T. microcarpa Sarg., Gard. & For. 9:162. 1896. = T. tnorrisii T. floridana Sarg., Bot. Gaz. 27:84 1899. = T. rndiata Lodd. T. keyensis Sarg. ihid. p. 86. = T. tnorrisii H. Tt'endl. T. praecefx 0. F. Cook, Bull. Torr. Bot. Club 28:536. 1901. T. poncenna 0. F. Cook, loc. cit. = T. tnorrisii H. Tt'endl. T. bahamensis 0. F. Cook, Mem. Torr. Bot. Club 12:20. 1902. T. wendlnndiana Becc., TVebbia 23265. 1907. = T. radiata T. drudei Becc. ihid. p. 269. = T. ttiorrisii H. Tt'endl. T. tessellnta Becc. op. cit. 271. = T. pnrviflora Sw. T. punctulata Becc. op. cit. p. 280. = T. morrisii H. Tt'endl. T. harrisiatin Becc. in Fedde, Repert. 6:94. 1908. = T. parvi- T. rex Britt. & Harris, Bull. Torr. Bot. Club 37:352. 1910. T. longistyla Becc. in Urh., Symb. Antill. 7:170, 1912. = Coc- T. ekrnnnii Burret, Kungl. Sv. Vet-Akad. Handl. ter. 3, S(7): T. altissima Hort. ex Bailey, Gent. Herb. 4:149. 1938. nom. T. niirantiaca Fulch.? ex Bailey, ibid. nom. nud. T. compacta Griseh. & Tt'endl. ex Bailey, ibid. nom. nud. T. havenensis Hort. ex Bailey, ibid. nom. nud. cothrinax miraguama (H. B. K.) Becc. tutu (Jacq.) Bailey. nom. incert. pro syn. 10:700. 1891. nom. nud. H. TVendl. ex. J. A. & J. H. Schult. = T. morrisii H. TYendl. = T. morrisii H. Tt'endl. Lodd. ex J. 4. & J. H. Schult. flora Sw. = T. excelsa Lodd. ex Griseh. cothrinax sp. 27. 1929. = T. ~norrisii H. TVendl. nud. 94 Appendix I1 Nomina Incerta et Dubia Thrinax pumilio Lodd. ex J. A. & J. H. Schult., Linn. Syst. T. purnila Fulch. ? ex J. A. & J. H. Schult. loc. cit. in synon. T. pumilio Lodd. Cat. Palm. 1846. nom. nud. Porothrznav H. TVendl. ex Griseb. Cat. PI. Cub. p. 221. 1866. Veg. sec. 7 (2):1301. 1830. nom. incert. nom. nud. The original description of Thrinax pumilio by J. A. & J. H. Schultes (1830) was based on material from a young plant sent to the Munich Herbarium by Loddiges. No specimen has since been found there that could be identified with the description. It could represent almost any palmate genus since Loddiges included plants of both Coccothrznax and Thrinax under Thrinax. It is impossible to apply the very ample description to any known species or for that matter to ascribe it to any genus. A description drawn from a young palmate leaf with only 10 to 14 segments is impossible to identify lacking a specimen. The statement that a hastula is not present is disconcerting, for even very young Thrinax and Coccothrinax exhibit this organ. Moreover it would seem that a Thrinax leaf blade 2 feet in diameter should have more than 14 segments. The additional statement (p. 1301) that T. pumilio “Differt a Thr. parviflol-a et argentea praesertim defectu prominentiae in centro frondis a prolongatione stipites” suggests a generic difference rather than a specific one. The mention of the embryo must be disregarded, since it came from Martius and no doubt does not apply to the taxon in question because it is a juvenile plant by definition. Specimens cited at the time of the publication of Porothrinax pumilio by Grisebach (1866:221) are merely associated with the name and are not to be considered as the type. The mention of the seed having “the albumin centrally perforate, the margin not at all ruminate” is taken from associated specimens, not from type material and thus must be ignored in typifying Thrinax pumilio. Porothrinax H. Wendl. ex Griseb. was not accompanied by a separate diagnosis and is therefore not validly published (4rticles 41 and 42 of the International Code of Botanical Nomenclature). Thrinax section Porothrinax ascribed to Drude (1887) and validated by C. S. Sargent (1896) is a new name based on Thrinax microcarpa and should not be confused with the earlier invalid name published by Grisebach. 95 Literature Cited Aiton, W. 1789. Aiton, W. T. 1811. Asprey, G. F. 1959. Hortus Kewensis. Volume 3. London. Horfus Kewensis. 2nd ed., volume 3. London. Vegetation in the Caribbean Area. Caribbean Quarterly, 5:245-263. Asprey, G. F., and 4. R. Loveless The Dry Evergreen Formations of Jamaica, 11: The Raised Coral Beaches of the North Coast. Journal 1958. of Ecology, 46:547-570. Asprey, G. F., and R. G. Robbins 1953. The Vegetation of Jamaica. Ecological Monographs, 23 : 359-4 12. Ayensu, E. S. 1967. Aerosol OT Solution, an Effective Softener of Herbarium Specimens for .4natomical Study. Stain Technology, 42: 155-156. 1938. Thrinax-The Peaberry Palms, Gentes Herbarum, 4:129-149, figures 75-84. 1939. Coccothrinax in the Southern Greater Antilles. Gentes Herbarum, 43247-259. 1949. Palms Uncertain and New. Gentes Herbarum, 8: 95-99. The Classification of Tropical American Vegetationtypes. Ecology, 36:89-100. Le Palme Americane della Tribu delle Corypheae. Webbia 2:l-288. Palmae Novae Antillanae, XXIV. In Refiertorium Novarum Specierum Regni l’egetnbilis (auctore F. Fedde), 6:94-95. The Palms Indigenous to Cuba. The Poinona College Journal of Economic Botany, 2:402-407, figures 1933. Asiatic Palms-Corypheae. Annals of the Royal Botanic Garden, Calcutta, 13:327-336, plates 24, 28, 29. [Published posthumously, revised and edited by Prof. Ugolino hlartelli; dated 19311. Bailey, L. H. Beard, J. S. 1955. Beccari, 0. 1907. 1908. 1912. 164-167. Bentham, G., and J. D. Hooker 1883. Genera Plantarum. Volume 3. Bond, J. 1961. Britton, N. L. 1908. Beccari’s American Palms. Torreya, 8:238-241. 1909. Botanical Exploration in the West Indies and Florida. Journal of The Sew York Botanical Garden, 10:99-114. Birds of the West Indies. London. Britton, N. L., and TY. Harris 1910. Studies of IVest Indian Plants, 14: Hitherto Undescribed Species of Jamaica. Bulletin of the Torrey Botanical Club, 37:352. Britton, N. L. and P. Wilson 1923. Scientific Survey of Porto Rico and the Virgin Islands, New York Academy of Sciences, 5:116-117. Browne, P. 1756. The Civil and Xatural History of Tamaica. London. Burret, M. 1929. Palmae Cubenses et Domingenses .4. CL. E. L. Ekman. Kungl. Svenska l’etenskapsakndeniiens Handlingar, series 3, 6 (7):27. 1878. .4n Enumeration of Some Plants. Bomtanical Gazette, 3:12. 1883. Flora of the Southern United States. Supplement, 2nd ed. New York. 1901. A Synopsis of the Palms of Puerto Rico. Bulletin of the Torrey Botanical Club, 28:.525-569, plate 45. 1902. Palms from the Bahamas. In Alice R. Sorthrop, Flora of New Providence and Andros. Memoirs of the Torrey Botanical Club, 12:20-21. 1937. Hurricane Palms in Florida, Including a New Genus Simpsonin. Science, 85:332-333. The Xatural His,tory of Palms. Berkeley and Los iingeles: University of California Press. Chapman, A. W. Cook, 0. F. Corner, E. J. H. 1966. Desfontaines, R. 1829. Catalogus Plan tarurn Horti Regii Parisiensis. 3rd ed. Paris. Drabble, E. 1904. On the Anatomy of the Roots of Palms. Transactions of the Linnean Society of London, Botany, series 2, 6:427-490. Drnde, 0. 1887. Palmae. In Engler and Prantl, Die Satiirlichen Pflanzenfamilien, 2 (3):34. Gatin, C. L. 1906. Germination des Palmiers. Annales des Sciences A’aturelles, Botnnique, Paris, series 9, 3: 192-314. Beitrzge ziir Anatomie der Palmen- und Pandanaceen- Tl’urzeln. Botanisches Centralblatt, 83:339-345. 1864. Flora of the British West Indian Islands. London. 1866. Catalogus Plantaruin Cubensiuiii. Leipzig. 1884. 1889. Gillain, G. 1900. Grisebach, A. H. Hooker, J. D. Kew Report for 1882. London. Thrinax excelsa. Curtis’s Botanical iVfagazine, tabula 7088. 96 KUMBER 19 97 Hooker, J. D., and T. Thomson 1855. Introductory Essay. In Flora Indica. xv + 285 pages. London. Thrinax rex-.4 Regal Palm of Jamaica. Principes, Howard, R. A. 1960. Jost, L. 1887. 4:133-137. Ein Beitrag zur Kenntniss der Athmungsorgane der Pflanzen. Botanische Zeitztng, 45:600-606; 617-628; 633-642. Kerchove de Denterghem, 0. 1878. Les Palmiers. Paris. Kunth, C. S. 1841. Enumeratio Plantarum. Volume 3. Stuttgart and Turbingen. L e h , Hno. 1939. Contribncion a1 Estudio de las Palmas de Cuba, 111. Memorias de la Sociedad Cubana de Historia Natural, 13: 153. 1946. Flora de Cuba, 1. Contribuciones Ocasionales del Museo de Historia Satitral del Colegio de la Salle, 8: 260-262. 1956. Identifying Coccothrinax. Principes, 1:16. Ligon, R. 1657. A True L- Exact History of the Island of Barbados. Linnaens, C. 1753. Species Plantaritm. Stockholm. 1845. Palms in the Collection of Conrad Loddiges and Sons, Hackney Sear London with Their Native Countries. London. Loddiges, C., and Sons Loveless, A. R., and G. F. .4sprey 1957. The Dry Evergreen Formations of Jamaica, I: The Limestone Hills of the South Coast. Journal of Ecology, 45:799-822. Martius, C. F. Moore, H. E. 1838. Historia Suturalis Palmarttm. Volume 3. Leipzig. 1963. The Typification and Species of Palma Miller (1754). Gentes Herbarum, 9:242-244. Report of a Botanical Mission to the \Test Indies. Royal Gardens, Kew, B d l e t i n of Miscellaneous Information, 1891:131. Morris, D. 1891. Morrow, L. 1965. Morphology and Anatomy of Coryphoid Palm Flowers. .4 thesis, Cornell University. Parthasarathy, M. V. 1968. Observations on Metaphloem in the Vegetative Parts of Palms. American Journal of Botany, 55(10): 1152-1167. Pfister, R. 1892. Ray, J. Beitrag zur vergleichenden Anatomie der Sabaleenblatter. 51 pages. Dissertation, Zurich. 1688. 1963. Palm Chromosomes. Principes, 7:85-88. 1964. Palm Chromosome Studies Facilitated by Pollen Culture on a Colchicine-lactose Medium. Stain Technology, 39:99-106. 1965. Chromosome Numbers in the Coryphoideae. Cytologia, 30:385-391. 196515. Palm Chromosomes by Air Mail. Principes, 9:4-10. 1966. Coccothrinax jamaicensis-The Jamaican Silver Thatch. Principes, 10: 133-141. 1968. A Study of Thrinax in Jamaica. .4 thesis, The University of the It’est Indies, Mona, Jamaica. 1911. Der Spaltoffnnngsapparat de Plamenblatter. Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften . . . Klasse, 1 (120):1049-1086. 1896. Thrinax in Florida. Garden and Forest, 9:162. 1896. Silva of North America. Volume 10. Cambridge, Mass.: The Riverside Press. 1899. Sew Sorth American Trees. Botanical Gazette, 27: 1902. S i h of A’orth America. I’olume 14. Cambridge, Historia PEantarum. Volume 2. London. Read, R. W. Rudolph, K. Sargent, C. S. 83-87. Mass.: The Riverside Press. Sauvalle, F. .4. 1871. Flora Cnbana. Angles de la Academia de Ciencias MPrlicas, Fisicas y Saturales de la Habana, 83152. Schreber, J. D. C. (editor) 1791. Cnroli a Linne‘ . , . Genera Plantarum. Editio Octavo. Frankfurt. Schultes, J. A. and J. H. (editors) 1830. Caroli a Linne‘ , . . Systema Vegetabilium. Volume 7, part 2. Schumann, K. 1901. Neue Arten der Siphonogamen 1899, VIII. Just’s Botanischer Jahresbericht, 27 (1):469. Shreve, F. 1914. A Montane Rain-Forest. Carnegie Institution of Washington, Publication number 199. Sloane, H. 1696. Catalogus Plantaruni Qztae in Insula Jamaica. London. 1725. A l’oynge to the Islands Madera, Barbados, Niezies, S. Christopher. Volume 2. London. Small, J. K. 192.5. Silk-top Thatch-Thrinax parviflora. Journal of the A’ew York Botanical Garden, 26:49-54. Statistical Methods. Iowa State College Press. Palmae. Volume 3 in Systernatische Anatomie der Monoktyledonen. Berlin. Caroli Linnaei , . . Genera Plantai i i m . Editio nona, volume 2. Gottigen. Snedecor, G. W. Solereder, H., and F. J. Meyer 1948. 1928. Sprengel, C. (editor) 1830. 98 5hIITHSONI4S COSTRIBUTIONS TO BOTANY Swartz, 0. 1788. 1797. Xoua Genera 3 Species Plantarum seu Prodromus. Stockholm, Uppsala. Flora lndiae Occidentalis. Volume 1. Erlangen. Tomlinson, P. B. 1960. Essays on the Morphology of Palms, I: Germination and the Seedling. Principes, 4:56-61. Palmae. Volume 2 in Anatomy of the Monocotyledons. Oxford: The Clarendon Press. 1961. Vasey, G. 1876. A Catalogue of the Forest Tree? of the United States. U.S. Department of Agriculture Report, number 11. Venkatasubban, K. E. 1945. Cytological Studies in Palmae, Part I: Chromosome Numbers in a Few Species of Palms of British India and Ceylon. Proceedings of the Indian Academy of Sciences, 22:193-207. New or Noteworthy Plants. The Gnrdners’ Chroiiicle, ser. 3, 11:104, figures 20, 21. Flrendland, H. 1892. TVilldetiow, C. L. (editor) 1799. Caroli a Linne‘ . . . Species Plantartc~n. Editio Quarta. Berlin. Das Anatomische Verhal ten der Palmenblatter den1 System dieser Familie. 40 pages, Dissertation. Erlangen. Zawada, K. 1890. & U.S. GOVERNMENT PRINTING OFFICE 1075-. 546-365!33