Relocation Movement in a Stalked Crinoid (Echinodermata)
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Isocrinid Crinoids from the Late Cenozoic of Jamaica
A tlantic G eology 195 Isocrinid crinoids from the late Cenozoic of Jamaica Stephen K. Donovan Department of Geology, University of the West Indies, Mona, Kingston 7, Jamaica Date Received April 8, 1994 Date A ccepted A ugust 26, 1994 Eight species of isocrinines have been documented from the Lower Cretaceous to Pleistocene of Jamaica. New finds include a second specimen of a Miocene species from central north Jamaica, previously regarded as Diplocrinus sp. but reclassified as Teliocrinus? sp. herein. Extant Teliocrinus is limited to the Indian Ocean, although Miocene specimens have been recorded from Japan, indicating a wider distribution during the Neogene. One locality in the early Pleistocene Manchioneal Formation of eastern Jamaica has yielded three species of isocrinine, Cenocrirtus asterius (Linne), Diplocrinus maclearanus (Thomson) and Neocrinus decorus Thomson. These occur in association with the bourgueticrinine Democrinus sp. or Monachocrinus sp. These taxa are all extant and suggest a minimum depositional depth for the Manchioneal Formation at this locality of about 180 m. This early Pleistocene fauna represents the most diverse assemblage of fossil crinoids docu mented from the Antillean region. Huit especes d’isocrinines de la periode du Cretace inferieur au Pleistocene de la Jamai'que ont ete documentees. Les nouvelles decouvertes comprennent un deuxieme specimen d’une espece du Miocene du nord central de la Jamai'que, auparavant consideree comme l’espece Diplocrinus, mais reclassifiee en tant que Teliocrinus? aux presentes. Le Teliocrinus existant est limite a l’ocean Indien, meme si on a releve des specimens du Miocene au Japon, ce qui est revelateur d’une distribution plus repandue au cours du Neogene. -
Crinoids from the Barremian (Lower Cretaceous) of the Serre De Bleyton (Drôme, SE France)
©Naturhistorisches Museum Wien, download unter www.biologiezentrum.at Ann. Naturhist. Mus. Wien, Serie A 112 733-774 Wien, Juni 2010 Crinoids from the Barremian (Lower Cretaceous) of the Serre de Bleyton (Drôme, SE France) By Manfred JÄGER (With 2 figures and 7 plates) Manuscript submitted on September 11th 2009, the revised manuscript on January 11th 2010 Abstract The Barremian of the Serre de Bleyton has yielded many disarticulated but well-preserved ele- ments of a diverse crinoid fauna of at least six species, dominated by comatulids (three species) and isocrinids (two species). The single apiocrinitid species is rare. Except for the large and well- known comatulid Decameros ricordeanus D’ORBIGNY, 1850, with specimens similar to the subspe- cies or variety vagnasensis (DE LORIOL, 1888), five of the six species are new. However, only for three of them a new species name is introduced, Isocrinus? bleytonensis nov. spec., Comatulina moosleitneri nov. spec. and Semiometra barremiensis nov. spec. Two fairly rare species, Per- cevalicrinus sp. and Apiocrinites sp., are described in open nomenclature. This Barremian fauna fills a stratigraphic gap from which only few crinoids had so far been de- scribed. Apart from some Hauterivian crinoids (mainly isocrinids), the stratigraphically nearest crinoid-rich (and especially comatulid-rich) horizons are the Valanginian of western Switzerland and southeastern France and especially the Aptian of southeastern France and Spain. The high percentage of new species is not surprising due to phylogenetic changes during the time span Valanginian – Aptian. Apart from these differences at species level, the crinoid fauna from the Serre de Bleyton fits well into the overall faunal composition known from Late Jurassic to Early Cretaceous sites. -
The First Record of an Isocrinid Crinoid from the Tertiary of Australia
Rec. Wes/. AWl. Mw 1989 14(Jj J85-J89 The first record of an isocrinid crinoid from the Tertiary of Australia Gregory J. Milner* Abstract An isocrinid crinoid. tcntatively assigned to :'Nielsenicrinus sp., from the Paleogcne Cardabia Calcarenite, Carnarvon Basin, Western Australia is the first record of the group in the Australian lertiary. Foraminiferal evidencc dates the cnnoid as latc Paleocene (mid Thanetian, planktonic foraminiferal Planorotalites pseudomenardii Zone 1'4). The crinoid lived in an open shelf sea at SOm to lOOm depth. Introduction Within Australia articulate crinoids of the Isocrinidae have previously been described only from Cretaceous deposits in Queensland and New South Wales (eg: Moore 1870; Jack and Etheridge 1892, Etheridge 190 I, 1902). During recent stratigraphic fieldwork in Toothawarra Creek, northern Carnarvon Basin, Western Australia (latitude 220 49' 45" S and longitude 1140 08' 30" E, Fig. I) crinoidal remains were collected from a homogenous, soft, white, bryozoal calcarenite bed ofthe Wadera Member type-section, Cardabia Calcarenite (Condon et al. 1956; Hocking et al. 1987) near the contact with the underlying Boongerooda Greensand Member. Indian 30' OCean 40 km 30' x Figure I Locality map showing collection location as denoted by X. *Department of Geology, the University of Western Australia, Nedlands, 6009 3~5 F'irst record of isocrinid crinoid Many isocrinids have been assigned generic names on the basis of stem elements (Rasmussen 1961). Although reservations concerning this practice were expressed by Moore as early as 1939, and later Donovan (1984), it has continued, mainly because of the lack of diagnostic calyx or cup elements in recovered material. -
The Isocrinine Crinoid Isselicrinus Rovereto from the Paleogene of the Americas
Swiss Journal of Palaeontology (2019) 138:317–324 https://doi.org/10.1007/s13358-019-00195-3 (0123456789().,-volV)(0123456789().,- volV) REGULAR RESEARCH ARTICLE The isocrinine crinoid Isselicrinus Rovereto from the Paleogene of the Americas 1 2 3 4 Stephen K. Donovan • Sven N. Nielsen • J. Velez-Juarbe • Roger W. Portell Received: 8 May 2019 / Accepted: 30 May 2019 / Published online: 15 June 2019 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2019 Abstract Crinoids are uncommon fossils in the Cenozoic. This scarcity means that even disarticulated elements are of note. Two species of the isocrinine Isselicrinus Rovereto are described from their disarticulated columns. Isselicrinus sp. A is from the upper Eocene Moritzian Stage of Tierra del Fuego. These crinoids have a robust column, varying from pentalobate (proximal?) to rounded pentagonal (distal?) in section and with consistently depressed areola petals. Isselicrinus sp. B is from the Lower Oligocene Juana Diaz Formation of Puerto Rico. This species is typified by slender pluricolumnals, always rounded pentagonal in section, and long noditaxes. Proximal and distal pluricolumnal morphologies are not distinguishable. Keywords Tierra del Fuego Á Puerto Rico Á Oligocene Á Systematics Á Taphonomy Introduction water deposits from this interval were the comatulids, whose fossil record remains patchy because of their low ‘‘As a result of the distribution of sea and land during preservation potential and the small size of their compo- the Tertiary, which was similar to that of today, most nent parts. The tiny ossicles of comatulids rarely occur in marine sediments were deposited in shallow water concentrations, so it takes a keen eye to spot them. -
Artificial Keys to the Genera of Living Stalked Crinoids (Echinodermata) Michel Roux Universite De Reims - France
Nova Southeastern University NSUWorks Marine & Environmental Sciences Faculty Articles Department of Marine and Environmental Sciences 5-1-2002 Artificial Keys to the Genera of Living Stalked Crinoids (Echinodermata) Michel Roux Universite de Reims - France Charles G. Messing Nova Southeastern University, [email protected] Nadia Améziane Muséum national d'Histoire naturelle - Paris, France Find out more information about Nova Southeastern University and the Halmos College of Natural Sciences and Oceanography. Follow this and additional works at: https://nsuworks.nova.edu/occ_facarticles Part of the Marine Biology Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons Recommended Citation Roux, Michel, Charles G. Messing, and Nadia Ameziane. "Artificial keys to the genera of living stalked crinoids (Echinodermata)." Bulletin of Marine Science 70, no. 3 (2002): 799-830. This Article is brought to you for free and open access by the Department of Marine and Environmental Sciences at NSUWorks. It has been accepted for inclusion in Marine & Environmental Sciences Faculty Articles by an authorized administrator of NSUWorks. For more information, please contact [email protected]. BULLETIN OF MARINE SCIENCE, 70(3): 799–830, 2002 ARTIFICIAL KEYS TO THE GENERA OF LIVING STALKED CRINOIDS (ECHINODERMATA) Michel Roux, Charles G. Messing and Nadia Améziane ABSTRACT Two practical, illustrated, dichotomous keys to the 29 genera of living stalked crinoids are provided: one for entire animals and one for stalk ossicles and fragments. These are accompanied by (1) an overview of taxonomically important morphology, and (2) an alphabetical list by family and genus of the ~95 nominal living species and their distribu- tion by region. This is the first compilation of such data for all living stalked crinoids since Carpenter (1884) recognized 27 species in six genera in his monograph based on the H.M.S. -
10Th Deep-Sea Biology Symposiu M
10th Deep-Sea Biology Symposiu m Coos Bay, Oregon August 25-29, 2003 10th Deep-Sea Biology Symposiu m Program and Abstracts Coos Bay Oregon August 25-29, 2003 Sponsor: Oregon Institute of Marine Biology, University of Orego n Venue: Southwestern Oregon Community College Organizing Committee: Prof. Craig M . Young (chair) Dr. Sandra Brooke Prof. Anna-Louise Reysenbac h Prof. Emeritus Andrew Carey Prof. Robert Y. George Prof. Paul Tyler CONTENTS Program & Activity Schedule Page 1 Abstracts of Oral Presentations (alphabetical) Page 1 1 Abstracts of Poster Presentations (alphabetical) Page 49 Participant List and Contact Information Page 76 CampusMap Page 85 ACKNOWLEDGMENT S Many individuals in addition to the organizing committee assisted with the preparations and logistics of the symposium . Mary Peterson and Torben Wolff advised on matters of publicity and advertizing . The web site, conference logo and t-shirt were created by Andrew Young of Splint Web Design (http ://www.splintmedia.com/) . Marge LeBow helped organize housin g and meals at OIMB, and Pat Hatzel helped format the participant list . Shawn Arellano, Isabel Tarjuelo and Ahna Van Gaes t assisted with the formatting and reformatting of abstracts and made decisions on housing assignments . Larry Draper, Toby Shappell, Mike Allman and Melanie Snodgrass prepared the OIMB campus for visitors . Local graduate students an d postdocs Tracy Smart, John Young, Ali Helms, Michelle Phillips, Mike Berger, Hope Anderson, Ahna Van Gaest, Shaw n Arellano, and Isabel Tarjuelo assisted with last-minute logistics, including transportation and registration . We thank Kay Heikilla, Sarah Callison and Paul Comfort for assistance with the SWOCC venue and housing arrangements, Sid Hall, Davi d Lewis and Sharon Clarke for organized the catering, and Sharron Foster and Joe Thompson for facilitating the mid-conferenc e excursion . -
Relocation Movement in a Stalked Crinoid (Echinodermata) Charles G
Nova Southeastern University NSUWorks Marine & Environmental Sciences Faculty Articles Department of Marine and Environmental Sciences 5-1-1988 Relocation Movement in a Stalked Crinoid (Echinodermata) Charles G. Messing Nova Southeastern University, [email protected] M. Christine RoseSmyth Research Submersibles, Ltd. Stuart R. Mailer Research Submersibles, Ltd. John E. Miller Harbor Branch Oceanographic Institution Find out more information about Nova Southeastern University and the Halmos College of Natural Sciences and Oceanography. Follow this and additional works at: https://nsuworks.nova.edu/occ_facarticles Part of the Marine Biology Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons Recommended Citation Messing, Charles G., Christine M. RoseSmyth, Stuart R. Mailer, and John E. Miller. "Relocation movement in a stalked crinoid (Echinodermata)." Bulletin of Marine Science 42, no. 3 (1988): 480-487. This Article is brought to you for free and open access by the Department of Marine and Environmental Sciences at NSUWorks. It has been accepted for inclusion in Marine & Environmental Sciences Faculty Articles by an authorized administrator of NSUWorks. For more information, please contact [email protected]. NOTES BULLETINOFMARINESCIENCE,42(3): 480-487, 1988 RELOCATION MOVEMENT IN A STALKED CRINOID (ECHINODERMATA) Charles G, Messing, M, Christine RoseSmyth, Stuart R, Mailer and John E. Miller Of about 80 species I of extant stalked crinoids, or sea lilies, more than half attach permanently to hard substrates by cementation of a terminal stalk plate or to sediments by branching rootlets. The remainder compose the family Isocrinidae and anchor chiefly to hard substrates via segmented prehensile cirri that arise in whorls of five at intervals along the stalk. -
Echinoderm Research and Diversity in Latin America Juan José Alvarado Francisco Alonso Solís-Marín Editors
Echinoderm Research and Diversity in Latin America Juan José Alvarado Francisco Alonso Solís-Marín Editors Echinoderm Research and Diversity in Latin America 123 Editors Juan José Alvarado Francisco Alonso Solís-Marín Centro de Investigaciónes en Ciencias Instituto de Ciencias del Mar, y Limnologia del Mar y Limnologia Universidad Nacional Autónoma de México Universidad de Costa Rica México City San José Mexico Costa Rica ISBN 978-3-642-20050-2 ISBN 978-3-642-20051-9 (eBook) DOI 10.1007/978-3-642-20051-9 Springer Heidelberg New York Dordrecht London Library of Congress Control Number: 2012941234 Ó Springer-Verlag Berlin Heidelberg 2013 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Duplication of this publication or parts thereof is permitted only under the provisions of the Copyright Law of the Publisher’s location, in its current version, and permission for use must always be obtained from Springer. Permissions for use may be obtained through RightsLink at the Copyright Clearance Center. Violations are liable to prosecution under the respective Copyright Law. -
Migration Confirms Asynchronous Marine Mesozoic Revolution
ARTICLE DOI: 10.1038/s42003-018-0048-0 OPEN Globally discordant Isocrinida (Crinoidea) migration confirms asynchronous Marine Mesozoic Revolution Rowan J. Whittle1, Aaron W. Hunter2,3, David J. Cantrill4 & Kenneth J. McNamara2,3 1234567890():,; The Marine Mesozoic Revolution (MMR, starting ~200 million years ago) changed the ecological structure of sea floor communities due to increased predation pressure. It was thought to have caused the migration of less mobile invertebrates, such as stalked isocrinid crinoids, into deeper marine environments by the end of the Mesozoic. Recent studies questioned this hypothesis, suggesting the MMR was globally asynchronous. Alternatively, Cenozoic occurrences from Antarctica and South America were described as retrograde reversions to Palaeozoic type communities in cool water. Our results provide conclusive evidence that isocrinid migration from shallow to deep water did not occur at the same time all over the world. The description of a substantial new fauna from Antarctica and Australia, from often-overlooked isolated columnals and articulated crinoids, in addition to the first compilation to our knowledge of Cenozoic Southern Hemisphere isocrinid data, demonstrates a continuous record of shallow marine isocrinids from the Cretaceous-Paleogene to the Eocene/Oligocene boundary. 1 British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK. 2 Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK. 3 School of Earth Sciences, The University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia. 4 Royal Botanic Gardens Victoria, Birdwood Avenue, Melbourne, VIC 3004, Australia. Correspondence and requests for materials should be addressed to R.J.W. (email: [email protected]) or to A.W.H. -
Inter and Intraspecific Morphological Disparity of Crinoid
Inter- and Intraspecific Morphological Variation of Crinoid Columnals in Relation to Water Depth in the Type Cincinnatian (Upper Ordovician) A thesis submitted to The Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in the Department of Geology of the College of Arts and Sciences 2005 by Bradley Deline B.S. University of Michigan, Ann Arbor, 2003 Committee Chair David L. Meyer Abstract Crinoid columnals are a major constituent in the Upper Ordovician fossil assemblage of the Cincinnati Arch Region. Several species of Cincinnatian crinoids are identifiable based on columnal morphology alone. Disarticulated columnals of two crinoids were measured throughout a 68-meter section of the Kope and lower Fairview Formations to examine the relationship between columnal morphology and sea level fluctuations. The columnal diameter of two disparid crinoids increased in the upward shallowing sequence. Detrended Correspondence Analysis axis 1 scores computed using columnal measurements of two crinoids correlated significantly with a proxy for depth. Therefore, crinoid columnals may provide a metric for the study of small-scale sea level fluctuation in a depositional sequence. A larger scale study showed similar morphological shifts in five taxa of crinoids, but to differing degrees. The morphologic shifts in the columnals are likely due to differences in nutrient levels and flow regimes between depths. Table of Contents List of Figures 2 List of Tables 3 Acknowledgments 4 Introduction 5 Materials and Methods 8 Results 13 Discussion 17 Summary 24 References 26 Appendix 1 (Species Description) 33 Appendix 2 (Crenularium Area Calculation) 40 Appendix 3 (Localities) 43 Appendix 4 (Data) 44 Figure Captions 54 Figures 59 Table Captions 80 Tables 81 1 LIST OF FIGURES Figure 1. -
New Crinoids from the Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula
NEW CRINOIDS FROM THE EOCENE LA MESETA FORMATION OF SEYMOUR ISLAND, ANTARCTIC PENINSULA TOMASZ K. BAUMILLER and ANDRZEJ GAZDZICKI Baumiller, T.K. and Gaidzic ki, A. 1996. New crinoids from the Eoce ne La Meseta Form a tion of Sey mour Island , Antarctic Peninsula. In: A. Gaidzicki (ed.) Palae ontological Re sults of the Polish Antarctic Expe ditions. Part Il. - Palaeontologia Polonica 55 , 101-11 6. The exce llent record of marin e invertebrates from the Eoce ne La Meseta Formation of Sey mour Island (Antarc tic Penin sula) includ es several well-prese rved crinoids. Two cri noid species have been previously reported from the upper part of the La Meseta Form a tion; here we describe three addit ional taxa from the lower units (Telm l-2) of this forma tion: an isocrini d, Eometacrin us australis gen . et sp. n., a comatulid, Notocrinus seym ourensis sp. n., and a cyrtocrinid, Cyathidium holopus Steenstrup , 1847. These data are important in prov iding new infor mation for the time-envi ronm ent distribution of crinoids and for constraining phylogenetic hypotheses and evo lutionary scenarios . The co-occurr ence of these three taxa is unusual because sedimentological, stratig raphic, and paleoeco logical evidence suggests that the lower part of the La Meseta Formation was deposited in a shallow-marine setting whereas today, isocrinids, cyrtocrinids, and coma tulids eo-occ ur only in deep wate r. Also , the morphology of E. australis indicates that the syzyg ial articulation between the first and seco nd primib rachials, thought to represent a character of primary phylogenetic importance among the Isocrin idae, may have evo lved more than once. -
Lower Miocene Echinoderms of Jamaica, West Indies
Lower Miocene echinoderms of Jamaica, West Indies S.K. Donovan, R.W. Portell & C.J. Veltkamp Donovan, S.K., Portell, R.W. & Veltkamp, C.J. Lower Miocene echinoderms of Jamaica, West Indies. Scripta Geologica, 129: 91-135, 1 fig., 8 pls., 6 tables, Leiden, April 2005. Stephen K. Donovan, Department of Palaeontology, Nationaal Natuurhistorisch Museum, Postbus 9517, NL-2300 RA Leiden, The Netherlands ([email protected]); Roger W. Portell, Florida Museum of Natural History, University of Florida, Gainesville, Florida 32611, U.S.A. (portell@flmnh.ufl.edu); Cornelis J. Veltkamp, School of Biological Sciences, Nicholson Building, University of Liverpool, P.O. Box 147, Liverpool, L69 3BX, England ([email protected]). Key words — systematics, crinoids, asteroids, ophiuroids, echinoids, Neogene, Caribbean. Despite being diverse globally, Miocene echinoids are poorly known from Jamaica. Moderately diverse echinoids and other echinoderms have been identified mainly from fragmentary specimens collected from chalks and mass-flow deposits of the Lower Miocene Montpelier Formation, White Limestone Group, near Duncans, parish of Trelawny. This locality has yielded the most diverse association of fossil echinoderms known from the Miocene of Jamaica, including at least ten species in four classes. This fauna is comprised of the isocrinid crinoids Neocrinus sp. cf. N. decorus (Wyville Thomson) and Isocrinus sp.; the ophiuroid Ophiomusium? sp.; the asteroids Astropecten? spp.; and the echinoids Prionocidaris? sp., Histocidaris sp., Echinometra sp. cf. E. lucunter (Linné), Echinoneus cyclostomus Leske, Clypeaster? sp. and spatangoid sp. Some echinoids are preserved as “crystal apples”. The deep water echinoderm taxa in this death assemblage suggest the depth of deposition to have been at least 200 m.