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Adhesion in Echinoderms
Adhesion in echinoderms PATRICK FLAMMANG* Laboratoire de Biologie marine, Universite' de Mons-Hainaut, Mons, Belgium Final manuscript acceptance: August 1995 KEYWORDS: Adhesive properties, podia, larvae, Cuvierian tubules, Echinodermata. CONTENTS 1 Introduction 2 The podia 2.1 Diversity 2.2 Basic structure and function 2.3 Adhesivity 3 Other attachment mechanisms of echinoderms 3.1 Larval and postlarval adhesive structures 3.2 Cuvierian tubules 4 Comparison with other marine invertebrates 5 Conclusions and prospects Acknowledgements References 1 INTRODUCTION Marine organisms have developed a wide range of mechanisms allowing them to attach to or manipulate a substratum (Nachtigall 1974). Among 1 these mechanisms, one can distinguish between mechanical attachments (e.g. hooks or suckers) and chemical attachments (with adhesive sub- stances). The phylum Echinodermata is quite exceptional in that all its species, *Senior research assistant, National Fund for Scientific Research, Belgium. I whatever their life style, use attachment mechanisms. These mechanisms allow some of them to move, others to feed, and others to burrow in par- ticulate substrata. In echinoderms, adhesivity is usually the function of specialized structures, the podia or tube-feet. These podia are the exter- nal appendages of the arnbulacral system and are also probably the most advanced hydraulic structures in the animal kingdom. 2 THE PODIA From their presumed origin as simple respiratory evaginations of the am- bulacral system (Nichols 1962), podia have diversified into the wide range of specialized structures found in extant echinoderms. This mor- phological diversity of form reflects the variety of functions that podia perform (Lawrence 1987). Indeed, they take part in locomotion, burrow- ing, feeding, sensory perception and respiration. -
Silurian Crinoids of the New Brunswick Museum, Saint John, Canada Stephen K
Document generated on 09/28/2021 1:58 p.m. Atlantic Geology Silurian crinoids of the New Brunswick Museum, Saint John, Canada Stephen K. Donovan and Randall F. Miller Volume 52, 2016 Article abstract The New Brunswick Museum’s collection of Silurian crinoids from eastern URI: https://id.erudit.org/iderudit/ageo52art09 Canada is small, and includes specimens from New Brunswick, Quebec and Nova Scotia. Material considered herein is, with one exception, from New See table of contents Brunswick. Included are: the cladid Syndetocrinus dartae (Upper Silurian of Quebec); the camerates Scyphocrinites sp. (Pridoli or Lochkovian) and camerate crinoid arms gen. et sp. indet. (Lower Silurian); columnal Publisher(s) morphotaxa Floricrinus (col.) sp. (Ludlow or Pridoli) and Lanxocolumnus (col.) sp. cf. L. chaleurensis Donovan and Keighley (probably Llandovery, Telychian); Atlantic Geoscience Society distal dendritic radicular attachments (Ludlow or Pridoli); and disarticulated brachials (Ludlow or Pridoli). The fossil record of crinoids from the Silurian of ISSN New Brunswick appears depauperate, but this most likely reflects the poor preservation of the specimens (commonly disarticulated and moldic) and the 0843-5561 (print) lack of interest shown by collectors. The only remedy for this problem would 1718-7885 (digital) be either discovery of a crinoid Lagerstätte, which would be attractive to collectors, or a focused campaign of collecting of disarticulated material from Explore this journal multiple outcrops. Cite this article Donovan, S. K. & Miller, R. F. (2016). Silurian crinoids of the New Brunswick Museum, Saint John, Canada. Atlantic Geology, 52, 223–236. All rights reserved © Atlantic Geology, 2016 This document is protected by copyright law. -
Evidence for Cospeciation Events in the Host–Symbiont System Involving Crinoids (Echinodermata) and Their Obligate Associates, the Myzostomids (Myzostomida, Annelida)
Molecular Phylogenetics and Evolution 54 (2010) 357–371 Contents lists available at ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev Evidence for cospeciation events in the host–symbiont system involving crinoids (Echinodermata) and their obligate associates, the myzostomids (Myzostomida, Annelida) Déborah Lanterbecq a,*, Grey W. Rouse b, Igor Eeckhaut a a Marine Biology Laboratory, University of Mons, 6 Av. du Champ de Mars, Bât. Sciences de la vie, B-7000 Mons, Belgium b Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093-0202, USA article info abstract Article history: Although molecular-based phylogenetic studies of hosts and their associates are increasingly common Received 14 April 2009 in the literature, no study to date has examined the hypothesis of coevolutionary process between Revised 3 August 2009 hosts and commensals in the marine environment. The present work investigates the phylogenetic Accepted 12 August 2009 relationships among 16 species of obligate symbiont marine worms (Myzostomida) and their echino- Available online 15 August 2009 derm hosts (Crinoidea) in order to estimate the phylogenetic congruence existing between the two lin- eages. The combination of a high species diversity in myzostomids, their host specificity, their wide Keywords: variety of lifestyles and body shapes, and millions years of association, raises many questions about Coevolution the underlying mechanisms triggering their diversification. The phylogenetic -
Jan Jansen, Dipl.-Biol
The spatial, temporal and structural distribution of Antarctic seafloor biodiversity by Jan Jansen, Dipl.-Biol. Under the supervision of Craig R. Johnson Nicole A. Hill Piers K. Dunstan and John McKinlay Submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Quantitative Antarctic Science Institute for Marine and Antarctic Studies (IMAS), University of Tasmania May 2019 In loving memory of my dad, whose passion for adventure, sport and all of nature’s life and diversity inspired so many kids, including me, whose positive and generous attitude touched so many people’s lives, and whose love for the ocean has carried over to me. The spatial, temporal and structural distribution of Antarctic seafloor biodiversity by Jan Jansen Abstract Biodiversity is nature’s most valuable resource. The Southern Ocean contains significant levels of marine biodiversity as a result of its isolated history and a combination of exceptional environmental conditions. However, little is known about the spatial and temporal distribution of biodiversity on the Antarctic continental shelf, hindering informed marine spatial planning, policy development underpinning regulation of human activity, and predicting the response of Antarctic marine ecosystems to environmental change. In this thesis, I provide detailed insight into the spatial and temporal distribution of Antarctic benthic macrofaunal and demersal fish biodiversity. Using data from the George V shelf region in East Antarctica, I address some of the main issues currently hindering understanding of the functioning of the Antarctic ecosystem and the distribution of biodiversity at the seafloor. The focus is on spatial biodiversity prediction with particular consideration given to previously unavailable environmental factors that are integral in determining where species are able to live, and the poor relationships often found between species distributions and other environmental factors. -
Smithsonian Miscellaneous Collections [Vol
NEW GENERA OF RECENT FREE CRINOIDS By AUSTIN HOBART CLARK Assistant, Bureau of Fisheries Since the publication of Dr. P. H. Carpenter's great monograph on the recent unstalked crinoids in 1888, the group has received very- little attention from systematists, probably because of the rarity of most of the species and the difficulty in getting together representative material of even the more common ones. Dr. Carpenter included in the family Comatulidse the genera Thaumatocrinus, Eudiocrinus, Promachocrinus (including the subsequently differentiated Decame- trocrinus), Atelecrinus, Antedon, Comatula (=Actinometra) , and Thiolliericrinus. All of these, with the exception of Antedon and Comatula, are comparatively small, strictly homogeneous genera; with them, however, the case is quite different. The genus Antedon was divided by Dr. Carpenter into four "series," and all but the first series into two or more "groups," the characters used in the differ- entiation of the groups and series being (1) the character of the joint between the costals, (2) the number of arms, (3) the number of the distichals, (4) the character of the lower pinnules, (5) the development or absence of covering plates on the ambulacra, and (6) the rounded or "wall-sided" character of the costals and lower brachials. Of all these characters, the first alone is the only one not common to two or more of his series or groups, as diagnosed by him. Taking No. 2, for instance, five of his groups and also several unassigned species are ten-armed ; all the rest have more than ten arms. A number of single species have both ten and more than ten arms, as a result of purely individual variation. -
The Crinoids of Madagascar
Bull. Mus. nain. Hist, nat., Paris, 4e sér., 3, 1981, section A, n° 2 : 379-413. The Crinoids of Madagascar by Janet I. MARSHALL and F. W. E. ROWE * Abstract. — A collection of crinoids from the vicinity of the Malagasy Republic, held in the Muséum national d'Histoire naturelle, in Paris, is identified. Three new species are described in the genera Chondrometra, Iridometra and Pentametrocrinus. The nominal species Comissia hartmeyeri A. H. Clark is considered to be conspecific with C. ignota A. H. Clark, and Dichro- metra afra A. H. Clark with D. flagellata (J. Müller). Comments are included on several syste- matic problems which have arisen during the study of this collection. Résumé. — Détermination d'une collection de Crinoïdes de Madagascar, déposée au Muséum national d'Histoire naturelle de Paris. Trois nouvelles espèces sont décrites pour les genres Chon- drometra, Iridometra et Pentametrocrinus. L'espèce Comissia hartmeyeri A. H. Clark est considérée comme synonyme de C. ignota A. H. Clark, et Dichrometra afra A. H. Clark comme synonyme de D. flagellata (J. Müller). Quelques problèmes systématiques sont discutés. INTRODUCTION The echinoderm fauna of South Africa and some parts of the Indian Ocean have been well documented, but that of Madagascar and of the African coast north of Mozambique is less well known. The island of Madagascar (the Malagasy Republic) stretches from approximately 12° S to 26° S through tropical to warm-temperate waters. The echino- derms found along the Malagasy coast are for the most part distinctly different from that of southern Africa as delimited by the Tropic of Capricorn (23°3(V S) (see A. -
1395 Kaim.Vp
Early Triassic gastropods from Salt Range, Pakistan ANDRZEJ KAIM, ALEXANDER NÜTZEL, MICHAEL HAUTMANN & HUGO BUCHER Five gastropod species are described from the Early Triassic (Smithian, Spathian) of the Salt Range in Pakistan, which is the first detailed documentation of gastropods from this key area of the Palaeozoic-Mesozoic transition. Bellerophontoidea are represented by Warthia hisakatsui. Bellerophontoidea were widespread in the Paleozoic and had their last appearance in the early Smithian. Anisian and later reports of this group are discussed, but currently remain doubtful. Soleniscidae, a typical Late Palaeozoic caenogastropod family, are present with two new species: Strobeus batteni and S. pakistanensis. The neritimorph genus Naticopsis and the caenogastropod Coelostylina are present with one species each, provisionally treated in open nomenclature. Naticopsis? sp. shows preservation of original colour pat- terns, which is very rare in Early Triassic gastropods. All identified genera originated during the Paleozoic (perhaps with the exception of Coelostylina) and are thus survivors or holdovers. Warthia and Strobeus survived the end-Permian mass extinction but went extinct during the Smithian when environmental conditions deteriorated again. • Key words: Gastropoda, Pakistan, Salt Range, Early Triassic, extinction, recovery, taxonomy. KAIM, A., NÜTZEL, A., HAUTMANN,M.&BUCHER, H. 2013. Early Triassic gastropods from Salt Range, Pakistan. Bul- letin of Geosciences 88(3), 505–516 (7 figures). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript re- ceived November 9, 2012; accepted in revised form February 8, 2013; published online March 4, 2013; issued July 3, 2013. Andrzej Kaim, Instytut Paleobiologii PAN, ul. Twarda 51/55, 00-818 Warszawa, Poland; [email protected] • Alex- ander Nützel, Bayerische Staatssammlung für Paläontologie und Geologie, Ludwig-Maximilians-University Munich, Department für Geo- und Umweltwissenschaften, Paläontologie und Geobiologie, Geobio-CenterLMU, Richard Wagner Str. -
First Molecular Report and Phylogenetic Analysis of Crinoidea from Rameswaram Island, South East Coast of India
Available online a t www.scholarsresearchlibrary.com Scholars Research Library Annals of Biological Research, 2014, 5 (8):1-7 (http://scholarsresearchlibrary.com/archive.html) ISSN 0976-1233 CODEN (USA): ABRNBW First Molecular Report and Phylogenetic Analysis of Crinoidea from Rameswaram Island, South East Coast of India Nina Tabitha S and Gunalan B CAS in Marine Biology, Annamalai University, Parangipettai, Tamilnadu, India. _____________________________________________________________________________________________ ABSTRACT Crinoidea is a class of echinoderms that degenerate very easily due to the presence of very temperature sensitive proteins, hence the samples obtained could not be identified easily, resulting in the identification of the samples at a molecular level by sequencing the 650 –bp region from the 5’ end of the mitochondrial CO1 region. The sequenced genes were identified as three different species of Crinoids; Cenometra sp, Tropiometra sp and Comatella sp submitted to the National center of bioinformatics (NCBI) which provided the three finds with accession numbers. The sequences were compared with other closely related sequences and analyzed using the CLUSTAL X software to attain a multiple sequence alignment and Mega (Molecular Evolutionary Genetic Analysis) to construct a Phylogenic tree through which the evolutionary relationships of the three samples analyzed could be observed in the study. Key words: Crinoidea, Echinoderm, Phylogeny, Cenometra sp , Tropiometra sp, Comatella sp, Molecular taxonomy. _____________________________________________________________________________________________ INTRODUCTION Sustainable conservation of species requires, among other things, appropriate knowledge about the diversity of life at different hierarchical levels, including physiological, ecological, biogeographical, and systematic information [1,2], taxonomists [3,4,5], accurate species identification remains an imperative condition to investigate on biodiversity and conservation. -
Microstructural Evidence of the Stylophyllid Affinity of the Genus Cyathophora (Scleractinia, Mesozoic)
Annales Societatis Geologorum Poloniae (2016), vol. 86: 1–16. doi: http://dx.doi.org/10.14241/asgp.2015.023 MICROSTRUCTURAL EVIDENCE OF THE STYLOPHYLLID AFFINITY OF THE GENUS CYATHOPHORA (SCLERACTINIA, MESOZOIC) El¿bieta MORYCOWA1 & Ewa RONIEWICZ2 1 Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-630 Kraków, Poland; e-mail: [email protected] 2 Institute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, 01-818 Warszawa, Poland; e-mail: [email protected] Morycowa, E. & Roniewicz, E., 2016. Microstructural evidence of the stylophyllid affinity of the genus Cyatho- phora (Scleractinia, Mesozoic). Annales Societatis Geologorum Poloniae, 86: 1–16. Abstract: The genus Cyathophora Michelin, 1843 (Cyathophoridae) is removed from the suborder Stylinina Alloiteau, 1952 and transferred to the Stylophyllina Beauvais, 1980. Morphologically, it differs from stylinine corals in that rudimentary septa are developed in the form of ridges or spines on the wall and may continue onto the endothecal elements as amplexoid septa. Relics of primary aragonite microstructure, preserved in silicified colonies of Cyathophora steinmanni Fritzsche, 1924 (Barremian–early Aptian) and in a calcified colony of C. richardi Michelin, 1843 (middle Oxfordian), indicate a non-trabecular structure of their skeletons. The scleren- chyme of radial elements is differentiated into fascicles of fibres, and in the form of fascicles or a non-differen- tiated layer of fibres, it continues as the upper part of endothecal elements and as the incremental layers of the wall. A micro-lamellation of the skeleton corresponds to the accretionary mode of skeleton growth found in Recent corals. A similarity between the septal microstructure of Cyathophora and that of the stylophyllid genera, the Triassic Anthostylis Roniewicz, 1989 and the Triassic–Early Jurassic Stylophyllopsis Frech, 1890, is interpre- ted as a result of their being phylogenetically related. -
A Framework for the Development of a Global Standardised Marine Taxon
bioRxiv preprint doi: https://doi.org/10.1101/670786; this version posted June 17, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. This article is a US Government work. It is not subject to copyright under 17 USC 105 and is also made available for use under a CC0 license. 1 A framework for the development of a global standardised marine taxon 2 reference image database (SMarTaR-ID) to support image-based analyses 3 Short title: Global marine taxon reference image database 4 Kerry L. Howell1*, Jaime S. Davies1, A. Louise Allcock2, Andreia Braga-Henriques3,4, 5 Pål Buhl-Mortensen5, Marina Carreiro-Silva6,7, Carlos Dominguez-Carrió6,7, Jennifer 6 M. Durden8, Nicola L. Foster1, Chloe A. Game9, Becky Hitchin10, Tammy Horton8, 7 Brett Hosking8, Daniel O. B. Jones8, Christopher Mah11, Claire Laguionie Marchais2, 8 Lenaick Menot12, Telmo Morato6,7, Tabitha R. R. Pearman8, Nils Piechaud1, Rebecca 9 E. Ross1,5, Henry A. Ruhl8,13, Hanieh Saeedi14,15,16, Paris V. Stefanoudis17,18, Gerald 10 H. Taranto6,7, Michael B, Thompson19, James R. Taylor20, Paul Tyler21, Johanne 11 Vad22, Lissette Victorero23,24,25, Rui P. Vieira20,26, Lucy C. Woodall16,17, Joana R. 12 Xavier27,28, Daniel Wagner29 13 * Corresponding author: [email protected] 14 1 School of Biological and Marine Science, Plymouth University, Drake Circus, 15 Plymouth, PL4 8AA. UK. 16 2 Zoology, School of Natural Sciences, and Ryan Institute, National University of 17 Ireland, Galway, University Road, Galway, Ireland. 18 3 MARE-Marine and Environmental Sciences Centre, Estação de Biologia Marinha 19 do Funchal, Cais do Carvão, 9900-783 Funchal, Madeira Island, Portugal. -
OREGON ESTUARINE INVERTEBRATES an Illustrated Guide to the Common and Important Invertebrate Animals
OREGON ESTUARINE INVERTEBRATES An Illustrated Guide to the Common and Important Invertebrate Animals By Paul Rudy, Jr. Lynn Hay Rudy Oregon Institute of Marine Biology University of Oregon Charleston, Oregon 97420 Contract No. 79-111 Project Officer Jay F. Watson U.S. Fish and Wildlife Service 500 N.E. Multnomah Street Portland, Oregon 97232 Performed for National Coastal Ecosystems Team Office of Biological Services Fish and Wildlife Service U.S. Department of Interior Washington, D.C. 20240 Table of Contents Introduction CNIDARIA Hydrozoa Aequorea aequorea ................................................................ 6 Obelia longissima .................................................................. 8 Polyorchis penicillatus 10 Tubularia crocea ................................................................. 12 Anthozoa Anthopleura artemisia ................................. 14 Anthopleura elegantissima .................................................. 16 Haliplanella luciae .................................................................. 18 Nematostella vectensis ......................................................... 20 Metridium senile .................................................................... 22 NEMERTEA Amphiporus imparispinosus ................................................ 24 Carinoma mutabilis ................................................................ 26 Cerebratulus californiensis .................................................. 28 Lineus ruber ......................................................................... -
Echinodermata) and Their Permian-Triassic Origin
Molecular Phylogenetics and Evolution 66 (2013) 161-181 Contents lists available at SciVerse ScienceDirect FHYLÖGENETICS a. EVOLUTION Molecular Phylogenetics and Evolution ELSEVIER journal homepage:www.elsevier.com/locate/ympev Fixed, free, and fixed: The fickle phylogeny of extant Crinoidea (Echinodermata) and their Permian-Triassic origin Greg W. Rouse3*, Lars S. Jermiinb,c, Nerida G. Wilson d, Igor Eeckhaut0, Deborah Lanterbecq0, Tatsuo 0 jif, Craig M. Youngg, Teena Browning11, Paula Cisternas1, Lauren E. Helgen-1, Michelle Stuckeyb, Charles G. Messing k aScripps Institution of Oceanography, UCSD, 9500 Gilman Drive, La Jolla, CA 92093, USA b CSIRO Ecosystem Sciences, GPO Box 1700, Canberra, ACT 2601, Australia c School of Biological Sciences, The University of Sydney, NSW 2006, Australia dThe Australian Museum, 6 College Street, Sydney, NSW 2010, Australia e Laboratoire de Biologie des Organismes Marins et Biomimétisme, University of Mons, 6 Avenue du champ de Mars, Life Sciences Building, 7000 Mons, Belgium fNagoya University Museum, Nagoya University, Nagoya 464-8601, Japan s Oregon Institute of Marine Biology, PO Box 5389, Charleston, OR 97420, USA h Department of Climate Change, PO Box 854, Canberra, ACT 2601, Australia 1Schools of Biological and Medical Sciences, FI 3, The University of Sydney, NSW 2006, Sydney, Australia * Department of Entomology, NHB E513, MRC105, Smithsonian Institution, NMNH, P.O. Box 37012, Washington, DC 20013-7012, USA k Oceanographic Center, Nova Southeastern University, 8000 North Ocean Drive, Dania Beach, FL 33004, USA ARTICLE INFO ABSTRACT Añicle history: Although the status of Crinoidea (sea lilies and featherstars) as sister group to all other living echino- Received 6 April 2012 derms is well-established, relationships among crinoids, particularly extant forms, are debated.