Echinodermata: Echinothuriidae) with Descriptions of Seven New Species
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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. -
Parks Victoria Technical Series No
Deakin Research Online This is the published version: Barton, Jan, Pope, Adam and Howe, Steffan 2012, Marine protected areas of the Flinders and Twofold Shelf bioregions Parks Victoria, Melbourne, Vic. Available from Deakin Research Online: http://hdl.handle.net/10536/DRO/DU:30047221 Reproduced with the kind permission of the copyright owner. Copyright: 2012, Parks Victoria. Parks Victoria Technical Paper Series No. 79 Marine Natural Values Study (Vol 2) Marine Protected Areas of the Flinders and Twofold Shelf Bioregions Jan Barton, Adam Pope and Steffan Howe* School of Life & Environmental Sciences Deakin University *Parks Victoria August 2012 Parks Victoria Technical Series No. 79 Flinders and Twofold Shelf Bioregions Marine Natural Values Study EXECUTIVE SUMMARY Along Victoria’s coastline there are 30 Marine Protected Areas (MPAs) that have been established to protect the state’s significant marine environmental and cultural values. These MPAs include 13 Marine National Parks (MNPs), 11 Marine Sanctuaries (MSs), 3 Marine and Coastal Parks, 2 Marine Parks, and a Marine Reserve, and together these account for 11.7% of the Victorian marine environment. The highly protected Marine National Park System, which is made up of the MNPs and MSs, covers 5.3% of Victorian waters and was proclaimed in November 2002. This system has been designed to be representative of the diversity of Victoria’s marine environment and aims to conserve and protect ecological processes, habitats, and associated flora and fauna. The Marine National Park System is spread across Victoria’s five marine bioregions with multiple MNPs and MSs in each bioregion, with the exception of Flinders bioregion which has one MNP. -
Larval Development of the Tropical Deep-Sea Echinoid Aspidodiademajacobyi: Phylogenetic Implications
FAU Institutional Repository http://purl.fcla.edu/fau/fauir This paper was submitted by the faculty of FAU’s Harbor Branch Oceanographic Institute. Notice: ©2000 Marine Biological Laboratory. The final published version of this manuscript is available at http://www.biolbull.org/. This article may be cited as: Young, C. M., & George, S. B. (2000). Larval development of the tropical deep‐sea echinoid Aspidodiadema jacobyi: phylogenetic implications. The Biological Bulletin, 198(3), 387‐395. Reference: Biol. Bull. 198: 387-395. (June 2000) Larval Development of the Tropical Deep-Sea Echinoid Aspidodiademajacobyi: Phylogenetic Implications CRAIG M. YOUNG* AND SOPHIE B. GEORGEt Division of Marine Science, Harbor Branch Oceanographic Institution, 5600 U.S. Hwy. 1 N., Ft. Pierce, Florida 34946 Abstract. The complete larval development of an echi- Introduction noid in the family Aspidodiadematidaeis described for the first time from in vitro cultures of Aspidodiademajacobyi, Larval developmental mode has been inferredfrom egg a bathyal species from the Bahamian Slope. Over a period size for a large numberof echinodermspecies from the deep of 5 months, embryos grew from small (98-,um) eggs to sea, but only a few of these have been culturedinto the early very large (3071-pum)and complex planktotrophicechino- larval stages (Prouho, 1888; Mortensen, 1921; Young and pluteus larvae. The fully developed larva has five pairs of Cameron, 1989; Young et al., 1989), and no complete red-pigmented arms (preoral, anterolateral,postoral, pos- ontogenetic sequence of larval development has been pub- lished for invertebrate.One of the terodorsal,and posterolateral);fenestrated triangular plates any deep-sea species whose have been described et at the bases of fenestratedpostoral and posterodorsalarms; early stages (Young al., 1989) is a small-bodied sea urchin with a complex dorsal arch; posterodorsalvibratile lobes; a ring Aspidodiademajacobyi, flexible that lives at in the of cilia around the region of the preoral and anterolateral long spines bathyal depths eastern Atlantic 1). -
Echinodermata: Echinoidea) Alexander Ziegler*1, Cornelius Faber2 and Thomas Bartolomaeus3
Frontiers in Zoology BioMed Central Research Open Access Comparative morphology of the axial complex and interdependence of internal organ systems in sea urchins (Echinodermata: Echinoidea) Alexander Ziegler*1, Cornelius Faber2 and Thomas Bartolomaeus3 Address: 1Institut für Immungenetik, Charité-Universitätsmedizin Berlin, Freie Universität Berlin, Thielallee 73, 14195 Berlin, Germany, 2Institut für Klinische Radiologie, Universitätsklinikum Münster, Westfälische Wilhelms-Universität Münster, Waldeyerstraße 1, 48149 Münster, Germany and 3Institut für Evolutionsbiologie und Zooökologie, Rheinische Friedrich-Wilhelms-Universität Bonn, An der Immenburg 1, 53121 Bonn, Germany Email: Alexander Ziegler* - [email protected]; Cornelius Faber - [email protected]; Thomas Bartolomaeus - [email protected] * Corresponding author Published: 9 June 2009 Received: 4 December 2008 Accepted: 9 June 2009 Frontiers in Zoology 2009, 6:10 doi:10.1186/1742-9994-6-10 This article is available from: http://www.frontiersinzoology.com/content/6/1/10 © 2009 Ziegler et al; licensee BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Abstract Background: The axial complex of echinoderms (Echinodermata) is composed of various primary and secondary body cavities that interact with each other. In sea urchins (Echinoidea), structural differences of the axial complex in "regular" and irregular species have been observed, but the reasons underlying these differences are not fully understood. In addition, a better knowledge of axial complex diversity could not only be useful for phylogenetic inferences, but improve also an understanding of the function of this enigmatic structure. -
Redalyc.Echinoids of the Pacific Waters of Panama: Status Of
Revista de Biología Tropical ISSN: 0034-7744 [email protected] Universidad de Costa Rica Costa Rica Lessios, H.A. Echinoids of the Pacific Waters of Panama: Status of knowledge and new records Revista de Biología Tropical, vol. 53, núm. 3, -diciembre, 2005, pp. 147-170 Universidad de Costa Rica San Pedro de Montes de Oca, Costa Rica Available in: http://www.redalyc.org/articulo.oa?id=44919815009 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Echinoids of the Pacific Waters of Panama: Status of knowledge and new records H.A. Lessios Smithsonian Tropical Research Institute, Apartado 0843-03092, Balboa, Panama; Fax: 507-212-8790; [email protected] Received 14-VI-2004. Corrected 09-XII-2004. Accepted 17-V-2005. Abstract: This paper is primarily intended as a guide to researchers who wish to know what echinoid species are available in the Bay of Panama and in the Gulf of Chiriqui, how to recognize them, and what has been published about them up to 2004. Fifty seven species of echinoids have been reported in the literature as occurring in the Pacific waters of Panama, of which I have collected and examined 31, including two species, Caenopedina diomediae and Meoma frangibilis, that have hitherto only been mentioned in the literature from single type specimens. For the 31 species I was able to examine, I list the localities in which they were found, my impression as to their relative abundance, the characters that distinguish them, and what is known about their biology and evolution. -
A Phylogenomic Resolution of the Sea Urchin Tree of Life
bioRxiv preprint doi: https://doi.org/10.1101/430595; this version posted September 29, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. A phylogenomic resolution of the sea urchin tree of life Nicolás Mongiardino Koch ([email protected]) – Corresponding author Department of Geology and Geophysics, Yale University, New Haven CT, USA Simon E. Coppard ([email protected]) Department of Biology, Hamilton College, Clinton NY, USA. Smithsonian Tropical Research Institute, Balboa, Panama. Harilaos A. Lessios ([email protected]) Smithsonian Tropical Research Institute, Balboa, Panama. Derek E. G. Briggs ([email protected]) Department of Geology and Geophysics, Yale University, New Haven CT, USA. Peabody Museum of Natural History, Yale University, New Haven CT, USA. Rich Mooi ([email protected]) Department of Invertebrate Zoology and Geology, California Academy of Sciences, San Francisco CA, USA. Greg W. Rouse ([email protected]) Scripps Institution of Oceanography, UC San Diego, La Jolla CA, USA. bioRxiv preprint doi: https://doi.org/10.1101/430595; this version posted September 29, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Abstract Background: Echinoidea is a clade of marine animals including sea urchins, heart urchins, sand dollars and sea biscuits. -
Phylogenomic Analyses of Echinoid Diversification Prompt a Re
bioRxiv preprint doi: https://doi.org/10.1101/2021.07.19.453013; this version posted August 4, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Phylogenomic analyses of echinoid diversification prompt a re- 2 evaluation of their fossil record 3 Short title: Phylogeny and diversification of sea urchins 4 5 Nicolás Mongiardino Koch1,2*, Jeffrey R Thompson3,4, Avery S Hatch2, Marina F McCowin2, A 6 Frances Armstrong5, Simon E Coppard6, Felipe Aguilera7, Omri Bronstein8,9, Andreas Kroh10, Rich 7 Mooi5, Greg W Rouse2 8 9 1 Department of Earth & Planetary Sciences, Yale University, New Haven CT, USA. 2 Scripps Institution of 10 Oceanography, University of California San Diego, La Jolla CA, USA. 3 Department of Earth Sciences, 11 Natural History Museum, Cromwell Road, SW7 5BD London, UK. 4 University College London Center for 12 Life’s Origins and Evolution, London, UK. 5 Department of Invertebrate Zoology and Geology, California 13 Academy of Sciences, San Francisco CA, USA. 6 Bader International Study Centre, Queen's University, 14 Herstmonceux Castle, East Sussex, UK. 7 Departamento de Bioquímica y Biología Molecular, Facultad de 15 Ciencias Biológicas, Universidad de Concepción, Concepción, Chile. 8 School of Zoology, Faculty of Life 16 Sciences, Tel Aviv University, Tel Aviv, Israel. 9 Steinhardt Museum of Natural History, Tel-Aviv, Israel. 10 17 Department of Geology and Palaeontology, Natural History Museum Vienna, Vienna, Austria 18 * Corresponding author. -
Echinodermata: Echinoidea)Del Mar Caribe Colombiano Biota Colombiana, Vol
Biota Colombiana ISSN: 0124-5376 [email protected] Instituto de Investigación de Recursos Biológicos "Alexander von Humboldt" Colombia Borrero Pérez, Giomar Helena; Solano, Oscar David; Benavides Serrato, Milena Lista revisada de los erizos(Echinodermata: Echinoidea)del Mar Caribe Colombiano Biota Colombiana, vol. 3, núm. 1, junio, 2002, pp. 141-148 Instituto de Investigación de Recursos Biológicos "Alexander von Humboldt" Bogotá, Colombia Disponible en: http://www.redalyc.org/articulo.oa?id=49103104 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto MoraBiota Colombiana & Orozco 3 (1) 141 - 148, 2002 Cestrum of Colombia -141 Lista revisada de los erizos (Echinodermata: Echinoidea) del Mar Caribe Colombiano Giomar Helena Borrero-Pérez1, Oscar David Solano2 y Milena Benavides-Serrato3 Instituto de Investigaciones Marinas y Costeras, INVEMAR, A.A. 1016. Cerro de Punta Betín. Santa Marta. Colombia 1Bióloga Marina. Museo de Historia Natural Marina de Colombia. INVEMAR. [email protected]. 2Biólogo Marino M Sc. Coordinador de la Línea de Investigación Biología de Ecosistemas y de la Oficina de Servicios Científicos. INVEMAR. odsolano@ invemar.org.co. 3Bióloga Marina. Museo de Historia Natural Marina de Colombia. INVEMAR. mbenavides@ invemar.org.co. Palabras Clave: Erizos, Echinoidea, Echinodermata, Caribe colombiano, Lista de especies. L os erizos son un grupo de invertebrados exclusiva- El inventario se ha complementado con registros realizados mente marinos que comprende unas 900 especies vivientes en Islas del Rosario, donde Caycedo (1979) colectó a distribuidas desde los polos hasta el Ecuador y desde la Lytechinus williamsi y Clypeaster rosaceus y en el Parque zona intermareal hasta profundidades mayores a 5000 m. -
Echinodermata: Echinoidea) in the Miocene of Styria
©Institut f. Erdwissensch., Geol. u. Paläont., Karl-Franzens-Universität Graz; download www.biologiezentrum.at Ber. Inst. Erdwiss. K.-F.-Univ. Graz ISSN 1608-8166 Band 9 Graz 2004 CLOSING A GAP – DISCOVERY OF A RARE ECHINOTHURIOID (ECHINODERMATA: ECHINOIDEA) IN THE MIOCENE OF STYRIA Andreas KROH Institut für Geologie und Paläontologie, Karl-Franzens-Universität Graz, Heinrichstraße 26, A-8010 Graz, Austria; e-mail: [email protected] The echinothurioids or ”leather sea urchins” are a group of echinoids characterised by their delicate skeleton with imbricate plates. Unlike most other echinoids, which have a relatively strong corona and are often preserved as fossils, the echinothurioids have an extremely poor fossil record. Apart from Echinothuria floris WOODWARD from the Santonian of England of which eight specimens are known (SMITH & WRIGHT, 1990) the present record is the only other fossil echinothurioid known from ”complete” tests. Disarticulated material, mainly spines, have been reported from the Santonian of France (”Phormosoma” homoei LAMBERT, 1907), the Maastrichtian and Danian of Denmark (”Araeosoma” mortenseni RAVN, 1928, ”A.” brunnichi RAVN, 1928 and ”Asthenosoma” striatissimum RAVN, 1928) and the Netherlands (Echinothuria ? sp., JAGT, 2000; SMITH & JEFFERY, 2000), the Miocene of Sardinia (”Phormosoma” lovisatoi LAMBERT, 1907) and the Maltese Islands (KROH, unpublished data), and the Pliocene of New Zealand [Araeosoma aff. thetidis (CLARK), FELL, 1966; spine and test fragments]. The present specimens were recovered from the Lower Badenian (Langhian, Middle Miocene) marls overlying the corallinacean limestone of the Weissenegg Formation, outcropping in the quarries of the Lafarge cement company in Retznei, Styria. One of the two specimens is a nearly complete, albeit crushed corona, the other consists mainly of fragmented plates and spines. -
Phylogenomic Analyses of Echinoid Diversification Prompt a Re
bioRxiv preprint doi: https://doi.org/10.1101/2021.07.19.453013; this version posted July 24, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Phylogenomic analyses of echinoid diversification prompt a re- 2 evaluation of their fossil record 3 Short title: Phylogeny and diversification of sea urchins 4 5 Nicolás Mongiardino Koch1,2*, Jeffrey R Thompson3,4, Avery S Hatch2, Marina F McCowin2, A 6 Frances Armstrong5, Simon E Coppard6, Felipe Aguilera7, Omri Bronstein8,9, Andreas Kroh10, Rich 7 Mooi5, Greg W Rouse2 8 9 1 Department of Earth & Planetary Sciences, Yale University, New Haven CT, USA. 2 Scripps Institution of 10 Oceanography, University of California San Diego, La Jolla CA, USA. 3 Department of Earth Sciences, 11 Natural History Museum, Cromwell Road, SW7 5BD London, UK. 4 University College London Center for 12 Life’s Origins and Evolution, London, UK. 5 Department of Invertebrate Zoology and Geology, California 13 Academy of Sciences, San Francisco CA, USA. 6 Bader International Study Centre, Queen's University, 14 Herstmonceux Castle, East Sussex, UK. 7 Departamento de Bioquímica y Biología Molecular, Facultad de 15 Ciencias Biológicas, Universidad de Concepción, Concepción, Chile. 8 School of Zoology, Faculty of Life 16 Sciences, Tel Aviv University, Tel Aviv, Israel. 9 Steinhardt Museum of Natural History, Tel-Aviv, Israel. 10 17 Department of Geology and Palaeontology, Natural History Museum Vienna, Vienna, Austria 18 * Corresponding author. -
Checklist of the Echinoderms of British Columbia (April 2007) by Philip
Checklist of the Echinoderms of British Columbia (April 2007) by Philip Lambert, Curator Emeritus of Invertebrates Royal British Columbia Museum [email protected] This checklist is based on the information contained in three echinoderm books on Sea Stars, Sea Cucumbers and Brittle Stars (Lambert 1997, 2000; and Lambert and Austin 2007) as well as on unpublished data from the collections of the Royal BC Museum and from Dr. Bill Austin. Many references in the primary literature were consulted for distribution, and the classifications are based in part on the Treatise on Invertebrate Paleontology (Moore 1966); Austin (1985); crinoid monograph by A.H. Clark (1907 to 1967); asteroids by Fisher (1911 to 1930) and Smith Paterson and Lafay (1995) for ophiuroids. This is a work in progress as we process the deep water collections that Fisheries and Oceans Canada has collected over the last 6 years. Several new species have been recorded for BC and more are expected. Species in bold occur in less than 200 metres in BC. The stated depth range refers to the entire geographic range of the species. Species not yet recorded in BC but occurring nearby to the north and south of BC have been included in the list with *. CLASS CRINOIDEA (7 species in BC) Sea Lilies and Feather Stars Depth (metres) Order Hyocrinida Family Hyocrinidae 1. Ptilocrinus pinnatus A.H. Clark, 1907 Five-Armed Sea Lily 2904 Order Bourgueticrinida Family Bathycrinidae 2. Bathycrinus pacificus A.H. Clark, 1907 Ten-armed Abyssal Sea Lily 1655 Order Comatulida Family Pentametrocrinidae 3. Pentametrocrinus cf. varians (P.H. -
Lower Pliocene Mollusks and Echinoids from the Los Angeles Basin, California
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mcndenhull, Director Professional Paper 190 LOWER PLIOCENE MOLLUSKS AND ECHINOIDS FROM THE LOS ANGELES BASIN, CALIFORNIA AND THEIR INFERRED ENVIRONMENT BY W. P. WOODRING UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1938 For sale by the Superintendent of Documents, Washington, D. C. ------ Trice 30 cents CONTENTS Page Abstract._____________----______-_-_-- Inferred environment of larger fossils Continued. Introduction __________-_-___-___---_-_ Inferred depth range of larger fossils______________ 13 New systematic names proposed_______-_ Interpretation of fossils of deep-water facies----.... 15 General features of Los Angeles Basin____ Distribution of fossils of different depth facies...... 16 Repetto formation of Los Angeles Basin __ Paleogeographic implications_____________________ 16 General features.___________________ Bearing on geologic history of Los Angeles Basin.__. 17 Outcrop localities._-_--____-_-_____ Comparison between Los Angeles Basin during Subsurface section.________________ Repetto time and modern deep-water basins on Larger fossils from Repetto formation____ Continental Shelf of southern California._________ 18 Outcrop localities._________________ Age relations of larger fossils.__________________'______ 18 Subsurface localities.---______.__-_- Fossils of deep-water facies__-____________________ 18 Fossils. _ _-____-____---___-_-______. Fossils of intermediate and shallow-water facies.____ 20 Inferred environment of larger fossils..... Descriptions of species_____-___--__-_-____-__-_.____ 22 Depth range of allied modern species. Index.______.________________________ 65 ILLUSTRATIONS Page Page PLATE 1. Relief map of California showing principal areas PLATE 7. Pliocene mollusks from Los Angeles Basin_____ 62 of marine Pliocene formations._____________ 2 8.