Microstructure and Micromechanics of the Sea Urchin, Colobocentrotus Atratus
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Skeletonized Microfossils from the Lower–Middle Cambrian Transition of the Cantabrian Mountains, Northern Spain
Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain SÉBASTIEN CLAUSEN and J. JAVIER ÁLVARO Clausen, S. and Álvaro, J.J. 2006. Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain. Acta Palaeontologica Polonica 51 (2): 223–238. Two different assemblages of skeletonized microfossils are recorded in bioclastic shoals that cross the Lower–Middle Cambrian boundary in the Esla nappe, Cantabrian Mountains. The uppermost Lower Cambrian sedimentary rocks repre− sent a ramp with ooid−bioclastic shoals that allowed development of protected archaeocyathan−microbial reefs. The shoals yield abundant debris of tube−shelled microfossils, such as hyoliths and hyolithelminths (Torellella), and trilobites. The overlying erosive unconformity marks the disappearance of archaeocyaths and the Iberian Lower–Middle Cambrian boundary. A different assemblage occurs in the overlying glauconitic limestone associated with development of widespread low−relief bioclastic shoals. Their lowermost part is rich in hyoliths, hexactinellid, and heteractinid sponge spicules (Eiffelia), chancelloriid sclerites (at least six form species of Allonnia, Archiasterella, and Chancelloria), cambroclaves (Parazhijinites), probable eoconchariids (Cantabria labyrinthica gen. et sp. nov.), sclerites of uncertain af− finity (Holoplicatella margarita gen. et sp. nov.), echinoderm ossicles and trilobites. Although both bioclastic shoal com− plexes represent similar high−energy conditions, the unconformity at the Lower–Middle Cambrian boundary marks a drastic replacement of microfossil assemblages. This change may represent a real community replacement from hyolithelminth−phosphatic tubular shells to CES (chancelloriid−echinoderm−sponge) meadows. This replacement coin− cides with the immigration event based on trilobites previously reported across the boundary, although the partial infor− mation available from originally carbonate skeletons is also affected by taphonomic bias. -
Endemic Species of Christmas Island, Indian Ocean D.J
RECORDS OF THE WESTERN AUSTRALIAN MUSEUM 34 055–114 (2019) DOI: 10.18195/issn.0312-3162.34(2).2019.055-114 Endemic species of Christmas Island, Indian Ocean D.J. James1, P.T. Green2, W.F. Humphreys3,4 and J.C.Z. Woinarski5 1 73 Pozieres Ave, Milperra, New South Wales 2214, Australia. 2 Department of Ecology, Environment and Evolution, La Trobe University, Melbourne, Victoria 3083, Australia. 3 Western Australian Museum, Locked Bag 49, Welshpool DC, Western Australia 6986, Australia. 4 School of Biological Sciences, The University of Western Australia, 35 Stirling Highway, Crawley, Western Australia 6009, Australia. 5 NESP Threatened Species Recovery Hub, Charles Darwin University, Casuarina, Northern Territory 0909, Australia, Corresponding author: [email protected] ABSTRACT – Many oceanic islands have high levels of endemism, but also high rates of extinction, such that island species constitute a markedly disproportionate share of the world’s extinctions. One important foundation for the conservation of biodiversity on islands is an inventory of endemic species. In the absence of a comprehensive inventory, conservation effort often defaults to a focus on the better-known and more conspicuous species (typically mammals and birds). Although this component of island biota often needs such conservation attention, such focus may mean that less conspicuous endemic species (especially invertebrates) are neglected and suffer high rates of loss. In this paper, we review the available literature and online resources to compile a list of endemic species that is as comprehensive as possible for the 137 km2 oceanic Christmas Island, an Australian territory in the north-eastern Indian Ocean. -
The Effects of Oxygen Supply When Immersed on the Thermal Limits and Performance of the Wave Zone Echinoderm Colobocentrotus Atratus
THE EFFECTS OF OXYGEN SUPPLY WHEN IMMERSED ON THE THERMAL LIMITS AND PERFORMANCE OF THE WAVE ZONE ECHINODERM COLOBOCENTROTUS ATRATUS A THESIS SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI‘I AT MĀNOA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTERS OF SCIENCE IN ZOOLOGY AUGUST 2017 By Sean L. Wilbur Thesis Committee: Amy L. Moran, Chairperson Amber N. Wright Celia M. Smith ACKNOWLEDGMENTS I would like to thank those who have provided their support and guidance during my stint in graduate school. First and foremost, I would like to thank my major advisor Amy Moran for taking a chance on me from the beginning and always providing support, both intellectual and material. The entire Moran lab played a huge part in helping me develop as a scientist and refine my research goals. I want to thank all my colleagues in both the Moran lab and at Kewalo marine lab, who both helped provide guidance and were critical in assisting in dangerous field work. I would also like to thank my committee members Amber Wright and Celia Smith for providing assistance with data analysis and intellectual input into my research. Additionally, I would like to acknowledge my undergraduate advisor, Michael Hadfield, who helped mold me as a young scientist and encouraged me to continue my intellectual pursuits. Lastly, I would like to thank my family for never doubting my resolve and always supporting me in my endeavors. I would like to thank my wife, Ashley Wilbur, for all she has sacrificed to support me and being patient with me. -
Māhā'ulepū, Island of Kaua'i Reconnaissance Survey
National Park Service U.S. Department of the Interior Pacific West Region, Honolulu Office February 2008 Māhā‘ulepū, Island of Kaua‘i Reconnaissance Survey THIS PAGE INTENTIONALLY LEFT BLANK TABLE OF CONTENTS 1 SUMMARY………………………………………………………………………………. 1 2 BACKGROUND OF THE STUDY……………………………………………………..3 2.1 Background of the Study…………………………………………………………………..……… 3 2.2 Purpose and Scope of an NPS Reconnaissance Survey………………………………………4 2.2.1 Criterion 1: National Significance………………………………………………………..4 2.2.2 Criterion 2: Suitability…………………………………………………………………….. 4 2.2.3 Criterion 3: Feasibility……………………………………………………………………. 4 2.2.4 Criterion 4: Management Options………………………………………………………. 4 3 OVERVIEW OF THE STUDY AREA…………………………………………………. 5 3.1 Regional Context………………………………………………………………………………….. 5 3.2 Geography and Climate…………………………………………………………………………… 6 3.3 Land Use and Ownership………………………………………………………………….……… 8 3.4. Maps……………………………………………………………………………………………….. 10 4 STUDY AREA RESOURCES………………………………………..………………. 11 4.1 Geological Resources……………………………………………………………………………. 11 4.2 Vegetation………………………….……………………………………………………...……… 16 4.2.1 Coastal Vegetation……………………………………………………………………… 16 4.2.2 Upper Elevation…………………………………………………………………………. 17 4.3 Terrestrial Wildlife………………..........…………………………………………………………. 19 4.3.1 Birds……………….………………………………………………………………………19 4.3.2 Terrestrial Invertebrates………………………………………………………………... 22 4.4 Marine Resources………………………………………………………………………...……… 23 4.4.1 Large Marine Vertebrates……………………………………………………………… 24 4.4.2 Fishes……………………………………………………………………………………..26 -
Echinodermata Associated with Coral Reefs of Andaman and Nicobar Islands
Rec. zoo!. Surv. India: 100 (Part 3-4) : 21-60, 2002 ECHINODERMATA ASSOCIATED WITH CORAL REEFS OF ANDAMAN AND NICOBAR ISLANDS D. R. K. SASTRY Zoological Survey of India, A & N Regional Station, Port Blair - 744 102 INTRODUCTION Coral reefs are an important ecosystem of the coastal environment. The reef ecosystem IS highly productive and provides substratum, shelter, food etc. to a variety of biota. Consequently a number of faunal and floral elements are attracted towards the reef ecosystem and are closely associated with each other to form a community. Thus the reefs are also rich in biodiversity. Among the coral reef associates echinoderms are a conspicuous element on account of their size, abundance and effect on the reef ecosystem including the corals. In spite of their importance in the coral reef ecosystem and its conservation, very few studies were made on the echinoderm associates of the coral reefs. Though there were some studies elsewhere, the information on reef associated echinoderms of Indian coast is meager and scattered (see Anon, 1995). Hence an attempt is made here to collate the scattered accounts and unpublished information available with Zoological Survey of India. Since the information is from several originals and quoted references and many are to be cited often, these are avoided in the text and a comprehensive bibliography is appended which served as source material and also provides additional references of details and further information. ECHINODERMS OF CORAL REEFS More than 200 species of echinoderms occur in the reef ecosystem of Andaman and Nicobar Islands. These belong to five extant classes with 30 to 60 species of each class. -
The Echinoderm Newsletter
! ""'".--'"-,,A' THE ECHINODERM NEWSLETTER NUlIlber 24. 1999 Editor: Cynthia Ahearn Smithsonian Institution National Museum of Natural History Room W-31S, Mail Stop 163 Washington D.C. 20560-0163 U.S.A. [email protected] Distributed by: David Pawson Smithsonian Institution National Museum of Natural History Room W-323, Mail Stop 163 Washington D.C. 20560-0163 U.S.A. The newsletter contains information concerning meetings and conferences, publications of interest to echinoderm biologists, titles of theses on echinoderms, and research interests, and addresses of echinoderm biologists. Individuals who desire to receive the newsletter should send their name, address and research interests to the editor. scientific literature. and a published document. Koehler, 1899 '•.:.•/'i9 VIRTUAL ECHINODERM NEWSLETTER http://www.nmnh.si.edu/iz/echinoderm • TABLE OF CONTENTS Echinoderm Specialists Addresses; (p-); Fax (f-); e-mail numbers 1 Current Research 39 Papers Presented at Meetings (by country or region) Algeria 63 Australia 64 Europe. .................................................................64 Hong Kong 67 India 67 Jamaica ',' 67 Malaysia 68 Mexico 68 New Zealand 68 Pakistan 68 Russia 68 South America 69 United States 69 Papers Presented at Meetings (by conference) SYmposium on Cenozoic Paleobiology, Florida 71 Annual Meeting of Society for Integrative and Comparative Biology 71 Sixty-Ninth Annual Meeting of the Zoological Society of Japan 73 XIX Congreso de Ciencias del Mar, Chile 76 Evo 1uti on '99......................................................... 77 Fifth Florida Echinoderm Festival 78 10th International Echinoderm Conference 79 Theses and Dissertations 80 Announcements, Notices and Conference Announcements 86 Information Requests and Suggestions 88 Ailsa's Section Contribution by Lucia Campos-Creasey 90 Echinoderms in Literature 91 How I Began Studying Echinoderms - part 9 92 Obituaries Maria da Natividade Albuquerque 93 Alan S. -
A Stem Group Echinoderm from the Basal Cambrian of China and the Origins of Ambulacraria
ARTICLE https://doi.org/10.1038/s41467-019-09059-3 OPEN A stem group echinoderm from the basal Cambrian of China and the origins of Ambulacraria Timothy P. Topper 1,2,3, Junfeng Guo4, Sébastien Clausen 5, Christian B. Skovsted2 & Zhifei Zhang1 Deuterostomes are a morphologically disparate clade, encompassing the chordates (including vertebrates), the hemichordates (the vermiform enteropneusts and the colonial tube-dwelling pterobranchs) and the echinoderms (including starfish). Although deuter- 1234567890():,; ostomes are considered monophyletic, the inter-relationships between the three clades remain highly contentious. Here we report, Yanjiahella biscarpa, a bilaterally symmetrical, solitary metazoan from the early Cambrian (Fortunian) of China with a characteristic echinoderm-like plated theca, a muscular stalk reminiscent of the hemichordates and a pair of feeding appendages. Our phylogenetic analysis indicates that Y. biscarpa is a stem- echinoderm and not only is this species the oldest and most basal echinoderm, but it also predates all known hemichordates, and is among the earliest deuterostomes. This taxon confirms that echinoderms acquired plating before pentaradial symmetry and that their history is rooted in bilateral forms. Yanjiahella biscarpa shares morphological similarities with both enteropneusts and echinoderms, indicating that the enteropneust body plan is ancestral within hemichordates. 1 Shaanxi Key Laboratory of Early Life and Environments, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, 710069 Xi’an, China. 2 Department of Palaeobiology, Swedish Museum of Natural History, Box 50007104 05, Stockholm, Sweden. 3 Department of Earth Sciences, Durham University, Durham DH1 3LE, UK. 4 School of Earth Science and Resources, Key Laboratory for the study of Focused Magmatism and Giant Ore Deposits, MLR, Chang’an University, 710054 Xi’an, China. -
Ambulacraria - Andrew B
PHYLOGENETIC TREE OF LIFE – Ambulacraria - Andrew B. Smith AMBULACRARIA Andrew B. Smith Department of Palaeontology, The Natural History Museum, London SW7 5BD, UK Keywords: Echinoderms, crinoids, ophiuroids, asteroids, echinoids, holothurians, hemichordates, enteropneustes, pterobranchs, Xenoturbella, phylogeny, evolution, mode of life, developmental biology, fossil record, biodiversity Contents 1. General Introduction 2. The Echinodermata 2.1. General features 2.2. Crinoidea (sea lillies and feather stars) 2.3. Asteroidea (starfishes and cushion stars) 2.4. Ophiuroidea (brittlestars and basket stars) 2.5. Holothuroidea (sea cucumbers) 2.6. Echinoidea (sea urchins) 2.7. Stem group echinoderms 3. The Hemichordata 3.1. General features 3.2. Pterobranchs 3.3. Enteropneusts. 4. Plactosphaeroidea (Xenoturbella) Bibliography Bibliographical sketch Summary The Ambulacraria is a major clade of invertebrates that are the immediate sister group to the chordates. It comprises the phyla Echinodermata and Hemichordata and the puzzling genus Xenoturbella, the latter being included on the basis of its molecular similarity. The morphological characters uniting Echinodermata and Hemichordata are listed, as are those that characterize each phylum separately. The five classes of echinoderm and two classes of hemichordate are brief described, and information is provided about their mode of life, development, geological history and current views on their phylogenetic relationships. 1. General Introduction Ambulacraria is the formal name applied to a group of invertebrate animals that includes the echinoderms and hemichordates. They are exclusively marine and their origins extend back some 525 Ma to the Cambrian radiation when the earliest examples appear in the fossil record, although their actual origins probably lie slightly earlier, based on molecular clock studies. -
Ultrastructural and Microanalytical Results from Echinoderm Calcite: Implications for Biomineralization and Diagenesis of Skeletal Material
Micron and Microscopica Acta, Vol. 15, No. 2, pp. 85-90, 1984. 0739-6260/84 83.00+0.00 Printed in Great Britain. C) 1984 Pergamon Press Ltd. ULTRASTRUCTURAL AND MICROANALYTICAL RESULTS FROM ECHINODERM CALCITE: IMPLICATIONS FOR BIOMINERALIZATION AND DIAGENESIS OF SKELETAL MATERIAL DAVID F. BLAKE, DONALD R. PEACOR Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, U.S.A. and LAWRENCE F. ALLARD Department of Materials and Metallurgical Engineering, University of Michigan, Ann Arbor, MI 48109, U.S.A. (Received 9 January 1984) Abstract—Magnesian calcite skeletal elements ofthe modern crinoid echinoderm Neocrinus blakei were studied using high resolution TEM, high voltage TEM and STEM microanalysis. Unlike inorganic magnesian calcites which are compositionally heterogeneous, magnesium in these skeletal calcites is homogeneous to at least the 0.1 jim level. While a mosaic structure exists in echinoderm calcite, high voltage TEM reveals the absence of defects or dislocation features which should exist as a consequence ofthe structure. By comparison, inorganic magnesian calcites show a plethora of defects and dislocation features. High resolution lattice fringe images of the echinoderm calcite exhibit a kinking of fringes between mosaic domains, the boundaries ofwhich are largely coherent. Large scale dislocation structures are not observed. Such a ‘stressed’ lattice structure, if pervasive, explains conflicting observations concerning the ‘single crystal’ or ‘polycrystalline aggregate’ nature of echinoderm calcite. The microstructural and microchemical data demonstrate strong organismal control of skeletal deposition in Echinodermata. Both ultrastructural and compositional heterogeneity/homogeneity should be assessed when determining the susceptibility of skeletal material to diagenetic change. Index key words: Echinoderm calcite, biomineralization, analytical electron microscopy, skeletal diagenesis, magnesian calcite. -
Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea
animals Article Chemical Composition and Microstructural Morphology of Spines and Tests of Three Common Sea Urchins Species of the Sublittoral Zone of the Mediterranean Sea 1, , 1, , 2 3 Anastasios Varkoulis * y, Konstantinos Voulgaris * y, Stefanos Zaoutsos , Antonios Stratakis and Dimitrios Vafidis 1 1 Department of Ichthyology and Aquatic Environment, Nea Ionia, University of Thessaly, 38445 Volos, Greece; dvafi[email protected] 2 Department of Energy Systems, University of Thessaly, 41334 Larisa, Greece; [email protected] 3 School of Mineral Resources Engineering, Crete Technical University of Crete, 73100 Chania, Greece; [email protected] * Correspondence: [email protected] (A.V.); [email protected] (K.V.) These authors contributed equally to this work. y Received: 19 June 2020; Accepted: 2 August 2020; Published: 4 August 2020 Simple Summary: Arbacia lixula, Paracentrotus lividus and Sphaerechinus granularis play a key role in many sublittoral biocommunities of the Mediterranean Sea. However, their skeletons seem to differ, both morphologically and in chemical composition. Thus, the skeletal elements display different properties, which are affected not only by the environment, but also by the vital effect of each species. We studied the microstructural morphology and crystalline phase of the test and spines, while also examining the effect of time on their elemental composition. Results showed morphologic differences among the three species both in spines and tests. They also seem to respond differently to possible time-related changes. The mineralogical composition of P.lividus appears to be quite different compare to the other two species. The results of the present study may contribute to a better understanding of the skeletal properties of these species, this being especially useful in predicting the effects of ocean acidification. -
Middle Ordovician) of Västergötland, Sweden - Faunal Composition and Applicability As Environmental Proxies
Microscopic echinoderm remains from the Darriwilian (Middle Ordovician) of Västergötland, Sweden - faunal composition and applicability as environmental proxies Christoffer Kall Dissertations in Geology at Lund University, Bachelor’s thesis, no 403 (15 hp/ECTS credits) Department of Geology Lund University 2014 Microscopic echinoderm remains from the Darriwilian (Middle Ordovician) of Västergötland, Sweden - faunal composition and applicability as environmental proxies Bachelor’s thesis Christoffer Kall Department of Geology Lund University 2014 Contents 1 Introduction ......................................................................................................................................................... 7 1.1 The Ordovician world and faunas 8 1.2 Phylum Echinodermata 8 1.3 Ordovician echinoderms 9 1.3.1 Asterozoans, 1.3.2 Blastozoans 9 1.3.3 Crinoids 10 1.3.4 Echinozoans 10 1.3.4.1 Echinoidea, 1.3.4.2 Holothuroidea, 1.3.4.3 Ophiocistoidea,…., 1.3.4.6 Stylophorans 10 1.4 Pelmatozoan morphology 10 2 Geologocal setting ............................................................................................................................................. 11 3 Materials and methods ..................................................................................................................................... 13 4 Results ................................................................................................................................................................ 14 4.1 Morphotypes 15 4.1.1 Morphotype -
Antarctic Urchin Ctenocidaris Speciosa Spines: Lessons from the Deep
Cali. Biol. Mar. (2013) 54 : 649-655 Antarctic urchin Ctenocidaris speciosa spines: lessons from the deep Ana I. CATARINO1, Virginie GUIBOURT1, Claire MOUREAUX1, Chantai DE RIDDER1, Philippe COMPERE2 and Philippe DUBOIS1 H) Laboratoire de Biologie Marine, Université Libre de Bruxelles, CP 160/10; av FD Roosevelt 50; 1050 Brussels, Belgium. Telephone: +32-2-650.29.70, fax: +32-2-650.27.96, E-mail:[email protected] O) Département des Sciences et Gestion de IEnvironnement, Université de Liège, Bât. B6c, allée du 6 Août 10; 4000 Liège, Belgium Abstract: Ocean acidification is leading to changes in the oceanic carbonate system. As a result, calcium carbonate saturation horizon is shallowing, especially at high latitudes. Biogenic high magnesium-calcites could be particularly vulnerable, since their solubility is either similar or greater than that of aragonite. Cidaroid urchins have magnesium-calcite spines covered by a polycrystalline cortex which becomes exposed to seawater when mature (not covered by an epidermis). However, deep species live at low calcium carbonate saturation states, especially at high latitudes. We describe here the morphology and the magnesium content of Ctenocidaris speciosa spines collected at different depths from the Weddell Sea (Antarctica) and relate the features with seawater calcium carbonate saturation. We observed that the spines cortex of C. speciosa presented a thicker inner cortex layer and a lower [Mg2+] below the aragonite saturation horizon. We suggest that the cortex of cidaroid spines is able to resist to low calcium carbonate saturation state. Résumé : Les épines de l ’oursin antarctique Ctenocidaris speciosa : leçons venues des profondeurs. L’acidification des océans apporte des changements dans le système des carbonates de l’eau de mer.