Echinodermata: Echinoidea)
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https://doi.org/10.24199/j.mmv.1934.8.08 September 1934 Mem. Nat. Mus. Vict., viii, 1934. THE CAINOZOIG CIDARIDAE OF AUSTRALIA. By Frederick Chapman, A.L.S., F.G.S., Commonwealth Palaeon- tologist, and Francis A. Cudmore, Hon. Palaeontologist, National Museum. Plates XII-XV. Nearly 60 years ago Professor P. M. Duncan described the first Australian Cainozoic cidaroid before the Geological Society of London. During the next 20 years Professors R. Tate and J. W. Gregory published references to our fossil cidaroids, but further descriptive work was not attempted until the present authors undertook to examine the accumulated material in the National Museum, the Tate Collection at Adelaide University Museum, the Commonwealth Palaeontological Collection, and the private collections made by the late Dr. T. S. Hall, F. A. Singleton, the Rev. Geo. Cox and the authors. The classification of the Cidaridae is founded mainly upon living species and it is partly based on structures which are only rarely preserved in fossils. Fossil cidaroid tests are usually imperfect. On abraded tests the conjugation of ambulacral pores is obscure. The apical system is preserved only in one specimen among those examined. The spines are rarely attached to the test and pedicellariae are wanting. Therefore, in dealing with our specimens we have been guided mainly by the appear- ance and structure of ambulacral and interambulacral areas. Certain features used in our classification vary with the growth stage of the test : for instance, the number of coronal plates in vertical series, the number of ambulacral plates adjacent to the largest coronal plate, and sometimes the number of granules on the inner end of ambulacral plates. -
Marine Animal Behaviour in a High CO2 Ocean
Vol. 536: 259–279, 2015 MARINE ECOLOGY PROGRESS SERIES Published September 29 doi: 10.3354/meps11426 Mar Ecol Prog Ser REVIEW Marine animal behaviour in a high CO2 ocean Jeff C. Clements*, Heather L. Hunt Department of Biology, University of New Brunswick Saint John Campus, 100 Tucker Park Road, Saint John E2L 4L5, NB, Canada ABSTRACT: Recently, the effects of ocean acidification (OA) on marine animal behaviour have garnered considerable attention, as they can impact biological interactions and, in turn, ecosystem structure and functioning. We reviewed current published literature on OA and marine behaviour and synthesize current understanding of how a high CO2 ocean may impact animal behaviour, elucidate critical unknowns, and provide suggestions for future research. Although studies have focused equally on vertebrates and invertebrates, vertebrate studies have primarily focused on coral reef fishes, in contrast to the broader diversity of invertebrate taxa studied. A quantitative synthesis of the direction and magnitude of change in behaviours from current conditions under OA scenarios suggests primarily negative impacts that vary depending on species, ecosystem, and behaviour. The interactive effects of co-occurring environmental parameters with increasing CO2 elicit effects different from those observed under elevated CO2 alone. Although 12% of studies have incorporated multiple factors, only one study has examined the effects of carbonate system variability on the behaviour of a marine animal. Altered GABAA receptor functioning under elevated CO2 appears responsible for many behavioural responses; however, this mechanism is unlikely to be universal. We recommend a new focus on determining the effects of elevated CO2 on marine animal behaviour in the context of multiple environmental drivers and future carbonate system variability, and the mechanisms governing the association between acid-base regulation and GABAA receptor functioning. -
Morphological Investigations of Selected Echinoids
Morphological investigations of selected echinoids Katja Jaszkowiak; [email protected] Sascha Hentschel; [email protected] Abstract Echinoids have a radial pattern that is formed by sceletal plates which are fused to each other and form rows that run from the oral to the aboral surface. These plates can be divided into ambulacral and interambulacral plates. The ambulacral plates are perforated and therefore allow the ambulacral system within the animal a connection with its surrounding. Another important aspect of echinoid morphology is the digestive tract that is situated in a special way within the animal and can be used as a phylogenetic marker showing an additi- onal caecum in some echinoid groups (Ziegler et al., 2010). We also investigated the gonads as they where situated in different positions within the investigated species and also show a different morphology. There are numerous different studies into echinoid biology but many of them focus on very specialized aspects. By investigating three different species belonging to two different echinoid groups (Gracilechinus acutus (Lamarck, 1816), Echinus esculentus (Linnaeus, 1758) - Echinidae (Echinodermata – Echinoidea – Carin- acea ); Brissopsis lyrifera (Forbes, 1841) - (Echinodermata – Echinoidea – Irregularia)) we tried to give a Einleitung Die Echinoidea verfuegen häufig ueber einen ebenfalls sehr komplex und kann fuer phylogene- speziellen radiärsymmetrischen Aufbau. Hierbei tische Studien verwendet werden (Ziegler et al., liegen miteinander verbundene Skelettplatten in 2010). Der After befindet sich bei vielen Arten Form von Reihen, welche von oral nach aboral gegenueber des Mundes auf der Aboralseite des verlaufen, nebeneinander und bilden ein meist Tieres. Um ihn herum sind verschiedene spezielle annähernd globuläres Innenskelett. Diese Platten Platten angeordnet, welche Poren zur Abgabe von lassen sich in Ambulakralplatten und Interabu- Sperma bzw. -
Regular Echinoids, Other Than Hemicidaroida, from Upper Cretaceous Deposits in the Wadi Qena-Area (Eastern Desert, Egypt)
BULLETIN DE L'INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE, SCIENCES DE LA TERRE, 62: 139-154, 1992 BULLETIN VAN HET KONINKLIJK BELGISCH INSTITUT VOOR NATUURWETENSCHAPPEN^ AARDWETENSCHAPPEN, 62: 139-154, 1992 Regular Echinoids, other than Hemicidaroida, from Upper Cretaceous deposits in the Wadi Qena-area (Eastern Desert, Egypt) Joris F. GEYS Abstract been described by GREGORY (1906), by FOURTAU (1900, 1901, 1905, 1909, 1912, 1913 and 1914) and by Numerous regular echinoids have been collected by a German expedi• STEFANINI (1918). GREGORY (1906) mentioned five tion in the Upper Cretaceous of Wadi Qena, Egypt. In this paper, the species: presence of six non-Hemicidaroid species in these deposits is discus• "Micropedina bipatellis sed. Two genera (Desoricidaris and Bandelicyphus) and one species Cyphosoma beadnelli, n. sp. (Bandelicyphus qenaensis) are new. Thylechinus quincuncialis, n. sp. Keywords: Echinoids, Cretaceous, Egypt, Taxonomy. Coptosoma abbatei (Gauthier), 1899 Coptosoma gunnehensis, n. sp." A compilation of his earlier papers, published by Résumé FOURTAU (1914), yields the following list of 38 species and subspecies: De nombreux échinides réguliers ont été récoltés par une expédition "Cidaris Thomasi, Gauthier 1901 allemande dans le Crétacé Supérieur du Wadi Qena, en Egypte. La Dorocidaris Schweinfurthi, Gauthier 1901 présence, dans ces dépôts, de six espèces non-hémicidarides est discu• Typocidaris cenomanensis, Cotteau 1885 tée. Deux genres (Desoricidaris et Bandelicyphus) et une espèce (Ban• Typocidaris chercherensis, -
(Echinoidea, Echinidae) (Belgium) by Joris Geys
Meded. Werkgr. Tert. Kwart. Geol. 26(1) 3-10 1 fig., 1 tab., 1 pi. Leiden, maart 1989 On the presence of Gracilechinus (Echinoidea, Echinidae) in the Late Miocene of the Antwerp area (Belgium) by Joris Geys University of Antwerp (RUCA), Antwerp, Belgium and Robert Marquet Antwerp, Belgium. Geys, J., & R. Marquet. On the presence of Gracilechinus (Echinoidea, in the of — Echinidae) Late Miocene the Antwerp area (Belgium). Meded. Werkgr. Tert. Kwart. Geol., 26(1): 00-00, 1 fig., 1 tab., 1 pi. Leiden, March 1989. Some well-preserved specimens of the regular echinoid Gracilechinus gracilis nysti (Cotteau, 1880) were collected in a temporary outcrop at Borgerhout-Antwerp, in sandstones reworked from the Deurne Sands (Late Miocene). The systematic status of this subspecies is discussed. The present state of knowledge of the Echinidae from the Neogene of the North Sea Basin is reviewed. Prof. Dr J. Geys, Dept. of Geology, University of Antwerp (RUCA), Groenenborgerlaan 171, B-2020 Antwerp, Belgium. Dr R. Marquet, Constitutiestraat 50, B-2008 Antwerp, Belgium, Contents — 3 Introduction, p. 4 Systematic palaeontology, p. 6 Discussion, p. Echinidae in the Neogene of the North Sea Basin—some considerations on 8 systematics, p. 10. References, p. INTRODUCTION extensive excavations the of E17-E18 indicated E3 Because of along western verge motorway (also as ‘Kleine and Ring’) at Borgerhout-Antwerp (Belgium), a remarkable outcrop of Neogene Quaternary beds accessible from The was March to November 1987. outcrop was situated between this motorway and the and extended from the the both ‘Singel’-road, ‘Stenenbrug’ to ‘Zurenborgbrug’, on sides 4 of the exit. -
E Urban Sanctuary Algae and Marine Invertebrates of Ricketts Point Marine Sanctuary
!e Urban Sanctuary Algae and Marine Invertebrates of Ricketts Point Marine Sanctuary Jessica Reeves & John Buckeridge Published by: Greypath Productions Marine Care Ricketts Point PO Box 7356, Beaumaris 3193 Copyright © 2012 Marine Care Ricketts Point !is work is copyright. Apart from any use permitted under the Copyright Act 1968, no part may be reproduced by any process without prior written permission of the publisher. Photographs remain copyright of the individual photographers listed. ISBN 978-0-9804483-5-1 Designed and typeset by Anthony Bright Edited by Alison Vaughan Printed by Hawker Brownlow Education Cheltenham, Victoria Cover photo: Rocky reef habitat at Ricketts Point Marine Sanctuary, David Reinhard Contents Introduction v Visiting the Sanctuary vii How to use this book viii Warning viii Habitat ix Depth x Distribution x Abundance xi Reference xi A note on nomenclature xii Acknowledgements xii Species descriptions 1 Algal key 116 Marine invertebrate key 116 Glossary 118 Further reading 120 Index 122 iii Figure 1: Ricketts Point Marine Sanctuary. !e intertidal zone rocky shore platform dominated by the brown alga Hormosira banksii. Photograph: John Buckeridge. iv Introduction Most Australians live near the sea – it is part of our national psyche. We exercise in it, explore it, relax by it, "sh in it – some even paint it – but most of us simply enjoy its changing modes and its fascinating beauty. Ricketts Point Marine Sanctuary comprises 115 hectares of protected marine environment, located o# Beaumaris in Melbourne’s southeast ("gs 1–2). !e sanctuary includes the coastal waters from Table Rock Point to Quiet Corner, from the high tide mark to approximately 400 metres o#shore. -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
X-Ray Microct Study of Pyramids of the Sea Urchin Lytechinus Variegatus
Journal of Structural Biology Journal of Structural Biology 141 (2003) 9–21 www.elsevier.com/locate/yjsbi X-ray microCT study of pyramids of the sea urchin Lytechinus variegatus S.R. Stock,a,* S. Nagaraja,b J. Barss,c T. Dahl,c and A. Veisc a Institute for Bioengineering and Nanoscience in Advanced Medicine, Northwestern University, 303 E. Chicago Avenue, Tarry 16-717, Chicago, IL 60611-3008, USA b School of Mechanical Engineering, Georgia Institute of Technology, Atlanta, GA 30332, USA c Department of Cell and Molecular Biology, Northwestern University, Chicago, IL 60611, USA Received 19 June 2002, and in revised form 23 September 2002 Abstract This paper reports results of a novel approach, X-ray microCT, for quantifying stereom structures applied to ossicles of the sea urchin Lytechinus variegatus. MicroCT, a high resolution variant of medical CT (computed tomography), allows noninvasive mapping of microstructure in 3-D with spatial resolution approaching that of optical microscopy. An intact pyramid (two demi- pyramids, tooth epiphyses, and one tooth) was reconstructed with 17 lm isotropic voxels (volume elements); two individual demipyramids and a pair of epiphyses were studied with 9–13 lm isotropic voxels. The cross-sectional maps of a linear attenuation coefficient produced by the reconstruction algorithm showed that the structure of the ossicles was quite heterogeneous on the scale of tens to hundreds of micrometers. Variations in magnesium content and in minor elemental constitutents could not account for the observed heterogeneities. Spatial resolution was insufficient to resolve the individual elements of the stereom, but the observed values of the linear attenuation coefficient (for the 26 keV effective X-ray energy, a maximum of 7.4 cmÀ1 and a minimum of 2cmÀ1 away from obvious voids) could be interpreted in terms of fractions of voxels occupied by mineral (high magnesium calcite). -
SI Appendix for Hopkins, Melanie J, and Smith, Andrew B
Hopkins and Smith, SI Appendix SI Appendix for Hopkins, Melanie J, and Smith, Andrew B. Dynamic evolutionary change in post-Paleozoic echinoids and the importance of scale when interpreting changes in rates of evolution. Corrections to character matrix Before running any analyses, we corrected a few errors in the published character matrix of Kroh and Smith (1). Specifically, we removed the three duplicate records of Oligopygus, Haimea, and Conoclypus, and removed characters C51 and C59, which had been excluded from the phylogenetic analysis but mistakenly remain in the matrix that was published in Appendix 2 of (1). We also excluded Anisocidaris, Paurocidaris, Pseudocidaris, Glyphopneustes, Enichaster, and Tiarechinus from the character matrix because these taxa were excluded from the strict consensus tree (1). This left 164 taxa and 303 characters for calculations of rates of evolution and for the principal coordinates analysis. Other tree scaling methods The most basic method for scaling a tree using first appearances of taxa is to make each internal node the age of its oldest descendent ("stand") (2), but this often results in many zero-length branches which are both theoretically questionable and in some cases methodologically problematic (3). Several methods exist for modifying zero-length branches. In the case of the results shown in Figure 1, we assigned a positive length to each zero-length branch by having it share time equally with a preceding, non-zero-length branch (“equal”) (4). However, we compared the results from this method of scaling to several other methods. First, we compared this with rates estimated from trees scaled such that zero-length branches share time proportionally to the amount of character change along the branches (“prop”) (5), a variation which gave almost identical results as the method used for the “equal” method (Fig. -
Field Keys to Common Hawaiian Marine Animals and Plants
DOCUMENT RESUME ED 197 993 SE 034 171 TTTTE Field Keys to Common Hawaiian Marine Animals and Plants: INSTITUTTON Hawaii State Dept. of Education, Honolulu. Officeof In::tructional Services. SEPOPT NO RS-78-5247 PUB DATE Mar 78 NOT? 74p.: Not available in he*:dcopy due to colored pages throughout entire document. EDRS PRICE MFO1 Plus Postage. PC Not Available frcm EPRS. DESCRIPTORS *Animals: Biology: Elementary Secondary Education: Environmental Education: *Field Trips: *Marine Biology: Outdoor Education: *Plant Identification: Science Educat4on TDENTIFTERS Hawaii ABSTRACT Presented are keys for identifyingcommon Hawaiian marine algae, beach plants, reef corals,sea urci.ins, tidepool fishes, and sea cucumbers. Nearly all speciesconsidered can be distinguished by characte-istics visible to- thenaked eye. Line drawings illustrate most plants atd animals included,and a list of suggested readings follows each section. (WB) *********************************************************************** Reproductions supplied by FDPS are the best thatcan be lade from the original document. **************************t***************************************** Field Keys to Common Hawaiian Marine Animals and Plants Office of Instructional Services/General Education Branch Department of Education State of Hawaii RS 78-5247 March 1978 "PERMISSION TO REPRODUCE THIS U S DEPARTMENT OF HEALTH. MATERIAL HAS BEEN GRANTED BY EDUCATION &WELFARE NATIONAL INSTITUTE OF EDUCATION P. Tz_urylo THIS DOCUMENT HAS BEEN qEPRO. DuCED EXACTLY AS PECE1VEDPO.` THE PE PSON OP OPC,AN7ATION ORIGIN. TING IT POINTS Or vIEW OR OPINIONS SATED DO NOT NECESSARILY PE PPE. TO THE EDUCATIONAL RESOURCES SENTO<<IC I AL NATIONAL INSTITUTE 0, INFORMATION CENTER (ERIC)." EDuCA T,ON POSIT.ON OR CY O A N 11 2 The Honorable George R. Arlyoshl Governor, State of Hawaii BOARD OF EDUCATION Rev. -
Variation in Coral-Associated Cryptofaunal Communities Across Spatial Scales and Environmental Gradients
Coral Reefs (2018) 37:827–840 https://doi.org/10.1007/s00338-018-1709-7 REPORT Variation in coral-associated cryptofaunal communities across spatial scales and environmental gradients 1 1 2 Chelsie W. W. Counsell • Megan J. Donahue • Kyle F. Edwards • 1 3 Erik C. Franklin • Mark A. Hixon Received: 2 March 2018 / Accepted: 20 June 2018 / Published online: 5 July 2018 Ó Springer-Verlag GmbH Germany, part of Springer Nature 2018 Abstract Most of the diversity on coral reefs is in the wave height, and chlorophyll-a were significant drivers of cryptofauna, the hidden organisms that inhabit the inter- occurrence. Depth and percent live coral tissue were also stitial spaces of corals and other habitat-forming benthos. identified as important correlates for community compo- However, little is known about the patterns and drivers of sition with distinct responses across taxa. Analyzing spe- diversity in cryptofauna. We investigated how the crypto- cies-specific responses to environmental gradients faunal community associated with the branching coral documented a unique pattern for the guard crab Trapezia Pocillopora meandrina varies across spatial scales and intermedia, which had a higher probability of occurring on environmental gradients. We performed nondestructive smaller colonies (in contrast to 18 other common taxa). visual surveys of the cryptofaunal community on 751 P. The results of a principal coordinates analysis on com- meandrina colonies around the island of O‘ahu (30–73 munity composition and a co-occurrence analysis further colonies per site, 3–6 sites per region, five regions). We supported T. intermedia as having a unique distribution identified 91 species, including 48 fishes and 43 inverte- across colonies, even in comparison with four other Tra- brates. -
SNH Commissioned Report
Scottish Natural Heritage Commissioned Report No. 574 Biological analyses of underwater video from research cruises in Lochs Kishorn and Sunart, off the Mull of Kintyre and islands of Rum, Tiree and Islay, and in the Firth of Lorn and Sound of Mull approaches COMMISSIONED REPORT Commissioned Report No. 574 Biological analyses of underwater video from research cruises in Lochs Kishorn and Sunart, off the Mull of Kintyre and islands of Rum, Tiree and Islay, and in the Firth of Lorn and Sound of Mull approaches For further information on this report please contact: Laura Steel Scottish Natural Heritage Great Glen House INVERNESS IV3 8NW Telephone: 01463 725236 E-mail: [email protected] This report should be quoted as: Moore, C. G. 2013. Biological analyses of underwater video from research cruises in Lochs Kishorn and Sunart, off the Mull of Kintyre and islands of Rum, Tiree and Islay, and in the Firth of Lorn and Sound of Mull approaches. Scottish Natural Heritage Commissioned Report No. 574. This report, or any part of it, should not be reproduced without the permission of Scottish Natural Heritage. This permission will not be withheld unreasonably. The views expressed by the author(s) of this report should not be taken as the views and policies of Scottish Natural Heritage. © Scottish Natural Heritage 2013. COMMISSIONED REPORT Summary Biological analyses of underwater video from research cruises in Lochs Kishorn and Sunart, off the Mull of Kintyre and islands of Rum, Tiree and Islay, and in the Firth of Lorn and Sound of Mull approaches Commissioned Report No.: 574 Project no: 13879 Contractor: Dr Colin Moore Year of publication: 2013 Background To help target marine nature conservation in Scotland, SNH and JNCC have generated a focused list of habitats and species of importance in Scottish waters - the Priority Marine Features (PMFs).