Sweeper Tentacles of the Brain Coral Platygyra Daedalea: Induced Development and Effects on Competitors
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Genetic Variation in Heat Tolerance of the Coral Platygyra Daedalea Offers the Potential for 2 Adaptation to Ocean Warming
bioRxiv preprint doi: https://doi.org/10.1101/2020.10.13.337089; this version posted October 17, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 1 Title: Genetic variation in heat tolerance of the coral Platygyra daedalea offers the potential for 2 adaptation to ocean warming. 3 4 Running head: Genetics of corals’ heat tolerance 5 6 Holland Elder1* 7 Virginia Weis1 8 Jose Montalvo-Proano2,3 9 Veronique J.L Mocellin2 10 Andrew H. Baird3 11 Eli Meyer1, 4 12 Line K. Bay2, 4 13 14 1. Oregon State University, Corvallis, OR, USA. 97331 15 2. Australian Institute of Marine Science, 1526 Cape Cleveland Road, Cape Cleveland 16 4810, Queensland, Australia 17 AIMS@JCU 18 3. ARC Centre of Excellence for Coral Reef Studies, James Cook University, 1 James Cook 19 Dr, Douglas QLD 4814, Australia 20 4. These authors contributed equally 21 22 *corresponding author 23 760-622-9116 24 [email protected] 25 26 Keywords: coral reefs; resilience, heritability, genomic markers, allele frequency change 27 28 Paper type: Primary research article. 29 Global Change Biology 30 bioRxiv preprint doi: https://doi.org/10.1101/2020.10.13.337089; this version posted October 17, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 31 Abstract 32 Reef-building corals are foundational species in coral reef ecosystems and are threatened 33 by many stressors including rising ocean temperatures. -
(Symbiodinium) in Scleractinian Corals from Tropical Reefs in Southern Hainan
Journal of Systematics and Evolution 49 (6): 598–605 (2011) doi: 10.1111/j.1759-6831.2011.00161.x Research Article Low genetic diversity of symbiotic dinoflagellates (Symbiodinium) in scleractinian corals from tropical reefs in southern Hainan Island, China 1,2Guo-Wei ZHOU 1,2Hui HUANG∗ 1(Key Laboratory of Marine Bio-resources Sustainable Utilization, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China) 2(Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya 572000, China) Abstract Endosymbiotic dinoflagellates in the genus Symbiodinium are among the most abundant and important group of photosynthetic protists found in coral reef ecosystems. In order to further characterize this diversity and compare with other regions of the Pacific, samples from 44 species of scleractinian corals representing 20 genera and 9 families, were collected from tropical reefs in southern Hainan Island, China. Denaturing gradient gel electrophoresis fingerprinting of the ribosomal internal transcribed spacer 2 identified 11 genetically distinct Symbiodinium types that have been reported previously. The majority of reef-building coral species (88.6%) harbored only one subcladal type of symbiont, dominated by host-generalist C1 and C3, and was influenced little by the host’s apparent mode of symbiont acquisition. Some species harbored more than one clade of Symbiodinium (clades C, D) concurrently. Although geographically isolated from the rest of the Pacific, the symbiont diversity in southern Hainan Island was relatively low and similar to both the Great Barrier Reef and Hawaii symbiont assemblages (dominated by clade C Symbiodinium). These results indicate that a specialist symbiont is not a prerequisite for existence in remote and isolated areas, but additional work in other geographic regions is necessary to test this idea. -
Checklist of Fish and Invertebrates Listed in the CITES Appendices
JOINTS NATURE \=^ CONSERVATION COMMITTEE Checklist of fish and mvertebrates Usted in the CITES appendices JNCC REPORT (SSN0963-«OStl JOINT NATURE CONSERVATION COMMITTEE Report distribution Report Number: No. 238 Contract Number/JNCC project number: F7 1-12-332 Date received: 9 June 1995 Report tide: Checklist of fish and invertebrates listed in the CITES appendices Contract tide: Revised Checklists of CITES species database Contractor: World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge, CB3 ODL Comments: A further fish and invertebrate edition in the Checklist series begun by NCC in 1979, revised and brought up to date with current CITES listings Restrictions: Distribution: JNCC report collection 2 copies Nature Conservancy Council for England, HQ, Library 1 copy Scottish Natural Heritage, HQ, Library 1 copy Countryside Council for Wales, HQ, Library 1 copy A T Smail, Copyright Libraries Agent, 100 Euston Road, London, NWl 2HQ 5 copies British Library, Legal Deposit Office, Boston Spa, Wetherby, West Yorkshire, LS23 7BQ 1 copy Chadwick-Healey Ltd, Cambridge Place, Cambridge, CB2 INR 1 copy BIOSIS UK, Garforth House, 54 Michlegate, York, YOl ILF 1 copy CITES Management and Scientific Authorities of EC Member States total 30 copies CITES Authorities, UK Dependencies total 13 copies CITES Secretariat 5 copies CITES Animals Committee chairman 1 copy European Commission DG Xl/D/2 1 copy World Conservation Monitoring Centre 20 copies TRAFFIC International 5 copies Animal Quarantine Station, Heathrow 1 copy Department of the Environment (GWD) 5 copies Foreign & Commonwealth Office (ESED) 1 copy HM Customs & Excise 3 copies M Bradley Taylor (ACPO) 1 copy ^\(\\ Joint Nature Conservation Committee Report No. -
Coral Species ID
Coral Species ID Colony shape (branching, mound, plates, column, crust, etc) Colony surface (bumpy, smooth, ridges) Polyp/Corallite Size (small, big) Polyp/Corallite shape (round/elliptical, irregular, y- shaped, „ innies vs outies‟ ridge/valley) Polyp color (green, brown, tan, yellow, olive, red) Different Corallite Shapes and Sizes Examples of Massive Stony Corals Montastraea Montastraea Suleimán © W.Harrigan © faveolata cavernosa S. © Diploria strigosa Porites astreoides © M. White© Montastraea faveolata MFAV Small, round polyps Form very large mounds, plates or crusts (to 4-5 m /12-15 ft) © S. ThorntonS. © Montastraea faveolata MFAV Surfaces smooth, ridged, or with bumps aligned in vertical rows © W. Harrigan © M. Weber © R. Steneck Montastraea faveolata MFAV Colonies are flattened, massive- plates with smooth surfaces under conditions of low light. Montastrea annularis MANN How similar to M. faveolata Small polyps Smooth surface How different Colonies are subdivided into numerous mounds or columns with live polyps at their summits. Plates at colony bases under low light conditions. (to 3-4 m/9-12 ft) Which is which? M. annularis M. faveolata MANN MFAV Montastrea franksi MFRA How similar to M. faveolata Small polyps and bumps Close-up How different Some polyps in bumps are larger, irregularly shaped, and may lack zooxanthellae. More aggressive spatial competitor. © P. Humann Montastrea franksi MFRA How similar to M. faveolata Form mounds, short columns, crusts, and/or plates. How different Bumps are scattered over colony surface. (to 3-4 m/9-12 ft) Montastrea franksi MFRA Flattened, massive plate morphology in low light conditions. Solenastrea bournoni SBOU How similar to M. annularis Small round polyps Mounds How different Lighter colors in life, Walls of some polyps are more distinct (“outies”) Bumpy colony surface (to ~1/2 m/<20 in) Solenastrea hyades SHYA How similar to S. -
Guide to the Identification of Precious and Semi-Precious Corals in Commercial Trade
'l'llA FFIC YvALE ,.._,..---...- guide to the identification of precious and semi-precious corals in commercial trade Ernest W.T. Cooper, Susan J. Torntore, Angela S.M. Leung, Tanya Shadbolt and Carolyn Dawe September 2011 © 2011 World Wildlife Fund and TRAFFIC. All rights reserved. ISBN 978-0-9693730-3-2 Reproduction and distribution for resale by any means photographic or mechanical, including photocopying, recording, taping or information storage and retrieval systems of any parts of this book, illustrations or texts is prohibited without prior written consent from World Wildlife Fund (WWF). Reproduction for CITES enforcement or educational and other non-commercial purposes by CITES Authorities and the CITES Secretariat is authorized without prior written permission, provided the source is fully acknowledged. Any reproduction, in full or in part, of this publication must credit WWF and TRAFFIC North America. The views of the authors expressed in this publication do not necessarily reflect those of the TRAFFIC network, WWF, or the International Union for Conservation of Nature (IUCN). The designation of geographical entities in this publication and the presentation of the material do not imply the expression of any opinion whatsoever on the part of WWF, TRAFFIC, or IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The TRAFFIC symbol copyright and Registered Trademark ownership are held by WWF. TRAFFIC is a joint program of WWF and IUCN. Suggested citation: Cooper, E.W.T., Torntore, S.J., Leung, A.S.M, Shadbolt, T. and Dawe, C. -
The Reproduction of the Red Sea Coral Stylophora Pistillata
MARINE ECOLOGY PROGRESS SERIES Vol. 1, 133-144, 1979 - Published September 30 Mar. Ecol. Prog. Ser. The Reproduction of the Red Sea Coral Stylophora pistillata. I. Gonads and Planulae B. Rinkevich and Y.Loya Department of Zoology. The George S. Wise Center for Life Sciences, Tel Aviv University. Tel Aviv. Israel ABSTRACT: The reproduction of Stylophora pistillata, one of the most abundant coral species in the Gulf of Eilat, Red Sea, was studied over more than two years. Gonads were regularly examined using histological sections and the planula-larvae were collected in situ with plankton nets. S. pistillata is an hermaphroditic species. Ovaries and testes are situated in the same polyp, scattered between and beneath the septa and attached to them by stalks. Egg development starts in July preceding the spermaria, which start to develop only in October. A description is given on the male and female gonads, their structure and developmental processes. During oogenesis most of the oocytes are absorbed and usually only one oocyte remains in each gonad. S. pistillata broods its eggs to the planula stage. Planulae are shed after sunset and during the night. After spawning, the planula swims actively and changes its shape frequently. A mature planula larva of S. pistillata has 6 pairs of complete mesenteries (Halcampoides stage). However, a wide variability in developmental stages exists in newly shed planulae. The oral pole of the planula shows green fluorescence. Unique organs ('filaments' and 'nodules') are found on the surface of the planula; -
Pleistocene Reefs of the Egyptian Red Sea: Environmental Change and Community Persistence
Pleistocene reefs of the Egyptian Red Sea: environmental change and community persistence Lorraine R. Casazza School of Science and Engineering, Al Akhawayn University, Ifrane, Morocco ABSTRACT The fossil record of Red Sea fringing reefs provides an opportunity to study the history of coral-reef survival and recovery in the context of extreme environmental change. The Middle Pleistocene, the Late Pleistocene, and modern reefs represent three periods of reef growth separated by glacial low stands during which conditions became difficult for symbiotic reef fauna. Coral diversity and paleoenvironments of eight Middle and Late Pleistocene fossil terraces are described and characterized here. Pleistocene reef zones closely resemble reef zones of the modern Red Sea. All but one species identified from Middle and Late Pleistocene outcrops are also found on modern Red Sea reefs despite the possible extinction of most coral over two-thirds of the Red Sea basin during glacial low stands. Refugia in the Gulf of Aqaba and southern Red Sea may have allowed for the persistence of coral communities across glaciation events. Stability of coral communities across these extreme climate events indicates that even small populations of survivors can repopulate large areas given appropriate water conditions and time. Subjects Biodiversity, Biogeography, Ecology, Marine Biology, Paleontology Keywords Coral reefs, Egypt, Climate change, Fossil reefs, Scleractinia, Cenozoic, Western Indian Ocean Submitted 23 September 2016 INTRODUCTION Accepted 2 June 2017 Coral reefs worldwide are threatened by habitat degradation due to coastal development, 28 June 2017 Published pollution run-off from land, destructive fishing practices, and rising ocean temperature Corresponding author and acidification resulting from anthropogenic climate change (Wilkinson, 2008; Lorraine R. -
Volume 2. Animals
AC20 Doc. 8.5 Annex (English only/Seulement en anglais/Únicamente en inglés) REVIEW OF SIGNIFICANT TRADE ANALYSIS OF TRADE TRENDS WITH NOTES ON THE CONSERVATION STATUS OF SELECTED SPECIES Volume 2. Animals Prepared for the CITES Animals Committee, CITES Secretariat by the United Nations Environment Programme World Conservation Monitoring Centre JANUARY 2004 AC20 Doc. 8.5 – p. 3 Prepared and produced by: UNEP World Conservation Monitoring Centre, Cambridge, UK UNEP WORLD CONSERVATION MONITORING CENTRE (UNEP-WCMC) www.unep-wcmc.org The UNEP World Conservation Monitoring Centre is the biodiversity assessment and policy implementation arm of the United Nations Environment Programme, the world’s foremost intergovernmental environmental organisation. UNEP-WCMC aims to help decision-makers recognise the value of biodiversity to people everywhere, and to apply this knowledge to all that they do. The Centre’s challenge is to transform complex data into policy-relevant information, to build tools and systems for analysis and integration, and to support the needs of nations and the international community as they engage in joint programmes of action. UNEP-WCMC provides objective, scientifically rigorous products and services that include ecosystem assessments, support for implementation of environmental agreements, regional and global biodiversity information, research on threats and impacts, and development of future scenarios for the living world. Prepared for: The CITES Secretariat, Geneva A contribution to UNEP - The United Nations Environment Programme Printed by: UNEP World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge CB3 0DL, UK © Copyright: UNEP World Conservation Monitoring Centre/CITES Secretariat The contents of this report do not necessarily reflect the views or policies of UNEP or contributory organisations. -
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https://theses.gla.ac.uk/ Theses Digitisation: https://www.gla.ac.uk/myglasgow/research/enlighten/theses/digitisation/ This is a digitised version of the original print thesis. Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Enlighten: Theses https://theses.gla.ac.uk/ [email protected] Physiology and Ecology of Stylophora pistillata and Echinopora gemmacea From the Red Sea ABDULMOHSIN ABDULLAH AL-SOFYANI A thesis submitted for the degree of Doctor of Philosophy in the Faculty of Science at the University of Glasgow Department of Zoology, University of Glasgow, October 1991 ProQuest Number: 11011401 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 11011401 Published by ProQuest LLC(2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. -
Molecular Phylogeny of Scleractinian Corals From
Huang et al. BMC Evolutionary Biology 2011, 11:37 http://www.biomedcentral.com/1471-2148/11/37 RESEARCH ARTICLE Open Access Cleaning up the ‘Bigmessidae’: Molecular phylogeny of scleractinian corals from Faviidae, Merulinidae, Pectiniidae and Trachyphylliidae Danwei Huang1,2*, Wilfredo Y Licuanan3, Andrew H Baird4, Hironobu Fukami5 Abstract Background: Molecular phylogenetic studies on scleractinian corals have shown that most taxa are not reflective of their evolutionary histories. Based principally on gross morphology, traditional taxonomy suffers from the lack of well-defined and homologous characters that can sufficiently describe scleractinian diversity. One of the most challenging clades recovered by recent analyses is ‘Bigmessidae’, an informal grouping that comprises four conventional coral families, Faviidae, Merulinidae, Pectiniidae and Trachyphylliidae, interspersed among one another with no apparent systematic pattern. There is an urgent need for taxonomic revisions in this clade, but it is vital to first establish phylogenetic relationships within the group. In this study, we reconstruct the evolutionary history of ‘Bigmessidae’ based on five DNA sequence markers gathered from 76 of the 132 currently recognized species collected from five reef regions in the central Indo-Pacific and the Atlantic. Results: We present a robust molecular phylogeny of ‘Bigmessidae’ based on the combined five-gene data, achieving a higher degree of resolution compared to previous analyses. Two Pacific species presumed to be in ‘Bigmessidae’ are more closely related to outgroup clades, suggesting that other unsampled taxa have unforeseen affinities. As expected, nested within ‘Bigmessidae’ are four conventional families as listed above, and relationships among them generally corroborate previous molecular analyses. Our more resolved phylogeny supports a close association of Hydnophora (Merulinidae) with Favites + Montastraea (Faviidae), rather than with the rest of Merulinidae, i.e., Merulina and Scapophyllia. -
Climate Change Impacts on Corals: BIOT and the Pitcairn Islands 1
Climate change impacts on corals: BIOT and the Pitcairn Islands 1 Climate change impacts on corals in the UK Overseas Territories of BIOT and the Pitcairn Islands 2 Climate change impacts on corals: BIOT and the Pitcairn Islands BIOT The British Indian Ocean Territory Changes in sea level and extreme (BIOT) consists of five atolls of low-lying weather events In BIOT, sea level is rising twice as fast as the global islands, including the largest atoll in average. Extreme sea levels appear related to El Niño the world, Great Chagos Bank, and a or La Niña events. When combined with bleaching and number of submerged atolls and banks. acidification sea level rise will reduce the effectiveness of reefs to perform as breakwaters. BIOT has experienced Diego Garcia is the only inhabited island. considerable shoreline erosion, which suggests loss of The BIOT Marine Protected Area (MPA) was designated breakwater effects from protective fringing reefs. in 2010. It covers the entire maritime zone and coastal waters, an approximate area of 640,000 km2. The Other human pressures marine environment is rich and diverse, attracting Rats have caused a crash of seabird populations, sea birds, sharks, cetaceans and sea turtles and with disrupting guano nutrient flows to the detriment of some extensive seagrass and coral reef habitats. It includes reef organisms including sponges and corals. Around the endangered Chagos brain coral (Ctenella chagius), an Diego Garcia, small scale fishing is allowed to residents endemic massive coral unique to BIOT. but illegal, unreported and unregulated (IUU) fishing is also known to occur, and there are concerns of pollution BIOT reefs have suffered extensive bleaching and mortality, and anchor damage within the lagoon. -
Spawning of the Grooved Brain Coral Diploria Labyrinthiformis – Follow-Up on the Webinar Q & a Session
Spawning of the grooved brain coral Diploria labyrinthiformis – Follow-up on the Webinar Q & A session by Co-chairs of the CRC’s Larval Propagation Working Group Dr. Valérie Chamberland SECORE International, CARMABI Foundation Dr. Anastazia Banaszak UNAM, Coralium May 2020 8 Questions #1 through 17 were answered during the webinar but are listed here in case they are of interest to those who could not attend and may want to watch the recording of the Q&A session. All questions that remained unanswered during the webinar are listed and addressed from # 18 through 41. Note that a full recording of this webinar along with slides is available on the CRC’s website at http://crc.reefresilience.org/resources/webinar-series/ 1. What is the name of the underwater photographer documenting spawning of many different species? The photographer´s name is Ellen Muller (see her photo gallery at https://www.pbase.com/imagine) 2. Is Diploria labyrinthiformis split spawning a partial spawning? In other words, is a partial spawning = some parts of the colony, or does the whole colony spawn three times (3 bundles released by a single polyp during the year)? Answered during webinar 3. What would be the correct way to cite the Caribbean-wide Diploria labyrinthiformis spawning monitoring information? Answered during webinar 4. How does full moon influence spawning? Answered during webinar 5. I remember you guys started thinking about an online database to collect spawning observation data. Are you still considering this option? Answered during webinar 6. P. strigosa and P. clivosa have been reported to spawn in Fall/Autumn.