Towards a Phylogenetic Classification of Reef Corals
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(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. -
Patterns in Marine Community Assemblages on Continental Margins: a Faunal and Floral Synthesis from Northern Western Australian Atolls
Journal of the Royal Society of Western Australia, 94: 267–284, 2011 Patterns in marine community assemblages on continental margins: a faunal and floral synthesis from northern Western Australian atolls A Sampey 1 & J Fromont 2 1 Aquatic Zoology, Western Australian Museum, Locked Bag 49, Welshpool DC, WA 6986 [email protected] 2 Aquatic Zoology, Western Australian Museum, Locked Bag 49, Welshpool DC, WA 6986 [email protected] Manuscript received November 2010; accepted January 2011 Abstract Corals and fishes are the most visually apparent fauna on coral reefs and the most often monitored groups to detect change. In comparison, data on noncoral benthic invertebrates and marine plants is sparse. Whether patterns in diversity and distribution for other taxonomic groups align with those detected in corals and fishes is largely unknown. Four shelf-edge atolls in the Kimberley region of Western Australia were surveyed for marine plants, sponges, scleractinian corals, crustaceans, molluscs, echinoderms and fishes in 2006, with a consequent 1521 species reported. Here, we provide the first community level assessment of the biodiversity of these atolls based on these taxonomic groups. Four habitats were surveyed and each was found to have a characteristic community assemblage. Different species assemblages were found among atolls and within each habitat, particularly in the lagoon and reef flat environments. In some habitats we found the common taxa groups (fishes and corals) provide adequate information for community assemblages, but in other cases, for example in the intertidal reef flats, these commonly targeted groups are far less useful in reflecting overall community patterns. -
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. -
Exceptional Development of Dissepimental Coenosteum in the New Eocene Scleractinian Coral Genus Nancygyra (Ypresian, Monte Postale, NE Italy)
TO L O N O G E I L C A A P I ' T A A T L E I I A Bollettino della Società Paleontologica Italiana, 59 (3), 2020, 291-298. Modena C N O A S S. P. I. Exceptional development of dissepimental coenosteum in the new Eocene scleractinian coral genus Nancygyra (Ypresian, Monte Postale, NE Italy) Francesca R. Bosellini*, Jarosław Stolarski, Cesare Andrea Papazzoni & Alessandro Vescogni F.R. Bosellini, Dipartimento di Scienze Chimiche e Geologiche, Università degli Studi di Modena e Reggio Emilia, Via Campi 103, I-41125 Modena, Italy; [email protected] *corresponding author J. Stolarski, Institute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, PL-00-818 Warsaw, Poland; [email protected] C.A. Papazzoni, Dipartimento di Scienze Chimiche e Geologiche, Università degli Studi di Modena e Reggio Emilia, Via Campi 103, I-41125 Modena, Italy; [email protected] A. Vescogni, Dipartimento di Scienze Chimiche e Geologiche, Università degli Studi di Modena e Reggio Emilia, Via Campi 103, I-41125 Modena, Italy; [email protected] KEY WORDS - Aphroid colony, dissepiments, Euphylliidae, coral diversity, EECO, lower Eocene. ABSTRACT - In colonial corals, the polyps are interconnected with a common tissue called coenosarc. Polyps and coenosarc secrete distinct skeletal structures: corallites and coenosteum, respectively. Ratio of corallite to coenosteum development may vary resulting in two extreme architectural patterns of coral colonies: corallite-dominated (e.g., cerioid) and coenosteum-dominated (e.g., aphroid) colonies. A large suite of examples of these patterns can be identified among extant and fossil corals, including Paleozoic rugosan corals. -
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. -
A Skeletal Sr/Ca Record Preserved Indipsastraea(Favia)Speciosaand Implications for Coral Sr/Ca Thermometry in Mid- Title Latitude Regions
A skeletal Sr/Ca record preserved inDipsastraea(Favia)speciosaand implications for coral Sr/Ca thermometry in mid- Title latitude regions Seo, Inah; Lee, Yong Il; Watanabe, Tsuyoshi; Yamano, Hiroya; Shimamura, Michiyo; Yoo, Chan Min; Hyeong, Author(s) Kiseong Geochemistry, Geophysics, Geosystems, 14(8), 2873-2885 Citation https://doi.org/10.1002/ggge.20195 Issue Date 2013-08-09 Doc URL http://hdl.handle.net/2115/55298 Rights Copyright(C)2013 American Geophysical Union Type article File Information GGG14_e20195.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP Article Volume 14, Number 8 9 August 2013 doi: 10.1002/ggge.20195 ISSN: 1525-2027 A skeletal Sr/Ca record preserved in Dipsastraea (Favia) speciosa and implications for coral Sr/Ca thermometry in mid-latitude regions Inah Seo School of Earth and Environmental Sciences, Seoul National University, Seoul, South Korea Deep-Sea and Seabed Resources Research Division, Korea Institute of Ocean Science and Technology, Ansan, South Korea Yong Il Lee School of Earth and Environmental Sciences, Seoul National University, Seoul, South Korea Tsuyoshi Watanabe Department of Natural History Sciences, Faculty of Sciences, Hokkaido University, Hokkaido, Japan Hiroya Yamano Center for Environmental Biology and Ecosystem Studies, National Institute for Environmental Studies, Ibaraki, Japan Michiyo Shimamura Faculty of Earth Environmental Science, Hokkaido University, Hokkaido, Japan Chan Min Yoo and Kiseong Hyeong Deep-Sea and Seabed Resources Research Division, Korea Institute of Ocean Science and Technology, Ansan, South Korea ([email protected]) [1] A core (900 mm long) of the scleractinian coral Dipsastraea (Favia) speciosa was collected from Iki Island (33480N), Japan, one of the highest latitude coral reefs known to exist at present, where winter monthly mean sea surface temperature (SST) drops to 13C. -
The Role of Body Size in Complex Food Webs: a Cold Case
Provided for non-commercial research and educational use only. Not for reproduction, distribution or commercial use. This chapter was originally published in the book Advances in Ecological Research, Vol. 45 published by Elsevier, and the attached copy is provided by Elsevier for the author's benefit and for the benefit of the author's institution, for non-commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues who know you, and providing a copy to your institution’s administrator. All other uses, reproduction and distribution, including without limitation commercial reprints, selling or licensing copies or access, or posting on open internet sites, your personal or institution’s website or repository, are prohibited. For exceptions, permission may be sought for such use through Elsevier's permissions site at: http://www.elsevier.com/locate/permissionusematerial From: Ute Jacob, Aaron Thierry, Ulrich Brose, Wolf E. Arntz, Sofia Berg, Thomas Brey, Ingo Fetzer, Tomas Jonsson, Katja Mintenbeck, Christian Möllmann, Owen Petchey, Jens O. Riede and Jennifer A. Dunne, The Role of Body Size in Complex Food Webs: A Cold Case. In Andrea Belgrano and Julia Reiss, editors: Advances in Ecological Research, Vol. 45, Amsterdam, The Netherlands, 2011, pp. 181-223. ISBN: 978-0-12-386475-8 © Copyright 2011 Elsevier Ltd. Academic press. Author's personal copy The Role of Body Size in Complex Food Webs: A Cold Case UTE JACOB,1,* AARON THIERRY,2,3 ULRICH BROSE,4 WOLF E. ARNTZ,5 SOFIA BERG,6 THOMAS BREY,5 INGO FETZER,7 TOMAS JONSSON,6 KATJA MINTENBECK,5 CHRISTIAN MO¨ LLMANN,1 OWEN L. -
Universiti Putra Malaysia Ecology of Scleractinian
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Universiti Putra Malaysia Institutional Repository UNIVERSITI PUTRA MALAYSIA ECOLOGY OF SCLERACTINIAN CORALS IN THE WATERS OF PORT DICKSON AND THEIR TOLERANCE TO SEDIMENTATION LEE YOKE LEE FSAS 2005 1 ECOLOGY OF SCLERACTINIAN CORALS IN THE WATERS OF PORT DICKSON AND THEIR TOLERANCE TO SEDIMENTATION By LEE YOKE LEE Thesis Submitted to the School of Graduate Studies, Universiti Putra Malaysia, in Fulfillment of the Requirements for the Degree of Master of Science January 2005 This thesis is dedicated to my beloved parents and brothers I love you Mom, Dad, Sherman and Sherwin. ii Abstract of thesis presented to the Senate of Universiti Putra Malaysia in fulfillment of the requirement for the degree of Master of Science ECOLOGY OF SCLERACTINIAN CORALS IN THE WATERS OF PORT DICKSON AND THEIR TOLERANCE TO SEDIMENTATION By LEE YOKE LEE January 2005 Chairman: Professor Mohd. Ibrahim Haji Mohamed, Ph.D Faculty: Environmental Studies This study was conducted in two parts, field data collection and laboratory experiments. Coral reef surveys were done using Line Intercept Transect and Random Sampling Method while an 8-month sedimentation rate monitoring programme was conducted along the coast of Port Dickson at Batu 7, 8, 9 and Tanjung Tuan using sediment traps. Laboratory experiments were conducted on 12 specimens of Porites lutea and Favites abdita respectively using the Buoyant Weighing Technique to monitor coral growth rates during Suspended Sediment Experiments (SSEs). The corals were also subjected to burial experiments to estimate their sediment tolerance and sediment rejection abilities. -
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. -
The Earliest Diverging Extant Scleractinian Corals Recovered by Mitochondrial Genomes Isabela G
www.nature.com/scientificreports OPEN The earliest diverging extant scleractinian corals recovered by mitochondrial genomes Isabela G. L. Seiblitz1,2*, Kátia C. C. Capel2, Jarosław Stolarski3, Zheng Bin Randolph Quek4, Danwei Huang4,5 & Marcelo V. Kitahara1,2 Evolutionary reconstructions of scleractinian corals have a discrepant proportion of zooxanthellate reef-building species in relation to their azooxanthellate deep-sea counterparts. In particular, the earliest diverging “Basal” lineage remains poorly studied compared to “Robust” and “Complex” corals. The lack of data from corals other than reef-building species impairs a broader understanding of scleractinian evolution. Here, based on complete mitogenomes, the early onset of azooxanthellate corals is explored focusing on one of the most morphologically distinct families, Micrabaciidae. Sequenced on both Illumina and Sanger platforms, mitogenomes of four micrabaciids range from 19,048 to 19,542 bp and have gene content and order similar to the majority of scleractinians. Phylogenies containing all mitochondrial genes confrm the monophyly of Micrabaciidae as a sister group to the rest of Scleractinia. This topology not only corroborates the hypothesis of a solitary and azooxanthellate ancestor for the order, but also agrees with the unique skeletal microstructure previously found in the family. Moreover, the early-diverging position of micrabaciids followed by gardineriids reinforces the previously observed macromorphological similarities between micrabaciids and Corallimorpharia as -
CNIDARIA Corals, Medusae, Hydroids, Myxozoans
FOUR Phylum CNIDARIA corals, medusae, hydroids, myxozoans STEPHEN D. CAIRNS, LISA-ANN GERSHWIN, FRED J. BROOK, PHILIP PUGH, ELLIOT W. Dawson, OscaR OcaÑA V., WILLEM VERvooRT, GARY WILLIAMS, JEANETTE E. Watson, DENNIS M. OPREsko, PETER SCHUCHERT, P. MICHAEL HINE, DENNIS P. GORDON, HAMISH J. CAMPBELL, ANTHONY J. WRIGHT, JUAN A. SÁNCHEZ, DAPHNE G. FAUTIN his ancient phylum of mostly marine organisms is best known for its contribution to geomorphological features, forming thousands of square Tkilometres of coral reefs in warm tropical waters. Their fossil remains contribute to some limestones. Cnidarians are also significant components of the plankton, where large medusae – popularly called jellyfish – and colonial forms like Portuguese man-of-war and stringy siphonophores prey on other organisms including small fish. Some of these species are justly feared by humans for their stings, which in some cases can be fatal. Certainly, most New Zealanders will have encountered cnidarians when rambling along beaches and fossicking in rock pools where sea anemones and diminutive bushy hydroids abound. In New Zealand’s fiords and in deeper water on seamounts, black corals and branching gorgonians can form veritable trees five metres high or more. In contrast, inland inhabitants of continental landmasses who have never, or rarely, seen an ocean or visited a seashore can hardly be impressed with the Cnidaria as a phylum – freshwater cnidarians are relatively few, restricted to tiny hydras, the branching hydroid Cordylophora, and rare medusae. Worldwide, there are about 10,000 described species, with perhaps half as many again undescribed. All cnidarians have nettle cells known as nematocysts (or cnidae – from the Greek, knide, a nettle), extraordinarily complex structures that are effectively invaginated coiled tubes within a cell.