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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:23:04Z</responseDate> <request identifier=oai:HAL:hal-01325704v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-01325704v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdv</setSpec> <setSpec>collection:UNIV-PERP</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-NC</setSpec> <setSpec>collection:EHESS</setSpec> <setSpec>collection:IFREMER</setSpec> <setSpec>collection:EPHE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:CRIOBE</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:PSL</setSpec> <setSpec>collection:UNIV-POLYNESIE</setSpec> <setSpec>collection:UPF</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Coral mass spawning predicted by rapid seasonal rise in ocean temperature</title> <creator>Keith, Sally A.</creator> <creator>Maynard, Jeffrey A.</creator> <creator>Edwards, Alasdair J.</creator> <creator>Guest, James R.</creator> <creator>Bauman, Andrew G.</creator> <creator>Hooidonk, Ruben van</creator> <creator>Heron, Scott F.</creator> <creator>Berumen, Michael L.</creator> <creator>Bouwmeester, Jessica</creator> <creator>Piromvaragorn, Srisakul</creator> <creator>Rahbek, Carsten</creator> <creator>Baird, Andrew H.</creator> <contributor>ARC Centre of Excellence for Coral Reef Studies (CoralCoE) ; James Cook University (JCU)</contributor> <contributor>Center for Macroecology ; University of Copenhagen (KU)</contributor> <contributor>Laboratoire d'Excellence CORAIL (LabEX CORAIL) ; Institut de Recherche pour le Développement (IRD) - Université des Antilles et de la Guyane (UAG) - École des hautes études en sciences sociales (EHESS) - École pratique des hautes études (EPHE) - Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) - Université de la Réunion (UR) - Université de la Polynésie Française (UPF) - Université de Nouvelle Calédonie - Institut d'écologie et environnement</contributor> <contributor>Centre de recherches insulaires et observatoire de l'environnement (CRIOBE) ; Université de Perpignan Via Domitia (UPVD) - École pratique des hautes études (EPHE) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>SymbioSeas</contributor> <contributor>Marine Applied Research & Exploration (MARE)</contributor> <contributor>School of Biology ; Newcastle University [Newcastle]</contributor> <contributor>SECORE international</contributor> <contributor>Experimental Marine Ecology Laboratory (EMEL) ; National University of Singapore (NUS)</contributor> <contributor>Cooperative Institute for Marine and Atmospheric Studies ; University of Miami [Coral Gables]</contributor> <contributor>NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML) ; National Oceanic and Atmospheric Administration (NOAA)</contributor> <contributor>Coral Reef Watch ; NOAA Center for Satellite Applications and Research (STAR) ; NOAA National Environmental Satellite, Data, and Information Service (NESDIS) ; National Oceanic and Atmospheric Administration (NOAA) - National Oceanic and Atmospheric Administration (NOAA) - NOAA National Environmental Satellite, Data, and Information Service (NESDIS) ; National Oceanic and Atmospheric Administration (NOAA) - National Oceanic and Atmospheric Administration (NOAA)</contributor> <contributor>Marine Geophysical Laboratory ; James Cook University (JCU)</contributor> <contributor>Red Sea Research Center ; King Abdullah University of Science and Technology (KAUST)</contributor> <contributor>Department of Geology ; University of Illinois at Urbana-Champaign [Urbana]</contributor> <contributor>Carl R. Woese Institute of Genomic Biology ; University of Illinois at Urbana-Champaign [Urbana]</contributor> <contributor>Center of Excellence for Biodiversity of Peninsular Thailand ; Prince of Songkla University</contributor> <contributor>Imperial College London</contributor> <description>International audience</description> <source>ISSN: 0962-8452</source> <source>Proceedings of the Royal Society B: Biological Sciences</source> <publisher>Royal Society, The</publisher> <identifier>hal-01325704</identifier> <identifier>https://hal-univ-perp.archives-ouvertes.fr/hal-01325704</identifier> <source>https://hal-univ-perp.archives-ouvertes.fr/hal-01325704</source> <source>Proceedings of the Royal Society B: Biological Sciences, Royal Society, The, 2016, 283 (1830), 〈10.1098/rspb.2016.0011 〉</source> <identifier>DOI : 10.1098/rspb.2016.0011 </identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1098/rspb.2016.0011 </relation> <language>en</language> <subject lang=en>phenology</subject> <subject lang=en>reproduction</subject> <subject lang=en>biogeography</subject> <subject lang=en>macroecology</subject> <subject lang=en>Acropora</subject> <subject lang=en>Indo-Pacific</subject> <subject>[SDV.EE] Life Sciences [q-bio]/Ecology, environment</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>Coral spawning times have been linked to multiple environmental factors; however, to what extent these factors act as generalized cues across multiple species and large spatial scales is unknown. We used a unique dataset of coral spawning from 34 reefs in the Indian and Pacific Oceans to test if month of spawning and peak spawning month in assemblages of Acropora spp. can be predicted by sea surface temperature (SST), photosynthetically available radiation, wind speed, current speed, rainfall or sunset time. Contrary to the classic view that high mean SST initiates coral spawning, we found rapid increases in SST to be the best predictor in both cases (month of spawning: R2 = 0.73, peak: R2 = 0.62). Our findings suggest that a rapid increase in SST provides the dominant proximate cue for coral mass spawning over large geographical scales. We hypothesize that coral spawning is ultimately timed to ensure optimal fertilization success.</description> <date>2016</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>