A unique coral biomineralization pattern has resisted 40 million years of major ocean chemistry change.
Identifieur interne : 001C76 ( PubMed/Curation ); précédent : 001C75; suivant : 001C77A unique coral biomineralization pattern has resisted 40 million years of major ocean chemistry change.
Auteurs : Jarosław Stolarski [Pologne] ; Francesca R. Bosellini [Italie] ; Carden C. Wallace [Australie] ; Anne M. Gothmann [États-Unis] ; Maciej Mazur [Pologne] ; Isabelle Domart-Coulon [France] ; Eldad Gutner-Hoch [Israël] ; Rolf D. Neuser [Allemagne] ; Oren Levy [Israël] ; Aldo Shemesh [Israël] ; Anders Meibom [Suisse]Source :
- Scientific reports [ 2045-2322 ] ; 2016.
Abstract
Today coral reefs are threatened by changes to seawater conditions associated with rapid anthropogenic global climate change. Yet, since the Cenozoic, these organisms have experienced major fluctuations in atmospheric CO2 levels (from greenhouse conditions of high pCO2 in the Eocene to low pCO2 ice-house conditions in the Oligocene-Miocene) and a dramatically changing ocean Mg/Ca ratio. Here we show that the most diverse, widespread, and abundant reef-building coral genus Acropora (20 morphological groups and 150 living species) has not only survived these environmental changes, but has maintained its distinct skeletal biomineralization pattern for at least 40 My: Well-preserved fossil Acropora skeletons from the Eocene, Oligocene, and Miocene show ultra-structures indistinguishable from those of extant representatives of the genus and their aragonitic skeleton Mg/Ca ratios trace the inferred ocean Mg/Ca ratio precisely since the Eocene. Therefore, among marine biogenic carbonate fossils, well-preserved acroporid skeletons represent material with very high potential for reconstruction of ancient ocean chemistry.
DOI: 10.1038/srep27579
PubMed: 27302371
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Neuser</name><affiliation wicri:level="1"><nlm:affiliation>Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, D-44780 Bochum, Germany.</nlm:affiliation><country xml:lang="fr">Allemagne</country><wicri:regionArea>Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, D-44780 Bochum</wicri:regionArea></affiliation></author><author><name sortKey="Levy, Oren" sort="Levy, Oren" uniqKey="Levy O" first="Oren" last="Levy">Oren Levy</name><affiliation wicri:level="1"><nlm:affiliation>The Mina &Everard Goodman Faculty of Life Science, Bar-Ilan University, 52900 Ramat-Gan, Israel.</nlm:affiliation><country xml:lang="fr">Israël</country><wicri:regionArea>The Mina &Everard Goodman Faculty of Life Science, Bar-Ilan University, 52900 Ramat-Gan</wicri:regionArea></affiliation></author><author><name sortKey="Shemesh, Aldo" sort="Shemesh, Aldo" uniqKey="Shemesh A" first="Aldo" last="Shemesh">Aldo Shemesh</name><affiliation wicri:level="1"><nlm:affiliation>Department of Earth and Planetary Sciences, The Weizmann Institute of Science, P.O. Box 26, 76100 Rehovot, Israel.</nlm:affiliation><country xml:lang="fr">Israël</country><wicri:regionArea>Department of Earth and Planetary Sciences, The Weizmann Institute of Science, P.O. Box 26, 76100 Rehovot</wicri:regionArea></affiliation></author><author><name sortKey="Meibom, Anders" sort="Meibom, Anders" uniqKey="Meibom A" first="Anders" last="Meibom">Anders Meibom</name><affiliation wicri:level="1"><nlm:affiliation>Laboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL), CH-1015 Lausanne, Switzerland.</nlm:affiliation><country xml:lang="fr">Suisse</country><wicri:regionArea>Laboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL), CH-1015 Lausanne</wicri:regionArea></affiliation></author></analytic><series><title level="j">Scientific reports</title><idno type="eISSN">2045-2322</idno><imprint><date when="2016" type="published">2016</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Today coral reefs are threatened by changes to seawater conditions associated with rapid anthropogenic global climate change. Yet, since the Cenozoic, these organisms have experienced major fluctuations in atmospheric CO2 levels (from greenhouse conditions of high pCO2 in the Eocene to low pCO2 ice-house conditions in the Oligocene-Miocene) and a dramatically changing ocean Mg/Ca ratio. Here we show that the most diverse, widespread, and abundant reef-building coral genus Acropora (20 morphological groups and 150 living species) has not only survived these environmental changes, but has maintained its distinct skeletal biomineralization pattern for at least 40 My: Well-preserved fossil Acropora skeletons from the Eocene, Oligocene, and Miocene show ultra-structures indistinguishable from those of extant representatives of the genus and their aragonitic skeleton Mg/Ca ratios trace the inferred ocean Mg/Ca ratio precisely since the Eocene. Therefore, among marine biogenic carbonate fossils, well-preserved acroporid skeletons represent material with very high potential for reconstruction of ancient ocean chemistry.</div></front></TEI><pubmed><MedlineCitation Status="In-Data-Review" Owner="NLM"><PMID Version="1">27302371</PMID><DateCreated><Year>2016</Year><Month>06</Month><Day>15</Day></DateCreated><DateRevised><Year>2017</Year><Month>02</Month><Day>20</Day></DateRevised><Article PubModel="Electronic"><Journal><ISSN IssnType="Electronic">2045-2322</ISSN><JournalIssue CitedMedium="Internet"><Volume>6</Volume><PubDate><Year>2016</Year><Month>Jun</Month><Day>15</Day></PubDate></JournalIssue><Title>Scientific reports</Title><ISOAbbreviation>Sci Rep</ISOAbbreviation></Journal><ArticleTitle>A unique coral biomineralization pattern has resisted 40 million years of major ocean chemistry change.</ArticleTitle><Pagination><MedlinePgn>27579</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1038/srep27579</ELocationID><Abstract><AbstractText>Today coral reefs are threatened by changes to seawater conditions associated with rapid anthropogenic global climate change. Yet, since the Cenozoic, these organisms have experienced major fluctuations in atmospheric CO2 levels (from greenhouse conditions of high pCO2 in the Eocene to low pCO2 ice-house conditions in the Oligocene-Miocene) and a dramatically changing ocean Mg/Ca ratio. Here we show that the most diverse, widespread, and abundant reef-building coral genus Acropora (20 morphological groups and 150 living species) has not only survived these environmental changes, but has maintained its distinct skeletal biomineralization pattern for at least 40 My: Well-preserved fossil Acropora skeletons from the Eocene, Oligocene, and Miocene show ultra-structures indistinguishable from those of extant representatives of the genus and their aragonitic skeleton Mg/Ca ratios trace the inferred ocean Mg/Ca ratio precisely since the Eocene. Therefore, among marine biogenic carbonate fossils, well-preserved acroporid skeletons represent material with very high potential for reconstruction of ancient ocean chemistry.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Stolarski</LastName><ForeName>Jarosław</ForeName><Initials>J</Initials><AffiliationInfo><Affiliation>Institute of Paleobiology, Polish Academy of Sciences, Twarda 51/55, PL-00-818 Warsaw, Poland.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Bosellini</LastName><ForeName>Francesca R</ForeName><Initials>FR</Initials><AffiliationInfo><Affiliation>Dipartimento di Scienze Chimiche e Geologiche, Università di Modena e Reggio Emilia, Via Campi 103, 41125 Modena, Italy.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Wallace</LastName><ForeName>Carden C</ForeName><Initials>CC</Initials><AffiliationInfo><Affiliation>Biodiversity &Geosciences Program, Queensland Museum, South Brisbane, Qld 4101, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Gothmann</LastName><ForeName>Anne M</ForeName><Initials>AM</Initials><AffiliationInfo><Affiliation>University of Washington, School of Oceanography, Box 357940, WA 98195-7940, Seattle, USA.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Mazur</LastName><ForeName>Maciej</ForeName><Initials>M</Initials><AffiliationInfo><Affiliation>Department of Chemistry, University of Warsaw, Pasteura 1, 02-093 Warsaw, Poland.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Domart-Coulon</LastName><ForeName>Isabelle</ForeName><Initials>I</Initials><AffiliationInfo><Affiliation>MCAM UMR7245 Muséum National d'Histoire Naturelle - CNRS, Sorbonne-Universités, Paris, France.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Gutner-Hoch</LastName><ForeName>Eldad</ForeName><Initials>E</Initials><AffiliationInfo><Affiliation>The Mina &Everard Goodman Faculty of Life Science, Bar-Ilan University, 52900 Ramat-Gan, Israel.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Neuser</LastName><ForeName>Rolf D</ForeName><Initials>RD</Initials><AffiliationInfo><Affiliation>Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, D-44780 Bochum, Germany.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Levy</LastName><ForeName>Oren</ForeName><Initials>O</Initials><AffiliationInfo><Affiliation>The Mina &Everard Goodman Faculty of Life Science, Bar-Ilan University, 52900 Ramat-Gan, Israel.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Shemesh</LastName><ForeName>Aldo</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>Department of Earth and Planetary Sciences, The Weizmann Institute of Science, P.O. Box 26, 76100 Rehovot, Israel.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Meibom</LastName><ForeName>Anders</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>Laboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL), CH-1015 Lausanne, Switzerland.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>Center for Advanced Surface Analysis, Institute of Earth Sciences, Université de Lausanne, CH-1015 Lausanne, Switzerland.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2016</Year><Month>06</Month><Day>15</Day></ArticleDate></Article><MedlineJournalInfo><Country>England</Country><MedlineTA>Sci Rep</MedlineTA><NlmUniqueID>101563288</NlmUniqueID><ISSNLinking>2045-2322</ISSNLinking></MedlineJournalInfo><CitationSubset>IM</CitationSubset><CommentsCorrectionsList><CommentsCorrections RefType="Cites"><RefSource>Proc Natl Acad Sci U S A. 2013 Mar 5;110(10):3788-93</RefSource><PMID Version="1">23431140</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Chem Rev. 2008 Nov;108(11):4433-54</RefSource><PMID Version="1">18937512</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2011 Jul 24;476(7360):320-3</RefSource><PMID Version="1">21785439</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Mol Ecol. 2012 May;21(10):2440-54</RefSource><PMID Version="1">22490231</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>PLoS One. 2011;6(10):e26411</RefSource><PMID Version="1">22065994</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>J Morphol. 2011 Feb;272(2):191-203</RefSource><PMID Version="1">21210490</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>J Struct Biol. 2014 Jan;185(1):79-88</RefSource><PMID Version="1">24511631</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>BMC Evol Biol. 2011 Oct 28;11:316</RefSource><PMID Version="1">22034946</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Mol Biol Evol. 2013 Sep;30(9):2099-112</RefSource><PMID Version="1">23765379</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>J Exp Biol. 1998 Jul;201 (Pt 13):2001-9</RefSource><PMID Version="1">9622572</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>PLoS One. 2008 Sep 16;3(9):e3222</RefSource><PMID Version="1">18795098</PMID></CommentsCorrections></CommentsCorrectionsList><OtherID Source="NLM">PMC4908604</OtherID></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2015</Year><Month>12</Month><Day>14</Day></PubMedPubDate><PubMedPubDate PubStatus="accepted"><Year>2016</Year><Month>05</Month><Day>17</Day></PubMedPubDate><PubMedPubDate PubStatus="entrez"><Year>2016</Year><Month>6</Month><Day>16</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2016</Year><Month>6</Month><Day>16</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2016</Year><Month>6</Month><Day>16</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>epublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">27302371</ArticleId><ArticleId IdType="pii">srep27579</ArticleId><ArticleId IdType="doi">10.1038/srep27579</ArticleId><ArticleId IdType="pmc">PMC4908604</ArticleId></ArticleIdList></PubmedData></pubmed></record>Pour manipuler ce document sous Unix (Dilib)
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