The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum.
Identifieur interne : 000B09 ( PubMed/Curation ); précédent : 000B08; suivant : 000B10The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum.
Auteurs : Silvia Frisia [Australie] ; Laura S. Weyrich [Australie] ; John Hellstrom [Australie] ; Andrea Borsato [Australie] ; Nicholas R. Golledge [Nouvelle-Zélande] ; Alexandre M. Anesio [Royaume-Uni] ; Petra Bajo [Australie] ; Russell N. Drysdale [Australie] ; Paul C. Augustinus [Nouvelle-Zélande] ; Camille Rivard [France] ; Alan Cooper [Australie]Source :
- Nature communications [ 2041-1723 ] ; 2017.
Abstract
Marine sediment records suggest that episodes of major atmospheric CO2 drawdown during the last glacial period were linked to iron (Fe) fertilization of subantarctic surface waters. The principal source of this Fe is thought to be dust transported from southern mid-latitude deserts. However, uncertainty exists over contributions to CO2 sequestration from complementary Fe sources, such as the Antarctic ice sheet, due to the difficulty of locating and interrogating suitable archives that have the potential to preserve such information. Here we present petrographic, geochemical and microbial DNA evidence preserved in precisely dated subglacial calcites from close to the East Antarctic Ice-Sheet margin, which together suggest that volcanically-induced drainage of Fe-rich waters during the Last Glacial Maximum could have reached the Southern Ocean. Our results support a significant contribution of Antarctic volcanism to subglacial transport and delivery of nutrients with implications on ocean productivity at peak glacial conditions.
DOI: 10.1038/ncomms15425
PubMed: 28598412
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Weyrich</name><affiliation wicri:level="1"><nlm:affiliation>Australian Centre for Ancient DNA (ACAD), The University of Adelaide, Adelaide, South Australia 5005, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Australian Centre for Ancient DNA (ACAD), The University of Adelaide, Adelaide, South Australia 5005</wicri:regionArea></affiliation></author><author><name sortKey="Hellstrom, John" sort="Hellstrom, John" uniqKey="Hellstrom J" first="John" last="Hellstrom">John Hellstrom</name><affiliation wicri:level="1"><nlm:affiliation>School of Earth Sciences, The University of Melbourne, Parkville, Victoria 3010, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>School of Earth Sciences, The University of Melbourne, Parkville, Victoria 3010</wicri:regionArea></affiliation></author><author><name sortKey="Borsato, Andrea" sort="Borsato, Andrea" uniqKey="Borsato A" first="Andrea" last="Borsato">Andrea Borsato</name><affiliation wicri:level="1"><nlm:affiliation>School of Environmental and Life Sciences, The University of Newcastle, Callaghan, New South Wales 2308, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>School of Environmental and Life Sciences, The University of Newcastle, Callaghan, New South Wales 2308</wicri:regionArea></affiliation></author><author><name sortKey="Golledge, Nicholas R" sort="Golledge, Nicholas R" uniqKey="Golledge N" first="Nicholas R" last="Golledge">Nicholas R. 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Augustinus</name><affiliation wicri:level="1"><nlm:affiliation>School of Environment, The University of Auckland, Private Bag, Auckland 92019, New Zealand.</nlm:affiliation><country xml:lang="fr">Nouvelle-Zélande</country><wicri:regionArea>School of Environment, The University of Auckland, Private Bag, Auckland 92019</wicri:regionArea></affiliation></author><author><name sortKey="Rivard, Camille" sort="Rivard, Camille" uniqKey="Rivard C" first="Camille" last="Rivard">Camille Rivard</name><affiliation wicri:level="1"><nlm:affiliation>European Synchrotron Radiation Facility, 38000 Grenoble, France.</nlm:affiliation><country xml:lang="fr">France</country><wicri:regionArea>European Synchrotron Radiation Facility, 38000 Grenoble</wicri:regionArea></affiliation></author><author><name sortKey="Cooper, Alan" sort="Cooper, Alan" uniqKey="Cooper A" first="Alan" last="Cooper">Alan Cooper</name><affiliation wicri:level="1"><nlm:affiliation>Australian Centre for Ancient DNA (ACAD), The University of Adelaide, Adelaide, South Australia 5005, Australia.</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Australian Centre for Ancient DNA (ACAD), The University of Adelaide, Adelaide, South Australia 5005</wicri:regionArea></affiliation></author></analytic><series><title level="j">Nature communications</title><idno type="eISSN">2041-1723</idno><imprint><date when="2017" type="published">2017</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Marine sediment records suggest that episodes of major atmospheric CO2 drawdown during the last glacial period were linked to iron (Fe) fertilization of subantarctic surface waters. The principal source of this Fe is thought to be dust transported from southern mid-latitude deserts. However, uncertainty exists over contributions to CO2 sequestration from complementary Fe sources, such as the Antarctic ice sheet, due to the difficulty of locating and interrogating suitable archives that have the potential to preserve such information. Here we present petrographic, geochemical and microbial DNA evidence preserved in precisely dated subglacial calcites from close to the East Antarctic Ice-Sheet margin, which together suggest that volcanically-induced drainage of Fe-rich waters during the Last Glacial Maximum could have reached the Southern Ocean. Our results support a significant contribution of Antarctic volcanism to subglacial transport and delivery of nutrients with implications on ocean productivity at peak glacial conditions.</div></front></TEI><pubmed><MedlineCitation Status="In-Data-Review" Owner="NLM"><PMID Version="1">28598412</PMID><DateCreated><Year>2017</Year><Month>06</Month><Day>09</Day></DateCreated><DateRevised><Year>2017</Year><Month>07</Month><Day>14</Day></DateRevised><Article PubModel="Electronic"><Journal><ISSN IssnType="Electronic">2041-1723</ISSN><JournalIssue CitedMedium="Internet"><Volume>8</Volume><PubDate><Year>2017</Year><Month>Jun</Month><Day>09</Day></PubDate></JournalIssue><Title>Nature communications</Title><ISOAbbreviation>Nat Commun</ISOAbbreviation></Journal><ArticleTitle>The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum.</ArticleTitle><Pagination><MedlinePgn>15425</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1038/ncomms15425</ELocationID><Abstract><AbstractText>Marine sediment records suggest that episodes of major atmospheric CO2 drawdown during the last glacial period were linked to iron (Fe) fertilization of subantarctic surface waters. The principal source of this Fe is thought to be dust transported from southern mid-latitude deserts. However, uncertainty exists over contributions to CO2 sequestration from complementary Fe sources, such as the Antarctic ice sheet, due to the difficulty of locating and interrogating suitable archives that have the potential to preserve such information. Here we present petrographic, geochemical and microbial DNA evidence preserved in precisely dated subglacial calcites from close to the East Antarctic Ice-Sheet margin, which together suggest that volcanically-induced drainage of Fe-rich waters during the Last Glacial Maximum could have reached the Southern Ocean. Our results support a significant contribution of Antarctic volcanism to subglacial transport and delivery of nutrients with implications on ocean productivity at peak glacial conditions.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Frisia</LastName><ForeName>Silvia</ForeName><Initials>S</Initials><Identifier Source="ORCID">http://orcid.org/0000-0001-6568-2696</Identifier><AffiliationInfo><Affiliation>School of Environmental and Life Sciences, The University of Newcastle, Callaghan, New South Wales 2308, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Weyrich</LastName><ForeName>Laura S</ForeName><Initials>LS</Initials><AffiliationInfo><Affiliation>Australian Centre for Ancient DNA (ACAD), The University of Adelaide, Adelaide, South Australia 5005, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Hellstrom</LastName><ForeName>John</ForeName><Initials>J</Initials><Identifier Source="ORCID">http://orcid.org/0000-0001-9427-3525</Identifier><AffiliationInfo><Affiliation>School of Earth Sciences, The University of Melbourne, Parkville, Victoria 3010, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Borsato</LastName><ForeName>Andrea</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>School of Environmental and Life Sciences, The University of Newcastle, Callaghan, New South Wales 2308, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Golledge</LastName><ForeName>Nicholas R</ForeName><Initials>NR</Initials><AffiliationInfo><Affiliation>Antarctic Research Centre, Victoria University of Wellington, Wellington 6140, New Zealand.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>GNS Science, Avalon, Lower Hut 5011, New Zealand.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Anesio</LastName><ForeName>Alexandre M</ForeName><Initials>AM</Initials><Identifier Source="ORCID">http://orcid.org/0000-0003-2990-4014</Identifier><AffiliationInfo><Affiliation>Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol BS8 1SS, UK.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Bajo</LastName><ForeName>Petra</ForeName><Initials>P</Initials><AffiliationInfo><Affiliation>School of Geography, The University of Melbourne, Parkville, Victoria 3010, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Drysdale</LastName><ForeName>Russell N</ForeName><Initials>RN</Initials><AffiliationInfo><Affiliation>School of Geography, The University of Melbourne, Parkville, Victoria 3010, Australia.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>Environnements, Dynamiques et Territoires de la Montagne, UMR CNRS, Université de Savoie-Mont Blanc, 73376 Le Bourget du Lac, France.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Augustinus</LastName><ForeName>Paul C</ForeName><Initials>PC</Initials><AffiliationInfo><Affiliation>School of Environment, The University of Auckland, Private Bag, Auckland 92019, New Zealand.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Rivard</LastName><ForeName>Camille</ForeName><Initials>C</Initials><AffiliationInfo><Affiliation>European Synchrotron Radiation Facility, 38000 Grenoble, France.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Cooper</LastName><ForeName>Alan</ForeName><Initials>A</Initials><Identifier Source="ORCID">http://orcid.org/0000-0002-7738-7851</Identifier><AffiliationInfo><Affiliation>Australian Centre for Ancient DNA (ACAD), The University of Adelaide, Adelaide, South Australia 5005, Australia.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate 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