Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.
Identifieur interne : 003262 ( PubMed/Curation ); précédent : 003261; suivant : 003263Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.
Auteurs : Kurt Lambeck [Australie] ; Hélène Rouby ; Anthony Purcell [Australie] ; Yiying Sun [République populaire de Chine] ; Malcolm Sambridge [Australie]Source :
- Proceedings of the National Academy of Sciences of the United States of America [ 1091-6490 ] ; 2014.
Descripteurs français
- KwdFr :
- MESH :
English descriptors
- KwdEn :
- MESH :
Abstract
The major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet's dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 y from localities far from former ice margins has provided new constraints on the fluctuation of ice volume in this interval. Key results are: (i) a rapid final fall in global sea level of ∼40 m in <2,000 y at the onset of the glacial maximum ∼30,000 y before present (30 ka BP); (ii) a slow fall to -134 m from 29 to 21 ka BP with a maximum grounded ice volume of ∼52 × 10(6) km(3) greater than today; (iii) after an initial short duration rapid rise and a short interval of near-constant sea level, the main phase of deglaciation occurred from ∼16.5 ka BP to ∼8.2 ka BP at an average rate of rise of 12 m⋅ka(-1) punctuated by periods of greater, particularly at 14.5-14.0 ka BP at ≥40 mm⋅y(-1) (MWP-1A), and lesser, from 12.5 to 11.5 ka BP (Younger Dryas), rates; (iv) no evidence for a global MWP-1B event at ∼11.3 ka BP; and (v) a progressive decrease in the rate of rise from 8.2 ka to ∼2.5 ka BP, after which ocean volumes remained nearly constant until the renewed sea-level rise at 100-150 y ago, with no evidence of oscillations exceeding ∼15-20 cm in time intervals ≥200 y from 6 to 0.15 ka BP.
DOI: 10.1073/pnas.1411762111
PubMed: 25313072
Links toward previous steps (curation, corpus...)
- to stream PubMed, to step Corpus: Pour aller vers cette notice dans l'étape Curation :003374
Links to Exploration step
pubmed:25313072Curation
No country items
Hélène Rouby<affiliation><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and.</nlm:affiliation><wicri:noCountry code="subField">France; and</wicri:noCountry></affiliation>Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en">Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.</title><author><name sortKey="Lambeck, Kurt" sort="Lambeck, Kurt" uniqKey="Lambeck K" first="Kurt" last="Lambeck">Kurt Lambeck</name><affiliation wicri:level="1"><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and kurt.lambeck@anu.edu.au.</nlm:affiliation><country wicri:rule="url">Australie</country><wicri:regionArea>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris</wicri:regionArea></affiliation></author><author><name sortKey="Rouby, Helene" sort="Rouby, Helene" uniqKey="Rouby H" first="Hélène" last="Rouby">Hélène Rouby</name><affiliation><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and.</nlm:affiliation><wicri:noCountry code="subField">France; and</wicri:noCountry></affiliation></author><author><name sortKey="Purcell, Anthony" sort="Purcell, Anthony" uniqKey="Purcell A" first="Anthony" last="Purcell">Anthony Purcell</name><affiliation wicri:level="1"><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200</wicri:regionArea></affiliation></author><author><name sortKey="Sun, Yiying" sort="Sun, Yiying" uniqKey="Sun Y" first="Yiying" last="Sun">Yiying Sun</name><affiliation wicri:level="1"><nlm:affiliation>Department of Earth Sciences, University of Hong Kong, Hong Kong, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Department of Earth Sciences, University of Hong Kong, Hong Kong</wicri:regionArea></affiliation></author><author><name sortKey="Sambridge, Malcolm" sort="Sambridge, Malcolm" uniqKey="Sambridge M" first="Malcolm" last="Sambridge">Malcolm Sambridge</name><affiliation wicri:level="1"><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200</wicri:regionArea></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">PubMed</idno><date when="2014">2014</date><idno type="RBID">pubmed:25313072</idno><idno type="pmid">25313072</idno><idno type="doi">10.1073/pnas.1411762111</idno><idno type="wicri:Area/PubMed/Corpus">003374</idno><idno type="wicri:explorRef" wicri:stream="PubMed" wicri:step="Corpus" wicri:corpus="PubMed">003374</idno><idno type="wicri:Area/PubMed/Curation">003262</idno><idno type="wicri:explorRef" wicri:stream="PubMed" wicri:step="Curation">003262</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en">Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.</title><author><name sortKey="Lambeck, Kurt" sort="Lambeck, Kurt" uniqKey="Lambeck K" first="Kurt" last="Lambeck">Kurt Lambeck</name><affiliation wicri:level="1"><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and kurt.lambeck@anu.edu.au.</nlm:affiliation><country wicri:rule="url">Australie</country><wicri:regionArea>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris</wicri:regionArea></affiliation></author><author><name sortKey="Rouby, Helene" sort="Rouby, Helene" uniqKey="Rouby H" first="Hélène" last="Rouby">Hélène Rouby</name><affiliation><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and.</nlm:affiliation><wicri:noCountry code="subField">France; and</wicri:noCountry></affiliation></author><author><name sortKey="Purcell, Anthony" sort="Purcell, Anthony" uniqKey="Purcell A" first="Anthony" last="Purcell">Anthony Purcell</name><affiliation wicri:level="1"><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200</wicri:regionArea></affiliation></author><author><name sortKey="Sun, Yiying" sort="Sun, Yiying" uniqKey="Sun Y" first="Yiying" last="Sun">Yiying Sun</name><affiliation wicri:level="1"><nlm:affiliation>Department of Earth Sciences, University of Hong Kong, Hong Kong, China.</nlm:affiliation><country xml:lang="fr">République populaire de Chine</country><wicri:regionArea>Department of Earth Sciences, University of Hong Kong, Hong Kong</wicri:regionArea></affiliation></author><author><name sortKey="Sambridge, Malcolm" sort="Sambridge, Malcolm" uniqKey="Sambridge M" first="Malcolm" last="Sambridge">Malcolm Sambridge</name><affiliation wicri:level="1"><nlm:affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;</nlm:affiliation><country xml:lang="fr">Australie</country><wicri:regionArea>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200</wicri:regionArea></affiliation></author></analytic><series><title level="j">Proceedings of the National Academy of Sciences of the United States of America</title><idno type="eISSN">1091-6490</idno><imprint><date when="2014" type="published">2014</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Ice Cover</term><term>Internationality</term><term>Oceans and Seas</term><term>Rheology</term><term>Time Factors</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Couche de glace</term><term>Facteurs temps</term><term>Internationalité</term><term>Océans et mers</term><term>Rhéologie</term></keywords><keywords scheme="MESH" xml:lang="en"><term>Ice Cover</term><term>Internationality</term><term>Oceans and Seas</term><term>Rheology</term><term>Time Factors</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Couche de glace</term><term>Facteurs temps</term><term>Internationalité</term><term>Océans et mers</term><term>Rhéologie</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet's dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 y from localities far from former ice margins has provided new constraints on the fluctuation of ice volume in this interval. Key results are: (i) a rapid final fall in global sea level of ∼40 m in <2,000 y at the onset of the glacial maximum ∼30,000 y before present (30 ka BP); (ii) a slow fall to -134 m from 29 to 21 ka BP with a maximum grounded ice volume of ∼52 × 10(6) km(3) greater than today; (iii) after an initial short duration rapid rise and a short interval of near-constant sea level, the main phase of deglaciation occurred from ∼16.5 ka BP to ∼8.2 ka BP at an average rate of rise of 12 m⋅ka(-1) punctuated by periods of greater, particularly at 14.5-14.0 ka BP at ≥40 mm⋅y(-1) (MWP-1A), and lesser, from 12.5 to 11.5 ka BP (Younger Dryas), rates; (iv) no evidence for a global MWP-1B event at ∼11.3 ka BP; and (v) a progressive decrease in the rate of rise from 8.2 ka to ∼2.5 ka BP, after which ocean volumes remained nearly constant until the renewed sea-level rise at 100-150 y ago, with no evidence of oscillations exceeding ∼15-20 cm in time intervals ≥200 y from 6 to 0.15 ka BP.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" Owner="NLM"><PMID Version="1">25313072</PMID><DateCreated><Year>2014</Year><Month>10</Month><Day>29</Day></DateCreated><DateCompleted><Year>2015</Year><Month>04</Month><Day>17</Day></DateCompleted><DateRevised><Year>2017</Year><Month>02</Month><Day>20</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1091-6490</ISSN><JournalIssue CitedMedium="Internet"><Volume>111</Volume><Issue>43</Issue><PubDate><Year>2014</Year><Month>Oct</Month><Day>28</Day></PubDate></JournalIssue><Title>Proceedings of the National Academy of Sciences of the United States of America</Title><ISOAbbreviation>Proc. Natl. Acad. Sci. U.S.A.</ISOAbbreviation></Journal><ArticleTitle>Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.</ArticleTitle><Pagination><MedlinePgn>15296-303</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1073/pnas.1411762111</ELocationID><Abstract><AbstractText>The major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet's dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 y from localities far from former ice margins has provided new constraints on the fluctuation of ice volume in this interval. Key results are: (i) a rapid final fall in global sea level of ∼40 m in <2,000 y at the onset of the glacial maximum ∼30,000 y before present (30 ka BP); (ii) a slow fall to -134 m from 29 to 21 ka BP with a maximum grounded ice volume of ∼52 × 10(6) km(3) greater than today; (iii) after an initial short duration rapid rise and a short interval of near-constant sea level, the main phase of deglaciation occurred from ∼16.5 ka BP to ∼8.2 ka BP at an average rate of rise of 12 m⋅ka(-1) punctuated by periods of greater, particularly at 14.5-14.0 ka BP at ≥40 mm⋅y(-1) (MWP-1A), and lesser, from 12.5 to 11.5 ka BP (Younger Dryas), rates; (iv) no evidence for a global MWP-1B event at ∼11.3 ka BP; and (v) a progressive decrease in the rate of rise from 8.2 ka to ∼2.5 ka BP, after which ocean volumes remained nearly constant until the renewed sea-level rise at 100-150 y ago, with no evidence of oscillations exceeding ∼15-20 cm in time intervals ≥200 y from 6 to 0.15 ka BP.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Lambeck</LastName><ForeName>Kurt</ForeName><Initials>K</Initials><AffiliationInfo><Affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and kurt.lambeck@anu.edu.au.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Rouby</LastName><ForeName>Hélène</ForeName><Initials>H</Initials><AffiliationInfo><Affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia; Laboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Purcell</LastName><ForeName>Anthony</ForeName><Initials>A</Initials><AffiliationInfo><Affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Sun</LastName><ForeName>Yiying</ForeName><Initials>Y</Initials><AffiliationInfo><Affiliation>Department of Earth Sciences, University of Hong Kong, Hong Kong, China.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Sambridge</LastName><ForeName>Malcolm</ForeName><Initials>M</Initials><AffiliationInfo><Affiliation>Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType><PublicationType UI="D013485">Research Support, Non-U.S. Gov't</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2014</Year><Month>10</Month><Day>13</Day></ArticleDate></Article><MedlineJournalInfo><Country>United States</Country><MedlineTA>Proc Natl Acad Sci U S A</MedlineTA><NlmUniqueID>7505876</NlmUniqueID><ISSNLinking>0027-8424</ISSNLinking></MedlineJournalInfo><CitationSubset>IM</CitationSubset><CommentsCorrectionsList><CommentsCorrections RefType="CommentIn"><RefSource>Proc Natl Acad Sci U S A. 2014 Nov 11;111(45):15861-2</RefSource><PMID Version="1">25368169</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2012 Mar 29;483(7391):559-64</RefSource><PMID Version="1">22460900</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2000 Aug 17;406(6797):713-6</RefSource><PMID Version="1">10963593</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2004 May 21;304(5674):1141-4</RefSource><PMID Version="1">15155944</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2003 Jun 19;423(6942):853-8</RefSource><PMID Version="1">12815427</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2010 Mar 5;327(5970):1235-7</RefSource><PMID Version="1">20075212</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2012 Jul 13;337(6091):216-9</RefSource><PMID Version="1">22798610</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 1995 Feb 17;267(5200):1005-10</RefSource><PMID Version="1">17811441</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2001 Apr 27;292(5517):679-86</RefSource><PMID Version="1">11326090</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Nature. 2009 Mar 19;458(7236):329-32</RefSource><PMID Version="1">19295608</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2000 May 12;288(5468):1033-5</RefSource><PMID Version="1">10807570</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Proc Natl Acad Sci U S A. 2011 Aug 16;108(33):13415-9</RefSource><PMID Version="1">21808034</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2003 Jan 3;299(5603):99-102</RefSource><PMID Version="1">12511648</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2002 Mar 29;295(5564):2438-41</RefSource><PMID Version="1">11896236</PMID></CommentsCorrections><CommentsCorrections RefType="Cites"><RefSource>Science. 2001 Jul 13;293(5528):283-7</RefSource><PMID Version="1">11452120</PMID></CommentsCorrections></CommentsCorrectionsList><MeshHeadingList><MeshHeading><DescriptorName UI="D046448" MajorTopicYN="Y">Ice Cover</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D038622" MajorTopicYN="Y">Internationality</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D009792" MajorTopicYN="Y">Oceans and Seas</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D012212" MajorTopicYN="N">Rheology</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D013997" MajorTopicYN="N">Time Factors</DescriptorName></MeshHeading></MeshHeadingList><OtherID Source="NLM">PMC4217469</OtherID><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="N">Holocene</Keyword><Keyword MajorTopicYN="N">Last Glacial Maximum</Keyword><Keyword MajorTopicYN="N">ice volumes</Keyword><Keyword MajorTopicYN="N">sea level</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="entrez"><Year>2014</Year><Month>10</Month><Day>15</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="pubmed"><Year>2014</Year><Month>10</Month><Day>15</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate><PubMedPubDate PubStatus="medline"><Year>2015</Year><Month>4</Month><Day>18</Day><Hour>6</Hour><Minute>0</Minute></PubMedPubDate></History><PublicationStatus>ppublish</PublicationStatus><ArticleIdList><ArticleId IdType="pubmed">25313072</ArticleId><ArticleId IdType="pii">1411762111</ArticleId><ArticleId IdType="doi">10.1073/pnas.1411762111</ArticleId><ArticleId IdType="pmc">PMC4217469</ArticleId></ArticleIdList></PubmedData></pubmed></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Asie/explor/AustralieFrV1/Data/PubMed/Curation
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 003262 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/PubMed/Curation/biblio.hfd -nk 003262 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Asie
|area= AustralieFrV1
|flux= PubMed
|étape= Curation
|type= RBID
|clé= pubmed:25313072
|texte= Sea level and global ice volumes from the Last Glacial Maximum to the Holocene.
}}
Pour générer des pages wiki
HfdIndexSelect -h $EXPLOR_AREA/Data/PubMed/Curation/RBID.i -Sk "pubmed:25313072" \
| HfdSelect -Kh $EXPLOR_AREA/Data/PubMed/Curation/biblio.hfd \
| NlmPubMed2Wicri -a AustralieFrV1
| This area was generated with Dilib version V0.6.33. |  |