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Loss of carbon from the deep sea since the last glacial maximum

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dc.contributor.authorYu, Jimin
dc.contributor.authorBroeker, Wally S.
dc.contributor.authorElderfield, H
dc.contributor.authorJin, Zhangdong
dc.contributor.authorMcManus, Jerry
dc.contributor.authorZhang, Fei
dc.date.accessioned2015-12-10T23:17:34Z
dc.date.issued2010
dc.date.updated2016-02-24T09:56:46Z
dc.description.abstractDeep-ocean carbonate ion concentrations ([CO32-]) and carbon isotopic ratios (δ13C) place important constraints on past redistributions of carbon in the ocean-land-atmosphere system and hence provide clues to the causes of atmospheric CO2 concentration c
dc.identifier.issn0036-8075
dc.identifier.urihttp://hdl.handle.net/1885/65274
dc.publisherAmerican Association for the Advancement of Science
dc.sourceScience
dc.subjectKeywords: boron; calcium; carbonic acid; absorption; air-sea interaction; benthic environment; biosphere; boron; calcium; carbon isotope; carbonate; concentration (composition); deep sea; deglaciation; foraminifera; Last Glacial Maximum; paleoceanography; paleoenvi
dc.titleLoss of carbon from the deep sea since the last glacial maximum
dc.typeJournal article
local.bibliographicCitation.issue6007
local.bibliographicCitation.lastpage1087
local.bibliographicCitation.startpage1084
local.contributor.affiliationYu, Jimin, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationBroeker, Wally S., Lamont-Doherty Earth Observatory of Columbia University
local.contributor.affiliationElderfield, H, University of Cambridge
local.contributor.affiliationJin, Zhangdong, Chinese Academy of Sciences
local.contributor.affiliationMcManus, Jerry, Lamont-Doherty Earth Observatory of Columbia University
local.contributor.affiliationZhang, Fei, Chinese Academy of Sciences
local.contributor.authoruidYu, Jimin, u5132511
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040303 - Geochronology
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationU3488905xPUB1081
local.identifier.citationvolume330
local.identifier.doi10.1126/science.1193221
local.identifier.scopusID2-s2.0-78449270061
local.identifier.thomsonID000284374700038
local.type.statusPublished Version

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