{"refrec":{"BRefID":347614,"RR":"<b>Ronge, T.A.; Frische, M.; Fietzke, J.; Stephens, A.L.; Bostock, H.; Tiedemann, R.</b> (2021). Southern Ocean contribution to both steps in deglacial atmospheric CO<sub>2</sub> rise. <i>NPG Scientific Reports 11(1)</i>: 22117. <a href=\"https://dx.doi.org/10.1038/s41598-021-01657-w\" target=\"_blank\">https://dx.doi.org/10.1038/s41598-021-01657-w</a>","BEntID":344306,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>NPG Scientific Reports 11(1)</i>: 22117. <a href=\"https://dx.doi.org/10.1038/s41598-021-01657-w\" target=\"_blank\">https://dx.doi.org/10.1038/s41598-021-01657-w</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ronge, T.A.; Frische, M.; Fietzke, J.; Stephens, A.L.; Bostock, H.; Tiedemann, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ronge, T.A. <i>et al.</i>","Englishabstract":"The transfer of vast amounts of carbon from a deep oceanic reservoir to the atmosphere is considered to be a dominant driver of the deglacial rise in atmospheric CO<sub>2</sub>. Paleoceanographic reconstructions reveal evidence for the existence of CO<sub>2</sub>-rich waters in the mid to deep Southern Ocean. These water masses ventilate to the atmosphere south of the Polar Front, releasing CO<sub>2</sub> prior to the formation and subduction of intermediate-waters. Changes in the amount of CO<sub>2</sub> in the sea water directly affect the oceanic carbon chemistry system. Here we present B/Ca ratios, a proxy for delta carbonate ion concentrations Δ[CO<sub>3</sub><sup>2−</sup>], and stable isotopes (δ<sup>13</sup>C) from benthic foraminifera from a sediment core bathed in Antarctic Intermediate Water (AAIW), offshore New Zealand in the Southwest Pacific. We find two transient intervals of rising [CO<sub>3</sub><sup>2−</sup>] and δ<sup>13</sup>C that that are consistent with the release of CO<sub>2</sub> via the Southern Ocean. These intervals coincide with the two pulses in rising atmospheric CO<sub>2</sub> at ~ 17.5–14.3&nbsp;ka and 12.9–11.1&nbsp;ka. Our results lend support for the release of sequestered CO<sub>2</sub> from the deep ocean to surface and atmospheric reservoirs during the last deglaciation, although further work is required to pin down the detailed carbon transfer pathways.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Southern Ocean contribution to both steps in deglacial atmospheric CO<sub>2</sub> rise","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-05-21 01:33:52.100261","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-11-25","DateCreate":"2021-11-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000717747400096","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41598-021-01657-w"},"refs":null,"anarec":{"AnaID":347614,"PubliDate":2021,"Pagination":"22117","XtraPublOfAnaID":null,"ISBN":null,"Volume":"11","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":208093,"SerRR":"Scientific Reports (Nature Publishing Group). 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