{"refrec":{"BRefID":285387,"RR":"<b>Kleinen, T.; Brovkin, V.; Munhoven, G.</b> (2016). Modelled interglacial carbon cycle dynamics during the Holocene, the Eemian and Marine Isotope Stage (MIS) 11. <i>Clim. Past 12(12)</i>: 2145-2160. <a href=\"https://dx.doi.org/10.5194/cp-12-2145-2016\" target=\"_blank\">https://dx.doi.org/10.5194/cp-12-2145-2016</a>","BEntID":277412,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Clim. Past 12(12)</i>: 2145-2160. <a href=\"https://dx.doi.org/10.5194/cp-12-2145-2016\" target=\"_blank\">https://dx.doi.org/10.5194/cp-12-2145-2016</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kleinen, T.; Brovkin, V.; Munhoven, G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kleinen, T. <i>et al.</i>","Englishabstract":"Trends in the atmospheric concentration of CO<sub>2</sub> during three recent interglacials – the Holocene, the Eemian and Marine Isotope Stage (MIS) 11 – are investigated using an earth system model of intermediate complexity, which we extended with process-based modules to consider two slow carbon cycle processes – peat accumulation and shallow-water CaCO<sub>3</sub> sedimentation (coral reef formation). For all three interglacials, model simulations considering peat accumulation and shallow-water CaCO<sub>3</sub> sedimentation substantially improve the agreement between model results and ice core CO<sub>2</sub> reconstructions in comparison to a carbon cycle set-up neglecting these processes. This enables us to model the trends in atmospheric CO<sub>2</sub>, with modelled trends similar to the ice core data, forcing the model only with orbital and sea level changes. During the Holocene, anthropogenic CO<sub>2</sub> emissions are required to match the observed rise in atmospheric CO<sub>2</sub> after 3 ka BP but are not relevant before this time. Our model experiments show a considerable improvement in the modelled CO<sub>2</sub> trends by the inclusion of the slow carbon cycle processes, allowing us to explain the CO<sub>2</sub> evolution during the Holocene and two recent interglacials consistently using an identical model set-up.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Modelled interglacial carbon cycle dynamics during the Holocene, the Eemian and Marine Isotope Stage (MIS) 11","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-18 01:31:57.941386","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2016,"MonPub":null,"DateUpdate":"2017-06-06","DateCreate":"2017-05-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000390142700001","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/cp-12-2145-2016"},"refs":null,"anarec":{"AnaID":285387,"PubliDate":2016,"Pagination":"2145-2160","XtraPublOfAnaID":null,"ISBN":null,"Volume":"12","Issue":"12","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":220505,"SerRR":"Climate of the Past. 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