{"refrec":{"BRefID":351417,"RR":"<b>Yamamoto, M.; Clemens, S.C.; Seki, O.; Tsuchiya, Y.; Huang, Y.; O’ishi, R.; Abe-Ouchi, A.</b> (2022). Increased interglacial atmospheric CO<sub>2</sub> levels followed the mid-Pleistocene Transition. <i>Nature Geoscience 15(4)</i>: 307-313. <a href=\"https://dx.doi.org/10.1038/s41561-022-00918-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-022-00918-1</a>","BEntID":349123,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 15(4)</i>: 307-313. <a href=\"https://dx.doi.org/10.1038/s41561-022-00918-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-022-00918-1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Yamamoto, M.; Clemens, S.C.; Seki, O.; Tsuchiya, Y.; Huang, Y.; O’ishi, R.; Abe-Ouchi, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Yamamoto, M. <i>et al.</i>","Englishabstract":"Atmospheric CO<sub>2</sub> and polar ice volume have been strongly coupled over the past 805,000 years. However, the prior extent of coupling, during times of lower-amplitude ice-volume variability, is unknown because continuous high-resolution CO<sub>2</sub> records are lacking. We reconstructed the past 1,460,000 years of atmospheric CO<sub>2</sub> (~1,700 year sample resolution) by taking advantage of the unique relationship between CO<sub>2</sub> concentration and leaf-wax δ<sup>13</sup>C resulting from changes in the extent of C<sub>3</sub> and C<sub>4</sub> vegetation in East India. Notably, reconstructed interglacial CO<sub>2</sub> concentrations were lower before the transition to large volume variability during the mid-Pleistocene Transition (900,000 years ago). Prior to the mid-Pleistocene Transition, CO<sub>2</sub> exhibited a secular trend similar to that of deep-ocean carbon isotopes. At orbital time scales, phase analysis indicates that the CO<sub>2</sub> lead relative to ice volume changed to a lag during the mid-Pleistocene Transition. Combined, these findings suggest that deep-ocean circulation controlled the long-term CO<sub>2</sub> trend, and that interaction between CO<sub>2</sub>, continental ice and deep-ocean circulation was reorganized during the mid-Pleistocene Transition, involving a decrease in carbon storage in the deep Pacific.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Increased interglacial atmospheric CO<sub>2</sub> levels followed the mid-Pleistocene Transition","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-04-14","DateCreate":"2022-04-14","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000777374800002","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41561-022-00918-1"},"refs":null,"anarec":{"AnaID":351417,"PubliDate":2022,"Pagination":"307-313","XtraPublOfAnaID":null,"ISBN":null,"Volume":"15","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":123796,"SerRR":"Nature Geoscience. 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