{"refrec":{"BRefID":252013,"RR":"<b>McMahon, K.W.; McCarthy, M.D.; Sherwood, O.A.; Larsen, T.; Guilderson, T.P.</b> (2015). Millennial-scale plankton regime shifts in the subtropical North Pacific Ocean. <i>Science (Wash.) 350(6267)</i>: 1530-1533. <a href=\"http://dx.doi.org/10.1126/science.aaa9942\" target=\"_blank\">http://dx.doi.org/10.1126/science.aaa9942</a>","BEntID":243710,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 350(6267)</i>: 1530-1533. <a href=\"http://dx.doi.org/10.1126/science.aaa9942\" target=\"_blank\">http://dx.doi.org/10.1126/science.aaa9942</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"McMahon, K.W.; McCarthy, M.D.; Sherwood, O.A.; Larsen, T.; Guilderson, T.P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"McMahon, K.W. <i>et al.</i>","Englishabstract":"Climate change is predicted to alter marine phytoplankton communities and affect productivity, biogeochemistry, and the efficacy of the biological pump. We reconstructed high-resolution records of changing plankton community composition in the North Pacific Ocean over the past millennium. Amino acid–specific d<sup>13</sup>C records preserved in long-lived deep-sea corals revealed three major plankton regimes corresponding to Northern Hemisphere  climate periods. Non–dinitrogen-fixing cyanobacteria dominated during the Medieval Climate Anomaly (950–1250 Common Era) before  giving way to a new regime in which eukaryotic microalgae contributed nearly half of all export production during the Little Ice Age (~1400–1850 Common Era). The third regime, unprecedented in the past millennium, began in the industrial era and is characterized by increasing production by dinitrogen-fixing cyanobacteria. This picoplankton community shift may provide a negative feedback to rising atmospheric carbon dioxide concentrations.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Millennial-scale plankton regime shifts in the subtropical North Pacific Ocean","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-14 01:31:31.611405","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2015-12-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000366591100059","VABBcode":null,"OpenAcc":0,"DOI":"10.1126/science.aaa9942"},"refs":null,"anarec":{"AnaID":252013,"PubliDate":2015,"Pagination":"1530-1533","XtraPublOfAnaID":null,"ISBN":null,"Volume":"350","Issue":"6267","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43776,"SerRR":"Science (Washington). 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