{"refrec":{"BRefID":260418,"RR":"<b>Kaboth, S.; Bahr, A.; Reichart, G.-J.; Jacobs, B.; Lourens, L.J.</b> (2016). New insights into upper MOW variability over the last 150 kyr from IODP 339 Site U1386 in the Gulf of Cadiz. <i>Mar. Geol. 377</i>: 136–145. <a href=\"http://dx.doi.org/10.1016/j.margeo.2015.08.014\" target=\"_blank\">dx.doi.org/10.1016/j.margeo.2015.08.014</a>","BEntID":252436,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Mar. Geol. 377</i>: 136–145. <a href=\"https://dx.doi.org/10.1016/j.margeo.2015.08.014\" target=\"_blank\">https://dx.doi.org/10.1016/j.margeo.2015.08.014</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kaboth, S.; Bahr, A.; Reichart, G.-J.; Jacobs, B.; Lourens, L.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kaboth, S. <i>et al.</i>","Englishabstract":"The upper Mediterranean Outflow Water (MOW) paleo-oceanographic history in the Gulf of Cadiz is poorly constrained due to the lack of high-resolution records that pre-date the last glaciation. Existing proxy records concentrate on MOW variability along the middle slope of the Gulf of Cadiz. Here we present a continuous high-resolution benthic foraminifera d18O record from the upper MOW core at IODP Expedition 339 Site U1386 in the Gulf of Cadiz of the past 150,000 years. Based on d18O, grain-size and Zr/Al variability comparison of our results with existing Mediterranean Sea (MD01-2472, MD95-2043), open ocean (LR04) and Gulf of Cadiz (MD99-2339) records we have gathered new insights into the evolution of the upper MOW core on glacial–interglacial timescales. The influence of the upper MOW at Site U1386 was strongest during MIS 5 and MIS 1. Similar d18O variability can be seen in the Levantine Intermediate Water (LIW) originating from the Levantine Basin of the Eastern Mediterranean Sea. We found clear indication for a vertical shift of the MOW from the upper to the middle slope of the Gulf of Cadiz during sea level lowstands coinciding with MIS 4 and MIS 2 but also during MIS 3. Additionally, our results indicate an increased upper MOW flow correlated with Heinrich Events 7 to 10 and the Younger Dryas, and also inversely relate to precession-forced monsoonal freshwater inputs into the Eastern Mediterranean. In the context of Sapropel formation, we could not find conclusive evidence of the proposed MOW shutdown in our data.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"New insights into upper MOW variability over the last 150 kyr from IODP 339 Site U1386 in the Gulf of Cadiz","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":"Mediterranean outflow; Glacial–interglacial variability; Sapropel; Heinrich events; Gulf of Cadiz  ","OtherDescriptors":null,"Notes":null,"AnaPub":2016,"MonPub":null,"DateUpdate":"2016-07-19","DateCreate":"2016-07-18","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000378430500010","VABBcode":null,"OpenAcc":1,"DOI":"10.1016/j.margeo.2015.08.014"},"refs":null,"anarec":{"AnaID":260418,"PubliDate":2016,"Pagination":"136–145","XtraPublOfAnaID":null,"ISBN":null,"Volume":"377","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43365,"SerRR":"Marine Geology. 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