{"refrec":{"BRefID":405685,"RR":"<b>Houedec, S.L.; Liebrand, D.; Hennekam, R.; Mojtahid, M.</b> (2024). Assessing atmospheric and oceanic teleconnections between the eastern and western Mediterranean over the past 8000 years. <i>Holocene 34(2)</i>: 162-174. <a href=\"https://dx.doi.org/10.1177/09596836231211807\" target=\"_blank\">https://dx.doi.org/10.1177/09596836231211807</a>","BEntID":403480,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Holocene 34(2)</i>: 162-174. <a href=\"https://dx.doi.org/10.1177/09596836231211807\" target=\"_blank\">https://dx.doi.org/10.1177/09596836231211807</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Houedec, S.L.; Liebrand, D.; Hennekam, R.; Mojtahid, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Houedec, S.L. <i>et al.</i>","Englishabstract":"<span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">Holocene climate records from the Mediterranean are marked by pervasive millennial to centennial-scale climate variability. Here, we investigate East-West Mediterranean atmospheric and oceanic teleconnections by computing phase-relationships between oxygen isotope (δ</span><sup>18</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">O) records generated on Soreq (East) and Chorchia (West) spelaeothems, as well as between δ</span><sup>18</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">O and carbon isotope (δ</span><sup>13</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">C) records from planktonic and benthic foraminifera from core PS009PC (East, Levantin Basin), ODP Site 963D (Central, Sicily Strait), and core KESC9-14 (West, Ligurian Basin). These marine sites are all located at intermediate water depths (560–460 m depth). Hence, the benthic foraminiferal δ</span><sup>18</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">O records reflect mainly the intermediate ocean temperature/δ</span><sup>18</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">O of the water mass, and the benthic δ</span><sup>13</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">C is a proxy for the intensity of water flowing at the studied depth called Levantine Intermediate Water (LIW). For both western and eastern cores, the planktonic stable isotopic records reflect the climate-induced activity of the nearby river system. We find broadly in-phase relationships between the spelaeothem δ</span><sup>18</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">O records and between the planktonic δ</span><sup>18</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">O and δ</span><sup>13</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">C records at most multi-centennial and millennial periodicities. This is indicative of closely linked (hydro-) climatic conditions in Southern Europe, the Levant, and North Africa over the last 8000 years. Conversely, at intermediate water depths, we find a distinct out-of-phase relationship between the East/Central and West Mediterranean benthic δ</span><sup>18</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">O and δ</span><sup>13</sup><span style=\"background-color:rgb(255,255,255);color:rgb(51,51,51);\">C records at 1000–2000 years periodicities. We interpret this see-saw pattern as indicative of a persistent regional influence of LIW on oceanographic conditions in the intermediate depths of the eastern basin. Conversely, we suggest a strong influence of the modified Atlantic Ocean inflow (MAW) in the intermediate water formation in the Western Mediterranean (‘Winter Intermediate Water’; WIW). This WIW overprints, at least partially, the LIW signal that reaches the western Mediterranean causing the out-of-phase relationship between the east and the west oceanographic signals at intermediate depths.</span>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Assessing atmospheric and oceanic teleconnections between the eastern and western Mediterranean over the past 8000 years","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-04 01:31:54.700303","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"E-W teleconnection; Holocene; Levantine intermediate water; Mediterranean Sea; Paleocirculation; spectral analyses","OtherDescriptors":null,"Notes":null,"AnaPub":2024,"MonPub":null,"DateUpdate":"2025-02-11","DateCreate":"2025-02-11","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1,"DOI":"10.1177/09596836231211807"},"refs":null,"anarec":{"AnaID":405685,"PubliDate":2024,"Pagination":"162-174","XtraPublOfAnaID":null,"ISBN":null,"Volume":"34","Issue":"2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":184250,"SerRR":"The Holocene. 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