{"refrec":{"BRefID":319791,"RR":"<b>Dimiza, M.D.; Fatourou, M.; Arabas, A.; Panagiotopoulos, I.; Gogou, A.; Kouli, K.; Parinos, C.; Rousakis, G.; Triantaphyllou, M.V.</b> (2020). Deep-sea benthic foraminifera record of the last 1500 years in the North Aegean Trough (northeastern Mediterranean): a paleoclimatic reconstruction scenario. <i>Deep-Sea Res., Part II, Top. Stud. Oceanogr. 171</i>: 104705. <a href=\"https://dx.doi.org/10.1016/j.dsr2.2019.104705\" target=\"_blank\">https://dx.doi.org/10.1016/j.dsr2.2019.104705</a>","BEntID":313230,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Deep-Sea Res., Part II, Top. Stud. Oceanogr. 171</i>: 104705. <a href=\"https://dx.doi.org/10.1016/j.dsr2.2019.104705\" target=\"_blank\">https://dx.doi.org/10.1016/j.dsr2.2019.104705</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Dimiza, M.D.; Fatourou, M.; Arabas, A.; Panagiotopoulos, I.; Gogou, A.; Kouli, K.; Parinos, C.; Rousakis, G.; Triantaphyllou, M.V.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Dimiza, M.D. <i>et al.</i>","Englishabstract":"A 1500-year, high-resolution deep-sea benthic foraminifera record from the Athos Basin of the North Aegean Trough (northeastern Mediterranean) has been analyzed for the development of a paleoclimatic scenario. The data analysis points out that the quantity and quality of the seafloor's organic matter could be a crucial controlling factor for the faunal succession. During 550–1000 AD (within the Medieval Climate Anomaly), the relatively high benthic foraminiferal accumulation rates together with the predominance of meso-eutrophic taxa, such as <em>Bolivina dilatata</em>/<em>spathulata</em>, may be interpreted as the result of high precipitation. Consequently, increased riverine discharges into the North Aegean Sea and the associated warm climatic conditions appear to persist for a long time and are related to a negative phase of the North Atlantic Oscillation. Later on, the establishment of an oligo-mesotrophic seafloor environment is documented by the diminishing benthic foraminiferal accumulation rates associated with an increment in the abundances of <em>Gyroidinoides altiformis</em>. During a colder phase of the Little Ice Age (17th century), the relative abundances of the opportunistic foraminiferal species <em>Bulimina inflata</em> and <em>Bulimina marginata</em> can be related to high marine productivity, most probably due to enhanced winter mixing conditions. Finally, during the last 100 years, a faunal shift to eutrophication preferent species, and the persistent occurrence of <em>Chilostomella mediterranensis</em>, reflects a pronounced change in trophic conditions, characterized by high amounts of potentially low-quality organic matter in the seafloor, which are the result of a gradual temperature increase accompanied with enhanced terrigenous inputs.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Deep-sea benthic foraminifera record of the last 1500 years in the North Aegean Trough (northeastern Mediterranean): a paleoclimatic reconstruction scenario","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-05-28 01:31:29.299990","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Benthic foraminifera variation; Organic matter fluxes; Major climatic events","OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2020-03-23","DateCreate":"2019-12-23","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000518878000022","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.dsr2.2019.104705"},"refs":null,"anarec":{"AnaID":319791,"PubliDate":2020,"Pagination":"104705","XtraPublOfAnaID":null,"ISBN":null,"Volume":"171","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45197,"SerRR":"Deep-Sea Research, Part II. 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