{"refrec":{"BRefID":332281,"RR":"<b>Dämmer, L.K.; de Nooijer, L.; van Sebille, E.; Haak, J.G.; Reichart, G.-J.</b> (2020). Evaluation of oxygen isotopes and trace elements in planktonic foraminifera from the Mediterranean Sea as recorders of seawater oxygen isotopes and salinity. <i>Clim. Past 16(6)</i>: 2401-2414. <a href=\"https://doi.org/10.5194/cp-16-2401-2020\" target=\"_blank\">https://doi.org/10.5194/cp-16-2401-2020</a>","BEntID":325893,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Clim. Past 16(6)</i>: 2401-2414. <a href=\"https://doi.org/10.5194/cp-16-2401-2020\" target=\"_blank\">https://doi.org/10.5194/cp-16-2401-2020</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Dämmer, L.K.; de Nooijer, L.; van Sebille, E.; Haak, J.G.; Reichart, G.-J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Dämmer, L.K. <i>et al.</i>","Englishabstract":"The Mediterranean Sea is characterized by a relatively strong west to east    salinity gradient, which makes it an area suitable for testing the effect    of salinity on foraminiferal shell geochemistry. We collected living    specimens of the planktonic foraminifer <i>Globigerinoides ruber albus</i>    to analyse the relation between element ∕ Ca ratios, stable oxygen isotopes    of their shells, and surface seawater salinity, isotopic composition and    temperature. The oxygen isotopes of sea surface water also correlate with    salinity in the Mediterranean during winter, which is when sampling for    this study took place. Seawater oxygen and hydrogen isotopes are positively    correlated in both the eastern and western Mediterranean Sea, although the    relationship differs from previously reported values, especially in the    eastern region. The slope between salinity and seawater oxygen isotopes is    lower than previously published results. Still, despite the rather modest    slope, seawater and foraminiferal carbonate oxygen isotopes are correlated    in our dataset, albeit with large residuals and high residual variability.    This scatter could be due to either biological variability in vital effects    or environmental variability. Numerical models backtracking particles show    that ocean-current-driven mixing of particles of different origins might    dampen sensitivity and could result in an offset caused by horizontal    transport. Results show that Na ∕ Ca is positively correlated with salinity    and independent of temperature. As expected, foraminiferal Mg ∕ Ca    increases with temperature, which is in line with earlier calibrations, and    in the high salinity environment. By using living foraminifera during    winter, the previously established Mg ∕ Ca–temperature calibration is    extended to temperatures below 18 <sup>∘</sup>C, which is a fundamental    prerequisite of using single foraminifera for reconstructing past    seasonality.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Evaluation of oxygen isotopes and trace elements in planktonic foraminifera from the Mediterranean Sea as recorders of seawater oxygen isotopes and salinity","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-08 01:31:21.597203","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2021-01-04","DateCreate":"2021-01-04","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000595587000001","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/cp-16-2401-2020"},"refs":null,"anarec":{"AnaID":332281,"PubliDate":2020,"Pagination":"2401-2414","XtraPublOfAnaID":null,"ISBN":null,"Volume":"16","Issue":"6","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":220505,"SerRR":"Climate of the Past. 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