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      Paleotemperature variations of Early Jurassic seawater recorded in geochemical trends of belemnites from the Basque–Cantabrian basin, northern Spain

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      Palaeogeography, Palaeoclimatology, Palaeoecology
      Elsevier BV

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          87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater

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            Cenozoic deep-Sea temperatures and global ice volumes from Mg/Ca in benthic foraminiferal calcite

            A deep-sea temperature record for the past 50 million years has been produced from the magnesium/calcium ratio (Mg/Ca) in benthic foraminiferal calcite. The record is strikingly similar in form to the corresponding benthic oxygen isotope (delta(18)O) record and defines an overall cooling of about 12 degrees C in the deep oceans with four main cooling periods. Used in conjunction with the benthic delta(18)O record, the magnesium temperature record indicates that the first major accumulation of Antarctic ice occurred rapidly in the earliest Oligocene (34 million years ago) and was not accompanied by a decrease in deep-sea temperatures.
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              Assessing the reliability of magnesium in foraminiferal calcite as a proxy for water mass temperatures

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                Author and article information

                Journal
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Elsevier BV
                00310182
                February 2004
                February 2004
                : 203
                : 3-4
                : 253-275
                Article
                10.1016/S0031-0182(03)00686-2
                ccfad4e7-cc19-45dd-8238-f8e45e9cbc41
                © 2004

                http://www.elsevier.com/tdm/userlicense/1.0/

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