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      Estimates of Arctic land surface temperatures during the early Pliocene from two novel proxies

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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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            Oxygen and carbon isotope fractionation in biogenic aragonite: Temperature effects

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              A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose

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                Author and article information

                Journal
                Earth and Planetary Science Letters
                Earth and Planetary Science Letters
                Elsevier BV
                0012821X
                April 2011
                April 2011
                : 304
                : 3-4
                : 291-299
                Article
                10.1016/j.epsl.2011.02.030
                6d426466-a9c7-445f-bef0-ec850b3c95e2
                © 2011

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

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