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      Ice-free conditions in Novaya Zemlya 35 000-30 000 cal years B.P., as indicated by radiocarbon ages and amino acid racemization evidence from marine molluscs

      1 , 2 , 3 , 1
      Polar Research
      Wiley

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          Most cited references26

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          Sea level change through the last glacial cycle.

          K Lambeck (2001)
          Sea level change during the Quaternary is primarily a consequence of the cyclic growth and decay of ice sheets, resulting in a complex spatial and temporal pattern. Observations of this variability provide constraints on the timing, rates, and magnitudes of the changes in ice mass during a glacial cycle, as well as more limited information on the distribution of ice between the major ice sheets at any time. Observations of glacially induced sea level changes also provide information on the response of the mantle to surface loading on time scales of 10(3) to 10(5) years. Regional analyses indicate that the earth-response function is depth dependent as well as spatially variable. Comprehensive models of sea level change enable the migration of coastlines to be predicted during glacial cycles, including the anthropologically important period from about 60,000 to 20,000 years ago.
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            Global glacial ice volume and Last Glacial Maximum duration from an extended Barbados sea level record

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              A new procedure for determining dl amino acid ratios in fossils using reverse phase liquid chromatography

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                Author and article information

                Journal
                Polar Research
                Polar Research
                Wiley
                1751-8369
                December 16 2016
                January 2008
                December 16 2016
                January 2008
                : 27
                : 2
                : 187-208
                Affiliations
                [1 ] Department of Earth Science and Bjerknes Centre for Climate Research, University of Bergen, Allégt. 41, NO-5007 Bergen, Norway
                [2 ] Department of Geology, Northern Arizona University, Flagstaff, AZ 86011, USA
                [3 ] Department of Natural Science, Tromsø University Museum, NO-9037 Tromsø, Norway
                Article
                10.1111/j.1751-8369.2008.00064.x
                cf626a79-a69a-488a-8fb8-022919c8868c
                © 2008
                History

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