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Paleoclimatic trends in the Late Quaternary as deduced from stable isotope and hydrochemical analyses of ground ice (Bykovsky Peninsula, Northern Siberia).

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Meyer, H. , Derevyagin, A. Y. , Siegert, C. and Hubberten, H. W. (2000): Paleoclimatic trends in the Late Quaternary as deduced from stable isotope and hydrochemical analyses of ground ice (Bykovsky Peninsula, Northern Siberia). , Workshop: Rhythms of natural processes in the Earth Cryosphere, Pushshino, Russia, May 12 - 15 .
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