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Paleoclimatic changes in the Late Quaternary as deduced from hydrogen and oxygen isotopes and hydrochemistry of ground ice of the Bykovsky Peninsula, Northern Siberia.

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Meyer, H. , Siegert, C. , Derevyagin, A. Y. and Hubberten, H. W. (2000): Paleoclimatic changes in the Late Quaternary as deduced from hydrogen and oxygen isotopes and hydrochemistry of ground ice of the Bykovsky Peninsula, Northern Siberia. , QUEEN Workshop, Lund, Sweden, April 7 - 10 .
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