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ISSN 1028-334X, Doklady Earth Sciences, 2006, Vol. 407, No. 2, pp. 259â261. © Pleiades Publishing, Inc., 2006. Original Russian Text © D.Yu. Demezhko, V.I. Utkin, A.D. Duchkov, D.G. Ryvkin, 2006, published in Doklady Akademii Nauk, 2006, Vol. 406, No. 5, pp. 688â690. GEOPHYSICS D. Yu. Demezhko1, Corresponding Member of the RAS V. I. Utkin1, A. D. Duchkov2, and D. G. Ryvkin1 Received October 28, 2005 DOI: 10.1134/S1028334X06020243 Periodic alternation of ice ages and warm interglacial periods is a characteristic feature of the Earthâs climatic system in the Quaternary Period. This is testiï¬ed by the data from oxygen isotopic analysis on deep-sea sediment and ice cores [1]. At the same time, the mechanism of glaciation ï¬uctuations remains unclear in many respects. Indications of the spatial distribution of climate characteristics during the periods of its global changes are needed to understand more clearly the causes of these ï¬uctuations. The last climate change occurred approximately 10 000 yr ago in the beginning of the modern interglacial period (Holocene). In our paper, we analyze the spatial distribution of geothermic estimates of the amplitudes of Holocene warming in Europe. The geothermic of the reconstruction of ground surface paleotemperatures is based on the analysis
Doklady Earth Sciences – Springer Journals
Published: Feb 1, 2006
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