Browsing by Author "Velichko A.A."
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Browsing by Author "Velichko A.A."
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Velichko A.A.; Kononov Yu.M.; Faustova M.A. (2000)The evaluated area and volume of ice sheets on the Earth during the Last Glacial Maximum (18-20 thousand years ago, oxygen isotope stage 2) are adjusted to the most recent data and our subglobal to global paleoglaciological ...
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Velichko A.A.; Faustova M.A.; Gribchenko Y.N.; Pisareva V.V.; Sudakova N.G. (2004)The quaternary chronology and distribution of glaciations through the last million years is described. The scheme of main paleogeographical events is based on multidisciplinary studies (geological, paleontological, ...
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PALEOMAGNETIC REFERENCE INTERVALS OF THE LATE PLEISTOCENE IN THE CENTRAL AREA OF THE RUSSIAN PLAIN Svetlitskaya T.V.; Velichko A.A. (1988)In the Pleistocene, which is encompassed entirely by the 0.73 million years long Brunhes paleomagnetic epoch, paleomagnetic episodes such as the Blake Espisode cannot be reliably traced. As a result, efforts to improve the ...
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Velichko A.A.; Faustova M.A. (1989)The principal phases in the development of the Late Valdai, Late Weichselian, and Late Wisconsin glaciations coincided with a global cooling maximum 18-20 thousand years ago. In recent years, new data allowing to more ...
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Pisaric M.F.J.; MacDonald G.M.; Velichko A.A.; Cwynar L.C. (2001)In order to reconstruct the Late- and Postglacial vegetation history of the northwestern edge of Beringia, a sediment core was collected from a lake north of the present treeline along the lower Lena River of northeastern ...
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Velichko A.A.; Zelikson E.M.; Borisova O.K. (1999)The phytomass (the biomass of terrestrial vegetation) is one of the main reservoirs of carbon, as carbon makes up approximately 0.45 of the phytomass by weight [Ajtay, G.L., Ketner, P., Duvigneaud, P., 1979. Terrestrial ...
Now showing items 1-6 of 6