The establishment of relationships between sediment composition and climatic - vironment in the sediment basin and subsequent evolution of climate relates to the classical problems of fundamental sedimentology. The widely known publications by the Russian academicians N. M. Strakhov, A. B. Ronov, and A. P. Lisitsin are dedicated to different aspects of this problem. In particular, the monograph p- lished by A. P. Lisitsin Sea-ice and iceberg sedimentation in the Ocean: recent and past (Lisitsin, 2002) closely corresponds to the issues examined in this book. This monograph discusses in detail…mehr
The establishment of relationships between sediment composition and climatic - vironment in the sediment basin and subsequent evolution of climate relates to the classical problems of fundamental sedimentology. The widely known publications by the Russian academicians N. M. Strakhov, A. B. Ronov, and A. P. Lisitsin are dedicated to different aspects of this problem. In particular, the monograph p- lished by A. P. Lisitsin Sea-ice and iceberg sedimentation in the Ocean: recent and past (Lisitsin, 2002) closely corresponds to the issues examined in this book. This monograph discusses in detail the environments and means of accumulations of recent marine and oceanic sediments in the ice zone of sedimentation of the Ocean, however, much less attention is given to the history of ice sedimentation, especially to high-resolution paleoceanography. In the present work the authors accepted the following basic principles: 1. StudynotonlyoftheArctic,butalsooftheSubarctic,especiallyofthoseregions, where there were conducted the original studies by the authors. 2. Study of climatic history in uence ( rst of all, the glaciation evolution of NorthernHemisphere)on sedimentationforthe last 130ka (MIS5e MIS1)not only in the marine periglacial environment (term of G. G. Matishov), but also in the deep water areas and on the adjacent continental blocks. 3. Imperative description of recent sedimentation environment for subsequent - plication of the comparative-lithologicalmethod. 4. Detailed consideration of accessible stratigraphic and geo-chronometricdata for partition and correlation of various sedimentary facies. Some of the above-mentionedprinciples require further explanation.
M.A. Levitan was born in 1946 and graduated from Moscow State University in 1969. Both scientific degrees (Ph. D. - 1975, and Dr. Sci. - 1990) are received for marine geology studies. Main scientific interests are concentrated in the fields of sedimentology and inorganic geochemistry of marine sediments, and paleoceanography. M.A. Levitan, Head of Laboratory of sedimentary geochemistry in V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry RAS (Moscow), is (co-) author of more than 200 publications including several monographs (in Russian). He participated in 21 scientific cruises in all main areas of the World Ocean. Yu.A. Lavrushin was born in 1931 and graduated from Moscow State University in 1954. He has both scienticfic degrees (Ph.D. - 1963, and Dr.Sci - 1973). Main scientific interests lay in the field of stratigraphy and sedimentology of terrestrial and marine sediments. Yu.A. Lavrushin, Head of RAS Comission on Quaternary Studies (Moscow), is (co-) author of about 200 publications including several monographies (in Russian). >15 major research cruises in the Arctic, Atlantic, and Pacific Oceans, and is (co-) author of >120 publications in international journals.
Inhaltsangabe
Geological and Paleoecological Events of the Late Pleistocene and Holocene in Northern Eurasia.- Geological and Paleoecological Events of the Late Pleistocene along Eurasian Coastal Areas of the Arctic Ocean.- Late Pleistocene Geologic-Paleoecological Events in the North of European Russia.- Main Geologic-Paleoecological Events of the Late Pleistocene in the North of Western Siberia.- Geologic-Paleoecological Events of the Late Pleistocene in the Northern-Siberian Lowland and Taimyr Peninsula.- The Late Glacial Time and Holocene of Northern Eurasia.- Outlines of the Late Pleistocene and Holocene History of the East Arctic Seas.- The Deglaciation Time and Holocene of Northern Eurasia.- Marine Sedimentation in the Arctic Ocean and Subarctic Seas.- The Seas of West Subarctic Region.- The Arctic Ocean.- The Western Arctic Seas.- Eastern Arctic Seas.- Seas of the Eastern Subarctic.- The Late Pleistocene Paleogeographic Events of Northern Eurasia and History of Sedimentation in the Subarctic Seas and the Arctic Ocean in Relation to the Northern Hemisphere Glaciation during the Last Climatic Cycle.- Characteristic Features of the Mikulino Landscapes.- Results of Paleoclimate Studies.- Particularities of Sedimentation Processes Within the Continental Blocks and Marine Basins.
Geological and Paleoecological Events of the Late Pleistocene and Holocene in Northern Eurasia.- Geological and Paleoecological Events of the Late Pleistocene along Eurasian Coastal Areas of the Arctic Ocean.- Late Pleistocene Geologic-Paleoecological Events in the North of European Russia.- Main Geologic-Paleoecological Events of the Late Pleistocene in the North of Western Siberia.- Geologic-Paleoecological Events of the Late Pleistocene in the Northern-Siberian Lowland and Taimyr Peninsula.- The Late Glacial Time and Holocene of Northern Eurasia.- Outlines of the Late Pleistocene and Holocene History of the East Arctic Seas.- The Deglaciation Time and Holocene of Northern Eurasia.- Marine Sedimentation in the Arctic Ocean and Subarctic Seas.- The Seas of West Subarctic Region.- The Arctic Ocean.- The Western Arctic Seas.- Eastern Arctic Seas.- Seas of the Eastern Subarctic.- The Late Pleistocene Paleogeographic Events of Northern Eurasia and History of Sedimentation in the Subarctic Seas and the Arctic Ocean in Relation to the Northern Hemisphere Glaciation during the Last Climatic Cycle.- Characteristic Features of the Mikulino Landscapes.- Results of Paleoclimate Studies.- Particularities of Sedimentation Processes Within the Continental Blocks and Marine Basins.
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