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- W62122896 abstract "This chapter analyzes the physical properties (mean grain size and water content) and biogenic silica content in sediment cores (BDP96) from Academician Ridge in Lake Baikal. The analyses provides information on long-term fluctuations in environmental conditions, revealing that the continental interior has gradually cooled over the past 5 my with a characteristic periodicity of about 1.0 my. Long-term fluctuations in environmental conditions represented by the physical and chemical properties of the 200 m core (BDP96 Hole 1) suggest that the continental interior has gradually cooled over the past 5 my and that the cooling is characterized by periodicity. There are long periods of cooling around 1.0 my and 0.4 my in the datasets analyzed, and both may be related to solar insolation. There are long periods around 1.0 my, 0.4 my, and 0.1 my in the datasets analyzed, which are related to the solar insolation. The 0.4 and 0.1 my are connected to eccentricity parameters (Milankovitch parameters) and the 1.0 my period may also be related to the fluctuation in paleomagnetic intensity. Three intervals of cooling are found at about 2.6–2.8 my BP, 1.7–2.0 my BP, and 0.7–1.0 my BP. These intervals correspond to the troughs in the 1.0 my period." @default.
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- W62122896 date "2000-01-01" @default.
- W62122896 modified "2023-09-26" @default.
- W62122896 title "Paleoclimatic signals printed in lake baikal sediments" @default.
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- W62122896 doi "https://doi.org/10.1016/b978-044450434-0/50005-6" @default.
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