Insolation regime in Siberia as a major factor controlling diatom production in Lake Baikal during the past 800,000 years

Quaternary International

Volumn 80-81, Issue , 2001, Pages 47-58

  Khursevich, Galina K ^a,b   Karabanov, Eugene B ^b,c   Prokopenko, Alexander A ^b,d   Williams, Douglas F ^b   Kuzmin, Mikhail I ^c   Fedenya, Svetlana A ^a   Gvozdkov, Alexander A ^c  

^a Institute of Geochemistry and Geophysics Minsk   (Belarus)

^b UNIVERSITY OF SOUTH CAROLINA   (United States)

^c VINOGRADOV INSTITUTE OF GEOCHEMISTRY   (Russian Federation)

^d SOBOLEV INSTITUTE OF GEOLOGY AND MINERALOGY   (Russian Federation)

Author keywords

[No Author keywords available]

Indexed keywords

BRUNHES CHRON; DIATOM; LACUSTRINE ENVIRONMENT; PALEOCLIMATE; SEDIMENT CORE;

EID: 18544404724     PISSN: 10406182     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1040-6182(01)00018-0     Document Type: Article

References (31)

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