Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Eugene B. Karabanov"'
Autor:
Anson W. Mackay, Melanie J. Leng, Galina K. Khursevich, Virginia N. Panizzo, Hilary J. Sloane, David Morley, Eugene B. Karabanov, Douglas F. Williams
Publikováno v:
Journal of Quaternary Science. 23:365-374
In this paper we reconstruct hydrological variability in Lake Baikal during Marine Isotope Stage 11 (MIS 11) (427-362 ka BP) from oxygen isotope analysis of diatom silica. Highest d 18 Odiatom values are found during MIS 11.3, highlighting the domina
Autor:
N. V. Kulagina, A. A. Abzaeva, P. P. Letunova, Takeshi Nakagawa, Mayke Wagner, Pavel E. Tarasov, Elena V. Bezrukova, Wojciech Granoszewski, Eugene B. Karabanov, Frank Riedel
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 252:440-457
The last interglacial (LI) and Holocene changes in annual precipitation ( P ann ), the mean temperature of the warmest ( T w ) and coldest ( T c ) month and the moisture index ( α ) were reconstructed from continuous pollen records from Lake Baikal.
Publikováno v:
Estuarine, Coastal and Shelf Science. 66:185-196
To reconstruct the variability of freshwater discharge to the Arctic via the Lena River, 22 gravity cores were collected along two transects that extend from the delta floodplain onto the Laptev Sea shelf. High magnetic susceptibility (MS) signals ap
Autor:
E. V. Kerber, Douglas F. Williams, Elena V. Bezrukova, L. Tkachenko, Alexander A. Prokopenko, P. P. Letunova, Galina K. Khursevich, A. N. Gvozdkov, Oleg Khlustov, Eugene B. Karabanov, Svetlana Krapivina, Mikhail Kuzmin, S. A. Fedenya, E. P. Solotchina, V. G. Sideleva
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 209:227-243
Sedimentary sections from Lake Baikal in Siberia and Lake Hovsgol in Mongolia show that during the Last Glacial Maximum (LGM), planktonic/benthic diatoms, chrysophyte cysts, sponge spicules and zooplankton remains did not accumulate in the lake sedim
Publikováno v:
Journal of Sedimentary Research. 73:941-956
The long, continuous, high-latitude, stratigraphic record of Lake Baikal was deposited in three broad sedimentary environ- ments, defined by high-resolution seismic-reflection and coring meth- ods: (1) turbidite depositional systems, by far the most
Autor:
Alexander A. Prokopenko, S. A. Fedenya, Mikhail I. Kuzmin, Galina K. Khursevich, D. F. Williams, Eugene B. Karabanov
Publikováno v:
International Journal on Algae. 5:77-89
Autor:
S. A. Fedenya, Alexander A. Prokopenko, D. F. Williams, Galina K. Khursevich, Eugene B. Karabanov, Mikhail I. Kuzmin
Publikováno v:
International Journal on Algae. 5:85-102
Autor:
Alexander A. Prokopenko, Douglas F. Williams, Mikhail I. Kuzmin, Eugene B. Karabanov, Galina K. Khursevich, John A. Peck
Publikováno v:
Nature. 418:65-68
The large difference in carbon and oxygen isotope data from the marine record between marine oxygen isotope stage 12 (MIS 12) and MIS 11, spanning the interval between about 480 and 380 kyr ago, has been interpreted as a transition between an extreme
Publikováno v:
Quaternary Research. 58:56-59
Paleoproductivity records from Lake Baikal indicate that the last interglaciation in southeastern Siberia lasted ca. 12,000 yr from 127,000 to 115,000 yr B.P., was punctuated by a climatic oscillation about 120,000 yr ago, and ended abruptly with a r
Autor:
Alexander A. Prokopenko, Galina K. Khursevich, Elena V. Bezrukova, Mikhail I. Kuzmin, Eugene B. Karabanov, Douglas F. Williams
Publikováno v:
Quaternary International. :3-18
Records of the tectonic and climatic evolution of continental interiors are important for understanding the dynamics of the Earth's climate system, evolutionary processes within the terrestrial biosphere, and human origins. Sediment drill cores recov