Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › глава/раздел › научная › Рецензирование
Climatic Stratigraphy of the Kazantsevo Horizon (as an Analogue of MIS-5) in the Boreal Zone of Western Siberia. / Laukhin, Stanislav; Kuznetsov, Vladislav; Maksimov, Fedor; Shilova, Galina; Firsov, Aleksey.
Strati 2013. First International Congress on Straigraphy. At the cutting edge of Stratigraphy. Springer. 2014.. Springer Nature, 2014. стр. 965-968 (Springer Geology).Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › глава/раздел › научная › Рецензирование
}
TY - CHAP
T1 - Climatic Stratigraphy of the Kazantsevo Horizon (as an Analogue of MIS-5) in the Boreal Zone of Western Siberia
AU - Laukhin, Stanislav
AU - Kuznetsov, Vladislav
AU - Maksimov, Fedor
AU - Shilova, Galina
AU - Firsov, Aleksey
PY - 2014
Y1 - 2014
N2 - Terrestrial deposits in western Siberia, the ages of which correspond to the interval of MIS-5, have been well studied using palaeobotanical methods. However, because of the small number of isotope data, there is no possibility for identifying the palaeoclimatic events relevant to the substages within MIS-5. Therefore, the large numbers of palaeobotanical results have been underused for the purposes of climatic stratigraphy. 230Th–U dates produced during the past two decades have allowed the changes in vegetation during the first half of the Late Pleistocene to be determined. This has enabled a comparison with palaeoclimatic events reflected in the Greenland ice core, and the identification in western Siberia of the analogues of substages MIS-5a, 5b, 5c, 5d, and 5e as well as events 5e1, 5e2, 5e3, 5e4, and 5e5 within MIS-5e.
AB - Terrestrial deposits in western Siberia, the ages of which correspond to the interval of MIS-5, have been well studied using palaeobotanical methods. However, because of the small number of isotope data, there is no possibility for identifying the palaeoclimatic events relevant to the substages within MIS-5. Therefore, the large numbers of palaeobotanical results have been underused for the purposes of climatic stratigraphy. 230Th–U dates produced during the past two decades have allowed the changes in vegetation during the first half of the Late Pleistocene to be determined. This has enabled a comparison with palaeoclimatic events reflected in the Greenland ice core, and the identification in western Siberia of the analogues of substages MIS-5a, 5b, 5c, 5d, and 5e as well as events 5e1, 5e2, 5e3, 5e4, and 5e5 within MIS-5e.
KW - Th–U dating
KW - Climatic stratigraphy
KW - Palaeobotany
KW - Western Siberia
UR - http://www.scopus.com/inward/record.url?scp=85078082432&partnerID=8YFLogxK
U2 - 10.1007/978-3-319-04364-7_181
DO - 10.1007/978-3-319-04364-7_181
M3 - Chapter
SN - 9783319043647; 9783319043630
T3 - Springer Geology
SP - 965
EP - 968
BT - Strati 2013. First International Congress on Straigraphy. At the cutting edge of Stratigraphy. Springer. 2014.
PB - Springer Nature
ER -
ID: 7029669