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Chronostratigraphy of the Cheremoshnik Key Section (Yaroslavl Volga Region) Based on New Geochronological, Palynological, and Paleosol Data. / Rusakov, A. V.; Savelieva, L. A.; Maksimov, F. E.; Kuznetsov, V. Yu.; Korkka, M. A.; Savenko, V. B.; Starikova, A. A.; Nikonov, A. A.; Simakova, A. N.
In:
Doklady Earth Sciences, Vol. 472, No. 2, 2017, p. 244-247.
Research output: Contribution to journal › Article › peer-review
Harvard
Rusakov, AV, Savelieva, LA, Maksimov, FE, Kuznetsov, VY, Korkka, MA, Savenko, VB
, Starikova, AA, Nikonov, AA & Simakova, AN 2017, '
Chronostratigraphy of the Cheremoshnik Key Section (Yaroslavl Volga Region) Based on New Geochronological, Palynological, and Paleosol Data',
Doklady Earth Sciences, vol. 472, no. 2, pp. 244-247.
https://doi.org/10.1134/S1028334X17020271
APA
Rusakov, A. V., Savelieva, L. A., Maksimov, F. E., Kuznetsov, V. Y., Korkka, M. A., Savenko, V. B.
, Starikova, A. A., Nikonov, A. A., & Simakova, A. N. (2017).
Chronostratigraphy of the Cheremoshnik Key Section (Yaroslavl Volga Region) Based on New Geochronological, Palynological, and Paleosol Data.
Doklady Earth Sciences,
472(2), 244-247.
https://doi.org/10.1134/S1028334X17020271
Vancouver
Author
Rusakov, A. V. ; Savelieva, L. A. ; Maksimov, F. E. ; Kuznetsov, V. Yu. ; Korkka, M. A. ; Savenko, V. B.
; Starikova, A. A. ; Nikonov, A. A. ; Simakova, A. N. /
Chronostratigraphy of the Cheremoshnik Key Section (Yaroslavl Volga Region) Based on New Geochronological, Palynological, and Paleosol Data. In:
Doklady Earth Sciences. 2017 ; Vol. 472, No. 2. pp. 244-247.
BibTeX
@article{6b50106ece7d487c8da2c33dce1957aa,
title = "Chronostratigraphy of the Cheremoshnik Key Section (Yaroslavl Volga Region) Based on New Geochronological, Palynological, and Paleosol Data",
abstract = "According to radiochemical and biostratigraphic studies of the buried peat layer in the Cheremoshnik key section on the East European plain, the first age dating of this peat was obtained and its assignment to the Mikulino interglacial was confirmed. The Th/U isotope age data obtained for the peat horizon allow us to state with confidence that it was formed during the MIS5e. It was found that a variety of signs, including the lithological characteristics of dated layers and climatic indexes, is evidence that the Cheremoshnik site and Borisoglebsk upland occurred in the periglacial zone during MIS3–MIS2.",
keywords = "Chronostratigraphy, buried peat layer, 230Th/U dating, MIS5, Cheremoshnik key section, the East European plain",
author = "Rusakov, {A. V.} and Savelieva, {L. A.} and Maksimov, {F. E.} and Kuznetsov, {V. Yu.} and Korkka, {M. A.} and Savenko, {V. B.} and Starikova, {A. A.} and Nikonov, {A. A.} and Simakova, {A. N.}",
year = "2017",
doi = "10.1134/S1028334X17020271",
language = "English",
volume = "472",
pages = "244--247",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",
}
RIS
TY - JOUR
T1 - Chronostratigraphy of the Cheremoshnik Key Section (Yaroslavl Volga Region) Based on New Geochronological, Palynological, and Paleosol Data
AU - Rusakov, A. V.
AU - Savelieva, L. A.
AU - Maksimov, F. E.
AU - Kuznetsov, V. Yu.
AU - Korkka, M. A.
AU - Savenko, V. B.
AU - Starikova, A. A.
AU - Nikonov, A. A.
AU - Simakova, A. N.
PY - 2017
Y1 - 2017
N2 - According to radiochemical and biostratigraphic studies of the buried peat layer in the Cheremoshnik key section on the East European plain, the first age dating of this peat was obtained and its assignment to the Mikulino interglacial was confirmed. The Th/U isotope age data obtained for the peat horizon allow us to state with confidence that it was formed during the MIS5e. It was found that a variety of signs, including the lithological characteristics of dated layers and climatic indexes, is evidence that the Cheremoshnik site and Borisoglebsk upland occurred in the periglacial zone during MIS3–MIS2.
AB - According to radiochemical and biostratigraphic studies of the buried peat layer in the Cheremoshnik key section on the East European plain, the first age dating of this peat was obtained and its assignment to the Mikulino interglacial was confirmed. The Th/U isotope age data obtained for the peat horizon allow us to state with confidence that it was formed during the MIS5e. It was found that a variety of signs, including the lithological characteristics of dated layers and climatic indexes, is evidence that the Cheremoshnik site and Borisoglebsk upland occurred in the periglacial zone during MIS3–MIS2.
KW - Chronostratigraphy
KW - buried peat layer
KW - 230Th/U dating
KW - MIS5
KW - Cheremoshnik key section
KW - the East European plain
U2 - 10.1134/S1028334X17020271
DO - 10.1134/S1028334X17020271
M3 - Article
VL - 472
SP - 244
EP - 247
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 2
ER -