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Bedoba - key section of Kazantsovian horizon in Central Siberia. / Arslanov, Kh A.; Laukhin, S. A.; Maksimov, F. E.; Kuznetsov, V. Yu; Velichkevich, F. Yu; San'ko, A. F.; Shilova, G. N.; Chernov, S. B.

в: Doklady Akademii Nauk, Том 396, № 6, 25.11.2004, стр. 796-799.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Arslanov, KA, Laukhin, SA, Maksimov, FE, Kuznetsov, VY, Velichkevich, FY, San'ko, AF, Shilova, GN & Chernov, SB 2004, 'Bedoba - key section of Kazantsovian horizon in Central Siberia', Doklady Akademii Nauk, Том. 396, № 6, стр. 796-799.

APA

Arslanov, K. A., Laukhin, S. A., Maksimov, F. E., Kuznetsov, V. Y., Velichkevich, F. Y., San'ko, A. F., Shilova, G. N., & Chernov, S. B. (2004). Bedoba - key section of Kazantsovian horizon in Central Siberia. Doklady Akademii Nauk, 396(6), 796-799.

Vancouver

Arslanov KA, Laukhin SA, Maksimov FE, Kuznetsov VY, Velichkevich FY, San'ko AF и пр. Bedoba - key section of Kazantsovian horizon in Central Siberia. Doklady Akademii Nauk. 2004 Нояб. 25;396(6):796-799.

Author

Arslanov, Kh A. ; Laukhin, S. A. ; Maksimov, F. E. ; Kuznetsov, V. Yu ; Velichkevich, F. Yu ; San'ko, A. F. ; Shilova, G. N. ; Chernov, S. B. / Bedoba - key section of Kazantsovian horizon in Central Siberia. в: Doklady Akademii Nauk. 2004 ; Том 396, № 6. стр. 796-799.

BibTeX

@article{8063b2edea62470cb5bd090fed318239,
title = "Bedoba - key section of Kazantsovian horizon in Central Siberia",
abstract = "The main disadvantage of paleoclimate reconstruction in Siberia is shortage of absolute data. Data on key section of Kazantsovian horizon have been considered. It has been shown that hotter climate was in the past. Rocks in the section have been considered. Regularities in variations of climate and rocks have been described. It has been shown that Sambucus racemosa under modern conditions is absent. Carex paucifloroides has been described. Sparganium microcarpum, Najas marina, Lemna trisulca, Calla palustris have been detected. Development of plants has been described. Time of Bedoba section formation has been determined.",
author = "Arslanov, {Kh A.} and Laukhin, {S. A.} and Maksimov, {F. E.} and Kuznetsov, {V. Yu} and Velichkevich, {F. Yu} and San'ko, {A. F.} and Shilova, {G. N.} and Chernov, {S. B.}",
year = "2004",
month = nov,
day = "25",
language = "English",
volume = "396",
pages = "796--799",
journal = "ДОКЛАДЫ АКАДЕМИИ НАУК",
issn = "0869-5652",
publisher = "Издательство {"}Наука{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Bedoba - key section of Kazantsovian horizon in Central Siberia

AU - Arslanov, Kh A.

AU - Laukhin, S. A.

AU - Maksimov, F. E.

AU - Kuznetsov, V. Yu

AU - Velichkevich, F. Yu

AU - San'ko, A. F.

AU - Shilova, G. N.

AU - Chernov, S. B.

PY - 2004/11/25

Y1 - 2004/11/25

N2 - The main disadvantage of paleoclimate reconstruction in Siberia is shortage of absolute data. Data on key section of Kazantsovian horizon have been considered. It has been shown that hotter climate was in the past. Rocks in the section have been considered. Regularities in variations of climate and rocks have been described. It has been shown that Sambucus racemosa under modern conditions is absent. Carex paucifloroides has been described. Sparganium microcarpum, Najas marina, Lemna trisulca, Calla palustris have been detected. Development of plants has been described. Time of Bedoba section formation has been determined.

AB - The main disadvantage of paleoclimate reconstruction in Siberia is shortage of absolute data. Data on key section of Kazantsovian horizon have been considered. It has been shown that hotter climate was in the past. Rocks in the section have been considered. Regularities in variations of climate and rocks have been described. It has been shown that Sambucus racemosa under modern conditions is absent. Carex paucifloroides has been described. Sparganium microcarpum, Najas marina, Lemna trisulca, Calla palustris have been detected. Development of plants has been described. Time of Bedoba section formation has been determined.

UR - http://www.scopus.com/inward/record.url?scp=8644220668&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:8644220668

VL - 396

SP - 796

EP - 799

JO - ДОКЛАДЫ АКАДЕМИИ НАУК

JF - ДОКЛАДЫ АКАДЕМИИ НАУК

SN - 0869-5652

IS - 6

ER -

ID: 35958113