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Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5-2. / Svendsen, J.I.; Krüger, L.C.; Mangerud, J.; Astakhov, V.I.; Paus, A.; Nazarov, D.; Murray, A.

в: Quaternary Science Reviews, Том 92, 15.05.2014, стр. 409-428.

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

Harvard

Svendsen, JI, Krüger, LC, Mangerud, J, Astakhov, VI, Paus, A, Nazarov, D & Murray, A 2014, 'Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5-2', Quaternary Science Reviews, Том. 92, стр. 409-428. https://doi.org/10.1016/j.quascirev.2013.10.008

APA

Svendsen, J. I., Krüger, L. C., Mangerud, J., Astakhov, V. I., Paus, A., Nazarov, D., & Murray, A. (2014). Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5-2. Quaternary Science Reviews, 92, 409-428. https://doi.org/10.1016/j.quascirev.2013.10.008

Vancouver

Svendsen JI, Krüger LC, Mangerud J, Astakhov VI, Paus A, Nazarov D и пр. Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5-2. Quaternary Science Reviews. 2014 Май 15;92:409-428. https://doi.org/10.1016/j.quascirev.2013.10.008

Author

Svendsen, J.I. ; Krüger, L.C. ; Mangerud, J. ; Astakhov, V.I. ; Paus, A. ; Nazarov, D. ; Murray, A. / Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5-2. в: Quaternary Science Reviews. 2014 ; Том 92. стр. 409-428.

BibTeX

@article{d063f638110d47999f39ccd02fa32213,
title = "Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5-2",
abstract = "We describe and discuss the glacial and climate variations in the Polar Ural Mountains in northern Russia over the last 100 000 years. A series of optically stimulated luminescence (OSL) and radiocarbon ages from sediment cores demonstrate that there has been continuous deposition of lacustrine sediments throughout the last 65 ka in Lake Gerdizty, a lake basin situated on the eastern foothills of the Urals. Below the lacustrine sequence are two till beds; the uppermost (unit B) was probably deposited by a large mountain-centred glacier complex that covered the lake basin during Marine Isotope Stage (MIS) 4.",
keywords = "Ural Mountains, Arctic Russia, Glaciation, Ice cap, Lake cores, BarentseKara Ice Sheet, Pollen stratigraphy, Ice-dammed lakes, Paleoclimate, OSL chronology",
author = "J.I. Svendsen and L.C. Kr{\"u}ger and J. Mangerud and V.I. Astakhov and A. Paus and D. Nazarov and A. Murray",
year = "2014",
month = may,
day = "15",
doi = "10.1016/j.quascirev.2013.10.008",
language = "English",
volume = "92",
pages = "409--428",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5-2

AU - Svendsen, J.I.

AU - Krüger, L.C.

AU - Mangerud, J.

AU - Astakhov, V.I.

AU - Paus, A.

AU - Nazarov, D.

AU - Murray, A.

PY - 2014/5/15

Y1 - 2014/5/15

N2 - We describe and discuss the glacial and climate variations in the Polar Ural Mountains in northern Russia over the last 100 000 years. A series of optically stimulated luminescence (OSL) and radiocarbon ages from sediment cores demonstrate that there has been continuous deposition of lacustrine sediments throughout the last 65 ka in Lake Gerdizty, a lake basin situated on the eastern foothills of the Urals. Below the lacustrine sequence are two till beds; the uppermost (unit B) was probably deposited by a large mountain-centred glacier complex that covered the lake basin during Marine Isotope Stage (MIS) 4.

AB - We describe and discuss the glacial and climate variations in the Polar Ural Mountains in northern Russia over the last 100 000 years. A series of optically stimulated luminescence (OSL) and radiocarbon ages from sediment cores demonstrate that there has been continuous deposition of lacustrine sediments throughout the last 65 ka in Lake Gerdizty, a lake basin situated on the eastern foothills of the Urals. Below the lacustrine sequence are two till beds; the uppermost (unit B) was probably deposited by a large mountain-centred glacier complex that covered the lake basin during Marine Isotope Stage (MIS) 4.

KW - Ural Mountains

KW - Arctic Russia

KW - Glaciation

KW - Ice cap

KW - Lake cores

KW - BarentseKara Ice Sheet

KW - Pollen stratigraphy

KW - Ice-dammed lakes

KW - Paleoclimate

KW - OSL chronology

U2 - 10.1016/j.quascirev.2013.10.008

DO - 10.1016/j.quascirev.2013.10.008

M3 - Article

VL - 92

SP - 409

EP - 428

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

ER -

ID: 5754671