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Late Quaternary ice sheet history of northern Eurasia. / Svendsen, John Inge; Alexanderson, Helena; Astakhov, Valery I.; Demidov, Igor; Dowdeswell, Julian A.; Funder, Svend; Gataullin, Valery; Henriksen, Mona; Hjort, Christian; Houmark-Nielsen, Michael; Hubberten, Hans W.; Ingólfsson, Ólafur; Jakobsson, Martin; Kjær, Kurt H.; Larsen, Eiliv; Lokrantz, Hanna; Lunkka, Juha Pekka; Lyså, Astrid; Mangerud, Jan; Matiouchkov, Alexei; Murray, Andrew; Möller, Per; Niessen, Frank; Nikolskaya, Olga; Polyak, Leonid; Saarnisto, Matti; Siegert, Christine; Siegert, Martin J.; Spielhagen, Robert F.; Stein, Ruediger.

в: Quaternary Science Reviews, Том 23, № 11-13, 01.06.2004, стр. 1229-1271.

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

Harvard

Svendsen, JI, Alexanderson, H, Astakhov, VI, Demidov, I, Dowdeswell, JA, Funder, S, Gataullin, V, Henriksen, M, Hjort, C, Houmark-Nielsen, M, Hubberten, HW, Ingólfsson, Ó, Jakobsson, M, Kjær, KH, Larsen, E, Lokrantz, H, Lunkka, JP, Lyså, A, Mangerud, J, Matiouchkov, A, Murray, A, Möller, P, Niessen, F, Nikolskaya, O, Polyak, L, Saarnisto, M, Siegert, C, Siegert, MJ, Spielhagen, RF & Stein, R 2004, 'Late Quaternary ice sheet history of northern Eurasia', Quaternary Science Reviews, Том. 23, № 11-13, стр. 1229-1271. https://doi.org/10.1016/j.quascirev.2003.12.008

APA

Svendsen, J. I., Alexanderson, H., Astakhov, V. I., Demidov, I., Dowdeswell, J. A., Funder, S., Gataullin, V., Henriksen, M., Hjort, C., Houmark-Nielsen, M., Hubberten, H. W., Ingólfsson, Ó., Jakobsson, M., Kjær, K. H., Larsen, E., Lokrantz, H., Lunkka, J. P., Lyså, A., Mangerud, J., ... Stein, R. (2004). Late Quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews, 23(11-13), 1229-1271. https://doi.org/10.1016/j.quascirev.2003.12.008

Vancouver

Svendsen JI, Alexanderson H, Astakhov VI, Demidov I, Dowdeswell JA, Funder S и пр. Late Quaternary ice sheet history of northern Eurasia. Quaternary Science Reviews. 2004 Июнь 1;23(11-13):1229-1271. https://doi.org/10.1016/j.quascirev.2003.12.008

Author

Svendsen, John Inge ; Alexanderson, Helena ; Astakhov, Valery I. ; Demidov, Igor ; Dowdeswell, Julian A. ; Funder, Svend ; Gataullin, Valery ; Henriksen, Mona ; Hjort, Christian ; Houmark-Nielsen, Michael ; Hubberten, Hans W. ; Ingólfsson, Ólafur ; Jakobsson, Martin ; Kjær, Kurt H. ; Larsen, Eiliv ; Lokrantz, Hanna ; Lunkka, Juha Pekka ; Lyså, Astrid ; Mangerud, Jan ; Matiouchkov, Alexei ; Murray, Andrew ; Möller, Per ; Niessen, Frank ; Nikolskaya, Olga ; Polyak, Leonid ; Saarnisto, Matti ; Siegert, Christine ; Siegert, Martin J. ; Spielhagen, Robert F. ; Stein, Ruediger. / Late Quaternary ice sheet history of northern Eurasia. в: Quaternary Science Reviews. 2004 ; Том 23, № 11-13. стр. 1229-1271.

BibTeX

@article{fb26f4a1ff37492492b983bc3bf2e145,
title = "Late Quaternary ice sheet history of northern Eurasia",
abstract = "The maximum limits of the Eurasian ice sheets during four glaciations have been reconstructed: (1) the Late Saalian (2) the Early Weichselian (100-80ka), (3) the Middle Weichselian (60-50ka) and (4) the Late Weichselian (25-15ka). The reconstructed ice limits are based on satellite data and aerial photographs combined with geological field investigations in Russia and Siberia, and with marine seismic- and sediment core data. The Barents-Kara Ice Sheet got progressively smaller during each glaciation, whereas the dimensions of the Scandinavian Ice Sheet increased. During the last Ice Age the Barents-Kara Ice Sheet attained its maximum size as early as 90-80,000 years ago when the ice front reached far onto the continent. A regrowth of the ice sheets occurred during the early Middle Weichselian, culminating about 60-50,000 years ago. During the Late Weichselian the Barents-Kara Ice Sheet did not reach the mainland east of the Kanin Peninsula, with the exception of the NW fringe of Taimyr. A numerical ice-sheet model, forced by global sea level and solar changes, was run through the full Weichselian glacial cycle. The modeling results are roughly compatible with the geological record of ice growth, but the model underpredicts the glaciations in the Eurasian Arctic during the Early and Middle Weichselian. One reason for this is that the climate in the Eurasian Arctic was not as dry then as during the Late Weichselian glacial maximum.",
author = "Svendsen, {John Inge} and Helena Alexanderson and Astakhov, {Valery I.} and Igor Demidov and Dowdeswell, {Julian A.} and Svend Funder and Valery Gataullin and Mona Henriksen and Christian Hjort and Michael Houmark-Nielsen and Hubberten, {Hans W.} and {\'O}lafur Ing{\'o}lfsson and Martin Jakobsson and Kj{\ae}r, {Kurt H.} and Eiliv Larsen and Hanna Lokrantz and Lunkka, {Juha Pekka} and Astrid Lys{\aa} and Jan Mangerud and Alexei Matiouchkov and Andrew Murray and Per M{\"o}ller and Frank Niessen and Olga Nikolskaya and Leonid Polyak and Matti Saarnisto and Christine Siegert and Siegert, {Martin J.} and Spielhagen, {Robert F.} and Ruediger Stein",
year = "2004",
month = jun,
day = "1",
doi = "10.1016/j.quascirev.2003.12.008",
language = "English",
volume = "23",
pages = "1229--1271",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier",
number = "11-13",

}

RIS

TY - JOUR

T1 - Late Quaternary ice sheet history of northern Eurasia

AU - Svendsen, John Inge

AU - Alexanderson, Helena

AU - Astakhov, Valery I.

AU - Demidov, Igor

AU - Dowdeswell, Julian A.

AU - Funder, Svend

AU - Gataullin, Valery

AU - Henriksen, Mona

AU - Hjort, Christian

AU - Houmark-Nielsen, Michael

AU - Hubberten, Hans W.

AU - Ingólfsson, Ólafur

AU - Jakobsson, Martin

AU - Kjær, Kurt H.

AU - Larsen, Eiliv

AU - Lokrantz, Hanna

AU - Lunkka, Juha Pekka

AU - Lyså, Astrid

AU - Mangerud, Jan

AU - Matiouchkov, Alexei

AU - Murray, Andrew

AU - Möller, Per

AU - Niessen, Frank

AU - Nikolskaya, Olga

AU - Polyak, Leonid

AU - Saarnisto, Matti

AU - Siegert, Christine

AU - Siegert, Martin J.

AU - Spielhagen, Robert F.

AU - Stein, Ruediger

PY - 2004/6/1

Y1 - 2004/6/1

N2 - The maximum limits of the Eurasian ice sheets during four glaciations have been reconstructed: (1) the Late Saalian (2) the Early Weichselian (100-80ka), (3) the Middle Weichselian (60-50ka) and (4) the Late Weichselian (25-15ka). The reconstructed ice limits are based on satellite data and aerial photographs combined with geological field investigations in Russia and Siberia, and with marine seismic- and sediment core data. The Barents-Kara Ice Sheet got progressively smaller during each glaciation, whereas the dimensions of the Scandinavian Ice Sheet increased. During the last Ice Age the Barents-Kara Ice Sheet attained its maximum size as early as 90-80,000 years ago when the ice front reached far onto the continent. A regrowth of the ice sheets occurred during the early Middle Weichselian, culminating about 60-50,000 years ago. During the Late Weichselian the Barents-Kara Ice Sheet did not reach the mainland east of the Kanin Peninsula, with the exception of the NW fringe of Taimyr. A numerical ice-sheet model, forced by global sea level and solar changes, was run through the full Weichselian glacial cycle. The modeling results are roughly compatible with the geological record of ice growth, but the model underpredicts the glaciations in the Eurasian Arctic during the Early and Middle Weichselian. One reason for this is that the climate in the Eurasian Arctic was not as dry then as during the Late Weichselian glacial maximum.

AB - The maximum limits of the Eurasian ice sheets during four glaciations have been reconstructed: (1) the Late Saalian (2) the Early Weichselian (100-80ka), (3) the Middle Weichselian (60-50ka) and (4) the Late Weichselian (25-15ka). The reconstructed ice limits are based on satellite data and aerial photographs combined with geological field investigations in Russia and Siberia, and with marine seismic- and sediment core data. The Barents-Kara Ice Sheet got progressively smaller during each glaciation, whereas the dimensions of the Scandinavian Ice Sheet increased. During the last Ice Age the Barents-Kara Ice Sheet attained its maximum size as early as 90-80,000 years ago when the ice front reached far onto the continent. A regrowth of the ice sheets occurred during the early Middle Weichselian, culminating about 60-50,000 years ago. During the Late Weichselian the Barents-Kara Ice Sheet did not reach the mainland east of the Kanin Peninsula, with the exception of the NW fringe of Taimyr. A numerical ice-sheet model, forced by global sea level and solar changes, was run through the full Weichselian glacial cycle. The modeling results are roughly compatible with the geological record of ice growth, but the model underpredicts the glaciations in the Eurasian Arctic during the Early and Middle Weichselian. One reason for this is that the climate in the Eurasian Arctic was not as dry then as during the Late Weichselian glacial maximum.

UR - http://www.scopus.com/inward/record.url?scp=2642542707&partnerID=8YFLogxK

U2 - 10.1016/j.quascirev.2003.12.008

DO - 10.1016/j.quascirev.2003.12.008

M3 - Article

AN - SCOPUS:2642542707

VL - 23

SP - 1229

EP - 1271

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

IS - 11-13

ER -

ID: 50791122