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Glaciations : Early Quaternary (Pleistocene) and Precursors. / Ehlers, J.; Астахов, Валерий Иванович; Gibbard, P.L.; Ingólfsson, Ólafur; Mangerud, Jan; Svendsen, J.I.

Encyclopedia of Quaternary Science: : Second Edition. ed. / Scott Elias. Vol. 1 Amsterdam : Elsevier, 2013. p. 167-171.

Research output: Chapter in Book/Report/Conference proceedingEntry for encyclopedia/dictionaryResearchpeer-review

Harvard

Ehlers, J, Астахов, ВИ, Gibbard, PL, Ingólfsson, Ó, Mangerud, J & Svendsen, JI 2013, Glaciations: Early Quaternary (Pleistocene) and Precursors. in S Elias (ed.), Encyclopedia of Quaternary Science: : Second Edition. vol. 1, Elsevier, Amsterdam, pp. 167-171. https://doi.org/10.1016/B978-0-444-53643-3.00115-1

APA

Ehlers, J., Астахов, В. И., Gibbard, P. L., Ingólfsson, Ó., Mangerud, J., & Svendsen, J. I. (2013). Glaciations: Early Quaternary (Pleistocene) and Precursors. In S. Elias (Ed.), Encyclopedia of Quaternary Science: : Second Edition (Vol. 1, pp. 167-171). Elsevier. https://doi.org/10.1016/B978-0-444-53643-3.00115-1

Vancouver

Ehlers J, Астахов ВИ, Gibbard PL, Ingólfsson Ó, Mangerud J, Svendsen JI. Glaciations: Early Quaternary (Pleistocene) and Precursors. In Elias S, editor, Encyclopedia of Quaternary Science: : Second Edition. Vol. 1. Amsterdam: Elsevier. 2013. p. 167-171 https://doi.org/10.1016/B978-0-444-53643-3.00115-1

Author

Ehlers, J. ; Астахов, Валерий Иванович ; Gibbard, P.L. ; Ingólfsson, Ólafur ; Mangerud, Jan ; Svendsen, J.I. / Glaciations : Early Quaternary (Pleistocene) and Precursors. Encyclopedia of Quaternary Science: : Second Edition. editor / Scott Elias. Vol. 1 Amsterdam : Elsevier, 2013. pp. 167-171

BibTeX

@inbook{dd493924b625430d85dbab6f04217f2f,
title = "Glaciations: Early Quaternary (Pleistocene) and Precursors",
abstract = "While glaciation of Antarctica began as early as the Oligocene, glaciation of South America and Greenland started only some 14. Ma. Continental-scale glaciation of the Northern Hemisphere began only some 1. Ma in the Late Matuyama Chron, although smaller-scale glaciation was established in Greenland and Iceland at the beginning of the Quaternary. So far, evidence of this early glaciation is largely restricted to North America. The Scandinavian mountains may have been glaciated, but most of Asia was probably still ice free.",
keywords = "четвертичный период",
author = "J. Ehlers and Астахов, {Валерий Иванович} and P.L. Gibbard and {\'O}lafur Ing{\'o}lfsson and Jan Mangerud and J.I Svendsen",
note = "Энциклопедия в 4 томах, 375 статей, 3631 стр. ",
year = "2013",
month = apr,
day = "15",
doi = "10.1016/B978-0-444-53643-3.00115-1",
language = "English",
isbn = "978-0-444-53642-6",
volume = "1",
pages = "167--171",
editor = "Elias, {Scott }",
booktitle = "Encyclopedia of Quaternary Science:",
publisher = "Elsevier",
address = "Netherlands",

}

RIS

TY - CHAP

T1 - Glaciations

T2 - Early Quaternary (Pleistocene) and Precursors

AU - Ehlers, J.

AU - Астахов, Валерий Иванович

AU - Gibbard, P.L.

AU - Ingólfsson, Ólafur

AU - Mangerud, Jan

AU - Svendsen, J.I

N1 - Энциклопедия в 4 томах, 375 статей, 3631 стр.

PY - 2013/4/15

Y1 - 2013/4/15

N2 - While glaciation of Antarctica began as early as the Oligocene, glaciation of South America and Greenland started only some 14. Ma. Continental-scale glaciation of the Northern Hemisphere began only some 1. Ma in the Late Matuyama Chron, although smaller-scale glaciation was established in Greenland and Iceland at the beginning of the Quaternary. So far, evidence of this early glaciation is largely restricted to North America. The Scandinavian mountains may have been glaciated, but most of Asia was probably still ice free.

AB - While glaciation of Antarctica began as early as the Oligocene, glaciation of South America and Greenland started only some 14. Ma. Continental-scale glaciation of the Northern Hemisphere began only some 1. Ma in the Late Matuyama Chron, although smaller-scale glaciation was established in Greenland and Iceland at the beginning of the Quaternary. So far, evidence of this early glaciation is largely restricted to North America. The Scandinavian mountains may have been glaciated, but most of Asia was probably still ice free.

KW - четвертичный период

U2 - 10.1016/B978-0-444-53643-3.00115-1

DO - 10.1016/B978-0-444-53643-3.00115-1

M3 - Entry for encyclopedia/dictionary

SN - 978-0-444-53642-6

VL - 1

SP - 167

EP - 171

BT - Encyclopedia of Quaternary Science:

A2 - Elias, Scott

PB - Elsevier

CY - Amsterdam

ER -

ID: 48925637