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Glaciations | Early quaternary. / Ehlers, J.; Astakhov, V.; Gibbard, P. L.; Ingólfsson; Mangerud, J.; Svendsen, J. I.

Encyclopedia of Quaternary Science. Elsevier, 2006. p. 1031-1036.

Research output: Chapter in Book/Report/Conference proceeding › Chapter › Research › peer-review

Harvard

Ehlers, J, Astakhov, V, Gibbard, PL, Ingólfsson, Mangerud, J & Svendsen, JI 2006, Glaciations | Early quaternary. in Encyclopedia of Quaternary Science. Elsevier, pp. 1031-1036. https://doi.org/10.1016/B0-44-452747-8/00123-X

APA

Ehlers, J., Astakhov, V., Gibbard, P. L., Ingólfsson, Mangerud, J., & Svendsen, J. I. (2006). Glaciations | Early quaternary. In Encyclopedia of Quaternary Science (pp. 1031-1036). Elsevier. https://doi.org/10.1016/B0-44-452747-8/00123-X

Vancouver

Ehlers J, Astakhov V, Gibbard PL, Ingólfsson, Mangerud J, Svendsen JI. Glaciations | Early quaternary. In Encyclopedia of Quaternary Science. Elsevier. 2006. p. 1031-1036 https://doi.org/10.1016/B0-44-452747-8/00123-X

Author

Ehlers, J. ; Astakhov, V. ; Gibbard, P. L. ; Ingólfsson ; Mangerud, J. ; Svendsen, J. I. / Glaciations | Early quaternary. Encyclopedia of Quaternary Science. Elsevier, 2006. pp. 1031-1036

BibTeX

@inbook{fafaceb379e542439d9b156912885131,
title = "Glaciations | Early quaternary",
abstract = "Whilst glaciation of Antarctica goes back to the Oligocene, glaciation of South America and Greenland started some 14 Mya. Massive glaciation of the Northern Hemisphere started only some 1 Mya in the late Matuyama Chron. So far, evidence of this early glaciation is largely restricted to North America. Scandinavia may have been glaciated, but most of Asia probably was still ice-free.",
keywords = "Europe, Marine isotope stage (MIS)",
author = "J. Ehlers and V. Astakhov and Gibbard, {P. L.} and Ing{\'o}lfsson and J. Mangerud and Svendsen, {J. I.}",
year = "2006",
month = jan,
day = "1",
doi = "10.1016/B0-44-452747-8/00123-X",
language = "English",
pages = "1031--1036",
booktitle = "Encyclopedia of Quaternary Science",
publisher = "Elsevier",
address = "Netherlands",

}

RIS

TY - CHAP

T1 - Glaciations | Early quaternary

AU - Ehlers, J.

AU - Astakhov, V.

AU - Gibbard, P. L.

AU - Ingólfsson,

AU - Mangerud, J.

AU - Svendsen, J. I.

PY - 2006/1/1

Y1 - 2006/1/1

N2 - Whilst glaciation of Antarctica goes back to the Oligocene, glaciation of South America and Greenland started some 14 Mya. Massive glaciation of the Northern Hemisphere started only some 1 Mya in the late Matuyama Chron. So far, evidence of this early glaciation is largely restricted to North America. Scandinavia may have been glaciated, but most of Asia probably was still ice-free.

AB - Whilst glaciation of Antarctica goes back to the Oligocene, glaciation of South America and Greenland started some 14 Mya. Massive glaciation of the Northern Hemisphere started only some 1 Mya in the late Matuyama Chron. So far, evidence of this early glaciation is largely restricted to North America. Scandinavia may have been glaciated, but most of Asia probably was still ice-free.

KW - Europe

KW - Marine isotope stage (MIS)

UR - http://www.scopus.com/inward/record.url?scp=85079789364&partnerID=8YFLogxK

U2 - 10.1016/B0-44-452747-8/00123-X

DO - 10.1016/B0-44-452747-8/00123-X

M3 - Chapter

AN - SCOPUS:85079789364

SP - 1031

EP - 1036

BT - Encyclopedia of Quaternary Science

PB - Elsevier

ER -

ID: 53752386