After the Ice: Parallelus Meets Erythropus in the Pyrenees
Abstract The Pleistocene Ice Ages greatly modified the geographic distributions of most organ isms, with changes in distributions particularly marked in the temperate regions, including Europe and North America for which we have a growing amount of info mation. At the last glacial maximum in western...
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Oxford University PressNew York, NY
1993
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croxfordunivpr:10.1093/oso/9780195069174.003.0006 2024-06-23T07:50:17+00:00 After the Ice: Parallelus Meets Erythropus in the Pyrenees Hewitt, Godfrey M 1993 http://dx.doi.org/10.1093/oso/9780195069174.003.0006 https://academic.oup.com/book/chapter-pdf/52331107/isbn-9780195069174-book-part-6.pdf en eng Oxford University PressNew York, NY Hybrid Zones and the Evolutionary Process page 140-164 ISBN 9780195069174 9780197701362 book-chapter 1993 croxfordunivpr https://doi.org/10.1093/oso/9780195069174.003.0006 2024-06-11T04:20:56Z Abstract The Pleistocene Ice Ages greatly modified the geographic distributions of most organ isms, with changes in distributions particularly marked in the temperate regions, including Europe and North America for which we have a growing amount of info mation. At the last glacial maximum in western Europe (18,000-20,000 BP) the Arctic ice sheet extended down across England and North Germany, with separate ice sheets on the Alps, Pyrenees, and other high mountains scattered across from Iberia to Transylvania. There was tundra vegetation in France and largely treeless steppe over much of Spain and southern Europe (Huntley and Birks, 1983; Huntley, 1988). Today in western Europe tundra conditions are found only in northern Norway and the Kola Peninsula in northwestern Russia. Book Part Arctic Ice Sheet kola peninsula Northern Norway Tundra Oxford University Press Arctic Birks ENVELOPE(-62.163,-62.163,-65.290,-65.290) Kola Peninsula Norway 140 164 |
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Open Polar |
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Oxford University Press |
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croxfordunivpr |
language |
English |
description |
Abstract The Pleistocene Ice Ages greatly modified the geographic distributions of most organ isms, with changes in distributions particularly marked in the temperate regions, including Europe and North America for which we have a growing amount of info mation. At the last glacial maximum in western Europe (18,000-20,000 BP) the Arctic ice sheet extended down across England and North Germany, with separate ice sheets on the Alps, Pyrenees, and other high mountains scattered across from Iberia to Transylvania. There was tundra vegetation in France and largely treeless steppe over much of Spain and southern Europe (Huntley and Birks, 1983; Huntley, 1988). Today in western Europe tundra conditions are found only in northern Norway and the Kola Peninsula in northwestern Russia. |
format |
Book Part |
author |
Hewitt, Godfrey M |
spellingShingle |
Hewitt, Godfrey M After the Ice: Parallelus Meets Erythropus in the Pyrenees |
author_facet |
Hewitt, Godfrey M |
author_sort |
Hewitt, Godfrey M |
title |
After the Ice: Parallelus Meets Erythropus in the Pyrenees |
title_short |
After the Ice: Parallelus Meets Erythropus in the Pyrenees |
title_full |
After the Ice: Parallelus Meets Erythropus in the Pyrenees |
title_fullStr |
After the Ice: Parallelus Meets Erythropus in the Pyrenees |
title_full_unstemmed |
After the Ice: Parallelus Meets Erythropus in the Pyrenees |
title_sort |
after the ice: parallelus meets erythropus in the pyrenees |
publisher |
Oxford University PressNew York, NY |
publishDate |
1993 |
url |
http://dx.doi.org/10.1093/oso/9780195069174.003.0006 https://academic.oup.com/book/chapter-pdf/52331107/isbn-9780195069174-book-part-6.pdf |
long_lat |
ENVELOPE(-62.163,-62.163,-65.290,-65.290) |
geographic |
Arctic Birks Kola Peninsula Norway |
geographic_facet |
Arctic Birks Kola Peninsula Norway |
genre |
Arctic Ice Sheet kola peninsula Northern Norway Tundra |
genre_facet |
Arctic Ice Sheet kola peninsula Northern Norway Tundra |
op_source |
Hybrid Zones and the Evolutionary Process page 140-164 ISBN 9780195069174 9780197701362 |
op_doi |
https://doi.org/10.1093/oso/9780195069174.003.0006 |
container_start_page |
140 |
op_container_end_page |
164 |
_version_ |
1802641158753484800 |