Paleosols and the Forest Border in Keewatin, N.W.T.
The morphology of paleosols and radiocarbon-dated charcoal from buried surface horizons of soils provide evidence to suggest that between periods of northward forest encroachment tundra climate has dominated areas at least 50 km south of the present forest/tundra border in southwest Keewatin. The pr...
Published in: | Quaternary Research |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1971
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Online Access: | http://dx.doi.org/10.1016/0033-5894(71)90059-7 http://api.elsevier.com/content/article/PII:0033589471900597?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589471900597?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400003197 |
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crcambridgeupr:10.1016/0033-5894(71)90059-7 2024-06-09T07:47:26+00:00 Paleosols and the Forest Border in Keewatin, N.W.T. Sorenson, Curtis J. Knox, James C. Larsen, James A. Bryson, Reid A. 1971 http://dx.doi.org/10.1016/0033-5894(71)90059-7 http://api.elsevier.com/content/article/PII:0033589471900597?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589471900597?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400003197 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 1, issue 4, page 468-473 ISSN 0033-5894 1096-0287 journal-article 1971 crcambridgeupr https://doi.org/10.1016/0033-5894(71)90059-7 2024-05-15T13:04:18Z The morphology of paleosols and radiocarbon-dated charcoal from buried surface horizons of soils provide evidence to suggest that between periods of northward forest encroachment tundra climate has dominated areas at least 50 km south of the present forest/tundra border in southwest Keewatin. The present forest/tundra border climate is nearly as severe as any climate that has prevailed in the area since deglaciation. Article in Journal/Newspaper Keewatin Tundra Cambridge University Press Quaternary Research 1 4 468 473 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
The morphology of paleosols and radiocarbon-dated charcoal from buried surface horizons of soils provide evidence to suggest that between periods of northward forest encroachment tundra climate has dominated areas at least 50 km south of the present forest/tundra border in southwest Keewatin. The present forest/tundra border climate is nearly as severe as any climate that has prevailed in the area since deglaciation. |
format |
Article in Journal/Newspaper |
author |
Sorenson, Curtis J. Knox, James C. Larsen, James A. Bryson, Reid A. |
spellingShingle |
Sorenson, Curtis J. Knox, James C. Larsen, James A. Bryson, Reid A. Paleosols and the Forest Border in Keewatin, N.W.T. |
author_facet |
Sorenson, Curtis J. Knox, James C. Larsen, James A. Bryson, Reid A. |
author_sort |
Sorenson, Curtis J. |
title |
Paleosols and the Forest Border in Keewatin, N.W.T. |
title_short |
Paleosols and the Forest Border in Keewatin, N.W.T. |
title_full |
Paleosols and the Forest Border in Keewatin, N.W.T. |
title_fullStr |
Paleosols and the Forest Border in Keewatin, N.W.T. |
title_full_unstemmed |
Paleosols and the Forest Border in Keewatin, N.W.T. |
title_sort |
paleosols and the forest border in keewatin, n.w.t. |
publisher |
Cambridge University Press (CUP) |
publishDate |
1971 |
url |
http://dx.doi.org/10.1016/0033-5894(71)90059-7 http://api.elsevier.com/content/article/PII:0033589471900597?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589471900597?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400003197 |
genre |
Keewatin Tundra |
genre_facet |
Keewatin Tundra |
op_source |
Quaternary Research volume 1, issue 4, page 468-473 ISSN 0033-5894 1096-0287 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1016/0033-5894(71)90059-7 |
container_title |
Quaternary Research |
container_volume |
1 |
container_issue |
4 |
container_start_page |
468 |
op_container_end_page |
473 |
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1801378517642903552 |