The periglacial record of Holocene environmental change, subantarctic Marion Island
Abstract This paper examines the evidence for cold‐climate conditions on Marion Island, both present and past, and discusses the palaeoenvironmental implications. Under present conditions frost penetration, except in the highest‐altitude areas, is limited to the upper 0.05–0.3 m of the soil. Relict...
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Online Access: | http://dx.doi.org/10.1002/ppp.439 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.439 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.439 |
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crwiley:10.1002/ppp.439 2024-09-15T18:18:19+00:00 The periglacial record of Holocene environmental change, subantarctic Marion Island Holness, S. D. 2003 http://dx.doi.org/10.1002/ppp.439 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.439 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.439 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 14, issue 1, page 69-74 ISSN 1045-6740 1099-1530 journal-article 2003 crwiley https://doi.org/10.1002/ppp.439 2024-07-25T04:22:05Z Abstract This paper examines the evidence for cold‐climate conditions on Marion Island, both present and past, and discusses the palaeoenvironmental implications. Under present conditions frost penetration, except in the highest‐altitude areas, is limited to the upper 0.05–0.3 m of the soil. Relict periglacial features include large stone‐banked lobes and terraces, vegetation‐banked features and blockstreams. It is suggested that these features are the result of deep seasonal frost. Copyright © 2003 John Wiley & Sons, Ltd. Article in Journal/Newspaper Marion Island Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 14 1 69 74 |
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English |
description |
Abstract This paper examines the evidence for cold‐climate conditions on Marion Island, both present and past, and discusses the palaeoenvironmental implications. Under present conditions frost penetration, except in the highest‐altitude areas, is limited to the upper 0.05–0.3 m of the soil. Relict periglacial features include large stone‐banked lobes and terraces, vegetation‐banked features and blockstreams. It is suggested that these features are the result of deep seasonal frost. Copyright © 2003 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Holness, S. D. |
spellingShingle |
Holness, S. D. The periglacial record of Holocene environmental change, subantarctic Marion Island |
author_facet |
Holness, S. D. |
author_sort |
Holness, S. D. |
title |
The periglacial record of Holocene environmental change, subantarctic Marion Island |
title_short |
The periglacial record of Holocene environmental change, subantarctic Marion Island |
title_full |
The periglacial record of Holocene environmental change, subantarctic Marion Island |
title_fullStr |
The periglacial record of Holocene environmental change, subantarctic Marion Island |
title_full_unstemmed |
The periglacial record of Holocene environmental change, subantarctic Marion Island |
title_sort |
periglacial record of holocene environmental change, subantarctic marion island |
publisher |
Wiley |
publishDate |
2003 |
url |
http://dx.doi.org/10.1002/ppp.439 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.439 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.439 |
genre |
Marion Island Permafrost and Periglacial Processes |
genre_facet |
Marion Island Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 14, issue 1, page 69-74 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.439 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
14 |
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1 |
container_start_page |
69 |
op_container_end_page |
74 |
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1810456447485476864 |