The formation of vertical edges on Antarctic moss peat banks
Moss peat banks, which can be up to 3 m deep, greater than 2500 m2 in area, and up to 5000 yr old, occur in the Antarctic. Radiocarbon dates show that the peat accumulation rate has varied from 0.25 to 2.00 mm yr-1. These peat banks have an abrupt vertical edge of exposed peat, which does not appear...
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Taylor and Francis
1982
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Online Access: | http://nora.nerc.ac.uk/id/eprint/524362/ https://doi.org/10.2307/1550811 |
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ftnerc:oai:nora.nerc.ac.uk:524362 2023-05-15T13:41:43+02:00 The formation of vertical edges on Antarctic moss peat banks Fenton, J.H.C. 1982 http://nora.nerc.ac.uk/id/eprint/524362/ https://doi.org/10.2307/1550811 unknown Taylor and Francis Fenton, J.H.C. 1982 The formation of vertical edges on Antarctic moss peat banks. Arctic and Alpine Research, 14 (1). 21-26. https://doi.org/10.2307/1550811 <https://doi.org/10.2307/1550811> Botany Publication - Article PeerReviewed 1982 ftnerc https://doi.org/10.2307/1550811 2023-02-04T19:48:50Z Moss peat banks, which can be up to 3 m deep, greater than 2500 m2 in area, and up to 5000 yr old, occur in the Antarctic. Radiocarbon dates show that the peat accumulation rate has varied from 0.25 to 2.00 mm yr-1. These peat banks have an abrupt vertical edge of exposed peat, which does not appear to be due to erosion of a once-larger peat bank. These edges seem to have arisen because, as peat accumulates and the moss banks become deeper, increased snow-lie prevents outward growth of the banks at their edges. Article in Journal/Newspaper Antarc* Antarctic Arctic Arctic and Alpine Research Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Arctic and Alpine Research 14 1 21 |
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Open Polar |
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Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
unknown |
topic |
Botany |
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Botany Fenton, J.H.C. The formation of vertical edges on Antarctic moss peat banks |
topic_facet |
Botany |
description |
Moss peat banks, which can be up to 3 m deep, greater than 2500 m2 in area, and up to 5000 yr old, occur in the Antarctic. Radiocarbon dates show that the peat accumulation rate has varied from 0.25 to 2.00 mm yr-1. These peat banks have an abrupt vertical edge of exposed peat, which does not appear to be due to erosion of a once-larger peat bank. These edges seem to have arisen because, as peat accumulates and the moss banks become deeper, increased snow-lie prevents outward growth of the banks at their edges. |
format |
Article in Journal/Newspaper |
author |
Fenton, J.H.C. |
author_facet |
Fenton, J.H.C. |
author_sort |
Fenton, J.H.C. |
title |
The formation of vertical edges on Antarctic moss peat banks |
title_short |
The formation of vertical edges on Antarctic moss peat banks |
title_full |
The formation of vertical edges on Antarctic moss peat banks |
title_fullStr |
The formation of vertical edges on Antarctic moss peat banks |
title_full_unstemmed |
The formation of vertical edges on Antarctic moss peat banks |
title_sort |
formation of vertical edges on antarctic moss peat banks |
publisher |
Taylor and Francis |
publishDate |
1982 |
url |
http://nora.nerc.ac.uk/id/eprint/524362/ https://doi.org/10.2307/1550811 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Arctic Arctic and Alpine Research |
genre_facet |
Antarc* Antarctic Arctic Arctic and Alpine Research |
op_relation |
Fenton, J.H.C. 1982 The formation of vertical edges on Antarctic moss peat banks. Arctic and Alpine Research, 14 (1). 21-26. https://doi.org/10.2307/1550811 <https://doi.org/10.2307/1550811> |
op_doi |
https://doi.org/10.2307/1550811 |
container_title |
Arctic and Alpine Research |
container_volume |
14 |
container_issue |
1 |
container_start_page |
21 |
_version_ |
1766155475687047168 |