The contribution of Antarctic moss peat to the understanding of global peatland processes

Abstract The moss banks of the Maritime Antarctic composed of one or both of the mosses Chorisodontium aciphyllum and Polytrichum strictum form peat banks up to 3.4 m thick and 5500 years of age. They represent perhaps the simplest peat-forming systems in the world, so studying their dynamics can he...

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Published in:Antarctic Science
Main Author: Fenton, James H.C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102022000141
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102022000141
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spelling crcambridgeupr:10.1017/s0954102022000141 2024-03-03T08:37:36+00:00 The contribution of Antarctic moss peat to the understanding of global peatland processes Fenton, James H.C. 2022 http://dx.doi.org/10.1017/s0954102022000141 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102022000141 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 34, issue 3, page 266-278 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2022 crcambridgeupr https://doi.org/10.1017/s0954102022000141 2024-02-08T08:37:22Z Abstract The moss banks of the Maritime Antarctic composed of one or both of the mosses Chorisodontium aciphyllum and Polytrichum strictum form peat banks up to 3.4 m thick and 5500 years of age. They represent perhaps the simplest peat-forming systems in the world, so studying their dynamics can help in the understanding of peatland dynamics generally, particularly those of temperate blanket peat. They can provide insights into how the balance of growth, decomposition and compaction of peat results in peat formation, how downhill creep can be the cause of both vertical edges and the creation of patterned bogs and how erosion of peat can be a natural process. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Cambridge University Press Antarctic Antarctic Science 34 3 266 278
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
spellingShingle Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Fenton, James H.C.
The contribution of Antarctic moss peat to the understanding of global peatland processes
topic_facet Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
description Abstract The moss banks of the Maritime Antarctic composed of one or both of the mosses Chorisodontium aciphyllum and Polytrichum strictum form peat banks up to 3.4 m thick and 5500 years of age. They represent perhaps the simplest peat-forming systems in the world, so studying their dynamics can help in the understanding of peatland dynamics generally, particularly those of temperate blanket peat. They can provide insights into how the balance of growth, decomposition and compaction of peat results in peat formation, how downhill creep can be the cause of both vertical edges and the creation of patterned bogs and how erosion of peat can be a natural process.
format Article in Journal/Newspaper
author Fenton, James H.C.
author_facet Fenton, James H.C.
author_sort Fenton, James H.C.
title The contribution of Antarctic moss peat to the understanding of global peatland processes
title_short The contribution of Antarctic moss peat to the understanding of global peatland processes
title_full The contribution of Antarctic moss peat to the understanding of global peatland processes
title_fullStr The contribution of Antarctic moss peat to the understanding of global peatland processes
title_full_unstemmed The contribution of Antarctic moss peat to the understanding of global peatland processes
title_sort contribution of antarctic moss peat to the understanding of global peatland processes
publisher Cambridge University Press (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/s0954102022000141
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102022000141
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Antarctic
Antarctic Science
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Antarctic
Antarctic Science
op_source Antarctic Science
volume 34, issue 3, page 266-278
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102022000141
container_title Antarctic Science
container_volume 34
container_issue 3
container_start_page 266
op_container_end_page 278
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