The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming
Abstract Plant remains accumulate as variably decomposed material, often in highly organic deposits above the mineral surface. These may occur as mor humus in the case of unsaturated forest and heath soils (Romell and Heiberg 1931), where the deposit is seldom more than 10-20 cm deep, or as peat (Cl...
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1995
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croxfordunivpr:10.1093/oso/9780195086409.003.0011 2024-09-15T18:05:55+00:00 The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming Gorham, Eville 1995 http://dx.doi.org/10.1093/oso/9780195086409.003.0011 https://academic.oup.com/book/chapter-pdf/52438425/isbn-9780195086409-book-part-11.pdf en eng Oxford University PressNew York, NY Biotic Feedbacks in the Global Climatic System page 169-187 ISBN 9780195086409 9780197709474 book-chapter 1995 croxfordunivpr https://doi.org/10.1093/oso/9780195086409.003.0011 2024-08-27T04:16:37Z Abstract Plant remains accumulate as variably decomposed material, often in highly organic deposits above the mineral surface. These may occur as mor humus in the case of unsaturated forest and heath soils (Romell and Heiberg 1931), where the deposit is seldom more than 10-20 cm deep, or as peat (Clymo 1983) in waterlogged wetlands. Where the organic wetland deposit is shallow and mixed with a good deal of mineral matter, it is often designated muck. Where the wetland accumulates more than 30 cm of highly organic peat (40 cm in Canada), it is said to be a peatland. Peatlands, sometimes several meters in depth, are particularly common in the northern landscapes of Russia and the Baltic republics, Canada, the northern United States (especially Alaska), and Fennoscandia, where they cover 342 x 106 ha (Gorham 1991a) and account for about 9.7% of the total land surface. Book Part Fennoscandia Alaska Oxford University Press 169 187 |
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Oxford University Press |
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croxfordunivpr |
language |
English |
description |
Abstract Plant remains accumulate as variably decomposed material, often in highly organic deposits above the mineral surface. These may occur as mor humus in the case of unsaturated forest and heath soils (Romell and Heiberg 1931), where the deposit is seldom more than 10-20 cm deep, or as peat (Clymo 1983) in waterlogged wetlands. Where the organic wetland deposit is shallow and mixed with a good deal of mineral matter, it is often designated muck. Where the wetland accumulates more than 30 cm of highly organic peat (40 cm in Canada), it is said to be a peatland. Peatlands, sometimes several meters in depth, are particularly common in the northern landscapes of Russia and the Baltic republics, Canada, the northern United States (especially Alaska), and Fennoscandia, where they cover 342 x 106 ha (Gorham 1991a) and account for about 9.7% of the total land surface. |
format |
Book Part |
author |
Gorham, Eville |
spellingShingle |
Gorham, Eville The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming |
author_facet |
Gorham, Eville |
author_sort |
Gorham, Eville |
title |
The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming |
title_short |
The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming |
title_full |
The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming |
title_fullStr |
The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming |
title_full_unstemmed |
The Biogeochemistry of Northern Peatlands and Its Possible Responses to Global Warming |
title_sort |
biogeochemistry of northern peatlands and its possible responses to global warming |
publisher |
Oxford University PressNew York, NY |
publishDate |
1995 |
url |
http://dx.doi.org/10.1093/oso/9780195086409.003.0011 https://academic.oup.com/book/chapter-pdf/52438425/isbn-9780195086409-book-part-11.pdf |
genre |
Fennoscandia Alaska |
genre_facet |
Fennoscandia Alaska |
op_source |
Biotic Feedbacks in the Global Climatic System page 169-187 ISBN 9780195086409 9780197709474 |
op_doi |
https://doi.org/10.1093/oso/9780195086409.003.0011 |
container_start_page |
169 |
op_container_end_page |
187 |
_version_ |
1810443432552824832 |