Bildung und Oxidation von Methan in tauendem Permafrost
Permafrost regions store between 1.100 and 1.500 gigatons of organic carbon and account for about 50 % of the world’s soil carbon storage. About 10–20 % of near-surface permafrost has been lost due to increases in surface temperatures between 1960 and 2000, and between 10–65 % of near-surface permaf...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5011180 2023-05-15T17:55:16+02:00 Bildung und Oxidation von Methan in tauendem Permafrost Liebner, S. Heslop, J. 2022 application/pdf https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180_1/component/file_5011670/5011180.pdf ger ger info:eu-repo/semantics/altIdentifier/doi/10.1007/s12268-022-1746-1 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180_1/component/file_5011670/5011180.pdf info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/deed.de CC-BY BIOspektrum info:eu-repo/semantics/article 2022 ftgfzpotsdam https://doi.org/10.1007/s12268-022-1746-1 2022-09-14T05:58:12Z Permafrost regions store between 1.100 and 1.500 gigatons of organic carbon and account for about 50 % of the world’s soil carbon storage. About 10–20 % of near-surface permafrost has been lost due to increases in surface temperatures between 1960 and 2000, and between 10–65 % of near-surface permafrost is expected to disappear by the year 2100. The organic matter in permafrost is only weakly protected and most of it is therefore available for microbial degradation. Microorganisms thus play a central role for the permafrost carbon feedback. Article in Journal/Newspaper permafrost GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) BIOspektrum 28 3 253 256 |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
German |
description |
Permafrost regions store between 1.100 and 1.500 gigatons of organic carbon and account for about 50 % of the world’s soil carbon storage. About 10–20 % of near-surface permafrost has been lost due to increases in surface temperatures between 1960 and 2000, and between 10–65 % of near-surface permafrost is expected to disappear by the year 2100. The organic matter in permafrost is only weakly protected and most of it is therefore available for microbial degradation. Microorganisms thus play a central role for the permafrost carbon feedback. |
format |
Article in Journal/Newspaper |
author |
Liebner, S. Heslop, J. |
spellingShingle |
Liebner, S. Heslop, J. Bildung und Oxidation von Methan in tauendem Permafrost |
author_facet |
Liebner, S. Heslop, J. |
author_sort |
Liebner, S. |
title |
Bildung und Oxidation von Methan in tauendem Permafrost |
title_short |
Bildung und Oxidation von Methan in tauendem Permafrost |
title_full |
Bildung und Oxidation von Methan in tauendem Permafrost |
title_fullStr |
Bildung und Oxidation von Methan in tauendem Permafrost |
title_full_unstemmed |
Bildung und Oxidation von Methan in tauendem Permafrost |
title_sort |
bildung und oxidation von methan in tauendem permafrost |
publishDate |
2022 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180_1/component/file_5011670/5011180.pdf |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
BIOspektrum |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s12268-022-1746-1 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5011180_1/component/file_5011670/5011180.pdf |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/deed.de |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1007/s12268-022-1746-1 |
container_title |
BIOspektrum |
container_volume |
28 |
container_issue |
3 |
container_start_page |
253 |
op_container_end_page |
256 |
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1766163188325285888 |