Massive remobilization of permafrost carbon during post-glacial warming; Nature Communications; Vol. 7, article 13653
| Parent link: | Nature Communications: open access journal.— , 2010- Vol. 7, article 13653.— 2016.— [10 р.] |
|---|---|
| Corporate Author: | Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ) Международная научно-образовательная лаборатория изучения углерода арктических морей (МНОЛ ИУАМ) |
| Other Authors: | Tesi T., Muschitiello F., Smittenberg R. H., Jakobsson M., Vonk J. E., Hill P., Andersson A., Kirchner N., Noormets N., Dudarev O. V. Oleg Viktorovich, Semiletov I. P. Igor Petrovich, Gustafsson Ö |
| Summary: | Title screen Recent hypotheses, based on atmospheric records and models, suggest that permafrost carbon (PF-C) accumulated during the last glaciation may have been an important source for the atmospheric CO2 rise during post-glacial warming. However, direct physical indications for such PF-C release have so far been absent. Here we use the Laptev Sea (Arctic Ocean) as an archive to investigate PF-C destabilization during the last glacial–interglacial period. Our results show evidence for massive supply of PF-C from Siberian soils as a result of severe active layer deepening in response to the warming. Thawing of PF-C must also have brought about an enhanced organic matter respiration and, thus, these findings suggest that PF-C may indeed have been an important source of CO2 across the extensive permafrost domain. The results challenge current paradigms on the post-glacial CO2 rise and, at the same time, serve as a harbinger for possible consequences of the present-day warming of PF-C soils. |
| Language: | English |
| Published: |
2016
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1038/ncomms13653 |
| Format: | Electronic Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=653175 |
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