In:
Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 33, No. 1 ( 2019-01), p. 2-14
Abstract:
A well‐dated marine sediment core reconstructs remobilization of permafrost carbon at the end of the last deglaciation Permafrost carbon delivery to the Chukchi Sea was during the late deglacial twice that of today Two thirds of the carbon input was from coastal erosion of Ice Complex permafrost with remainder from soil active layer and marine carbon
Type of Medium:
Online Resource
ISSN:
0886-6236
,
1944-9224
DOI:
10.1029/2018GB005969
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2021601-4
SSG:
12
SSG:
13
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