In:
Journal of Geophysical Research: Biogeosciences, American Geophysical Union (AGU), Vol. 126, No. 3 ( 2021-03)
Abstract:
Permafrost turnover and export can be traced using alkanoic acid δ 13 C and Δ 14 C whereas bulk organic carbon (OC) isotope values are biased by coal‐derived OC Alkanoic acid turnover in permafrost is multi‐millennial likely controlled by low mean annual air temperature and precipitation Long‐chain alkanoic acid Δ 14 C values in river and fjord sediments imply reburial of deep active layer and permafrost OC
Type of Medium:
Online Resource
ISSN:
2169-8953
,
2169-8961
DOI:
10.1029/2020JG006008
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
3094167-2
detail.hit.zdb_id:
2220777-6
SSG:
16,13
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