In:
Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 33, No. 1 ( 2019-01), p. 85-99
Abstract:
Surface sediments of the Laptev and East Siberian Sea contain 2.7 Tg terrigenous organic carbon (terrOC) of which 55% resist degradation Integrating cross‐shelf terrOC losses with millennial transport times yield degradation fluxes of about 1.7 Gg (= 1,700 t) carbon per year Degradation of terrOC in sediments is orders of magnitude smaller than estimates for degradation in the water column
Type of Medium:
Online Resource
ISSN:
0886-6236
,
1944-9224
DOI:
10.1029/2018GB005967
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2021601-4
SSG:
12
SSG:
13
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