In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 48, No. 19 ( 2021-10-16)
Abstract:
The effect of oxidative sulfide weathering on is dependent on the coupled oxygen–carbon–sulfur cycles Due to feedbacks, an increase in sulfide weathering will switch from a transient C source to a C sink on geologically short timescales This behavior is robust for a large range of oxygen feedback strengths
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2021GL094589
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13
Permalink