In:
Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 33, No. 12 ( 2019-12), p. 1715-1732
Abstract:
One fifth of organic matter on Arabian Sea seafloor could stem from bacterial carbon fixation in the oxygen minimum zone Evaluation of past anoxic events needs to take chemoautotrophic contribution into account in isotope balances Biogeochemical models ignoring dark carbon fixation could highly underestimate oxygen demand and thus expansion of oxygen minimum zones
Type of Medium:
Online Resource
ISSN:
0886-6236
,
1944-9224
DOI:
10.1029/2019GB006282
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2021601-4
SSG:
12
SSG:
13
Permalink