In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 22, No. 8 ( 2021-08)
Abstract:
The tectonic migration of ocean floor led to a transition from an organic carbon‐starved to an elevated organic carbon burial environment Diagenetic transformation of iron oxides into pyrite within the carbon‐lean sediments occurred several millions of years after deposition Reducible iron(III), which is mostly present in phyllosilicates, can potentially fuel microbially mediated mineral alteration
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2020GC009585
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2027201-7
