In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 49, No. 21 ( 2022-11-16)
Abstract:
Non‐quantitative Cr removal at the chemocline drives chromium (Cr) isotope fractionation and the accumulation of light Cr in euxinic deep waters Authigenic sediment δ 53 Cr differs from overlying water, contrary to paleoproxy application assumptions, and is similar to continental crust δ 53 Cr signals in these settings may therefore reflect internal redox processes and not fractionation due to oxidative subaerial weathering
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1029/2022GL099154
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2022
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13