Global marine redox evolution from the late Neoproterozoic to the early Paleozoic constrained by the integration of Mo and U isotope records-Reference-Cited by-同舟云学术

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Global marine redox evolution from the late Neoproterozoic to the early Paleozoic constrained by the integration of Mo and U isotope records

Published:2021-03 Issue: Volume:214 Page:103506
ISSN:0012-8252
Container-title:Earth-Science Reviews
language:en
Short-container-title:Earth-Science Reviews

Author:

Wei Guang-Yi,Planavsky Noah J.,He Tianchen,Zhang Feifei,Stockey Richard G.,Cole Devon B.,Lin Yi-Bo,Ling Hong-Fei

Funder

National Natural Science Foundation of China

Nanjing University

Chinese Academy of Sciences

Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference216 articles.

1. Uranium isotopes as a proxy for primary depositional redox conditions in organic-rich marine systems;Abshire;Earth Planet. Sci. Lett.,2020

2. Interpretation of the nitrogen isotopic composition of Precambrian sedimentary rocks: Assumptions and perspectives;Ader;Chem. Geol.,2016

3. Stepwise Earth oxygenation is an inherent property of global biogeochemical cycling;Alcott;Science,2019

4. Mo-total organic carbon covariation in modern anoxic marine environments: implications for analysis of paleoredox and paleohydro-graphic conditions;Algeo;Paleoceanography,2006

5. Environmental analysis of paleoceanographic systems based on molybdenum–uranium covariation;Algeo;Chem. Geol.,2009

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