The effects of diagenesis on geochemical paleoredox proxies in sedimentary carbonates-Reference-Cited by-同舟云学术

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The effects of diagenesis on geochemical paleoredox proxies in sedimentary carbonates

Published:2018-07 Issue: Volume:232 Page:265-287
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Hood Ashleigh v.S.,Planavsky Noah J.,Wallace Malcolm W.,Wang Xiangli

Funder

U.S. National Science Foundation Earth-Life Transitions Program

Alternative Earths NASA Astrobiology Institute

Australian Research Council

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference118 articles.

1. Metal stable isotopes in paleoceanography;Anbar;Annu. Rev. Earth Planet. Sci.,2007

2. A modern framework for the interpretation of 238 U/235 U in studies of ancient ocean redox;Andersen;Earth Planet. Sci. Lett.,2014

3. Closing in on the marine 238 U/235 U budget;Andersen;Chem. Geol.,2016

4. Coupled molybdenum, iron and uranium stable isotopes as oceanic paleoredox proxies during the Paleoproterozoic Shunga Event;Asael;Chem. Geol.,2013

5. Redox conditions across the Cambrian-Ordovician boundary: elemental and isotopic signatures retained in the GSSP carbonates;Azmy;Palaeogeogr., Palaeoclimatol., Palaeoecol.,2015

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