Uranium isotope evidence for an expansion of marine anoxia during the end‐ T riassic extinction-Reference-Cited by-同舟云学术

Uranium isotope evidence for an expansion of marine anoxia during the end‐ T riassic extinction

Published:2017-08 Issue:8 Volume:18 Page:3093-3108
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Jost Adam B.¹²^ORCID,Bachan Aviv¹,van de Schootbrugge Bas³^ORCID,Lau Kimberly V.¹⁴^ORCID,Weaver Karrie L.¹^ORCID,Maher Kate¹^ORCID,Payne Jonathan L.¹^ORCID

Affiliation:

1. Department of Geological SciencesStanford UniversityStanford California USA

2. Department of Earth, Atmospheric, and Planetary SciencesMassachusetts Institute of TechnologyCambridge Massachusetts USA

3. Marine Palynology and Paleoceanography Group, Department of Earth SciencesUtrecht UniversityUtrecht Netherlands

4. Department of Earth SciencesUniversity of California, RiversideRiverside California USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GC006941

Reference70 articles.

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2. Closing in on the marine 238 U/ 235 U budget

3. Uranium Isotope Fractionation

4. Concentration, oxidation state, and particulate flux of uranium in the Black Sea

5. Redox conditions across the Cambrian–Ordovician boundary: Elemental and isotopic signatures retained in the GSSP carbonates

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