LIP volcanism (not anoxia) tracked by Cr isotopes during Ocean Anoxic Event 2 in the proto-North Atlantic region-Reference-Cited by-同舟云学术

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LIP volcanism (not anoxia) tracked by Cr isotopes during Ocean Anoxic Event 2 in the proto-North Atlantic region

Published:2022-09 Issue: Volume:332 Page:138-155
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Nana Yobo Lucien,Holmden Chris,Brandon Alan D.,Lau Kimberly V.,Eldrett James S.,Bergman Steven

Funder

NSERC

National Science Foundation Directorate for Geosciences

AAPG Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference95 articles.

1. Kinetics and thermodynamics of chromium ions adsorption onto low-cost dolomite adsorbent;Albadarin;Chem. Eng. J.,2012

2. Modern rather than Mesoarchaean oxidative weathering responsible for the heavy stable Cr isotopic signatures of the 2.95 Ga old Ijzermijn iron formation (South Africa);Albut;Geochim. Cosmochim. Acta,2018

3. Modern weathering in outcrop samples versus ancient paleoredox information in drill core samples from a Mesoarchaean marine oxygen oasis in Pongola Supergroup, South Africa;Albut;Geochim. Cosmochim. Acta,2019

4. Chromium geochemistry of the ca. 1.85Ga Flin Flon paleosol;Babechuk;Geobiology,2017

5. Kinetic stable Cr isotopic fractionation between aqueous Cr(III)-Cl-H2O complexes at 25 C: Implications for Cr(III) mobility and isotopic variations in modern and ancient natural systems;Babechuk;Geochim. Cosmochim. Acta,2018

Cited by 4 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Statistical approaches for improved definition of carbon isotope excursions;Earth-Science Reviews;2024-08

2. Ocean redox evolution past and present;Reference Module in Earth Systems and Environmental Sciences;2024

3. Fractionation of iron and chromium isotopes in hydrothermal plumes from the northern Mid-Atlantic Ridge;Earth and Planetary Science Letters;2023-12

4. Cr stable isotope fractionation by evaporation from silicate melts;Chemical Geology;2022-11

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