Isotopically light Mo in sediments of methane seepage controlled by the benthic Fe–Mn redox shuttle process-Reference-Cited by-同舟云学术

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Isotopically light Mo in sediments of methane seepage controlled by the benthic Fe–Mn redox shuttle process

Published:2024-08 Issue: Volume:239 Page:104512
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Miao Xiaoming,Wei Jiangong,Li Jingrui,Liu Xiting,Wang Dong,Li Jie,Feng Xiuli

Funder

China Postdoctoral Science Foundation

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference93 articles.

1. Mo–total organic carbon covariation in modern anoxic marine environments: Implications for analysis ofpaleoredox and paleohydrographic conditions;Algeo;Paleoceanography,2006

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

3. A deep fluid source of radiogenic Sr and highly dynamic seepage conditions recorded in Miocene seep carbonates of the northern Apennines (Italy);Argentino;Chem. Geol.,2019

4. Evidence from molybdenum and iron isotopes and molybdenum–uranium covariation for sulphidic bottom waters during Eastern Mediterranean Sapropel S1 formation;Azrieli-Tal;Earth Planet. Sci. Lett.,2014

5. Molybdenum isotope fractionation during adsorption by manganese oxides;Barling;Earth Planet. Sci. Lett.,2004

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1. The formation of tubular seep carbonate deciphered from mineralogical and geochemical characteristics: an example from the South China Sea;Frontiers in Marine Science;2024-08-26

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