Beyond redox: Control of trace-metal enrichment in anoxic marine facies by watermass chemistry and sedimentation rate-Reference-Cited by-同舟云学术

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Beyond redox: Control of trace-metal enrichment in anoxic marine facies by watermass chemistry and sedimentation rate

Published:2020-10 Issue: Volume:287 Page:296-317
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Liu Jiangsi^ORCID,Algeo Thomas J.^ORCID

Funder

State Key Laboratory of Marine Environmental Science

State Key Laboratory of Biogeology and Environmental Geology

National Natural Science Foundation of China

China Postdoctoral Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference143 articles.

1. Can marine anoxic events draw down the trace element inventory of seawater?;Algeo;Geology,2004

2. An ancient estuarine-circulation nutrient trap: The Late Pennsylvanian Midcontinent Sea of North America;Algeo;Geology,2018

3. Sedimentary Corg: P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2;Algeo;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2007

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

5. Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems;Algeo;Chem. Geol.,2004

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