Black shale–gray shale transitions in a Late Devonian shale succession, Central Appalachian Basin (Northern Ohio): Sedimentary and geochemical evidence for terrestrial organic matter input driving anoxia events-Reference-Cited by-同舟云学术

Black shale–gray shale transitions in a Late Devonian shale succession, Central Appalachian Basin (Northern Ohio): Sedimentary and geochemical evidence for terrestrial organic matter input driving anoxia events

Published:2022-12 Issue: Volume:608 Page:111271
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Dunkel Caroline A.,Vázquez-Ortega Angélica,Evans James E.

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

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4. Trace-metal covariation as a guide to water-mass conditions in ancient anoxic marine environments;Algeo;Geosphere,2008

5. Late Devonian oceanic anoxic events and biotic crises: “rooted” in the evolution of land plants?;Algeo;GSA Today,1995

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