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

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

doi:10.1016/j.palaeo.2022.111271

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

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

School of Earth, Environment and Society

Research output: Contribution to journal › Article › peer-review

Original language	American English
Journal	Palaeogeograpy, Palaeoclimatology, Palaeoecology
Volume	608
DOIs	https://doi.org/10.1016/j.palaeo.2022.111271
State	Published - Oct 19 2022

Disciplines

Physical Sciences and Mathematics
Earth Sciences
Oceanography and Atmospheric Sciences and Meteorology

Access to Document

10.1016/j.palaeo.2022.111271License: Unspecified

Cite this

Dunkel, C. A., Vázquez-Ortega, A., & Evans, J. E. (2022). 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. Palaeogeograpy, Palaeoclimatology, Palaeoecology, 608. https://doi.org/10.1016/j.palaeo.2022.111271

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. / Dunkel, Caroline A; Vázquez-Ortega, Angélica; Evans, James E.
In: Palaeogeograpy, Palaeoclimatology, Palaeoecology, Vol. 608, 19.10.2022.

Research output: Contribution to journal › Article › peer-review

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