Biogeochemical Cycling and Paleoenvironmental Reconstructions of the Toarcian Oceanic Anoxic Event from Western North America

Biogeochemical Cycling and Paleoenvironmental Reconstructions of the Toarcian Oceanic Anoxic Event from Western North America

The Toarcian Oceanic Anoxic Event (T-OAE; ~183 million years ago) represents an interval during the Mesozoic when the emplacement of the Karoo-Ferrar Large Igneous Province (LIP) is thought to have resulted in significant environmental change. Associated with this interval was the widespread deposit...

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Bibliographic Details
Main Author: Them II, Theodore Roland
Other Authors: Geosciences
Format: Others
Published: Virginia Tech 2018
Subjects:
Toarcian Oceanic Anoxic Event
carbon isotope excursion
abrupt climate change
chemical weathering
anoxia
euxinia
iron speciation
Online Access:http://hdl.handle.net/10919/81908

Internet

http://hdl.handle.net/10919/81908

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