Authigenic carbonate burial in the Late Devonian–Early Mississippian Bakken Formation (Williston Basin, USA )
Abstract
Late Devonian (Famennian) marine successions globally are typified by organic‐rich black shales deposited in anoxic and euxinic waters and the cessation of shelf carbonate sedimentation. This global ‘carbonate crisis’, known as the Hangenberg Event, coincides with a major extinction of reef‐building metazoans and perturbations to the global carbon cycle, evidenced by positive carbon‐isotope excursions of up to 4‰. It has been suggested that...
Paper Details
Title
Authigenic carbonate burial in the Late Devonian–Early Mississippian Bakken Formation (Williston Basin, USA )
Published Date
Jan 29, 2020
Journal
Volume
67
Issue
4
Pages
2065 - 2094
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