Original paper
Persistent global marine euxinia in the early Silurian
Abstract
The second pulse of the Late Ordovician mass extinction occurred around the Hirnantian-Rhuddanian boundary (~444 Ma) and has been correlated with expanded marine anoxia lasting into the earliest Silurian. Characterization of the Hirnantian ocean anoxic event has focused on the onset of anoxia, with global reconstructions based on carbonate δ 238 U modeling. However, there have been limited attempts to quantify uncertainty in metal isotope mass...
Paper Details
Title
Persistent global marine euxinia in the early Silurian
Published Date
Apr 14, 2020
Journal
Volume
11
Issue
1
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Notes
History