Late Frasnian Mass Extinction: Conodont Event Stratigraphy, Global Changes, and Possible Causes
Volume: 673, Pages: 160
Published: Jan 1, 1988
Abstract
Several abrupt changes in conodont biofacies are documented to occur synchronously at six primary control sections across the Frasnian-Famennian boundary in Euramerica. These changes occurred within a time-span of only about 100,000 years near the end of the latest Frasnian linguiformis Zone, which is formally named to replace the Uppermost gigas Zone. The conodont-biofacies changes are interpreted to reflect a eustatic rise followed by an...
Paper Details
Title
Late Frasnian Mass Extinction: Conodont Event Stratigraphy, Global Changes, and Possible Causes
Published Date
Jan 1, 1988
Volume
673
Pages
160
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