Pelagic evolution and environmental recovery after the Cretaceous-Paleogene mass extinction
Author:
Publisher
Geological Society of America
Subject
Geology
Reference17 articles.
1. A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals
2. Productivity change as a control on planktonic foraminiferal evolution after the cretaceous/tertiary boundary
3. Benthic foraminifera across the Cretaceous–Tertiary (K–T) boundary: a review
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