CaCO3 dissolution experiments in Paleocene-Eocene agglutinated benthic foraminifera from Zumaya (Basque-Cantabric Basin, Spain)
The largest extinction of deep-sea benthic foraminifera in the Cenozoic occurred during the Paleocene-Eocene Thermal Maximum event (PETM, ~55.8 Ma). Much has been speculated about the causes of such extinction, and proposed mechanisms include changes in productivity and/or oxygenation of bottom wate...
Published in: | Estudios Geológicos |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | Spanish |
Published: |
Consejo Superior de Investigaciones Científicas
2015
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Subjects: | |
Online Access: | http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/917 https://doi.org/10.3989/egeol.41758.330 |