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...

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Bibliographic Details
Published in:Estudios Geológicos
Main Authors: Arreguín-Rodríguez, G. J., Alegret, L.
Format: Article in Journal/Newspaper
Language:Spanish
Published: Consejo Superior de Investigaciones Científicas 2015
Subjects:
Online Access:http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/917
https://doi.org/10.3989/egeol.41758.330