Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)

M. Dedert, H. Stoll, D. Kroon, N. Shimuzu, K. Kanamaru, P. Ziveri

Research output: Contribution to JournalArticleAcademicpeer-review

Abstract

The Early Eocene Thermal Maximum 2 (ETM2) at ∼53.7 Ma is one of multiple hyperthermal events that followed the Paleocene-Eocene Thermal Maximum (PETM, ∼56 Ma). The negative carbon excursion and deep ocean carbonate dissolution which occurred during the event imply that a substantial amount (103 Gt) of carbon (C) was added to the ocean-atmosphere system, consequently increasing atmospheric CO
Original languageEnglish
Pages (from-to)977-993
JournalClimate of the Past
Volume8
DOIs
Publication statusPublished - 2011

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