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18 p, 4.1 MB Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2) / Dedert, M. (Vrije Universiteit Amsterdam. Cluster Earth & Climate Department of Earth Sciences) ; Stoll, H. M. (Universidad de Oviedo. Departamento de Geologia) ; Kroon, D. (University of Edinburgh. School of GeoSciences) ; Shimizu, N. (Woods Hole Oceanographic Institute) ; Kanamaru, K. (University of Massachusetts at Amherst. Department of Geosciences) ; Ziveri, Patrizia (Universitat Autònoma de Barcelona. Departament de Biologia Animal, de Biologia Vegetal i d'Ecologia)
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 CO₂(pCO₂). [...]
2012 - 10.5194/cp-8-977-2012
Climate of the Past, Vol. 8, issue 3 (May 2012) , p. 977-993  

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