Organic carbon burial following the middle Eocene climatic optimum in the central western Tethys
- 24 August 2010
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 25 (3)
Abstract
No abstract availableKeywords
This publication has 66 references indexed in Scilit:
- Coupled greenhouse warming and deep‐sea acidification in the middle EocenePaleoceanography and Paleoclimatology, 2009
- Responses of calcareous nannofossil assemblages, mineralogy and geochemistry to the environmental perturbations across the Paleocene/Eocene boundary in the Venetian Pre-AlpsMarine Micropaleontology, 2007
- A REVISED TROPICAL TO SUBTROPICAL PALEOGENE PLANKTONIC FORAMINIFERAL ZONATIONJournal of Foraminiferal Research, 2005
- Do we have enough pieces of the jigsaw to integrate CO2 fluxes in the coastal ocean?Estuaries, 2005
- A humid climate state during the Palaeocene/Eocene thermal maximumNature, 2004
- Significant Southern Ocean warming event in the late middle EoceneGeology, 2003
- Palaeocene- early Eocene climatic evolution in the Tethyan realm: clay mineral evidenceClay Minerals, 2001
- GEOCARB III: A revised model of atmospheric CO2 over Phanerozoic timeAmerican Journal of Science, 2001
- Dynamics of fossil fuel CO2 neutralization by marine CaCO3Global Biogeochemical Cycles, 1998
- A Revised Cenozoic Geochronology and Chronostratigraphy1995