Paleocene-Eocene carbon isotope excursion in organic carbon and pedogenic carbonate: Direct comparison in a continental stratigraphic section
Authors:
- Roberto MagioncaldaRMRoberto Magioncalda
- Christian DupuisCDChristian Dupuis
- Thierry SmithTSThierry Smith
- Etienne SteurbautESEtienne Steurbaut
- Philip D. GingerichPGPhilip D. Gingerich
- 1 January 2004
- journal article
- Published by Geological Society of America in Geology
- Vol. 32 (7) , 553
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- The Dababiya Quarry Section: Lithostratigraphy, clay mineralogy, geochemistry and paleontologyMicropaleontology, 2003
- The destruction of paleoclimatic isotopic signals in Pleistocene carbonate soil nodules of Western AustraliaPalaeogeography, Palaeoclimatology, Palaeoecology, 2002
- Mammalian Dispersal at the Paleocene/Eocene BoundaryScience, 2002
- Global dinoflagellate event associated with the late Paleocene thermal maximumGeology, 2001
- Termination of global warmth at the Palaeocene/Eocene boundary through productivity feedbackNature, 2000
- Mechanisms of Climate Warming at the End of the PaleoceneScience, 1999
- Mammalian community response to the latest Paleocene thermal maximum: An isotaphonomic study in the northern Bighorn Basin, WyomingGeology, 1998
- Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the PaleocenePaleoceanography and Paleoclimatology, 1995
- Carbon dioxide in the atmosphere; evidence from Cenozoic and Mesozoic PaleosolsAmerican Journal of Science, 1991
- Depletion of 13C in lignin and its implications for stable carbon isotope studiesNature, 1987