Up in smoke: A role for organic carbon feedbacks in Paleogene hyperthermals
Author:
- Gabriel J. BowenGBGabriel J. Bowen
- 1 October 2013
- journal article
- Published by Elsevier in Global and Planetary Change
- Vol. 109, 18-29
Abstract
No abstract availableThis publication has 85 references indexed in Scilit:
- Coupled and decoupled responses of continental and marine organic‐sedimentary systems through the Paleocene‐Eocene thermal maximum, New Jersey margin, USAPaleoceanography and Paleoclimatology, 2013
- North American carbon dioxide sources and sinks: magnitude, attribution, and uncertaintyFrontiers in Ecology and the Environment, 2012
- North American Carbon Program (NACP) regional interim synthesis: Terrestrial biospheric model intercomparisonEcological Modelling, 2012
- Past extreme warming events linked to massive carbon release from thawing permafrostNature, 2012
- Production of n-alkyl lipids in living plants and implications for the geologic pastGeochimica et Cosmochimica Acta, 2011
- Coupled high-resolution marine and terrestrial records of carbon and hydrologic cycles variations during the Paleocene–Eocene Thermal Maximum (PETM)Earth and Planetary Science Letters, 2011
- Enhanced chemistry-climate feedbacks in past greenhouse worldsProceedings of the National Academy of Sciences, 2011
- Global patterns in leaf 13 C discrimination and implications for studies of past and future climateProceedings of the National Academy of Sciences, 2010
- North American continental margin records of the Paleocene‐Eocene thermal maximum: Implications for global carbon and hydrological cyclingPaleoceanography and Paleoclimatology, 2008
- Beyond methane: Towards a theory for the Paleocene–Eocene Thermal MaximumEarth and Planetary Science Letters, 2006