Author pages are created from data sourced from our academic publisher partnerships and public sources.
- Publications
- Influence
Share This Author
Marked Decline in Atmospheric Carbon Dioxide Concentrations During the Paleogene
- M. Pagani, J. Zachos, K. Freeman, B. Tipple, S. Bohaty
- Environmental Science, GeographyScience
- 22 July 2005
TLDR
Significant Southern Ocean warming event in the late middle Eocene
A prominent middle Eocene warming event is identified in Southern Ocean deep-sea cores, indicating that long-term cooling through the middle and late Eocene was not monotonic. At sites on Maud Rise…
A Transient Rise in Tropical Sea Surface Temperature During the Paleocene-Eocene Thermal Maximum
- J. Zachos, M. Wara, I. Premoli-Silva
- Environmental Science, GeographyScience
- 28 November 2003
TLDR
Coupled Greenhouse Warming and Deep Sea Acidification in the Middle Eocene
- S. Bohaty, J. Zachos, F. Florindo, M. Delaney
- Environmental Science, Geography
- 1 June 2009
[1] The Middle Eocene Climatic Optimum (MECO) is an enigmatic warming event that represents an abrupt reversal in long-term cooling through the Eocene. In order to further assess the timing and…
Warming the fuel for the fire: Evidence for the thermal dissociation of methane hydrate during the Paleocene-Eocene thermal maximum
- D. J. Thomas, J. Zachos, T. Bralower, Ellen Thomas, S. Bohaty
- Environmental Science, Geography
- 1 December 2002
Dramatic warming and upheaval of the carbon system at the end of the Paleocene Epoch have been linked to massive dissociation of sedimentary methane hydrate. However, testing the Paleocene-Eocene…
A 40-million-year history of atmospheric CO2
- Yi Ge Zhang, M. Pagani, Zhonghui Liu, S. Bohaty, R. DeConto
- Environmental Science, GeographyPhilosophical Transactions of the Royal Society A…
- 28 October 2013
TLDR
Extreme warming of mid-latitude coastal ocean during the Paleocene-Eocene Thermal Maximum: Inferences from TEX86 and isotope data
- J. Zachos, Stefan Schouten, T. Bralower
- Environmental Science, Geography
- 1 September 2006
Changes in sea surface temperature (SST) during the Paleocene-Eocene Thermal Max- imum (PETM) have been estimated primarily from oxygen isotope and Mg/Ca records generated from deep-sea cores. Here…
Middle Eocene-late Oligocene climate variability: calcareous nannofossil response at Kerguelen Plateau, Site 748
- G. Villa, C. Fioroni, Laura Pea, S. Bohaty, D. Persico
- Geography, Environmental Science
- 1 October 2008
The Palaeocene–Eocene carbon isotope excursion: constraints from individual shell planktonic foraminifer records
- J. Zachos, S. Bohaty, C. John, H. McCarren, D. Kelly, Tina M J Nielsen
- Environmental Science, GeographyPhilosophical Transactions of the Royal Society A…
- 15 July 2007
TLDR
North American continental margin records of the Paleocene‐Eocene thermal maximum: Implications for global carbon and hydrological cycling
- C. John, S. Bohaty, T. Bralower
- Environmental Science, Geography
- 1 June 2008
The impacts of the Paleocene-Eocene thermal maximum (PETM) (?55 Ma), one of the most rapid and extreme warming events in Earth history, are well characterized in open marine and terrestrial…
...
...