Beyond methane: Towards a theory for the Paleocene-Eocene Thermal Maximum

By J. Higgins, D. Schrag. 2006

323 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Environmental Chemistry

View Paper: https://www.semanticscholar.org/paper/99ab60e3f4b5ed15bfb5c7f991ad77cac82782ed

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. C. Labandeira
2. N. Stern
3. J. Blois
4. Elizabeth A. Hadly
5. A. Barnosky

In Ecology

1. J. Zachos
2. C. Labandeira
3. A. Barnosky

In Environmental Chemistry

1. N. Stern
2. J. Blois
3. Elizabeth A. Hadly

Citations in the corpus

• Fossil insect folivory tracks paleotemperature for six million years (2010, background): “It is marked by a negative carbon isotope excursion in both marine and terrestrial reservoirs, consistent with the release of a large amount of 13C-depleted carbon to the atmosphere and ocean (Dickens et al. 1995, Zachos et al. 2005, Higgins and Schrag 2006, Pagani et al. 2006).”
• Target atmospheric CO2: Where should humanity aim? (2008, unknown): “H owever, in g eneral the s ensitivities inferred from the Cenozoic and Phanerozoic [56, 57, 58] a gree well with our analysis, if we account for the ways in which sensitivity is defined and the periods emphasized in each empirical derivation (Table S1 ).”
• An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics (2008, background): “Another such source is the oxidation of organic matter in terrestrial environment”