Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary?

By K. Bice, Jochem Marotzke. 2002

140 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/06bf12c75afa47d2cd0d486a3f3466cfcebc0ca5

How researchers see this paper

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

1. J. Higgins
2. D. Schrag
3. R. Norris
4. K. Bice

Citations in the corpus

• Possible atmospheric CO2 extremes of the Middle Cretaceous (late Albian-Turonian) (2002, background): “Because high latitude upper ocean waters are quite warm, it is not necessary to invoke low latitude deep convection in order to reproduce bottom temperatures significantly warmer than modern [Bice and Marotzke, 2001].”
• Beyond methane: Towards a theory for the Paleocene-Eocene Thermal Maximum (2006, background): “In both shallow and deep marine records [2,26], the isotopic excursion is associated with a large increase in CaCO3 dissolution [4,18,27].”