CO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilization

Modelling the oxygen isotope distribution of ancient seawater using a coupled ocean–atmosphere GCM: Implications for reconstructing early Eocene climate

(2010) Julia Tindall et al.   EARTH AND PLANETARY SCIENCE LETTERS

A Palaeogene perspective on climate sensitivity and methane hydrate instability

(2010) T. Dunkley Jones et al.   PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES

Fossil soils constrain ancient climate sensitivity

(2010) D. L. Royer   PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA

Climate Response at the Paleocene–Eocene Thermal Maximum to Greenhouse Gas Forcing—A Model Study with CCSM3

(2009) A. Winguth et al.   JOURNAL OF CLIMATE

Evidence for middle Eocene Arctic sea ice from diatoms and ice-rafted debris

(2009) Catherine E. Stickley et al.   NATURE

Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming

(2009) Richard E. Zeebe et al.   Nature Geoscience

Global Cooling During the Eocene-Oligocene Climate Transition

(2009) Z. Liu et al.   SCIENCE

Sedimentary response to Paleocene-Eocene Thermal Maximum carbon release: A model-data comparison

(2008) K. Panchuk et al.   GEOLOGY

An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics

(2008) James C. Zachos et al.   NATURE