What caused the long duration of the Paleocene-Eocene Thermal Maximum?

Long-term legacy of massive carbon input to the Earth system: Anthropocene versus Eocene

(2013) R. E. Zeebe et al.   PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES

Seawater oxygenation during the Paleocene-Eocene Thermal Maximum

(2012) A. J. Dickson et al.   GEOLOGY

Reply to 'Constraints on hyperthermals'

(2012) Ying Cui et al.   Nature Geoscience

Constraints on hyperthermals

(2012) Appy Sluijs et al.   Nature Geoscience

Modeling sulfate reduction in methane hydrate-bearing continental margin sediments: Does a sulfate-methane transition require anaerobic oxidation of methane?

(2011) A. Malinverno et al.   GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS

Constraints on the numerical age of the Paleocene-Eocene boundary

(2011) Adam J. Charles et al.   GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS

Methane and environmental change during the Paleocene-Eocene thermal maximum (PETM): Modeling the PETM onset as a two-stage event

(2011) David A. Carozza et al.   GEOPHYSICAL RESEARCH LETTERS

Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum

(2011) Ying Cui et al.   Nature Geoscience

Comment on "A Persistent Oxygen Anomaly Reveals the Fate of Spilled Methane in the Deep Gulf of Mexico"

(2011) S. B. Joye et al.   SCIENCE

A Persistent Oxygen Anomaly Reveals the Fate of Spilled Methane in the Deep Gulf of Mexico

(2011) J. D. Kessler et al.   SCIENCE

An extraterrestrial 3He-based timescale for the Paleocene–Eocene thermal maximum (PETM) from Walvis Ridge, IODP Site 1266

(2010) B.H. Murphy et al.   GEOCHIMICA ET COSMOCHIMICA ACTA

Paleoredox changes across the Paleocene-Eocene thermal maximum, Walvis Ridge (ODP Sites 1262, 1263, and 1266): Evidence from Mn and U enrichment factors

(2010) Cecily O. J. Chun et al.   PALEOCEANOGRAPHY

The impact of remineralization depth on the air–sea carbon balance

(2009) Eun Young Kwon et al.   Nature Geoscience

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

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

Ocean methane hydrates as a slow tipping point in the global carbon cycle

(2008) D. Archer et al.   PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA