Stable carbon isotope values of TOC and biphytanes for three PETM sections in Denmark and for the ETM2 section of iODP Site 302-M0004A from the Lomonosov Ridge, supplement to: Schoon, Petra L; Heilmann-Clausen, Claus; Pagh Schultz, Bo; Sluijs, Appy; Sinninghe Damsté, Jaap S; Schouten, Stefan (2013): Recognition of Early Eocene global carbon isotope excursions using lipids of marine Thaumarchaeota. Earth and Planetary Science Letters, 373, 160-168

Petra L Schoon, Claus Heilmann-Clausen, Bo Pagh Schultz, Appy Sluijs, Jaap S Sinninghe Damsté & Stefan Schouten
The Paleocene-Eocene Thermal Maximum (PETM; ~56 Ma) and Eocene Thermal Maximum 2 (ETM2; ~53 Ma) are geological short (<200,000 years) episodes of extreme global warming and environmental change. Both the PETM and ETM2 are associated with the injection of 13C-depleted carbon into the ocean-atmosphere system as revealed through a globally recognized carbon isotope excursion (CIE) and massive dissolution of deep sea carbonate. However, the magnitude of these CIEs vary with the type of fossil matter,...
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