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Updated: Jul 6, 2026

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
Published on: October 21, 2016
Biomarker evidence for a major preservation pathway of sedimentary organic carbon
Y Hebting1, P Schaeffer, A Behrens
1Laboratoire de Géochimie Bioorganique, Unité Mixte de Recherche 7509 du CNRS, Université Louis Pasteur, Ecole de Chimie, Polymères, Matériaux de Strasbourg, 25 rue Becquerel, 67200 Strasbourg, France.
Abstract:
Hydrogenation processes leading from biomolecules to fossil biomarkers in anoxic sediments are crucial for the preservation of organic matter. However, these processes are still poorly understood. The present identification of several reduced carotenoids in recent sediments attests that these processes operate at the earliest stages of diagenesis without structural or stereochemical specificity, implying a nonbiological reduction pathway. Sulfur species (e.g., H2S) are the hydrogen donors involved in such reduction, as demonstrated with laboratory experiments. These reactions allow the preservation of abundant organic carbon in the rock record.
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