What is the meaning of hydrogen-to-carbon ratio determined in Archean organic matter?. (August 2018)

• Record Type: Journal Article
• Authors: Delarue, Frédéric; Derenne, Sylvie; Sugitani, Kenichiro; Baudin, François; Westall, Frances; Kremer, Barbara; Tartèse, Romain; Gonzalez, Adriana; Robert, François
• Is Part Of: Organic geochemistry. Volume 122(2018)
• Page Start: 140
• Page End: 146
• Publication Date: 2018-08
• Subjects: Bitumen -- Carbonization -- Early life -- Kerogen -- NanoSIMS -- Precambrian -- Raman -- Rock-Eval pyrolysis; Organic geochemistry -- Periodicals; Biogeochemistry -- Periodicals; Géochimie organique -- Périodiques; 553.205
• DOI: 10.1016/j.orggeochem.2018.05.013
• Languages: English
• ISSNs: 0146-6380

Abstract

Highlights: Archean organic matter can be enriched in H at odds with their thermal history. H does not solely originate from the thermal cleavage of the kerogen matrix. Cautions are required when studying the molecular content of Archean kerogens. Abstract: The search for hydrocarbon molecular biomarkers in Archean metasediments is of prime importance for deciphering the early evolution of life. Suitable criteria are required to identify promising targets for further molecular biomarkers. Possible criteria include the Hydrogen-to-Carbon (H/C) atomic ratio used as a proxy of the aliphatic content of the kerogen matrix. However, H/C ratio values exhibit large variation in Archean kerogens and their significance remains poorly understood. In this study, we thus investigate the significance of the H/C ratios of Archean kerogens by combining elemental analyses, Nanoscale Secondary Ion Mass Spectrometry (NanoSIMS), Rock-Eval pyrolysis and Raman spectroscopy. First, NanoSIMS investigations show the H/C ratio of kerogen can be compromised by residual minerals. In addition, Rock-Eval pyrolysis underlines the fact that thermal cracking of Archean kerogens does not just release hydrocarbon covalently linked to the macromolecular network but also a complex mixture of organic pools distinguished by their thermal maturity. Therefore, the H/C ratio alone cannot be used to probe the preservation of aliphatic compounds bound to kerogen since it can be biased by the presence of (i) residual bitumen, as well as (ii) refractory organic matter in secondary hydrothermal veins whose syngenecity is debatable. Rock-Eval pyrolysis then provides a useful and complementary method to check the significance of H/C atomic ratio as a proxy for hydrocarbon preservation in Archean kerogens.