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Hemoglobin-derived porphyrins preserved in a Middle Eocene blood-engorged mosquitoHeart fossilization is possible and informs the evolution of cardiac outflow tract in vertebratesThe evolutionary convergence of mid-Mesozoic lacewings and Cenozoic butterfliesExtreme (13)C depletion of carbonates formed during oxidation of biogenic methane in fractured graniteFungal colonization of an Ordovician impact-induced hydrothermal system.A reduced organic carbon component in martian basalts.Comet 67P/Churyumov-Gerasimenko sheds dust coat accumulated over the past four years.High-molecular-weight organic matter in the particles of comet 67P/Churyumov-Gerasimenko.Mechanical and electrostatic experiments with dust particles collected in the inner coma of comet 67P by COSIMA onboard Rosetta.Anaerobic consortia of fungi and sulfate reducing bacteria in deep granite fractures.Comparison of prototype and laboratory experiments on MOMA GCMS: results from the AMASE11 campaign.Analysis of hopanes and steranes in single oil-bearing fluid inclusions using time-of-flight secondary ion mass spectrometry (ToF-SIMS).The Mars Organic Molecule Analyzer (MOMA) Instrument: Characterization of Organic Material in Martian Sediments.Molecular Insights into Covalently Stained Carious Dentine Using Solid-State NMR and ToF-SIMS.COSIMA data analysis using multivariate techniquesOrganic synthesis on Mars by electrochemical reduction of COIntricate tunnels in garnets from soils and river sediments in Thailand - Possible endolithic microboringsUV irradiation of biomarkers adsorbed on minerals under Martian-like conditions: Hints for life detection on MarsMOMA: the challenge to search for organics and biosignatures on Mars
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25222014900
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0000-0002-4975-6074