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      Exceptional preservation of Palaeozoic steroids in a diagenetic continuum

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      a , 1 , b , 1 , c , 1 , 2
      Scientific Reports
      Nature Publishing Group

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          Abstract

          The occurrence of intact sterols has been restricted to immature Cretaceous (~125 Ma) sediments with one report from the Late Jurassic (~165 Ma). Here we report the oldest occurrence of intact sterols in a Crustacean fossil preserved for ca. 380 Ma within a Devonian concretion. The exceptional preservation of the biomass is attributed to microbially induced carbonate encapsulation, preventing full decomposition and transformation thus extending sterol occurrences in the geosphere by 250 Ma. A suite of diagenetic transformation products of sterols was also identified in the concretion, demonstrating the remarkable coexistence of biomolecules and geomolecules in the same sample. Most importantly the original biolipids were found to be the most abundant steroids in the sample. We attribute the coexistence of steroids in a diagenetic continuum -ranging from stenols to triaromatic steroids- to microbially mediated eogenetic processes.

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          A review of sterol markers for marine and terrigenous organic matter

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            Chemical fossils: the geological fate of steroids.

            Steroids are used to illustrate some of the significant advances that have been made in recent years in understanding the biological origin and geological fate of the organic compounds in sediments. The precursor sterols are transformed, initially by microbial activity and later by physicochemical constraints, into thermodynamically more stable saturated and aromatic hydrocarbons in mature sediments and petroleums. The steps in this transformation result in a complex web linking biogenesis, diagenesis, and catagenesis. Indeed, the complexity and variety of biological lipids such as the steroids are evidently matched in the corresponding geolipids. The extent of preservation of the biochemical imprint in the structures and stereochemistry of these geolipids, even over hundreds of millions of years, is startling, as is the systematic and sequential nature of the geochemical changes they evidently undergo. This new understanding of molecular organic geochemistry has applications in petroleum geochemistry, where biological marker compounds are valuable in the assessment of sediment maturity and in correlation work.
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              Variations in the sterane carbon number distributions of marine source rock derived crude oils through geological time

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                Author and article information

                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group
                2045-2322
                26 September 2013
                2013
                : 3
                : 2768
                Affiliations
                [1 ]WA Organic and Isotope Geochemistry Centre, Department of Chemistry, Curtin University , Perth, Western Australia 6845, Australia
                [2 ]Institute of Geoscience, Christian Albrechts University , 24118 Kiel, Germany
                Author notes
                Article
                srep02768
                10.1038/srep02768
                3783881
                24067597
                03bec8b1-7814-495b-9e19-e0057bafe19e
                Copyright © 2013, Macmillan Publishers Limited. All rights reserved

                This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/

                History
                : 10 April 2013
                : 06 September 2013
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