Abstract
The sediments that now comprise the Messel shale1 accumulated 47 ± 2 million years ago in anaerobic waters at the bottom of a lake2. Subsequent depths of burial have not exceeded 300 m, nor has the temperature of the shale exceeded 40 °C3. Contents of organic carbon reach 25%, and preservation of molecular structures has been excellent4,5. Sixteen different geoporphyrins, including three derived from bacteriochlorophyHs of the d series and thus indicative of the existence in the lake of an anaerobic photic zone, have been isolated and identified6–8. Here, we show that the carbon isotopic compositions of these and other biomarkers allow identification of specific sources for some materials and reconstruction of carbon flows within the lake and its sediments. The 13C content of organic matter synthesized by lacustrine primary producers can be estimated from the observed 13C content of the geoporphyrins derived from their chlorophylls. Total organic material in the shale is depleted in 13C by six parts per thousand relative to that input. This difference cannot be explained by selective loss of components enriched in 13C, nor, as shown by isotopic compositions of other biomarkers, by inputs from land plants surrounding the lake or from methanogenic bacteria.
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References
Matthes, G. Mém. Bur. Rech. geol. Minières 58, 327–337 (1968).
Von Koenigswald, W. Geol. Jb. Hessen 108, 23–38 (1980) and references therein.
Arpino, P., Albrecht, P. & Ourisson, G. in Advances in Organic Geochemistry 1971 (eds von Gaertner, H. R. & Wehner, H.) 173–187 (Pergamon, Oxford, 1972).
Chappe, B., Michaelis, W. & Albrecht, P. in Advances in Organic Geochemistry 1979 (eds Douglas, A. G. & Maxwell, J. R.) 265–274 (Pergamon, Oxford, 1981).
Dastillung, M., Albrecht, P. & Ourisson, G. J. chem. Research (S) 166–167; (M) 2325–2352 (1980).
Ocampo, R., Callot, H. J., Albrecht, P. & Kintzinger, J. P. Tetrahedron Lett. 25, 2589–2592 (1984).
Ocampo, R., Callot, H. J. & Albrecht, P. J. Chem. Soc. Chem. Commun. 198–200 (1985).
Ocampo, R., Callot, H. J. & Albrecht, P. J. Chem. Soc. Chem. Commun. 200–201 (1985).
Chicarelli, M. I. & Maxwell, J. R. Tetrahedron Lett. 25, 4701–4704 (1984).
Jeffrey, S. W. in Primary Productivity in the Sea (ed. Falkowski, P. G.) 33–58 (Plenum, New York, 1980).
Mattern, G., Albrecht, P. & Ourisson, G. J. chem. Soc. Chem. Commun. 1570–1571 (1970).
Robinson, N., Eglinton, G., Brassel, S. C. & Cranwell, P. A. Nature 308, 439–441 (1984).
Jackson, A. H. in Chemistry and Biochemistry of Plant Pigments, 2nd edn. Vol. 1 (ed. Goodwin, T. W.) 1–44 (Academic, London, 1976).
Wolff, G. A., Murray, M., Maxwell, J. A., Hunter, B. K. & Sanders, J. K. M. J. chem. Soc. Chem. Commun. 922–924 (1983).
Fookes, C. J. R. J. Chem. Soc. Chem. Commun. 1474–1476 (1983).
Karuso, P. et al. Tetrahedron Lett. 27, 2177–2178 (1986).
Park, R. & Dunning, H. N. Geochim. Cosmochim. Acta 22, 99–105 (1961).
Albrecht, P. & Ourisson, G. Science 163, 1192–1193 (1969).
Spyckerelle, C., Greiner, A. C., Albrecht, P. & Ourisson, G. J. chem. Research (S) 330–331; (M) 3746–3777 (1977).
Corbet, B., Albrecht, P. & Ourisson, G. J. Am. chem. Soc. 102, 1171–1173 (1980).
Redding, C. E., Schoell, M., Monin, J. C. & Durand, B. in Advances in Organic Geochemistry 1979 (eds Maxwell, J. R. & Douglas, A. G.) 711–723 (Pergamon, Oxford, 1980).
Potter, F. W. Jr Paleontographica 157, 44–96 (1976).
Sanger, J. E. Ecology 52, 1075–1089 (1971).
Tissot, B. P. & Welte, D. H. Petroleum Formation and Occurrence, 2nd edn 257 (Springer, Berlin, 1984).
DeNiro, J. & Epstein, S. Geochim. cosmochim. Acta 42, 495–506 (1984).
Chappe, B., Albrecht, P. & Michaelis, W. Science 217, 65–66 (1982).
Michaelis, W. & Albrecht, P. Naturwissenschaften 66, 420–422 (1979).
Irwin, H., Curtis, C. & Coleman, M. Nature 269, 209–213 (1977).
Fuchs, G., Thauer, R., Ziegler, H. & Stichler, W. Arch. Microbiol. 120, 135–139 (1979).
Belyaev, S. S. et al. Appl. Environ. Microbiol. 45, 691–697 (1983).
Whiticar, M. J., Faber, E. & Schoelle, M. Geochim. cosmochim. Acta 50, 693–709 (1986).
Hussler, G. et al. Tetrahedron Lett. 25, 1179–1182 (1984).
Wedeking, K. W., Hayes, J. M. & Matzigkeit, U. in Earth's Earliest Biosphere: Its Origin and Evolution (ed. Schopf, J. W.) 428–441 (Princeton, New Jersey, 1983).
Craig, H. Geochim. cosmochim. Acta 12, 133–149 (1957).
Tornabene, T. G. & Langworthy, T. A. Science 203, 51–53 (1978).
Panganamala, R. V., Sievert, C. F. & Cornwell, D. G. Chem. Phys. Lipids 7, 336–344 (1971).
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Hayes, J., Takigiku, R., Ocampo, R. et al. Isotopic compositions and probable origins of organic molecules in the Eocene Messel shale. Nature 329, 48–51 (1987). https://doi.org/10.1038/329048a0
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DOI: https://doi.org/10.1038/329048a0
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