-->>denn nicht ein klitzekleines Fitzelchen einer konkreten, dinglichen Analyse von Erdöl auf biologische Bestandteile ist beispielsweise dort zu finden.
>Das allereinfachste also, was man annehmen sollte, konkret aufgezeigt zu bekommen FEHLT!
>Bitte, bitte stelle einer eine solche KONKRETE Untersuchung von Proben mit allen dokumentierten Daten zu Herkunft, Erlangung, Analysemethodik und den KONKRETEN Ergebnissen hier ins Netz, oder bitte, bitte wenigstens einen Link dahin!
Hallo Maus,
Zu Biomarkern (also Stoffen, die nur an der Oberfläche gebildet worden sein können und die in Erdöl gefunden werden), bitte sehr, die Fernleihe in deiner Bibliothek wird sich freuen:
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Carlson, R. M. K., S. C. Teerman, J. M. Moldowan, S. R. Jacobson, E. I. Chan, K. S. Dorrough, W. C. Seetoo, and B. Mertani, (1993) High temperature gas chromatography of high-wax oils: Indonesian Petroleum Association, 22nd Annual Convention Proceedings, Jakarta, Indonesia, p. 483-507.
Douglas, A. G., J. S. S. Damste, M. G. Fowler, T. I. Eglinton, and J. W. de Leeuw (1991) Unique distributions of hydrocarbons and sulphur compounds released by flash pyrolysis from the fossilized alga Gloecapsomorpha prisca, a major constituent in one of four Ordovician kerogens: Geochimica et Cosmochimica Acta, v. 55, p. 275-291.
Fan Pu, J. D. King, and G. E. Claypool (1988) Characteristics of biomarker compounds in Chinese crude oils, in R. K. Kumar, P. Dwivedi, V. Banerjie, and V. Gubta, eds., Petroleum Geochemistry and Exploration in the Afro-Asian Region: proceedings of the first International Conference on Petroleum Geochemistry and Exploration in the Afro-Asian Region, Dehradun, 25-27 November 1985: Rotterdam, Balkema, p. 197-202.
Fowler, M. G. (1992) The influence of Gloeocapsomorpha prisca on the organic geochemistry of oils and organic rich rocks of Late Ordovician age from Canada, in M. Schidlowski, and et al., eds., Early Organic Evolution: Implications for Mineral and Energy Resources: Berlin, Springer-Verlag, p.336-356.
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ten Haven, H. L., J. W. de Leeuw, J. Rullkötter, and J. S. Sinninghe Damste (1987) Restricted utility of the pristane/phytane ratio as a paleoenvironmental indicator: Nature, v. 330, p. 641-643.
ten Haven, H. L., J. W. de Leeuw, J. S. Sinninghe Damste, P. A. Schenck, S. E. Palmer, and J. E. Zumberge (1988) Application of biological markers in the recognition of palaeo-hypersaline environments, in K. Kelts, A. Fleet, and M. Talbot, eds., Lacustrine Petroleum Source Rocks: Special Publication, v. 40: Blackwell, Geological Society, p. 123-130.
Holba, A. G., L. I. P. Dzou, W. D. Masterson, W. B. Huges, B. J. Huizinga, M. S. Singletary, J. M. Moldowan, M. R. Mello, and E. Tegelaar, (1998A) Application of 24-norcholestanes for constraining source age of petroleum: Organic Geochemistry, v. 29, p. 1269-1283.
Holba, A. G., E. Tegelaar, B. J. Huizinga, J. M. Moldowan, M. S. Singletary, M. A. McCaffrey, and L. I. Dzou (1998B) 24-norcholestanes as age-sensitive molecular fossils: Geology, v. 26, p. 783-786.
Holba, A. G., E. Tegelaar, L. Ellis, M. S. Singletary, and P. Albrecht (2000) Tetracyclic polyprenoids: Indicators of freshwater (lacustrine) algal input: Geology, v. 28, p. 251-254.
Hsieh, M., and R. P. Philp (2001) Ubiquitous occurrence of high molecular weight hydrocarbons in crude oils: Organic Geochemistry, v. 32, p. 955-966.
Huang, W.-Y., and W. G. Meinschein (1979) Sterols as ecological indicators: Geochimica et Cosmochimica Acta, v. 43, p. 739-745.
Hughes, W. B. (1984) Use of thiophenic organosulphur compounds in characterizing crude oils derived from carbonate versus siliciclastic sources, in J. G. Palacas, ed., Petroleum Geochemistry and Source Rock Potential of Carbonate Rocks, AAPG, Studies in Geology 18, p. 181-196.
Hughes, W. B., A. G. Holba, and L. I. P. Dzou (1995) The ratios of dibenzothiophene to phenanthrene and pristane to phytane as indicators of depositional environment and lithology of petroleum source rocks: Geochimica et Cosmochimica Acta, v. 59, p. 3581-3598.
Jiang Zusheng, and M. G. Fowler (1986), Carotenoid-derived alkanes in oils from northwestern China, in D. Leythaeuser, and J. Rullkötter, eds., Advances in Organic Geochemistry 1985, Organic Geochemistry, v. 10, Pergamon, p. 831-839.
Koopmans, M. P., H. M. E. Van Kaam-Peters, S. Schouten, J. W. De Leeuw, J. S. Sinninghe Damste, J. Koster, F. Kenig, and W. A. Hartgers (1996) Diagenetic and Catagenetic Products of Isorenieratene: Molecular Indicators For Photic Zone Anoxia: Geochimica et Cosmochimica Acta, v. 60, p. 4467-4496.
Lewan, M. D. (1984) Factors controlling the proportionality of vanadium to nickel in crude oils: Geochimica et Cosmochimica Acta, v. 48, p. 2231-2238.
McCaffrey M. A., Dahl J., Sundararaman P., Moldowan J. M. and Schoell M. (1994A) Source rock quality determination from oil biomarkers II. - A case study using Tertiary-reservoired Beaufort Sea oils. American Association of Petroleum Geologists Bulletin 78 (10), 1527-1540.
McCaffrey, M. A., J. M. Moldowan, P. A. Lipton, R. E. Summons, K. E. Peters, A. Jeganathan, and D. S. Watt (1994B) Paleoenvironmental implications of novel C30 steranes in Precambrian to Cenozoic age petroleum and bitumen: Geochimica et Cosmochimica Acta, v. 58, p. 529-532.
Metzger P. and Largeau C. (1999) Chemicals of Botryococcus braunii. In Chemicals from Microalgae (ed. Z. Cohen), pp. 205-260. Taylor & Francis.
Moldowan, J. M., W. K. Seifert, and E. J. Gallegos (1985) Relationship between petroleum composition and depositional environment of petroleum source rocks: AAPG Bulletin, v. 69, p. 1255-1268.
Moldowan J. M, Fago F. J., Lee C. Y., Jacobson S. R., Watt D.S., Slougui N.-E., Jeganathan A., Young D. C. (1990) Sedimentary 24-n-propylcholestanes, molecular fossils diagnostic of marine algae. Science, 247, 309-312.
Moldowan, J. M., C. Y. Lee, P. Sundararaman, R. Salvatori, A. Alajbeg, B. Gjukic, G. J. Demaison, N. E. Slougui, and D. S. Watt (1992) Source correlation and maturity assessment of select oils and rocks from the Central Adriatic basin (Italy and Yugoslavia), in J. M. Moldowan, P. Albrecht, and R. P. Philp, eds., Biological Markers in Sediments and Petroleum: Englewood Cliffs, New Jersey, Prentice Hall, p. 370-401.
Moldowan, J. M., and M. A. McCaffrey (1995) A novel microbial hydrocarbon degradation pathway revealed by hopane demethylation in a petroleum reservoir: Geochimica et Cosmochimica Acta, v. 59, p. 1891-1894.
Moldowan, J. M., J. Dahl, M. A. McCaffrey, W. J. Smith, and J. C. Fetzer (1995A) The application of biological marker technology to bioremediation of refinery by-products: Energy & Fuels, v. 9, p. 155-162.
Peters, K. E., and J. M. Moldowan (1991) Effects of source, thermal maturity and biodegradation on the distribution and isomerization of homohopanes in petroleum: Organic Geochemistry, v. 17, p. 47-61.
Subroto, E. A., R. Alexander, and R. I. Kagi (1991) 30-Norhopanes: their occurrence in sediments and crude oils: Chemical Geology, v. 93, p. 179-192.
Summons, R. E., and T. G. Powell (1987) Identification of arylisoprenoids in a source rock and crude oils: Biological markers for the green sulfur bacteria: Geochimica et Cosmochimica Acta, v. 51, p. 557-566.
Summons, R. E., L. L. Jahnke, J. M. Hope, and G. A. Logan (1999) 2-Methylhopanoids as biomarkers for cyanobacterial oxygenic photosynthesis: Nature, v. 400, p. 554-557.
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Du liest dir aber wenigstens zwei dieser Artikel durch, bevor wir hier wieder über abiotisches Ã-l weiterphantasieren, ja
Übrigens: mit Biomarkern lässt sich verglichen mit Abiotischen Theorien in der Ã-lindustrie auch nachweislich sehr gut Geld verdienen:
http://oiltracers.com/home.asp
ciao,
Sorrento
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