Abstract
Most Archean organic matter has been subjected to a high degree of alteration by thermal processes, often involving very high temperatures. The original morphology of possible organisms and their biochemical make up have been altered to such an extent that in many cases they are unidentifiable. There is, therefore, great difficulty and often uncertainty when trying to identify or compare Archean microorganisms with modern day analogues. On the other hand microbial populations have changed little over the geological time scale and may be the only organic remains to be positively identified. Their small size may enable them to be spared destruction when squeezed into microcavities in the organic and mineral matrix. Microorganisms such as bacteria may also be preserved due to incorporated or substituted metals, as documented in earlier studies (Degens and Ittekkot, 1982).
‘As happens in the case of an optical microscope, which is incapable of revealing the ultimate structure of matter to the observer, we can only choose between various degrees of enlargement; each one reveals a level of organization which has no more than a relative truth and, while it lasts, excludes the perception of other levels.’
Claude Levi-Strauss
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Barker, C.E. (1991) Implications for organic maturation studies of evidence for a geologically rapid increase and stabilization of vitrinite reflectance at peak temperature: Cerro Pieto geothermal system. Am. Assoc. Petrol. Geol. Bull. 75: 1852–1863.
Bauer, M.E., Hayes, J.M., Studley, S.A. and Walter, M.R. (1985) Millimeter-scale variations of stable isotope abundances in carbonates from banded iron-formations in the Hamersley Group of Western Australia. Econ. Geol. 80: 270–282.
Becker, L, Poreda, R.J. and Bada, J.L. (1996) Extraterrestrial helium trapped in fullerenes in the Sudbury impact structure. Science. 272: 249–252.
Beukes, N.J. and Klein, C. (1992) Model for iron-formation deposition. In: J.W. Schopf and C. Klein (eds). The Proterozoic Biosphere, Cambridge University Press, Cambridge: 147–151.
Breger, I.A., Zubovic, P., Chandler, J.C. and Clarke, R.S. (1972) Occurrence and significance of formaldehyde in Allende carbonaceous chondrite. Nature. 236: 155–158.
Buick, R. and Dunlop, J.S.R. (1990) Evaporitic sediments of Early Archaen age from the Warrawoona Group, North Pole, Western Australia. Sedimentology. 37: 247–277.
Buseck, P.R., Bo-Jun, H. and Miner, B. (1988) Structural order and disorder in Precambrian kerogens. Org . Geochem. 12: 221–234.
Cheney, E.S. (1996) Sequence stratigraphy and plate tectonic significance of the Transvaal succession of southern Africa and its equivalent in Western Australia. Precambrian Res. 79: 3–24.
Daniel, R., Morgan, H. and Hudson. J.A. (1987) Superbugs spring from hot water. New Sci. 19 February: 36–40.
Deamer, D.W., Harang-Mahon, E. and Bosco, G. (1994) Self-assembly and function of primitive membrane structures: In: S. Bengston (ed.) Early Life on Earth. Nobel Symposium No. 84. Columbia University Press, New York.
Degens, E.T. and Ittekkot, V. (1982) In-situ metal-staining of biological membranes in sediments. Nature. 298: 262–264.
Ewers, W.E. and Morris, R.C. (1981) Studies of the Dales Gorge Member of the Brockman Iron Formation, Western Australia. Econ. Geol. 76: 1929–1953.
Ferris, F.G., Beveridge, T.J. and Fyfe, W.S. (1986) Iron—silica crystallite nucleation by bacteria in a geothermal sediment. Nature. 320: 609–615.
Gieskes, J.M., Simoneit, B.R.T., Brown, T., Shaw T., Wang, Y-Ch. and Magrenhein, A. (1988) Hydrothermal fluids and petroleum in surface sediments of Guaymas Basin, Gulf of California: A case study. Can. Mineral. 26: 589–602.
Gize, A.P. (1986) The development of a thermal mesophase in bitumen from high temperature ore deposits. In: W.E. Dean (ed.) Organics and Ore Deposits. Proceedings Denver Region Exploration Geological Society Symposium. Denver Region Exploration Geologists Society: 137–150.
Glikson, A.Y. (1993) Asteroids and early Precambrian crustal evolution. Earth-Sci. Rev. 35: 285–319. Glikson, A.Y. (1996) Mega-impacts and mantle melting episodes: tests of possible correlations. Aust. Geol. Org. (AGSO) J. 16: 587–608.
Glikson, M. (1984) 3.5 billion year-old bacteria: earliest life forms? reported by Monastersky in: Science News. Washington; December issue.
Glikson, M. and Taylor, G.H. (1986) Cyanobacterial mats; major contributors to the organic matter in Toolebuc Formation oil shales. J. Geolog. Soc. Aust. Sp. Publ. 12: 276–286.
Glover, J.E. (1992) Sediments of Early Archaen coastal plains: a possible environment for the origin of life. Precambrian Res. 56: 159–166.
Hayes, J.M., Kaplan, I.R. and Wedeking, K.W. (1983) Precambrian organic geochemistry, preservation of the record. In J.W. Schopf (ed.) Earth’s Earliest Biosphere: 93–134. Princeton University Press.
Henley, R.W. (1996) Chemical and physical context for life in terrestrial hydrothermal systems: chemical reactions for the early development of life and hydrothermal ecosystems. Ciba Found. Symp. 202: 61–82.
Horneck, G. (1993) Responses of Bacillus subtilis spores to space environment: Results from experiments in space. Origins Life Evol. Biosphere. 23: 37–52.
Jeffrey, D. (1985) Nat. Geogr. Mag. 168: 182.
Juniper, S.K. and Fouquet, Y. (1988) Filamentous iron-silica deposits from modern and ancient hydrothermal sites. Can. Mineral. 26: 859–869.
Knoll, A.H. and Walter, M.R. (1996) The limits of palaeontological information: finding the gold among the dross. In: Evolution of Hydrothermal Ecosystems on Earth (And Mars?): 198–220. Wiley liuya Sons.
Lowe, D.R. (1980) Stromatolites 3400-Myr old from the Archean of Western Australia. Nature. 284: 441–443.
Lowe, D.R., Byerly, G.R., Asaro, F. and Kyte, F.J. (1989) Geological and geochemical record of 3400-million year-old terrestrial meteorite impacts. Science. 245: 959–962.
Lawless, J.G. and Boynton, C.D. (1973) Thermal synthesis of amino acids from a simulated primitive atmosphere. Nature. 243: 405–407.
Mackinnon, I.D.R. and Rietmeijer, F.M. (1987) Mineralogy of chondritic interplanetary dust particles. Rev. Geophys. 25: 1527–1553.
Mann, S., Hannington, J.P. and Williams, R.J.P. (1986) Phospholipid vesicles as a model system for biomineralization. Nature. 324: 565–567.
Margulis, L., Dyer Grosovsky, B.D., Stolz, J.F., Gong-Collins, E.J., Lenk, S., Read, D. and Lopez-Cortes, A. (1983): Distinctive microbial structures and the pre-phanerozoic fossil record. Precambrian Research, 20: 443–447.
McKay, D.S., Gibson, E.K., Thomas-Keprta, K.L., Hajatollah, V. et al. (1996) Search for past life on Mars: possible relic biogenic activity in Martian meteorite ALH84001. Science. 273: 924–930.
Morris, R.C. and Horwitz, R.C. (1983) The origin of the iron-formation-rich Hamersley Group of Western Australia-deposition on a platform. Precambrian Res. 21: 273–297.
Oberlin, A., Boulmier, J.L. and Villey, M. (1980) Electron microscopic study of kerogen microtexture. Selected criteria for determining the evolution path and evolution stage of kerogen. In: B. Durand (ed.) Kerogen. Editions Technip, Paris, pp. 1919–241.
Ourisson, G. (1994) Biomarkers in the Proterozoic record. In: Bengtson (ed.) Early Life on Earth. Nobel Symposium No. 84. Columbia U.P., New York, pp. 259–265.
Pardue, J.W., Scalan, R.S., Van Baalen, C. and Parker, P.L. (1976) Maximum carbon isotope fractionation in photosynthesis by blue-green algae and a green alga. Geochim. Cosmochim. Acta. 40: 309–312.
Philp, R.P. (1985) GC-MS of North Pole kerogen, unpublished data.
Robert, P. (1988) Organic Metamorphism and Geothermal History. Elf-Aquitaine and D. Reidel.
Nature of organic matter in the early Proterozoic, earliest life forms and metal associations
Schopf, J.W. and Walter, M.R. (1983) Archean microfossils: new evidence of ancient microbes. In: J.W. Schopf (ed.) Earth’s Earliest Biosphere. Princeton University Press, pp. 214–239.
Shimoyama, A., Harada, K. and Yanai, K. (1985) Amino acids from outer space. Reported in New Sci. 19/26, December 1985.
Simoneit, B.R.T. (1985) Hydrothermal petroleum: genesis, migration and deposition in Guaymas Basin, Gulf of California. Can. J. Earth Sci. 22: 1919–1929.
Simoneit, B.R.T. (1988) Petroleum generation in submarine hydrothermal systems: an update. Can. Mineral. 26: 827-–840.
Simonson, B.M. (1992) Geological evidence for a strewn field of impact spherules in the early Precambrian Hamersley Basin of Western Australia. Geol. Soc. Am. Bull. 104: 829–839.
Smith, P.P.K. and Buseck, P.R. (1981) Graphitic carbon in the Allende meteorite: A microstructural study. Science. 212: 322–324.
Stach, E., Mackowsky, M. Th., Teichmüller, M., Taylor, G.H., Chandra, D. and Teichmüller, R. 1975: Coal Petrology, Gebruder Borntraeger, Berlin. 311 pp.
Stetter, K.O. (1996) Hyperthermophiles in the history of life. Ciba Found. Symp. 202: 1–11.
Sugitani, K. (1992) Geochemical characteristics of Archean cherts and other sedimentary rocks in the Pilbara Block, Western Australia: evidence for Archean seawater enriched in hydrothermally-derived iron and silica. Precambrian Res. 57: 21–47.
Sumner, D.Y. and Bowering, S.A. (1996) U-Pb geochronologic constraints on deposition of the Campbellrand Subgroup, Transvaal Supergroup, South Africa. Precambrian Res. 79: 25–35.
Walter, M.R. (1994) The earliest life on earth clues to finding life on Mars. Search. 25: 117–119.
Walter, M.R. (1996) Ancient hydrothermal ecosystems on Earth: a new palaeobiological frontier. Ciba Found. Symp. 202: 112–127.
Walter, M.R., Buick, R. and Dunlop, J.S.R. (1980) Stromatolites 3400–3500 Mys old from the North Pole area, Western Australia. Nature. 284: 443–445.
Yanagawa, H. and Kojima, K. (1985) Thermophilic microspheres of peptide-like polymers and silicates formed at 250 degrees C. J. Biochem. 97: 1521–1524.
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2000 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Glikson, M., Taylor, D. (2000). Nature of organic matter in the early Proterozoic, earliest life forms and metal associations. In: Glikson, M., Mastalerz, M. (eds) Organic Matter and Mineralisation: Thermal Alteration, Hydrocarbon Generation and Role in Metallogenesis. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-9474-5_5
Download citation
DOI: https://doi.org/10.1007/978-94-015-9474-5_5
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-4019-0
Online ISBN: 978-94-015-9474-5
eBook Packages: Springer Book Archive