Other
Scientific paper
Dec 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001agufm.p21c..08v&link_type=abstract
American Geophysical Union, Fall Meeting 2001, abstract #P21C-08
Other
1010 Chemical Evolution, 1035 Geochronology, 1040 Isotopic Composition/Chemistry, 1050 Marine Geochemistry (4835, 4850), 1060 Planetary Geochemistry (5405, 5410, 5704, 5709, 6005, 6008)
Scientific paper
The highly metamorphosed 3.8 Ga old Isua Supracrustal Belt (ISB) in southern West Greenland contains the most widely studied example of ancient Archaean water-lain sediments that carry traces of ancient life. Carbonate deposits in the ISB were originally interpreted as primary platform deposits in a shallow marine environment. Graphite occurring in relatively high concentrations and associating with apatite in these rocks has been interpreted as a remnant of ancient biogenic matter, pointing to the existence of a vast microbial ecosystem in the early Archaean (1,2) Recent discoveries, however, cast considerable doubt on this scenario. The ISB metacarbonates are now found to be secondary deposits, resulting from extensive metasomatism (3,4). The apatite-associated occurrence of graphite, forming the basis for earlier biogenic interpretation, is entirely restricted to these metasomatic carbonate deposits, while true sediments like BIF's and metacherts contain virtually no graphite. Furthermore, within these metacarbonates graphite appears to be specifically associated with iron carbonate (siderite) and magnetite. Thermal decomposition of siderite; 6 FeCO3 ' 2Fe3O4 + 5CO2 + C, is the process seemingly responsible for the graphite formation (5,6). The cation composition (Fe, Mg, Mn, and Ca) of the carbonate minerals, carbon isotope analysis of carbonates and associated graphite and petrographic analysis of a suite of metacarbonates support the conclusion that multiple pulses of metasomatism affected the ISB, causing the deposition of siderite and subsequent partial degradation to graphite and magnetite. Equilibrium isotope fractionation between siderite and graphite in these rocks indicates a temperature of metasomatism between 500 and 600C, which coincides with other estimates of metamorphic temperature for the ISB. The siderite-graphite-apatite association in the ISB consequently appears to be an entirely abiogenic metasomatic feature, which does not point to traces of an ancient Early Archaean ecosystem. An exception to this general observation is a locality in the western part of the ISB, where isotopically light graphite occurs in sequences of graded beds, seemingly representing cyclic turbidites (7). The absence of siderite and/or magnetite makes it clear that inorganic formation of graphite by siderite dissociation can not be the source of carbon in these metasediments This particular formation is thus likely to contain the only currently verified remnant of Archaean life in the ISB with an age of 3.8 Ga. (1). Mojzsis,S.J, .Arrhenius,G., McKeegan, K.D.,.Harrison, T.M.,.Nutman, A.P & C.R.L.Friend.,1996. Nature 384: 55 (2) Schidlowski, M., Appel, P.W.U., Eichmann, R. & Junge, C.E., 1979. Geochim. Cosmochim. Acta 43: 189-190. (3). Rose, N.M., Rosing, M.T. & Bridgwater, D., 1996. Am. J. Sci. 296: 1004-1044. (4). Rosing, M.T.,Rose, N.M.,Bridgwater, D. & Thomsen, H.S., 1996. Geology 24: 43-46. (5). Perry, E.C. & Ahmad, S.N., 1977. Earth Planet. Sci. Lett. 36: 280-284. (6). Van Zuilen, M., Matthew, K., Marti,K., & Arrhenius,G.,1999. Abstract A173, AGU Fall Meeting, San Francisco, CA, Dec. 1999. (7). Rosing, M.T., 1999. Science 283: 674-676.
Arrhenius Gustaf
Lepland Aivo
van Zuilen Mark
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