Crystal-size distributions and possible biogenic origin of Fe sulfides
  • Metaadatok
Tartalom: http://dx.doi.org/10.1127/0935-1221/2001/0013-0691
Archívum: MTA Könyvtár
Gyűjtemény: Status = Published



Type = Conference or Workshop Item
Cím:
Crystal-size distributions and possible biogenic origin of Fe sulfides
Létrehozó:
Pósfai, Mihály
Cziner, Krisztina
Márton, Emő
Márton, Péter
Buseck, Peter R.
Frankel, Richard R B.
Bazylinski, Dennis A.
Dátum:
2001-07
Téma:
QD06 Mineralogy / ásványtan
QE01 Geophysics / geofizika
QE02 Geochemistry / geokémia
Tartalmi leírás:
Sedimentary greigite (Fe(3)S(4)) can form either by "biologically controlled" or by "biologically induced mineralization" (BCM and BIM, respectively). In order to identify the origin of magnetic Fe sulfides, we studied and compared the sizes and morphologies of greigite crystals produced by a magnetotactic microorganism (previously described and referred to as the "many-celled magnetotactic prokaryote", MMP) and Fe sulfides from two specimens of Miocene sedimentary rocks (from Laka: in the foredeep of the Western Carpathians and from Michalovce, in the Transcarpathian Depression). Greigite grains from the MMP and the Laka rock show nearly Gaussian crystal-size distributions (CSDs), whereas the CSD is lognormal for Fe sulfides from the Michalovce rock. We simulated various crystal-growth mechanisms and matched the calculated and observed CSDs; crystals from the MMP and the Laka rock have CSDs that are consistent with random grow-th of crystal nuclei in an open system, whereas the CSD of the Michalovce Fe sulfides is consistent with surface-controlled growth followed by supply-controlled growth in an open system. On the basis of CSDs and characteristic contrast features in the transmission electron microscope, greigite in the Laka rock is likely of BCM origin, whereas the Fe sulfide crystals in the other rock sample were produced by BIM processes. Our results indicate that the methods we applied in this study may contribute to the identification of the origin of magnetic Fe sulfide minerals in sedimentary rocks.
Típus:
Conference or Workshop Item
PeerReviewed
Formátum:
application/pdf
Azonosító:
Pósfai, Mihály and Cziner, Krisztina and Márton, Emő and Márton, Péter and Buseck, Peter R. and Frankel, Richard R B. and Bazylinski, Dennis A. (2001) Crystal-size distributions and possible biogenic origin of Fe sulfides. In: Symposium and Workshop on Biogenic Iron Materials, 2000. május 20-23., Tihany, Hungary.
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