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The first find of biogenic nanohematite in the bauxite-bearing weathering crust in basalt from South Vietnam
The abundance of microbial forms (bacteria, biofilms, bacterial mats, glycocalyx) participating in the formation of iron oxide and hydroxide minerals is a peculiar feature of weathering crusts (CW) in basalt from South Vietnam. Their maximal concentration is observed in the zone of lateritic bauxite...
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Published in: | Doklady earth sciences 2013-11, Vol.453 (1), p.1145-1149 |
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creator | Bortnikov, N. S. Novikov, V. M. Boeva, N. M. Zhukhlistov, A. P. Zhegallo, E. A. Gendler, T. S. Zaitseva, L. V. Soboleva, S. V. |
description | The abundance of microbial forms (bacteria, biofilms, bacterial mats, glycocalyx) participating in the formation of iron oxide and hydroxide minerals is a peculiar feature of weathering crusts (CW) in basalt from South Vietnam. Their maximal concentration is observed in the zone of lateritic bauxite and cuirass formed above in the undersoil horizon. Currently magnetite Fe3O4 is well studied as a product of iron biomineralization by modern organisms and included in the top ten by scientific and practical importance. Special attention has been paid to natural, as well as synthetic, minerals formed with participation of magnitotactic bacteria. |
doi_str_mv | 10.1134/S1028334X13110159 |
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subjects | Aluminum compounds Basalt Bauxite Biofilms Earth and Environmental Science Earth Sciences Ferric oxide Geochemistry Hydroxides Iron compounds Iron oxides Lithosphere Magnetite Microbiology Mineralization Minerals Nanomaterials Paleontology Studies Weathering |
title | The first find of biogenic nanohematite in the bauxite-bearing weathering crust in basalt from South Vietnam |
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