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Microbial thiosulphate reaction arrays: the interactive roles of Fe(III), O 2 and microbial strain on disproportionation and oxidation pathways
Author(s) -
WARREN L. A,
NORLUND K. L. I,
BERNIER L.
Publication year - 2008
Publication title -
geobiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.859
H-Index - 72
eISSN - 1472-4669
pISSN - 1472-4677
DOI - 10.1111/j.1472-4669.2008.00173.x
Subject(s) - microbial population biology , abiotic component , disproportionation , strain (injury) , chemistry , microbial metabolism , acidithiobacillus ferrooxidans , environmental chemistry , biofilm , bacteria , microbial ecology , microbial consortium , food science , bioleaching , microorganism , biochemistry , biology , ecology , catalysis , organic chemistry , genetics , anatomy , copper
In this work, we experimentally evaluate pH and  dynamics associated with abiotic and microbial  oxidation under varying [O 2 ], [Fe(III)] and microbial strain/consortia (two pure strains, Acidithiobacillus ferrooxidans , Acidithiobacillus thiooxidans , their consortia, and two enrichments from an acidic environmental system, Moose Lake 2002 and Moose Lake 2003). Results of the batch experiments demonstrate highly active microbial processing of  while abiotic controls under identical experimental conditions remain static with no pH decrease. When abiotic controls were manually titrated with acid to achieve similar pH decreases to those occurring in the microbial treatments, different S pathways were involved. In particular, disproportionation is a substantial component of initial microbial  processing, and is accelerated by the presence of Fe(III), indicating that recycling of S through intermediate oxidation states is likely to be widespread in acidic mine environments where high [Fe(III)] is common. Furthermore, the microbially mediated S reaction pathways were dependent on both environmental conditions and microbial strain/consortia, indicating that microbial community structure also plays a key role. Collectively, these results highlight the importance of microbial activity, their poor representation by abiotic S models, the likelihood that Fe(III), rather than O 2 , is a key control on microbial S processing in acid environments and the need to identify the microbial community/strain involved.

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