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The formation of As2S3 in nature as the mineral orpiment has been observed only in extreme environments, such as geothermal reservoir fluids and hot springs, and previously was assumed to be abiotic. We now know that certain types of bacteria can precipitate As2S3 both intra- an extra-cellulary. Microbial precipitation of As2S3 is an example of how biomineralization often is linked to fundamental cellular processes: in this case, As2S3 formation is tightly coupled to the repiration of arsenate and sulfate. In this transmission electron micrograph (cell length approximately 2 microns), a thin section of a bacteriaum that precipitates AS2S3 is shown. Notice how the small dark particles of As2S3 line the inside of the cytoplasmic membrane (the site of the electron transport chain).
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