

In acid creeks in mining regions like this at Contrary Creek, Va., iron-rich precipitates often contain sulfur and are yellow. Many iron-oxidizing bacteria such as Thiobacillus thiooxidans and T. ferrooxidans produce this "yellow boy." Not all water in mining regions is acid, however. Although Contrary Creek is acid, its tributary (slightly left of center) is neutral and has red flocs and the usual suite of neutral iron bacteria.

This oil-like film at Contrary Creek, Va., floats on acid water, as shown by the indicator paper. Under the microscope, the film is colonized by unknown rod-shaped bacteria.
U.S. Department of the Interior, U.S. Geological Survey
URL: http://pubs.usgs.gov/gip/microbes/viewing.html
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Last modified: 16:34:01 Fri 17 Feb 2006
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