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Applied and Environmental Microbiology, November 2000, p. 5092-5098, Vol. 66, No. 11
Department of Earth Sciences, University of
Cagliari, 09127 Cagliari,1 and
Department of Environmental Sciences, University Cà
Foscari, 30122 Venice,2 Italy
Received 24 April 2000/Accepted 21 July 2000
An iron-poor stream of nearly neutral pH polluted by mine tailings
has been investigated for a natural phenomenon responsible for the
polishing of heavy metals in mine wastewaters. A white mineralized mat,
which was determined to be hydrozincite
[Zn5(CO3)2(OH)6] by
X-ray diffraction analysis, was observed in the stream sediments mainly
in spring. The precipitate shows a total organic matter residue of 10%
dry weight and contains high concentrations of Pb, Cd, Ni, Cu, and
other metals. Scanning electron microscopy analysis suggests that
hydrozincite is mainly of biological origin. Dormant photosynthetic
microorganisms have been retrieved from 1-year-old dry hydrozincite.
The autofluorescent microorganisms were imaged by a scanning confocal
laser microscope. A photosynthetic filamentous bacterium, classified as
Scytonema sp. strain ING-1, was found associated with
microalga Chlorella sp. strain SA1. This microbial
community is responsible for the natural polishing of heavy metals in
the water stream by coprecipitation with hydrozincite.
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Heavy Metal Coprecipitation with Hydrozincite
[Zn5(CO3)2(OH)6] from
Mine Waters Caused by Photosynthetic Microorganisms
*
Corresponding author. Mailing address: Department of
Environmental Sciences, University Cà Foscari, La Celestia, Via
Castello 2737/b, I-30122 Venice, Italy. Phone: 39-041-2578432. Fax:
39-041-5281494. E-mail: baldi{at}unive.it or
baldi{at}unisi.it.
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