Diversity of 16S ribosomal DNA-defined bacterial population in acid rock drainage from Japanese pyrite mine

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Four acidophilic bacteria (YARDs1-4) were isolated from an acid rock drainage (ARD) from Yanahara mine, Okayama prefecture, Japan. The physiological and 16S rDNA sequence analyses revealed that YARD1 was closely affiliated with Acidithiobacillus ferrooxidans, YARD2 was an Acidiphilium-like bacterium, and YARD3 and YARD4 were sulfur-oxidizing bacteria with a relatively close relationship to A. ferrooxidans in the phylogenetic analysis. A molecular approach based on the construction of a 16S rDNA clone library was used to investigate the microbial population of the ARD. Small-subunit rRNA genes were PCR amplified, subsequently cloned and screened for variation by a restriction fragment length polymorphism (RFLP) analysis. A total of 284 clones were grouped into 133 operational taxonomic units (OTUs) by the RFLP analysis. Among them, an OTU showing the same RFLP pattern as those of the isolates from the ARD was not detected. The phylogenetic analysis based on the 16S rDNA sequences from 10 major OTUs and their close relatives revealed that 4 OTUs containing 32.1% of the total clones were loosely affiliated with Verrucomicrobia, 2 OTUs containing 6.6% of the total clones were loosely affiliated with Chloribi, and other OTUs were affiliated with Actinobacteria, Nitrospirae, and β-Proteobacteria.

Section snippets

Environmental samples of ARD and physico-chemical analysis of samples

Water samples were collected from the ARD of Yanahara mine in October 2003. Physico-chemical analyses of the water samples were carried out at the Research Institute for Bioresources, Okayama University. The analytical methods used are listed in Table 1. The water samples were treated within 6 h of collection.

Isolation of acidophilic bacteria

Isolation of acidophilic bacteria from ARD samples from the Yanahara mine was carried out using five different media. Ferrous sulfate (3%) in 9K-medium [0.3% (NH2) 2SO4, 0.05% K2HPO4,

Properties of acidophilic bacteria isolated from ARD

The physico-chemical properties of the ARD from the Yanahara mine are summarized in Table 1. The water was acidic due to the presence of sulfuric ions and had a high iron concentration. The concentrations of nitrate and phosphate ions were very low. In addition to iron, the concentrations of manganese, aluminum, nickel, and cobalt were relatively high. The temperature of the water is kept at approximately 22°C all year round. The high concentration of ferrous iron and the low concentration of

Acknowledgments

We thank Mr. Toshiyuki Takeshima, Dowa Mining Co., Ltd., Tokyo, for his cooperation in sampling ARD from the Yanahara mine. We thank Prof. Isao Aoyama and Mr. Hisao Nishizaki, Research Institute for Bioresources, Okayama University, for their help in physico-chemical analyses of the ARD from the Yanahara mine. This research was supported by the Yakumo Foundation for Environmental Science.

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