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GENG Hai-bo, HUANG Jian-xin, QIAO Hai-ming, ZHANG Fu-xin. Main MicrobeGroup in the Shihongtan Uranium Deposit in Xinjiang and Their Metallogenic Significance[J]. Acta Sedimentologica Sinica, 2005, 23(4): 626-630.
Citation: GENG Hai-bo, HUANG Jian-xin, QIAO Hai-ming, ZHANG Fu-xin. Main MicrobeGroup in the Shihongtan Uranium Deposit in Xinjiang and Their Metallogenic Significance[J]. Acta Sedimentologica Sinica, 2005, 23(4): 626-630.

Main MicrobeGroup in the Shihongtan Uranium Deposit in Xinjiang and Their Metallogenic Significance

  • Received Date: 2005-01-18
  • Rev Recd Date: 2005-03-14
  • Publish Date: 2005-12-10
  • By using biological method, microorganisms in the Shihong tan u ranium deposit were iso lated and identified for the first time at home. Results showed that the distribution of themainm icrobe groups changed w ith the level of oxidation of the rock samples. A great deal of ae robic and anae robic bacteriaw ere ve ry active in the in termediate zone of oxidation and reduction, while in the o re zone, the speciesw asmonotonous, mainly anaerobic sulfate-reducing bacteria.In addition, the func tion ofm icroorgan isms during the formation of uranium deposit and the effect on the meta llogenic env ironment were also discussed.
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    2 阎葆瑞,张锡根. 微生物成矿学[M].北京:科学出版社,2000.1-70.

    3 Lovley D R,Phillips E J P,Gorby Y A. Microbial reduction of uranium[J].NATURE,1991.414-416.

    4 陈戴生,李胜祥,蔡煜琦. 我国中新生代盆地砂岩型铀矿研究现状及发展方向的探讨[J].沉积学报,2003,(01):113-117.

    5 陈绍铭,郑福寿. 水生微生物实验法[M].北京:海洋出版社,1985.87-239.

    6 郑士民,颜望明,钱新民. 自养微生物[M].北京:科学出版社,1983.187-189.

    7 张子敏,马汉峰,蔡根庆. 吐哈盆地西南缘艾丁湖斜坡带层间氧化带分带性及其地球化学特征[J].世界核地质科学,2004,(01):5-8.

    8 赵瑞全,秦明宽,王正邦. 微生物和有机质在512层间氧化带砂岩型铀矿成矿中的作用[J].铀矿地质,1998,(06):338-343.

    9 周德庆. 微生物学[M].北京:高等教育出版社,1994.1-10.
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  • Received:  2005-01-18
  • Revised:  2005-03-14
  • Published:  2005-12-10

Main MicrobeGroup in the Shihongtan Uranium Deposit in Xinjiang and Their Metallogenic Significance

Abstract: By using biological method, microorganisms in the Shihong tan u ranium deposit were iso lated and identified for the first time at home. Results showed that the distribution of themainm icrobe groups changed w ith the level of oxidation of the rock samples. A great deal of ae robic and anae robic bacteriaw ere ve ry active in the in termediate zone of oxidation and reduction, while in the o re zone, the speciesw asmonotonous, mainly anaerobic sulfate-reducing bacteria.In addition, the func tion ofm icroorgan isms during the formation of uranium deposit and the effect on the meta llogenic env ironment were also discussed.

GENG Hai-bo, HUANG Jian-xin, QIAO Hai-ming, ZHANG Fu-xin. Main MicrobeGroup in the Shihongtan Uranium Deposit in Xinjiang and Their Metallogenic Significance[J]. Acta Sedimentologica Sinica, 2005, 23(4): 626-630.
Citation: GENG Hai-bo, HUANG Jian-xin, QIAO Hai-ming, ZHANG Fu-xin. Main MicrobeGroup in the Shihongtan Uranium Deposit in Xinjiang and Their Metallogenic Significance[J]. Acta Sedimentologica Sinica, 2005, 23(4): 626-630.
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