Karavaiko G I, Avakian Z A, Krutsko V S, Mel'nikova E O, Zhdanov A V
Mikrobiologiia. 1979 May-Jun;48(3):502-8.
A wide spectrum of heterotrophic and autotrophic microorganisms was detected in the zones of decomposition of spodumene and bed rocks, pegmatites and shales, in the spodumene deposit. The following aerobic microorganisms which did not from spores predominated in the deposit: Arthrobacter globiformis, A. pascens, A. simplex, Nocardia globerula, Pseudomonas fluorescens, Ps. putida, Ps. testosteronii. The following specific bacterial groups were found: thionic, sulfate reducing, and nitrifying bacteria. Degradation of spodumene and bed rocks was found to occur in moist regions containing cracks; it was accompanied with a decrease in pH. A possible role of microorganisms in decomposition of spodumene as well as removal of elements is discussed.
在锂辉石矿床中,在锂辉石和基岩、伟晶岩及页岩的分解区域检测到了各种各样的异养和自养微生物。该矿床中以不形成孢子的需氧微生物为主:球形节杆菌、巴斯德节杆菌、单一节杆菌、球孢诺卡氏菌、荧光假单胞菌、恶臭假单胞菌、睾丸酮假单胞菌。还发现了以下特定细菌类群:硫细菌、硫酸盐还原菌和硝化细菌。发现锂辉石和基岩的降解发生在有裂缝的潮湿区域;同时pH值降低。讨论了微生物在锂辉石分解以及元素去除中的可能作用。