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A Summary of Some Microbes Identified from Different Indian Caves and Their Possible Role in Mineral Formations

机译:来自不同印度洞穴的一些微生物的总结及其在矿物形成中的可能作用

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Microbe-mineral interactions in caves can lead to secondary mineralformations such as speleothems, moonmilk etc. In the present review, weprovide a summary of geomicrobiological work done so far in some Indiancaves. Microbially induced mineralization is documented in cave ecosystemsand microbial metabolisms help in mineral formations either throughdirect/active or indirect/passive processes. Laboratory based experimentsconducted on speleothems from Sahastradhara caves (Dehradun); Borra Cave(Andhra Pradesh); Krem Phyllut, Krem Mawsmai, Krem Mawmluh andRongai Dobhakol (Meghalaya) have clearly demonstrated that bacterialstrains isolated from these caves have the capability to precipitate mineralsundercontrolled conditions.
机译:洞穴中微生物与矿物质的相互作用会导致次生矿物形成,如speleothems,moonmilk等。在本篇综述中,我们提供了迄今为止在某些印第安洞穴中进行的地球微生物学工作的摘要。洞穴生态系统中记录了微生物诱导的矿化作用,微生物代谢通过直接/主动或间接/被动过程帮助矿物质形成。基于实验室的实验,是对Sahastradhara洞穴(Dehradun)的鞘脂进行的;博拉洞(Andhra Pradesh); Krem Phyllut,Krem Mawsmai,Krem Mawmluh和Rongai Dobhakol(梅加拉亚邦)已明确证明,从这些洞穴中分离出的细菌菌株具有在受控条件下沉淀矿物的能力。

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