Center for Applied Geoscience, Eberhard Karls University Tübingen, Sigwartstrasse 10, 72076 Tübingen, Germany.
Biophys Chem. 2013 Dec 15;183:30-41. doi: 10.1016/j.bpc.2013.06.019. Epub 2013 Jul 1.
Microbial life has been prevailing in the biosphere for the last 3.8 Ga at least. Throughout most of the Earth's history it has experienced a range of pressures; both dynamic pressure when the young Earth was heavily bombarded, and static pressure in subsurface environments that could have served as a refuge and where microbial life nowadays flourishes. In this review, we discuss the extent of high-pressure habitats in early and modern times and provide a short overview of microbial survival under dynamic pressures. We summarize the current knowledge about the impact of microbial activity on biogeochemical cycles under pressures characteristic of the deep subsurface. We evaluate the possibility that pressure can be a limiting parameter for life at depth. Finally, we discuss the open questions and knowledge gaps that exist in the field of high-pressure geomicrobiology.
微生物的生命至少在过去的 38 亿年中一直在生物圈中占主导地位。在地球历史的大部分时间里,它经历了一系列的压力;当年轻的地球受到强烈撞击时是动态压力,而在地下环境中是静态压力,地下环境可以作为避难所,微生物生命如今在那里繁荣发展。在这篇综述中,我们讨论了早期和现代高压栖息地的范围,并简要概述了微生物在动态压力下的生存情况。我们总结了目前关于微生物活动在深部地下压力特征下对生物地球化学循环影响的知识。我们评估了压力可能成为深部生命限制参数的可能性。最后,我们讨论了高压地质微生物学领域存在的悬而未决的问题和知识差距。