Zhu Hai-Zhen, Jiang Cheng-Ying, Liu Shuang-Jiang
State Key Laboratory of Microbial Resources and Environmental Microbiology Research Center, Institute of Microbiology, Chinese Academy of Sciences, Beijing, China.
College of Life Sciences, University of Chinese Academy of Sciences, Beijing, China.
Front Microbiol. 2022 Sep 28;13:950005. doi: 10.3389/fmicb.2022.950005. eCollection 2022.
Among fundamental research questions in subterranean biology, the role of subterranean microbiomes playing in key elements cycling is a top-priority one. Karst caves are widely distributed subsurface ecosystems, and cave microbes get more and more attention as they could drive cave evolution and biogeochemical cycling. Research have demonstrated the existence of diverse microbes and their participance in biogeochemical cycling of elements in cave environments. However, there are still gaps in how these microbes sustain in caves with limited nutrients and interact with cave environment. Cultivation of novel cave bacteria with certain functions is still a challenging assignment. This review summarized the role of microbes in cave evolution and mineral deposition, and intended to inspire further exploration of microbial performances on C/N/S biogeocycles.
在地下生物学的基础研究问题中,地下微生物群落在关键元素循环中所起的作用是首要问题。岩溶洞穴是广泛分布的地下生态系统,洞穴微生物因其能推动洞穴演化和生物地球化学循环而受到越来越多的关注。研究已经证明了洞穴环境中存在多样的微生物及其参与元素的生物地球化学循环。然而,在这些微生物如何在营养有限的洞穴中生存以及如何与洞穴环境相互作用方面仍存在空白。培养具有特定功能的新型洞穴细菌仍然是一项具有挑战性的任务。本综述总结了微生物在洞穴演化和矿物沉积中的作用,并旨在激发对微生物在碳/氮/硫生物地球化学循环中表现的进一步探索。