Instituto de Recursos Naturales y Agrobiologia (IRNAS-CSIC), Sevilla, Spain.
Instituto de Investigacion Cueva de Nerja, Nerja, Spain.
PeerJ. 2022 May 3;10:e13399. doi: 10.7717/peerj.13399. eCollection 2022.
Research on cave microorganisms has mainly focused on the microbial communities thriving on speleothems, rocks and sediments; however, drip water bacteria and calcite precipitation has received less attention. In this study, microbial communities of carbonate precipitates from drip waters in Nerja, a show cave close to the sea in southeastern Spain, were investigated. We observed a pronounced difference in the bacterial composition of the precipitates, depending on the galleries and halls. The most abundant phylum in the precipitates of the halls close to the cave entrance was , due to the low depth of this sector, the direct influence of a garden on the top soil and the infiltration of waters into the cave, as well as the abundance of members of the order , dispersing from plant roots, and other and , common soil inhabitants. The influence of marine aerosols explained the presence of and other bacteria due to the short distance from the cave to the sea. Nineteen out of forty six genera identified in the cave have been reported to precipitate carbonate and likely have a role in mineral deposition.
洞穴微生物的研究主要集中在在洞穴中的石笋、岩石和沉积物上繁衍生息的微生物群落上;然而,滴水细菌和方解石沉淀却较少受到关注。在这项研究中,研究了西班牙东南部靠近海洋的展示洞穴 Nerja 中滴水的碳酸盐沉淀物中的微生物群落。我们观察到,根据画廊和大厅的不同,沉淀物中的细菌组成有明显的差异。在靠近洞穴入口的大厅中的沉淀物中最丰富的门是 ,这是由于该区域的深度较浅,受到顶部花园的直接影响以及水渗透到洞穴中,以及来自植物根的 目和其他 和 的丰度,它们是常见的土壤居民。海洋气溶胶的影响解释了由于洞穴到海洋的距离较短, 和其他细菌的存在。在洞穴中鉴定的 46 个属中的 19 个被报道会沉淀碳酸盐,并且可能在矿物沉积中起作用。