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Microbial ecology of submerged marine caves and holes characterised by high levels of hydrogen sulphide

机译:以高浓度硫化氢为特征的海底洞穴和洞穴的微生物生态学

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摘要

Submarine caves,cavities and niches characterised by hydrogen sulphide (H2S) elevated concentrations are particularly interesting for their inhabiting microflora as well as for the overall chemical,geological and biological parameters. These ecosystems are usually populated by well-adapted living forms,physically distributed following the in situ concentration and gradient of micronutrients,O2 and H2S,and also according to the values of temperature and pH. The biota is primarily characterised by prokaryotes (both autotrophic and heterotrophic) adapted to anoxic and/or microaerophilic condition and capable to form extensive biofilms on the rocky surfaces and even on the bottom sediment. These habitats can be defined as extreme,because the scarcity or absence of solar irradiation,the chemo-physical traits and the fact that specialised prokaryotes are often the only inhabitants. This review is focused on the microbial ecology of marine caves and holes characterised by high levels of H2S. Ecological and geological data are already available but very few insights as far as regard microbiology were achieved in order to describe these fascinating habitats. The autochthonous mesophilic and thermotolerant microorganisms living in these caves may have interesting physiological traits and eventually may lead to potential application in biotechnological processes.
机译:以硫化氢(H2S)浓度升高为特征的海底洞穴,洞室和生态位,因其栖息的微生物群落以及整体化学,地质和生物学参数而特别受关注。这些生态系统通常居住着适应性强的生物形式,根据微量营养素O2和H2S的原位浓度和梯度以及温度和pH值在物理上分布。该生物群的主要特征是原核生物(自养和异养)适应缺氧和/或微需氧条件,并能够在岩石表面甚至底部沉积物上形成广泛的生物膜。这些栖息地可被定义为极端,因为缺乏或缺乏太阳辐射,化学物理特性以及专门的原核生物通常是唯一的居民。这篇综述集中在以高水平的H2S为特征的海洋洞穴和洞穴的微生物生态学上。生态和地质数据已经存在,但是就描述这些迷人的栖息地而言,关于微生物学的见解很少。生活在这些洞穴中的土生中温和耐热微生物可能具有有趣的生理特性,并最终可能在生物技术过程中得到潜在应用。

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