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印度泰米尔纳德邦历史遗址的印度石器遗址地球化学梯度的宏基因组。

Metagenome Across a Geochemical Gradient of Indian Stone Ruins Found at Historic Sites in Tamil Nadu, India.

机构信息

Department of Molecular, Cellular, and Biomedical Sciences, University of New Hampshire, 46 College Rd., Durham, NH, 03824-2617, USA.

Department of Microbiology, Bharathidasan University, Tiruchirappalli, Tamil Nadu, India.

出版信息

Microb Ecol. 2021 Feb;81(2):385-395. doi: 10.1007/s00248-020-01598-3. Epub 2020 Sep 12.

Abstract

Although stone surfaces seem unlikely to be habitable, they support microbial life. Life on these surfaces are subjected to many varying harsh conditions and require the inhabitants to exhibit resistance to environmental factors including UV irradiation, toxic metal exposure, and fluctuating temperatures and humidity. Here we report the effect of hosting stone geochemistry on the microbiome of stone ruins found in Tamil Nadu, India. The microbial communities found on the two lithologies, granite and granodiorite, hosted distinct populations of bacteria. Geochemical composition analysis of sampled stones revealed quartz mineral content as a major driver of microbial community structure, particularly promoting community richness and proportions of Cyanobacteria and Deinococcus-Thermus. Other geochemical parameters including ilmenite, albite, anorthite, and orthoclase components or elemental concentrations (Ti, Fe, Mn, Na, and K) also influenced community structure to a lesser degree than quartz. Core members of the stone microbiome community found on both lithologies were also identified and included Cyanobacteria (Chroococcidiopsaceae and Dapisostemonum CCIBt 3536), Rubrobacter, and Deinococcus. A cluster of taxa including Sphingomonas, Geodermatophilus, and Truepera were mostly found in the granodiorite samples. Community diversity correlated with quartz mineral content in these samples may indicate that the microbial communities that attach to quartz surfaces may be transient and regularly changing. This work has expanded our understanding of built-stone microbial community structure based on lithology and geochemistry.

摘要

虽然石材表面似乎不太可能存在生命,但它们确实支持微生物的生存。这些表面上的生命受到许多不同的恶劣条件的影响,需要其居民表现出对环境因素的抵抗力,包括紫外线辐射、有毒金属暴露以及温度和湿度的波动。在这里,我们报告了岩石地球化学对印度泰米尔纳德邦石质废墟微生物组的影响。在两种岩石类型(花岗岩和花岗闪长岩)上发现的微生物群落存在着截然不同的细菌种群。对采样石材的地球化学成分分析表明,石英矿物含量是微生物群落结构的主要驱动因素,特别是促进了群落的丰富度和蓝细菌和 Deinococcus-Thermus 的比例。其他地球化学参数,包括钛铁矿、钠长石、钙长石和正长石成分或元素浓度(Ti、Fe、Mn、Na 和 K),对群落结构的影响程度也小于石英。在两种岩石类型上发现的石质微生物群落的核心成员也被鉴定出来,包括蓝细菌(Chroococcidiopsaceae 和 Dapisostemonum CCIBt 3536)、Rubrobacter 和 Deinococcus。包括 Sphingomonas、Geodermatophilus 和 Truepera 在内的一个分类群主要存在于花岗闪长岩样品中。这些样本中与石英矿物含量相关的群落多样性可能表明,附着在石英表面的微生物群落可能是短暂的,并且经常发生变化。这项工作扩展了我们对基于岩性和地球化学的建筑石材微生物群落结构的理解。

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