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邦纳维尔盐滩高盐沉积物中微生物群落的代谢潜力。

Metabolic Potential of Microbial Communities in the Hypersaline Sediments of the Bonneville Salt Flats.

机构信息

School of Biological Sciences, University of Utahgrid.223827.e, Salt Lake City, UT, USA.

Department of Geology and Geophysics, University of Utahgrid.223827.e, Salt Lake City, UT, USA.

出版信息

mSystems. 2022 Dec 20;7(6):e0084622. doi: 10.1128/msystems.00846-22. Epub 2022 Nov 15.

Abstract

The Bonneville Salt Flats (BSF) appear to be entirely desolate when viewed from above, but they host rich microbial communities just below the surface salt crust. In this study, we investigated the metabolic potential of the BSF microbial ecosystem. The predicted and measured metabolic activities provide new insights into the ecosystem functions of evaporite landscapes and are an important analog for potential subsurface microbial ecosystems on ancient and modern Mars. Hypersaline and evaporite systems have been investigated previously as astrobiological analogs for Mars and other salty celestial bodies, but these studies have generally focused on aquatic systems and cultivation-dependent approaches. Here, we present an ecosystem-level examination of metabolic pathways within the shallow subsurface of evaporites. We detected aerobic and anaerobic respiration as well as methanogenesis in BSF sediments. Metagenome-assembled genomes of diverse bacteria and archaea encode a remarkable diversity of metabolic pathways, including those associated with carbon fixation, carbon monoxide oxidation, acetogenesis, methanogenesis, sulfide oxidation, denitrification, and nitrogen fixation. These results demonstrate the potential for multiple energy sources and metabolic pathways in BSF and highlight the possibility for vibrant microbial ecosystems in the shallow subsurface of evaporites. The Bonneville Salt Flats is a unique ecosystem created from 10,000 years of desiccation and serves as an important natural laboratory for the investigation of the habitability of salty, halite, and gypsum-rich environments. Here, we show that gypsum-rich mineral deposits host a surprising diversity of organisms and appear to play a key role in stimulating the microbial cycling of sulfur and nitrogen compounds. This work highlights how diverse microbial communities within the shallow subsurface sediments are capable of maintaining an active and sustainable ecosystem, even though the surface salt crust appears to be completely devoid of life.

摘要

从上面看,邦纳维尔盐滩似乎完全是一片荒芜,但在表面盐壳以下,却存在着丰富的微生物群落。在这项研究中,我们调查了盐滩微生物生态系统的代谢潜力。预测和测量的代谢活性为蒸发岩地貌的生态系统功能提供了新的见解,并且是对古代和现代火星潜在地下微生物生态系统的重要模拟。高盐和蒸发盐系统以前曾作为火星和其他咸天体的天体生物学模拟物进行过研究,但这些研究通常侧重于水生系统和依赖培养的方法。在这里,我们对蒸发盐浅层地下的生态系统代谢途径进行了生态系统水平的研究。我们在盐滩沉积物中检测到好氧和厌氧呼吸以及产甲烷作用。不同细菌和古菌的宏基因组组装基因组编码了丰富多样的代谢途径,包括与碳固定、一氧化碳氧化、乙酰生成、产甲烷作用、硫化物氧化、反硝化和固氮有关的途径。这些结果表明盐滩浅层地下存在多种能源和代谢途径的潜力,并强调了蒸发盐浅层地下可能存在充满活力的微生物生态系统的可能性。 邦纳维尔盐滩是一个由 10000 年干旱形成的独特生态系统,是研究咸水、卤盐和石膏丰富环境宜居性的重要天然实验室。在这里,我们表明石膏丰富的矿床中存在着令人惊讶的生物多样性,并且似乎在刺激硫和氮化合物的微生物循环中起着关键作用。这项工作强调了浅层地下沉积物中多样的微生物群落如何能够维持一个活跃和可持续的生态系统,尽管表面盐壳似乎完全没有生命。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/973e/9765009/c11b74a70a78/msystems.00846-22-f001.jpg

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