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酸性矿山排水作为铁纹层石形成的微生物生态位的能源:西班牙西南部的廷蒂略河。

Acid Mine Drainage as Energizing Microbial Niches for the Formation of Iron Stromatolites: The Tintillo River in Southwest Spain.

机构信息

Departamento de Geología, Facultad de Ciencias de la Tierra, Universidad Autónoma de Nuevo Léon (UANL), Linares, México.

Department of Applied Geosciences, CCTH-Science and Technology Research Centre, University of Huelva, Huelva, Spain.

出版信息

Astrobiology. 2021 Apr;21(4):443-463. doi: 10.1089/ast.2019.2164. Epub 2020 Dec 22.

Abstract

The Iberian Pyrite Belt in southwest Spain hosts some of the largest and diverse extreme acidic environments with textural variation across rapidly changing biogeochemical gradients at multiple scales. After almost three decades of studies, mostly focused on molecular evolution and metagenomics, there is an increasing awareness of the multidisciplinary potential of these types of settings, especially for astrobiology. Since modern automatized exploration on extraterrestrial surfaces is essentially based on the morphological recognition of biosignatures, a macroscopic characterization of such sedimentary extreme environments and how they look is crucial to identify life properties, but it is a perspective that most molecular approaches frequently miss. Although acid mine drainage (AMD) systems are toxic and contaminated, they offer at the same time the bioengineering tools for natural remediation strategies. This work presents a biosedimentological characterization of the clastic iron stromatolites in the Tintillo river. They occur as laminated terraced iron formations that are the most distinctive sedimentary facies at the Tintillo river, which is polluted by AMD. Iron stromatolites originate from fluvial abiotic factors that interact with biological zonation. The authigenic precipitation of schwertmannite and jarosite results from microbial-mineral interactions between mineral and organic matrices. The Tintillo iron stromatolites are composed of bacterial filaments and diatoms as , , , and sp. Furthermore, the active biosorption and bioleaching of sulfur are suggested by the black and white coloration of microbial filaments inside stromatolites. AMD systems are hazardous due to physical, chemical, and biological agents, but they also provide biogeochemical sources with which to infer past geochemical conditions on Earth and inform exploration efforts on extraterrestrial surfaces in the future.

摘要

西班牙西南部的伊比利亚黄铁矿带拥有一些最大和最多样化的极端酸性环境,这些环境在多个尺度上具有快速变化的生物地球化学梯度,纹理变化多样。经过近三十年的研究,主要集中在分子进化和宏基因组学上,人们越来越意识到这些类型的环境具有多学科的潜力,特别是对天体生物学而言。由于现代对外星表面的自动化探索基本上基于生物特征的形态识别,因此对这些沉积极端环境及其外观进行宏观特征描述对于识别生命特性至关重要,但这是大多数分子方法经常忽略的视角。虽然酸性矿山排水(AMD)系统具有毒性和污染性,但它们同时提供了用于自然修复策略的生物工程工具。本工作对 Tintillo 河流中的碎屑铁叠层石进行了生物沉积学特征描述。它们呈层状梯田状铁建造,是 Tintillo 河流中最具特色的沉积相,该河流受到 AMD 的污染。铁叠层石起源于与生物分带相互作用的河流非生物因素。水铁矿和黄钾铁矾的自生沉淀是矿物和有机基质之间微生物-矿物相互作用的结果。Tintillo 铁叠层石由细菌丝和硅藻组成,如 、 、 、和 种。此外,微生物丝内部的黑白颜色暗示了硫的主动生物吸附和生物沥滤。AMD 系统由于物理、化学和生物因素而具有危害性,但它们也提供了生物地球化学来源,可以据此推断地球上过去的地球化学条件,并为未来的外星表面探索工作提供信息。

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