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Prokaryotic diversity across a pH gradient in the "El Chichón" crater-lake: a naturally thermo-acidic environment. | LitMetric

Prokaryotic diversity across a pH gradient in the "El Chichón" crater-lake: a naturally thermo-acidic environment.

Extremophiles

Tecnológico Nacional de México/IT de Tuxtla Gutiérrez, Carretera Panamericana km. 1080, Tuxtla Gutiérrez CP, 29050, Chiapas, México.

Published: January 2022

AI Article Synopsis

  • The El Chichón crater-lake in Mexico features a unique thermo-acidic environment that has not been extensively studied, especially regarding its microorganisms.
  • Researchers conducted amplicon sequencing of the 16S rRNA gene on sediment and water samples across a pH and temperature gradient, revealing significant differences in microbial communities between sediments and water.
  • Dominant genera identified, such as Alicyclobacillus and Methanothermobacter, showcase the adaptability of these microorganisms to extreme conditions, including varying electron donors/acceptors and the ability to thrive as chemoorganotrophs and chemolithotrophs.

Article Abstract

The "El Chichón" crater-lake in Mexico is a thermo-acidic environment whose microorganisms have been scarcely studied. In this study, we surveyed the prokaryotic communities by amplicon sequencing of the 16S rRNA gene considering samples of sediment and water collected within a pH/temperature gradient (pH 1.9-5.1, 38-89 °C). Further, we interpreted these results within a physicochemical context. The composition of the microbial assemblage differed significantly between the sediments and water. Sediment communities were different in the site with the highest temperature and lower pH value compared to the other ones sampled, while those in the water were relatively similar at all points. Most of the genera found were related to Alicyclobacillus, Acinetobacter, Bacillus, Mesoaciditoga, Methanothermobacter, Desulfitobacterium, Therminicanus, Kyrpidia, Paenibacillus, Thermoanaerobacterium, and Gelria. Some of these genera are known by their thermo-acidic tolerant capacities with flexible metabolisms to use diverse electron donor/acceptors (S or Fe), while others are thermo(acid)philes that mainly occur in the most extreme sites of the lake. These results show the presence of a microbial community adapted to the changing conditions of a very dynamic crater-lake, that include chemoorganotrophs and chemolithotrophs.

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Source
http://dx.doi.org/10.1007/s00792-022-01257-0DOI Listing

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