A Metagenomic Time-Series Approach to Assess the Ecological Stability of Microbial Mats in a Seasonally Fluctuating Environment


Por: Madrigal-Trejo D., Sánchez-Pérez J., Espinosa-Asuar L., Valdivia-Anistro J.A., Eguiarte L.E., Souza V.

Publicada: 1 ene 2023 Ahead of Print: 1 jul 2023
Resumen:
Microbial mats are complex ecological assemblages that have been present in the rock record since the Precambrian and can still be found in extant marginalized environments. These structures are considered highly stable ecosystems. In this study, we evaluate the ecological stability of dome-forming microbial mats in a modern, water-level fluctuating, hypersaline pond located in the Cuatro Ciénegas Basin, Mexico. We conducted metagenomic sampling of the site from 2016 to 2019 and detected 2250 genera of Bacteria and Archaea, with only <20 belonging to the abundant taxa (>1%). The microbial community was dominated by Proteobacteria, Euryarchaeota, Bacteroidetes, Firmicutes, and Cyanobacteria, and was compositionally sensitive to disturbances, leading to high taxonomic replacement even at the phylum level, with a significant increase in Archaea from [Formula: see text]1-4% to [Formula: see text]33% throughout the 2016-2019 study period. Although a core community represented most of the microbial community (>75%), relative abundances shifted significantly between samples, as demonstrated by changes in the abundance of Coleofasciculus from 10.2% in 2017 to 0.05% in 2019. Although functional differences between seasons were subtle, co-occurrence networks suggest differential ecological interactions between the seasons, with the addition of a new module during the rainy season and the potential shift in hub taxa. Functional composition was slightly more similar between samples, but basic processes such as carbohydrate, amino acid, and nucleic acid metabolisms were widely distributed among samples. Major carbon fixation processes included sulfur oxidation, nitrogen fixation, and photosynthesis (both oxygenic and anoxygenic), as well as the Wood-Ljundgahl and Calvin cycles. © 2023. The Author(s).

Filiaciones:
Madrigal-Trejo D.:
 Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional AutÓnoma de MéxicoMexico City, Mexico

Sánchez-Pérez J.:
 Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional AutÓnoma de MéxicoMexico City, Mexico

Espinosa-Asuar L.:
 Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional AutÓnoma de MéxicoMexico City, Mexico

Valdivia-Anistro J.A.:
 Facultad de Estudios Superiores Zaragoza, Universidad Nacional Autónoma de México, Ciudad de México, Mexico

Eguiarte L.E.:
 Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional AutÓnoma de MéxicoMexico City, Mexico

Souza V.:
 Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional AutÓnoma de MéxicoMexico City, Mexico

 Centro de Estudios del Cuaternario de Fuego-Patagonia y Antártica (CEQUA), Punta Arenas, Chile
ISSN: 00953628
Editorial
Springer New York LLC, 233 SPRING ST, NEW YORK, NY 10013 USA, Estados Unidos America
Tipo de documento: Article
Volumen: 86 Número: 4
Páginas: 2252-2270
WOS Id: 001022223400001
ID de PubMed: 37393557
imagen Green Published, hybrid, All Open Access, Hybrid Gold, Green

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