# Karst-environments of the southeastern Yucatan Peninsula: Hotspots for modern freshwater microbialites

**Authors:** Alfredo Yanez-Montalvo, Bernardo Águila, Arit S. de León-Lorenzana, Arturo Bayona, Nuria Torrescano-Valle, Pavel Popoca, Luisa I. Falcón, Yizhi Sheng, Yizhi Sheng, Yizhi Sheng, Yizhi Sheng

PMC · DOI: 10.1371/journal.pone.0322625 · 2025-05-07

## TL;DR

This study explores microbialites in the Yucatan Peninsula, revealing their unique microbial and mineral composition and highlighting their importance for environmental conservation.

## Contribution

The study identifies potential new Cyanobacteriota families and highlights Cenote Azul as a biodiverse hotspot for microbialites.

## Key findings

- Microbialites in Cenote Azul showed the highest biodiversity and distinct microbial composition.
- Calcite, magnesian calcite, and gypsum were the primary minerals in the microbialites.
- Hydrogeochemical conditions varied among sites despite their connectivity.

## Abstract

Modern microbialites are sedimentary structures that offer a window into Earth’s geologic history and the intricate interplay between geology and microorganisms. Microbialites are formed by the interaction between microbial communities and the environment leading to mineral precipitation. This study provides a comprehensive analysis of the bacterial and archaeal composition (using the V4 region of the 16S rRNA), along with mineralogy, geochemistry, and hydrogeochemical characterizations of microbialites of five aquatic systems (Bacalar, Muyil, Chichancanab, Azul and Cenote Azul) in southeastern Yucatan Peninsula, México. Dominant taxa were distributed within Pseudomonadota, Cyanobacteriota, Bacillota, Bacteroidota, Chloroflexota, and Planctomycetota, while NB1-j, Myxoscoccota, Verrucomicrobiota, Acidobacteriota, and Crenarchaeota (Archaea) were less abundant. Microbialites from Cenote Azul, a deep sinkhole, were the most different and biodiverse. Notably, potential new families of Cyanobacteriota were observed in all microbialite sites. The primary mineral constituents in microbialites were calcite, magnesian calcite, and gypsum. Hydrogeochemical conditions differed among sites despite their hydrological connectivity. Overall, the karstic ecosystem, hydrogeochemical conditions, tropical climate, and shallow coastal landscapes have favored the occurrence of microbialites in the Yucatan Peninsula, a hotspot region for the formation of these communities. However, their safeguarding becomes crucial, emphasizing the urgency of our role in environmental conservation, in the face of challenging conditions associated with climate change and increased anthropogenic activities detrimental to the environment.

## Full-text entities

- **Species:** Acidobacteriota (phylum) [taxon 57723]

## Figures

11 figures with captions in the complete paper: https://tomesphere.com/paper/PMC12057922/full.md

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Source: https://tomesphere.com/paper/PMC12057922