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墨西哥巴卡拉尔泻湖现代微生物岩的微生物组。

The microbiome of modern microbialites in Bacalar Lagoon, Mexico.

机构信息

UNAM, Instituto de Ecología, Parque Científico y Tecnológico de Yucatán, Sierra Papacal, Yucatán, México.

El Colegio de la Frontera Sur Unidad Chetumal, Chetumal, Quintana Roo, Mexico.

出版信息

PLoS One. 2020 Mar 25;15(3):e0230071. doi: 10.1371/journal.pone.0230071. eCollection 2020.

DOI:10.1371/journal.pone.0230071
PMID:32210450
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7094828/
Abstract

Microbialites are highly diverse microbial communities that represent modern examples of the oldest life forms, stromatolites (dated >3.7 Ga). Bacalar Lagoon, in Mexico, harbors the largest freshwater microbialite occurrences of the world; yet diverse anthropogenic activities are changing the oligotrophic conditions of the lagoon. The objective of this work was to perform a spatial exploration of the microbialites of Bacalar Lagoon, analyze their prokaryote diversity, following a high throughput sequencing approach of the V4 region of the 16S rDNA, and correlate to the environmental parameters that influence the structure of these communities. The results indicate the presence of microbialites throughout the periphery of the lagoon. The microbiome of the microbialites is composed primarily of Proteobacteria (40-80%), Cyanobacteria (1-11%), Bacteroidetes (7-8%), Chloroflexi (8-14%), Firmicutes (1-23%), Planctomycetes (1-8%), and Verrucomicrobia (1-4%). Phylogenetic distance analyses suggests two distinct groups of microbialites associated with regions in the lagoon that have differences in their environmental parameters, including soluble reactive silicate (in the north), bicarbonates and available forms of nitrogen (ammonium, nitrates and nitrites) (in the south). These microbialite groups had differences in their microbiome composition associated to strong anthropogenic pressure on water quality (agriculture, landfill leachate, lack of water treatment infrastructure and intensive tourism), which were related to a loss of microbial diversity.

摘要

微生物岩是高度多样化的微生物群落,代表了最古老生命形式——叠层石(可追溯到 37 亿年前)的现代范例。墨西哥的巴卡拉尔泻湖拥有世界上最大的淡水微生物岩矿床;然而,多样化的人为活动正在改变泻湖的贫营养条件。本工作的目的是对巴卡拉尔泻湖的微生物岩进行空间探索,采用高通量测序方法对 16S rDNA 的 V4 区进行分析,研究其原核生物多样性,并与影响这些群落结构的环境参数相关联。结果表明,微生物岩存在于泻湖的周边地区。微生物岩的微生物组主要由变形菌门(40-80%)、蓝藻(1-11%)、拟杆菌门(7-8%)、绿弯菌门(8-14%)、厚壁菌门(1-23%)、浮霉菌门(1-8%)和疣微菌门(1-4%)组成。系统发育距离分析表明,两组不同的微生物岩与泻湖中具有不同环境参数的区域相关,包括可溶解反应性硅(在北部)、碳酸氢盐和可用形式的氮(铵、硝酸盐和亚硝酸盐)(在南部)。这些微生物岩组的微生物组组成存在差异,这与水质的强烈人为压力有关(农业、垃圾填埋场渗滤液、缺乏水处理基础设施和密集的旅游业),这与微生物多样性的丧失有关。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/44eb3aa1377b/pone.0230071.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/d7f07256fdcc/pone.0230071.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/4f7acad3493b/pone.0230071.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/36b1e7231943/pone.0230071.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/9ee6a97aba66/pone.0230071.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/c2e9c897a9ed/pone.0230071.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/44eb3aa1377b/pone.0230071.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/d7f07256fdcc/pone.0230071.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/4f7acad3493b/pone.0230071.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/36b1e7231943/pone.0230071.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/9ee6a97aba66/pone.0230071.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/c2e9c897a9ed/pone.0230071.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ed71/7094828/44eb3aa1377b/pone.0230071.g006.jpg

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