Diversity and structure of prokaryotic assemblages in a thermally stratified tropical lake

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS
Jesús Torres-Huesca , Jazmín Santillán , Yislem Beltrán , Rafael A. López-Martínez , Miroslav Macek , Luisa I. Falcón , Martín Merino-Ibarra , Patricia M. Valdespino-Castillo , Jesús T. Martínez-Díaz , Javier Alcocer , Rocío J. Alcántara-Hernández
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Abstract

The structure and diversity of prokaryotic assemblages in inland waters are strongly related to their habitat. Yet, there is a lack of integrative studies surveying them in different compartments in tropical lakes. This study estimated the diversity and composition of prokaryotic assemblages in sediments, microbialites, and water column in the tropical warm monomictic Lake Alchichica and identified the most representative phylotypes while thermally stratified. The 16S rRNA gene survey showed a distinctive prokaryotic assemblage for each compartment, with 60–78 % of the phylotypes being unique to each one. Sediments accounted for the major prokaryotic diversity in the lake, with chemoorganotrophic bacteria and sulphate reducers as major biogeochemical components. Microbialites showed a high abundance of oxygenic and anoxygenic phototrophs, as well as organotrophs. The prokaryoplancton in the water column was mainly composed of picocyanobacteria and Flavobacteria in the epilimnion, shifting to a high diversity of anaerobic microorganisms in the hypolimnion. These water column assemblages were significantly correlated to pH, ORP, DO, and nutrient concentration. This study shows an integral view of the prokaryotic assemblages in a deep tropical lake related to physicochemical characteristics, from their diversity to their biogeochemical implications, suggesting the role of lake sediments as a possible microbial seed bank.

热分层热带湖泊中原核生物群落的多样性和结构
内陆水域原核生物群的结构和多样性与其栖息地密切相关。然而,目前还缺乏对热带湖泊中不同分区的原核生物进行调查的综合研究。本研究估算了热带暖单相湖阿尔奇奇卡湖中沉积物、微生物岩和水体中原核生物群落的多样性和组成,并确定了热分层时最具代表性的系统型。16S rRNA 基因调查显示,每个分区都有独特的原核生物群,每个分区有 60-78% 的系统型是独一无二的。沉积物是湖中原核生物多样性的主要来源,其中化有机营养细菌和硫酸盐还原菌是主要的生物地球化学成分。微生物岩中富含含氧和缺氧光营养体以及有机营养体。水柱中的原核生物主要由上盐层中的皮蓝藻和黄杆菌组成,到了下盐层,厌氧微生物的多样性增加。这些水柱组合与 pH 值、ORP、溶解氧和营养浓度有明显的相关性。这项研究展示了一个热带深湖中与理化特征相关的原核生物群落从多样性到生物地球化学影响的整体视角,表明湖泊沉积物可能是微生物种子库。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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