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肯尼亚马加迪盐湖微生物群落的时空结构和组成。

Spatiotemporal structure and composition of the microbial communities in hypersaline Lake Magadi, Kenya.

机构信息

Department of Biological Sciences, University of Embu, Embu, Kenya.

Arthropod Pathology, International Centre of Insect Physiology and Ecology, Nairobi, Nairobi County, Kenya.

出版信息

F1000Res. 2024 May 17;13:11. doi: 10.12688/f1000research.134465.2. eCollection 2024.

Abstract

BACKGROUND

Soda lakes are habitats characterized by haloalkaline conditions also known to host unique microbial communities. The water chemistry changes with seasons due to evaporative concentration or floods from the surrounding grounds. However, it is not yet clear if the change in physiochemical changes influences the spatiotemporal diversity and structure of microbial communities in these ecosystems.

METHODS

Using 16S rRNA gene amplicon sequencing, we investigated the diversity and structure of microbial communities in water and brine samples taken from Lake Magadi between June and September 2018. Additionally, physicochemical parameters were also analyzed for every sampling site. Additionally, physicochemical parameters were also analyzed for every sampling site.

RESULTS

The abundant bacterial phyla were Proteobacteria, Cyanobacteria, Bacteroidetes, Actinobacteria, Firmicutes, Verrumicrobia, Deinococcus-Thermus, Spirochaetes, and Chloroflexi. The Archaeal diversity was represented by phyla Euryachaeota, Crenarchaeota, Euryarchaeota, and Thaumarchaeota. The dominant bacterial species were: sp. (10.3%), sp. (9.6%), sp. (5.8%), sp. (3.0%), sp. (2.4%), sp. (2.3%), sp. (2.2%), and sp. (2%). The dominant archaeal species included sp. (18.3%), sp. (5.3%), and sp. (1.3%). The composition of bacteria was higher than that of archaea, while their richness and diversity varied widely across the sampling seasons. The α-diversity indices showed that high diversity was recorded in August, followed by September, June, and July in that order. The findings demonstrated that temperature, pH, P+, K+, NO3 -, and total dissolved solids (TDS) contributed majorly to the diversity observed in the microbial community. Multivariate analysis revealed significant spatial and temporal effects on β-diversity and salinity and alkalinity were the major drivers of microbial composition in Lake Magadi.

CONCLUSIONS

We provide insights into the relationships between microbial structure and geochemistry across various sampling sites in Lake Magadi.

摘要

背景

苏打湖是具有高盐碱性的栖息地,也拥有独特的微生物群落。由于蒸发浓缩或周围地面洪水,水化学性质随季节而变化。然而,目前尚不清楚理化性质的变化是否会影响这些生态系统中微生物群落的时空多样性和结构。

方法

我们使用 16S rRNA 基因扩增子测序,于 2018 年 6 月至 9 月期间调查了马加迪湖(Magadi Lake)的水和卤水样本中的微生物群落多样性和结构。此外,还对每个采样点的理化参数进行了分析。

结果

优势细菌门为变形菌门(Proteobacteria)、蓝细菌门(Cyanobacteria)、拟杆菌门(Bacteroidetes)、放线菌门(Actinobacteria)、厚壁菌门(Firmicutes)、浮霉菌门(Verrucomicrobia)、Deinococcus-Thermus 门、螺旋体门(Spirochaetes)和绿弯菌门(Chloroflexi)。古菌多样性由广古菌门(Euryarchaeota)、泉古菌门(Crenarchaeota)、广古菌门和奇古菌门( Thaumarchaeota)代表。优势细菌物种包括: sp.(10.3%)、 sp.(9.6%)、 sp.(5.8%)、 sp.(3.0%)、 sp.(2.4%)、 sp.(2.3%)、 sp.(2.2%)和 sp.(2%)。优势古菌物种包括 sp.(18.3%)、 sp.(5.3%)和 sp.(1.3%)。细菌组成高于古菌,而它们的丰富度和多样性在采样季节之间差异很大。α多样性指数表明,8 月记录的多样性最高,其次是 9 月、6 月和 7 月。研究结果表明,温度、pH 值、P+、K+、NO3-和总溶解固体(TDS)对微生物群落的多样性有较大影响。多元分析显示,微生物组成存在显著的时空效应,盐度和碱度是马加迪湖微生物组成的主要驱动因素。

结论

我们提供了关于马加迪湖不同采样点微生物结构与地球化学关系的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4720/11555363/3fb0a7185c44/f1000research-13-166004-g0000.jpg

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