Abstract

Little is known about the distribution and ecological functions of abundant, intermediate, and rare biospheres and their correlations with environmental factors in hot springs. Here, we explored the microbial community composition of total, abundant, intermediate, and rare biospheres in 66 Tibetan hot springs (pairwise geographic distance 0–610 km, temperature 32–86°C, pH 3.0–9.5, and salinity 0.13–1.32 g/L) with the use of Illumina MiSeq high-throughput sequencing. The results showed that the abundant sub-communities were mainly composed of Chloroflexi, Proteobacteria, Deinococcus-Thermus, Aquificae, Bacteroidetes, and Firmicutes. In contrast, the rare sub-communities mainly consisted of most newly proposed or candidate phyla of Dictyoglomi, Hydrogenedentes, Atribacteria, Hadesarchaea, Aminicenantes, Microgenomates, Calescamantes, Omnitrophica, Altiarchaeales, and Chlamydiae. However, the abundant and rare sub-communities shared some common phyla (e.g., Crenarchaeota, Bathyarchaeota, and Chlorobi), which were composed of different OTUs. The abundant, intermediate, and rare sub-communities were mainly influenced by different environmental variables, which could be ascribed to the fact that they may have different growth and activity and thus respond differently to these variables. Spatial factors showed more contribution to shaping of the intermediate and rare communities than to abundant sub-community, suggesting that the abundant taxa were more easily dispersed than their rare counterparts among hot springs. Microbial ecological function prediction revealed that the abundant and rare sub-communities responded differently to the measured environmental factors, suggesting they may occupy different ecological niches in hot springs. The rare sub-communities may play more important roles in organic matter degradation than their abundant counterparts in hot springs. Collectively, this study provides a better understanding on the microbial community structure and potential ecological functions of the abundant and rare biospheres in hot spring ecosystems. The identified rare taxa provide new opportunities of ecological, taxonomic and genomic discoveries in Tibetan hot springs.

Highlights

  • Microbes are the dominant life form in hot springs, and their community compositions are commonly linked with ecological functions

  • For dissolved organic carbon (DOC) analysis, hot spring water was filtrated through 0.7-mm Whatman GF/F filters followed by acidification with concentrated phosphoric acid

  • The hot springs in this study possessed a range of temperature (32–86◦C), pH (3.0–9.5), salinity (0.13–1.32 g/L), and DOC (0– 958.60 mg/L) and total organic carbon (TOC) (0–12.60%) contents (Supplementary Table S1)

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Summary

Introduction

Microbes are the dominant life form in hot springs, and their community compositions are commonly linked with ecological functions. A large number of microbial investigations have been performed in hot springs worldwide, such as Yellowstone National Park (Meyer-Dombard et al, 2005) and the Great Basin in the United States (Costa et al, 2009), Kamchatka in Russia (Kublanov et al, 2009), Malaysian (Chan et al, 2015), Yunnan (Hou et al, 2013), and Tibetan Plateau in China (Lau et al, 2009; Song et al, 2010, 2013; Huang et al, 2011; Wang et al, 2013) Among some of these previous studies, temperature was shown more important in shaping microbial community than other environmental parameters (e.g., pH and water chemistry) and spatial factors (biogeography) (Skirnisdottir et al, 2000; Pearson et al, 2008; Hou et al, 2013; Wang et al, 2013; Saxena et al, 2017). Few researches have ever investigated the relative contribution of environmental and spatial factors to shaping of microbial communities in hot springs

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