Temperature governs the distribution of hot spring microbial community in three hydrothermal fields, Eastern Tibetan Plateau Geothermal Belt, Western China

Guo, Liang; Wang, Guangcai; Sheng, Yizhi; Sun, Xiangyu; Shi, Zheming; Xu, Qingyu; Mu, Wenqing

doi:10.1016/j.scitotenv.2020.137574

Cited by 57 publications

(46 citation statements)

References 76 publications

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“…The datasets with the lowest ranges of fitted Z C are those for water samples from neutral or alkaline hot springs in Southwestern Yunnan (Guo et al, 2021), the Eastern Tibetan Plateau (Guo et al, 2020) (see also Fig. 4), the circumneutralto-alkaline subset of New Zealand hot springs (Power et al, 2018), and Bison Pool in Yellowstone National Park, USA (Swingley et al, 2012) (A) Z C -Eh7 fits for hot spring datasets using only bacterial abundances, only archaeal abundances, or combined taxonomic abundances for both domains.…”

Section: Global-scale Analysismentioning

confidence: 99%

“…Dashed lines represent fits with a slope of less than 0.01 V -1 . Numbers for datasets are (1) Bison Pool, Yellowstone National Park (unlike the other datasets, DNA was extracted from biofilm samples) (Swingley et al, 2012), (2) acidic and (3) circumneutral to alkaline New Zealand hot springs (Power et al, 2018), (4) Dallol Geothermal Area (hypersaline and moderate to extremely acidic water) (Belilla et al, 2019), (5) Copahue Volcano-Río Agrio (Lopez Bedogni et al, 2020;Massello et al, 2020), (6) Southwestern Yunnan (seven samples with pH > 7 and two moderately acidic samples) (Guo et al, 2021), (7) Eastern Tibetan Plateau (Guo et al, 2020), (8) Uzon Caldera (nine samples for acidic water and sediment and one high-pH sample) (Peltek et al, 2020), (9) Southern Tibetan Plateau (Ma et al, 2021), (10) Japan Hydrothermal Sediment (Omae et al, 2019). See Figure S1 for individual sample values.…”

Section: Global-scale Analysismentioning

confidence: 99%

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Local and global chemical shaping of bacterial communities by redox potential

Dick

Meng

2021

Preprint

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Thermodynamics predicts a positive correlation between environmental redox potential and oxidation state of molecules; if found for microbial communities it would imply a new kind of deterministic eco-evolutionary process. This study examines evidence for local- and global-scale correlations between oxidation-reduction potential (ORP or Eh) in environmental samples and carbon oxidation state (ZC) of estimated bacterial and archaeal community proteomes. Seventy-nine public datasets for seven environment types (river & seawater, lake & pond, alkaline spring, hot spring, groundwater, sediment, and soil) were analyzed. Taxonomic abundances inferred from high-throughput 16S rRNA gene sequences were combined with NCBI Reference Sequence (RefSeq) proteomes to estimate the amino acid compositions and chemical formulas (CcHhNnOoSs) of community proteomes, which yield ZC. Alkaline hot springs have the lowest ZC for both bacterial and archaeal domains of any environment. Positive global correlations between redox potential and ZC are found for bacterial communities in lake & pond, groundwater, and soil environments, but not archaeal communities, suggesting a broad ecological signal of chemical shaping in Bacteria.

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Section: Global-scale Analysismentioning

confidence: 99%

Section: Global-scale Analysismentioning

confidence: 99%

Local and global chemical shaping of bacterial communities by redox potential

Dick

Meng

2021

Preprint

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“…Temperature is one of the important environmental factors affecting hot spring microorganisms ( Wang et al, 2013 ; Guo et al, 2020 ). For HPB, temperature is an important factor affecting the hydrogen production process ( Guo et al, 2010 ; Ghimire et al, 2015 ).…”

Section: Discussionmentioning

confidence: 99%

Distribution of Hydrogen-Producing Bacteria in Tibetan Hot Springs, China

Yang

et al. 2021

Front. Microbiol.

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Investigating the distribution of hydrogen-producing bacteria (HPB) is of great significance to understanding the source of biological hydrogen production in geothermal environments. Here, we explored the compositions of HPB populations in the sediments of hot springs from the Daggyai, Quzhuomu, Quseyongba, and Moluojiang geothermal zones on the Tibetan Plateau, with the use of Illumina MiSeq high-throughput sequencing of 16S rRNA genes and hydA genes. In the present study, the hydA genes were successfully amplified from the hot springs with a temperature of 46–87°C. The hydA gene phylogenetic analysis showed that the top three phyla of the HPB populations were Bacteroidetes (14.48%), Spirochaetes (14.12%), and Thermotogae (10.45%), while Proteobacteria were absent in the top 10 of the HPB populations, although Proteobacteria were dominant in the 16S rRNA gene sequences. Canonical correspondence analysis results indicate that the HPB community structure in the studied Tibetan hot springs was correlated with various environmental factors, such as temperature, pH, and elevation. The HPB community structure also showed a spatial distribution pattern; samples from the same area showed similar community structures. Furthermore, one HPB isolate affiliated with Firmicutes was obtained and demonstrated the capacity of hydrogen production. These results are important for us to understand the distribution and function of HPB in hot springs.

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“…Nonetheless, the differences GUO ET AL. We also compared microbial compositions of this study with three alkaline hot spring samples in our previous study in Sichuan geothermal fields, eastern Tibetan Plateau (Guo et al, 2020). The three samples were added in Figure 5.…”

Section: Microbial Diversity and Composition Of Hot Springs Between Acidic And Alkaline Springsmentioning

confidence: 99%

Hydrogeochemical Constraints Shape Hot Spring Microbial Community Compositions: Evidence From Acidic, Moderate‐Temperature Springs and Alkaline, High‐Temperature Springs, Southwestern Yunnan Geothermal Areas, China

et al. 2021

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As the most prominent feature of hot springs, springwater temperature is highly related to the heat source, circulation depth, tectonic activity, and reservoir temperatures (Du et al., 2005; Guo et al., 2017). High-temperature hot springs usually have deep circulation depths and emerge from hydrothermal fields with a high frequency of tectonic activities and large terrestrial heat flow values. In contrast, low/moderate-temperature hot springs have shallow circulation depths or mix with shallow cold groundwater (

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Temperature governs the distribution of hot spring microbial community in three hydrothermal fields, Eastern Tibetan Plateau Geothermal Belt, Western China

Cited by 57 publications

References 76 publications

Local and global chemical shaping of bacterial communities by redox potential

Local and global chemical shaping of bacterial communities by redox potential

Distribution of Hydrogen-Producing Bacteria in Tibetan Hot Springs, China

Hydrogeochemical Constraints Shape Hot Spring Microbial Community Compositions: Evidence From Acidic, Moderate‐Temperature Springs and Alkaline, High‐Temperature Springs, Southwestern Yunnan Geothermal Areas, China

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