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在中温和极高温条件下的氢营养型产甲烷作用的性能和微生物群落。

Performance and microbial community of hydrogenotrophic methanogenesis under thermophilic and extreme-thermophilic conditions.

机构信息

State Key Laboratory of Pollution Control and Resource Reuse, Key Laboratory of Yangtze River Water Environment, College of Environmental Science and Engineering, Tongji University, 1239 Siping Road, Shanghai 200092, PR China.

Department of Molecular Biosciences and Bioengineering (MBBE), University of Hawai'i at Mānoa, 1955 East-West Road, Agricultural Science Building 218, Honolulu, HI 96822, USA.

出版信息

Bioresour Technol. 2018 Oct;266:454-462. doi: 10.1016/j.biortech.2018.05.105. Epub 2018 Jun 1.

Abstract

In this study, hydrogenotrophic methanogenesis with respect to methanogenic activity and microbial structures under extreme-thermophilic conditions were examined, and compared with the conventional thermophilic condition. The hydrogenotrophic methanogens were successfully acclimated to the temperatures of 55, 65 and 70 °C. Although acclimation was slower at 65 and 70 °C, hydrogenotrophic methanogenesis remained fairly stable. High-throughput sequencing using 16S rRNA analysis showed that the higher temperatures resulted in single archaea community dominated by hydrogenotrophic Methanothermobacter. Moreover, the syntrophic bacteria changed from Coprothermobacter and Thermodesulfovibrio at 55 °C to Thermodesulfovibrio at 70 °C. Specific hydrogenotrophic methanogenic rate at 70 °C was 98.6 ± 4.2 Nml CH/g VS/hr, which was over 4-folds higher than that 8at 55 °C. The lag phase under extreme-thermophilic conditions was longer than thermophilic condition, which was probably due to the archaeal structure with low diversity. Extreme-thermophilic condition resulted in a shift in methanogenesis pathway from acetoclastic methanogenesis to hydrogenotrophic methanogenesis with the enrichment of Methanothermobacter thermautotrophicus.

摘要

在这项研究中,研究了极端嗜热条件下产甲烷菌的产甲烷活性和微生物结构的氢营养型产甲烷作用,并与传统的嗜热条件进行了比较。氢营养型产甲烷菌成功适应了 55、65 和 70°C 的温度。尽管在 65 和 70°C 时适应较慢,但氢营养型产甲烷作用仍相当稳定。使用 16S rRNA 分析的高通量测序表明,较高的温度导致了由氢营养型 Methanothermobacter 主导的单一古菌群落。此外,从 55°C 的 Coprothermobacter 和 Thermodesulfovibrio 变为 70°C 的 Thermodesulfovibrio。70°C 时的特定氢营养型产甲烷速率为 98.6±4.2Nml CH/g VS/hr,比 55°C 时高 4 倍以上。极端嗜热条件下的滞后期比嗜热条件下长,这可能是由于古菌结构多样性较低所致。极端嗜热条件导致产甲烷途径从乙酰营养型产甲烷作用转变为氢营养型产甲烷作用,伴随着 Methanothermobacter thermautotrophicus 的富集。

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