Temperature-controlled thermophilic bacterial communities in hot springs of western Sichuan, China
Abstract Background Ganzi Prefecture in Western China is situated geographically at the
transition regions between Tibetan Plateau and Sichuan Basin in a highly tectonically active
boundary area between the India and Eurasia plates. The region hosts various hot springs
that span a wide range of temperature from 30 to 98° C and are located at high altitude (up
to 4200 m above sea level) in the region of large geothermal anomalies and active
Xianshuihe slip-fault that has been active since Holocene. The site represents a biodiversity …
transition regions between Tibetan Plateau and Sichuan Basin in a highly tectonically active
boundary area between the India and Eurasia plates. The region hosts various hot springs
that span a wide range of temperature from 30 to 98° C and are located at high altitude (up
to 4200 m above sea level) in the region of large geothermal anomalies and active
Xianshuihe slip-fault that has been active since Holocene. The site represents a biodiversity …
Temperature-controlled thermophilic bacterial communities in hot springs of Western Sichuan, China.
TJ Tang Jie, LYM Liang YuanMei, JD Jiang Dong… - 2018 - cabidigitallibrary.org
Abstract Background: Ganzi Prefecture in Western China is situated geographically at the
transition regions between Tibetan Plateau and Sichuan Basin in a highly tectonically active
boundary area between the India and Eurasia plates. The region hosts various hot springs
that span a wide range of temperature from 30 to 98° C and are located at high altitude (up
to 4200 m above sea level) in the region of large geothermal anomalies and active
Xianshuihe slip-fault that has been active since Holocene. The site represents a biodiversity …
transition regions between Tibetan Plateau and Sichuan Basin in a highly tectonically active
boundary area between the India and Eurasia plates. The region hosts various hot springs
that span a wide range of temperature from 30 to 98° C and are located at high altitude (up
to 4200 m above sea level) in the region of large geothermal anomalies and active
Xianshuihe slip-fault that has been active since Holocene. The site represents a biodiversity …
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