“…In addition to the unusual high temperature, various dissolved minerals, such as magnesium, calcium, sodium, chlorides, sulfates, or silica, generally distinguish geothermal water from nongeothermal groundwater [10], thus supporting the presence of distinct microbial communities. For decades, researchers have been exploring the microbial diversity of thermal ecosystems in different continents worldwide, including the near-boiling silica-depositing thermal springs at Yellowstone National Park in the USA [11], hot springs with a wide range temperature (22-75 • C) across the Tibetan Plateau of China [12], intertidal hot springs of Iceland [13], acidic thermal pools of Russia [14], and alkaline hot springs of Kenya [15], using traditional culture-dependent methods [16][17][18], as well as recently developed high-throughput sequencing [15,18]. Novel thermophilic, alkaliphilic, and metal-tolerant species able to produce valuable biotechnological products, such as antibiotics [8], bioethanol [19], and thermostable enzymes [20], have been frequently discovered from hot springs [5,19,21].…”