Geothermal hot springs are a natural laboratory to study microbial adaptation to a wide range of temperatures reaching up to boiling. Temperature gradients lead to distinct microbial communities that inhabit their optimum niches. We sampled three distant but chemically similar hot springs in Yellowstone and Iceland that had outflows and presented a wide range of temperatures. The microbial composition at different niches was determined by deep DNA sequencing of rRNA gene amplicons. Over three dozen phyla of Archaea and Bacteria were identified, representing over 1700 unique organisms. We observed a significant reduction in the number of microbial taxa as the temperature increased from warm (38ºC) to boiling. The community structure was primarily driven by temperature and was similar between Yellowstone and Iceland, suggesting that the environment rather than biogeographic location play the largest role in the microbial ecology of hot springs. sterile 100mL Pyrex glass bottles, capped with no air headspace and secured using butyl rubber stoppers and aluminum crimps. Microbial mats and sediments (~1-2 grams) from one of the low volume outflow were collected using sterile syringes and stainless steel spatulas and placed into plastic tubes containing ceramic beads and 750µl Xpedition™ Lysis/Stabilization Solution (Zymo Research, Irvine, CA) and lysed by bead-beating for one minute with a battery-operated tube shaker. That ensured cellular lysis, inactivation of degradative enzymes and stabilization of the DNA until further processing. A total of seven different spots were sampled from and around the Vadmalahver spring, ranging from 98 to ºC. (Figure 1 and Table 1). The main source of an adjacent spring (temperature of 92ºC) that flows into Hveraholmi was also collected, as well as mat and water samples from the swimming pool (38ºC). The microbial community from the swimming lagoon (250 ml water sample) was collected on a Sterivex 0.2 mm syringe filter and preserved by adding Xpedition solution into the filter cartridge and then capping. A microbial mat sample was collected from a rock in the pool and processed as were the other mat samples. After reaching the laboratory the preserved samples were stored at -20ºC until DNA extraction or at 4ºC (water for geochemical analyses or high temperature, >80ºC sediments).The second location in Iceland was also an alkaline spring (pH 8.0) at the Hurdavbaksvegur farmland, in the Borgarfjörður region [GPS coordinates 64º41'18" N, 21º24'10" W] approximately 80 km NW of Flúðir. Samples were collected on June 16, 2016. Five sampling spots were selected, with temperatures ranging from 99-102ºC (the source spring) to 46ºC in the outflowing channel (Figure 2 and Table 1). Sample collection and processing were performed as described above.Yellowstone National Park hot spring samples. Microbial mats, sediment, and water samples were collected on December 31, 2016 at Mirror Pool, an alkaline (pH 8.0) thermal feature from the Upper Geyser Basin [GPS coordinates 44º28'59" N, 110º51'01" W]. ...