Champagne Pool
Champagne Pool is a prominent geothermal feature within the Waiotapu geothermal area in the North Island of New Zealand. The terrestrial hot spring is located about southeast of Rotorua and about northeast of Taupo. The name Champagne Pool is derived from the abundant efflux of carbon dioxide (CO), similar to a glass of bubbling champagne. The hot spring was formed 900 years ago by a hydrothermal eruption, which makes it in geological terms a relatively young system. Its crater is about in diameter with a maximum depth around and is filled with an estimated volume of of geothermal  fluid. Hydrochemistry. The deep geothermal water below Champagne Pool is of the order of but water temperature within the pool is maintained at to by losing heat to the atmosphere. The pH of 5.5 is relatively constant due to buffering by the flux of CO. Gases are mainly CO, but to lesser extent nitrogen (N), methane (CH), hydrogen (H), hydrogen sulphide (HS), and traces of oxygen (O). The siliceous geothermal fluid is oversaturated with metalloid compounds such as orpiment (AsS) and stibnite (SbS), which precipitate and form orange subaqueous deposits. The colourful deposits are in sharp contrast to the grey -white silica sinter surrounding Champagne Pool. Biology. Although Champagne Pool is geochemically well characterised, few studies have addressed its role as a potential habitat for microbial life forms. H and either CO or O would be available as metabolic energy sources for autotrophic growth of methanogenic or hydrogen-oxidising microorganisms. Culture-independent methods provided evidence for filamentous, coccoid, and rod-shaped cell morphologies in the hot spring. Two novel bacteria and a novel archaeon have been successfully isolated from Champagne Pool. Bacterial isolate CP.B2 named "Venenivibrio stagnispumantis" tolerates relatively high concentrations of arsenic and antimony compounds and represents a novel  genus and species within the order Aquificales.