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Thermophile

Organism that thrives at relatively high temperatures

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Through Bacteria, Fungus and Earth

Thermophiles are found in geothermally heated regions of the Earth, such as hot springs like those in Yellowstone National Park and deep sea hydrothermal vents, as well as decaying plant matter, such as peat bogs and compost. They can live at high temperatures, whereas other bacteria or archaea would be damaged and sometimes killed if exposed to the same temperatures.

The enzymes in thermophiles function at high temperatures. Some of these enzymes are used in molecular biology, for example the Taq polymerase used in PCR. "Thermophile" is derived from Greek: θέρμη, romanized: thérmē "heat", and Greek: φιλία, romanized: philía "love".

Comparative surveys suggest that thermophile diversity is principally driven by pH, not temperature.

Classification

Thermophiles can be classified in various ways. One classification sorts these organisms according to their optimal growth temperatures:

  1. Simple thermophiles: 50–64 °C (122–147 °F)
  2. Extreme thermophiles 65–79 °C (149–174 °F)
  3. Hyperthermophiles 80 °C (176 °F) and beyond, but not below 50 °C (122 °F)

In a related classification, thermophiles are sorted as follows:

  1. Facultative thermophiles (also called moderate thermophiles) can thrive at high temperatures, but also at lower temperatures (below 50 °C (122 °F)), whereas
  2. Obligate thermophiles (also called extreme thermophiles) require such high temperatures for growth.
  3. Hyperthermophiles are particularly extreme thermophiles for which the optimal temperatures are above 80 °C (176 °F).

Many hyperthermophilic Archaea require elemental sulfur for growth. Some are anaerobes that use the sulfur instead of oxygen as an electron acceptor during anaerobic cellular respiration. Some are lithotrophs that oxidize sulphur to create sulfuric acid as an energy source, thus requiring the microorganism to be adapted to very low pH (i.e., it is an acidophile as well as thermophile). These organisms are inhabitants of hot, sulfur-rich environments usually associated with volcanism, such as hot springs, geysers, and fumaroles. In these places, especially in Yellowstone National Park, zonation of microorganisms according to their temperature optima occurs. These organisms are often colored, due to the presence of photosynthetic pigments.

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