An
endolith is an
extremophile organism (
archaea,
bacterium, or
fungus) that lives inside
rock or in the pores between
mineral grains.
Endoliths have been found in rock down to a depth of ~2
miles (3
km), though it is unknown if that is their limit. Possible limitations do not result from the pressure in such depth, but from the increased temperature. Judging from
hypothermophile[?] organisms, the temperature limit is at about 110°
C, which limits the possible depth to 4 km below the
continental crust, and 7 km below the
ocean floor.
Endoliths can survive by feeding on traces of
iron,
potassium, or
sulfur. Whether they
metabolize these directly from the surrounding rock, or rather
excrete an
acid to dissolve them first, remains to be seen.
As water and nutrients are rather sparse, endoliths have a very slow procreation cycle. Early data suggests that some only engage in cell division once every hundred years.
As most endoliths are
autotroph[?], they can generate organic compounds essential for their survival on their own from inorganic matter. Inevitably, some endoliths have specialized in feeding on their autotroph relatives. The micro-
biotope of the different endolithic species is called
SLiME (Subsurface Lithotrophic Microscopic Environment).
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