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).
 
All Wikipedia text 
is available under the 
terms of the GNU Free Documentation License