Concept

Endolith

Summary
An endolith or endolithic is an organism (archaeon, bacterium, fungus, lichen, algae or amoeba) that is able to acquire the necessary resources for growth in the inner part of a rock, mineral, coral, animal shells, or in the pores between mineral grains of a rock. Many are extremophiles, living in places long considered inhospitable to life. The distribution, biomass, and diversity of endolith microorganisms are determined by the physical and chemical properties of the rock substrate, including the mineral composition, permeability, the presence of organic compounds, the structure and distribution of pores, water retention capacity, and the pH. Normally, the endoliths colonize the areas within lithic substrates to withstand intense solar radiation, temperature fluctuations, wind, and desiccation. They are of particular interest to astrobiologists, who theorize that endolithic environments on Mars and other planets constitute potential refugia for extraterrestrial microbial communities. The term "endolith", which defines an organism that colonizes the interior of any kind of rock, has been further classified into five subclasses: Chasmoendolith Colonizes fissures and cracks in the rock connected to the surface (chasm = cleft) Cryptoendolith Colonizes structural cavities within natural pore spaces within the rocks. These pores are usually indirectly connected to the rock surface; (crypto = hidden) Euendolith Penetrates actively into the interior of rocks forming channels and grooves that conform with the shape of its body, rock boring organism (eu = true) Hypoendolith Colonizes the pore spaces located on the underside of the rock and that make contact with the soil (hypo = under) Autoendolith Capable of rocks formation by mineral depositation (auto = self) Endolithic microorganisms have been reported in many areas around the globe. There are reports in warm hyper-arid and arid deserts such as Mojave and Sonora (USA), Atacama (Chile), Gobi (China, Mongolia), Negev (Israel), Namib (Namibia Angola), Al-Jafr basin (Jordan) and the Depression of Turpan (China),, also in cold deserts as Arctic and Antarctic, and deep subsoil and ocean trenches rocks.
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