About: Subsurface lithoautotrophic microbial ecosystem     Goto   Sponge   NotDistinct   Permalink

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Subsurface lithoautotrophic microbial ecosystems, or "SLIMEs" (also abbreviated "SLMEs" or "SLiMEs"), are a type of endolithic ecosystems. They are defined by Edward O. Wilson as "unique assemblages of bacteria and fungi that occupy pores in the interlocking mineral grains of igneous rock beneath Earth's surface."

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  • Podziemny litoautroficzny ekosystem mikroorganizmów (pl)
  • Subsurface lithoautotrophic microbial ecosystem (en)
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  • Podziemny litoautroficzny ekosystem mikroorganizmów (ang. Subsurface Lithoautotrophic Microbial Ecosystem, określany skrótami SLiME, SLIME lub SLME) – skupiska bakterii i grzybów zamieszkujących pory pomiędzy ziarnami minerałów w skałach magmowych na głębokościach 3 i więcej kilometrów pod powierzchnią ziemi. SLiME czerpią energię z substancji nieorganicznych. (pl)
  • Subsurface lithoautotrophic microbial ecosystems, or "SLIMEs" (also abbreviated "SLMEs" or "SLiMEs"), are a type of endolithic ecosystems. They are defined by Edward O. Wilson as "unique assemblages of bacteria and fungi that occupy pores in the interlocking mineral grains of igneous rock beneath Earth's surface." (en)
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  • Subsurface lithoautotrophic microbial ecosystems, or "SLIMEs" (also abbreviated "SLMEs" or "SLiMEs"), are a type of endolithic ecosystems. They are defined by Edward O. Wilson as "unique assemblages of bacteria and fungi that occupy pores in the interlocking mineral grains of igneous rock beneath Earth's surface." Endolithic systems are still at an early stage of exploration. In some cases its biota can support simple invertebrates, most organisms are unicellular. Near-surface layers of rock may contain blue-green algae but most energy comes from chemical synthesis of minerals. The limited supply of energy limits the rates of growth and reproduction. In deeper rock layers microbes are exposed to high pressures and temperatures. (en)
  • Podziemny litoautroficzny ekosystem mikroorganizmów (ang. Subsurface Lithoautotrophic Microbial Ecosystem, określany skrótami SLiME, SLIME lub SLME) – skupiska bakterii i grzybów zamieszkujących pory pomiędzy ziarnami minerałów w skałach magmowych na głębokościach 3 i więcej kilometrów pod powierzchnią ziemi. SLiME czerpią energię z substancji nieorganicznych. (pl)
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