Metabolism/ja: Difference between revisions

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[[Chemolithotroph]]~~y is a type of metabolism found in~~ [[prokaryote]]~~s where energy is obtained from the oxidation of~~ [[inorganic compound]]~~s. These organisms can use~~ [[hydrogen]]~~, reduced~~ [[sulfur]] ~~compounds (such as~~ [[sulfide]], [[hydrogen sulfide]] ~~and~~ [[thiosulfate]]), [[Iron(II) oxide|~~ferrous iron (Fe(II))~~]] or [[ammonia]] ~~as sources of reducing power and they gain energy from the oxidation of these compounds. These microbial processes are important in global~~ [[~~biogeochemical cycle~~]]~~s such as~~ [[~~acetogenesis~~]], [[~~nitrification~~]] ~~and~~ [[~~denitrification~~]] ~~and are critical for~~ [[fertility (soil)|~~soil fertility~~]].

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 {{further/ja|Microbial metabolism/ja|Nitrogen cycle/ja}}
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+[[Chemolithotroph/ja|ケモリソトロフ]]は[[prokaryote/ja|原核生物]]に見られる代謝の一種で、[[inorganic compound/ja|無機化合物]]の酸化からエネルギーを得る。これらの生物は還元力の源として[[hydrogen/ja|水素]]、還元された[[sulfur/ja|硫黄]]化合物（[[sulfide/ja|硫化物]]、[[hydrogen sulfide/ja|硫化水素]]、[[thiosulfate/ja|チオ硫酸]]など）、[[Iron(II) oxide/ja|鉄（Fe（II））]]、または[[ammonia/ja|アンモニア]]を用いることができ、これらの化合物の酸化からエネルギーを得る。これらの微生物プロセスは、[[acetogenesis/ja|酢酸生成]]、[[nitrification/ja|硝化]]、[[denitrification/ja|脱窒]]などの地球規模の[[biogeochemical cycle/ja|生物地球化学サイクル]]において重要であり、[[:en:fertility (soil)|土壌肥沃度]]にとって重要である。
-[[Chemolithotroph]]y is a type of metabolism found in [[prokaryote]]s where energy is obtained from the oxidation of [[inorganic compound]]s. These organisms can use [[hydrogen]], reduced [[sulfur]] compounds (such as [[sulfide]], [[hydrogen sulfide]] and [[thiosulfate]]), [[Iron(II) oxide|ferrous iron (Fe(II))]] or [[ammonia]] as sources of reducing power and they gain energy from the oxidation of these compounds. These microbial processes are important in global [[biogeochemical cycle]]s such as [[acetogenesis]], [[nitrification]] and [[denitrification]] and are critical for [[fertility (soil)|soil fertility]].
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