GEOMICROBIOLOGICAL CYCLING OF IRON

dc.contributor.author	Kappler A.
dc.contributor.author	Straub K.L.
dc.date.accessioned	2023-12-30T07:21:39Z
dc.date.available	2023-12-30T07:21:39Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=31306304
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2005, 59, С. , 85-108
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/42394
dc.description.abstract	Iron is the most abundant element on Earth and the most frequently utilized transition metal in the biosphere. It is a component of many cellular compounds and is involved in numerous physiological functions. Hence, iron is an essential micronutrient for all eukaryotes and the majority of prokaryotes. Prokaryotes that need iron for biosynthesis require micromolar concentrations, levels that are often not available in neutral pH oxic environments. Therefore, prokaryotes have evolved specific acquisition molecules, called siderophores, to increase iron bioavailability.
dc.subject	iron cycling
dc.subject	geomicrobiology
dc.title	GEOMICROBIOLOGICAL CYCLING OF IRON
dc.type	Статья
dc.identifier.doi	10.2138/rmg.2005.59.5

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