SIGNIFICANCE OF BACTERIA IN NATURAL AND EXPERIMENTAL SEDIMENTATION OF CARBONATES, PHOSPHATES, AND SILICATES

dc.contributor.author	Ushatinskaya G.T.
dc.contributor.author	Zhegallo E.A.
dc.contributor.author	Gerasimenko L.M.
dc.contributor.author	Zaitseva L.V.
dc.contributor.author	Orleanskii V.K.
dc.date.accessioned	2025-05-10T04:38:21Z
dc.date.available	2025-05-10T04:38:21Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=13506717
dc.identifier.citation	Paleontological Journal, 2006, 40, 4,
dc.identifier.issn	0031-0301
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/49205
dc.description.abstract	The role of bacteria in sedimentation of phosphorites, siliceous and carbonate rocks is discussed. Preservation of bacterial bodies in fossil condition, even in very ancient deposits, is connected with their very early mineralization. A series of laboratory experiments allowed conditions to be reproduced that could have led to mineralization of cyanobacteria and their preservation in sedimentary deposits. The experiments have also shown the important role of cyanobacteria and their metabolic products in the formation of some carbonate minerals, as well as in the accumulation of stromatolites. © Pleiades Publishing, Inc. 2006.
dc.subject	BACTERIAL PALEONTOLOGY
dc.subject	CYANOBACTERIA
dc.subject	EXPERIMENTAL GEOMICROBIOLOGY
dc.subject	STROMATOLITES
dc.title	SIGNIFICANCE OF BACTERIA IN NATURAL AND EXPERIMENTAL SEDIMENTATION OF CARBONATES, PHOSPHATES, AND SILICATES
dc.type	Статья
dc.identifier.doi	10.1134/S0031030106100121

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