THE ROLE OF CYANOBACTERIA IN CRYSTALLIZATION OF MAGNESIUM CALCITES

dc.contributor.authorZaitseva L.V.
dc.contributor.authorOrleanskii V.K.
dc.contributor.authorGerasimenko L.M.
dc.contributor.authorUshatinskaya G.T.
dc.date.accessioned2025-06-10T10:13:22Z
dc.date.available2025-06-10T10:13:22Z
dc.date.issued2006
dc.description.abstractLaboratory experiments showed the effect of the cyanobacterium Microcoleus chthonoplastes on the formation of magnesium calcites, using model solutions (2.14M MgCl2-0.05M CaCl2-0.6M NaCl-0.18M NaHCO3). The conditions of existence of cyanobacteria in such solutions in light or darkness significantly alter the structure of the sediment and the shape and size of the carbonate crystals. Cyanobacteria slow down crystallization due to the formation of exometabolites with a chelating effect, which leads to the precipitation of high-magnesium calcites. In the photosynthetic environment the presence of huntite (CaMg3(CO3) 4), possible forerunner of dolomite, is prominent. © Pleiades Publishing, Inc. 2006.
dc.identifierhttps://elibrary.ru/item.asp?id=13525629
dc.identifier.citationPaleontological Journal, 2006, 40, 2, 125-133
dc.identifier.doi10.1134/S003103010602002X
dc.identifier.issn0031-0301
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/49326
dc.subjectCYANOBACTERIA
dc.subjectHIGH MAGNESIUM CALCITE
dc.subjectHUNTITE
dc.subjectPRECIPITATION
dc.titleTHE ROLE OF CYANOBACTERIA IN CRYSTALLIZATION OF MAGNESIUM CALCITES
dc.typeСтатья

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