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Calcifying Bacteria Flexibility in Induction of CaCO(3) Mineralization

Microbially induced CaCO(3) precipitation (MICP) is considered as an alternative green technology for cement self-healing and a basis for the development of new biomaterials. However, some issues about the role of bacteria in the induction of biogenic CaCO(3) crystal nucleation, growth and aggregati...

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Detalles Bibliográficos
Autores principales: Golovkina, Darya A., Zhurishkina, Elena V., Ivanova, Lyubov A., Baranchikov, Alexander E., Sokolov, Alexey Y., Bobrov, Kirill S., Masharsky, Alexey E., Tsvigun, Natalia V., Kopitsa, Gennady P., Kulminskaya, Anna A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7759876/
https://www.ncbi.nlm.nih.gov/pubmed/33260571
http://dx.doi.org/10.3390/life10120317
Descripción
Sumario:Microbially induced CaCO(3) precipitation (MICP) is considered as an alternative green technology for cement self-healing and a basis for the development of new biomaterials. However, some issues about the role of bacteria in the induction of biogenic CaCO(3) crystal nucleation, growth and aggregation are still debatable. Our aims were to screen for ureolytic calcifying microorganisms and analyze their MICP abilities during their growth in urea-supplemented and urea-deficient media. Nine candidates showed a high level of urease specific activity, and a sharp increase in the urea-containing medium pH resulted in efficient CaCO(3) biomineralization. In the urea-deficient medium, all ureolytic bacteria also induced CaCO(3) precipitation although at lower pH values. Five strains (B. licheniformis DSMZ 8782, B. cereus 4b, S. epidermidis 4a, M. luteus BS52, M. luteus 6) were found to completely repair micro-cracks in the cement samples. Detailed studies of the most promising strain B. licheniformis DSMZ 8782 revealed a slower rate of the polymorph transformation in the urea-deficient medium than in urea-containing one. We suppose that a ureolytic microorganism retains its ability to induce CaCO(3) biomineralization regardless the origin of carbonate ions in a cell environment by switching between mechanisms of urea-degradation and metabolism of calcium organic salts.