Calcium carbonate precipitation by cave bacteria isolated from Kashmir Cave, Khyber Pakhtunkhwa, Pakistan.

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Tytuł:: Calcium carbonate precipitation by cave bacteria isolated from Kashmir Cave, Khyber Pakhtunkhwa, Pakistan.
Autorzy:: Jan SU; Department of Microbiology, Quaid-i-Azam University, Islamabad, Pakistan.
Zada S; Department of Environmental Engineering, Guangdong Technion-Israel Institute of Technology, Shantou, China.
Rafiq M; Department of Microbiology, Balochistan University of IT, Engineering and Management Sciences, Quetta, Pakistan.
Khan I; Department of Microbiology, Quaid-i-Azam University, Islamabad, Pakistan.
Sajjad W; State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China.
Khan MA; Department of Works (civil), University of Buner, Buner, Pakistan.
Hasan F; Department of Microbiology, Quaid-i-Azam University, Islamabad, Pakistan.
Źródło:: Microscopy research and technique [Microsc Res Tech] 2022 Jul; Vol. 85 (7), pp. 2514-2525. Date of Electronic Publication: 2022 Apr 06.
Typ publikacji:: Journal Article
Język:: English
Imprint Name(s):: Original Publication: New York, NY : Wiley-Liss, c1992-
MeSH Terms:: Bacteria*/genetics
Calcium Carbonate*/chemistry
Chemical Precipitation ; Pakistan ; RNA, Ribosomal, 16S/genetics
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Grant Information:: Higher Education Commission of Pakistan; 2020PC0052 Chinese Academy of Sciences
Contributed Indexing:: Keywords: Kashmir cave; calcium carbonate precipitation; culturable cave bacteria; vaterite
Substance Nomenclature:: 0 (RNA, Ribosomal, 16S)
H0G9379FGK (Calcium Carbonate)
Entry Date(s):: Date Created: 20220407 Date Completed: 20220621 Latest Revision: 20220621
Update Code:: 20240105
DOI:: 10.1002/jemt.24105
PMID:: 35388567
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The participation of numerous physicochemical and biological functions maintains the evolution and expansion of the remarkable nature. Due to its vast applicability in several engineering disciplines, naturally occurring bio-mineralization or microbially induced calcium carbonate (MICP) precipitation is attracting more interest. Cave bacteria contribute to the precipitation of calcium carbonate (CaCO 3 ). In the present study, soil sediments were collected from Kashmir cave, KPK, Pakistan, and plated on B4 specific nutrients limited medium for bacterial isolation and the viable bacterial count was calculated. Three bacterial strains named GSN-11, TFSN-14, and TFSN-15 were capable of precipitating CaCO 3 . These bacterial isolates were identified through 16S rRNA gene sequencing and strain GSN-11 was identified as Bacillus toyonensis, TFSN-14 as Paracoccus limosus and TFSN-15 as Brevundimonas diminuta. Enhanced CaCO 3 precipitation potential of these bacteria strains was observed at 25°C and pH 5. The precipitated CaCO 3 was confirmed by scanning electron microscopy, X-ray powder diffraction, and Fourier transform infra-red spectroscopy. The findings showed that the precipitates were dominated by calcite, aragonite, and nanosize vaterite. Current research suggests that precipitation of CaCO 3 by proteolytic cave bacteria is widespread in Kashmir cave and these bacterial communities can actively contribute to the formation of CaCO 3 by enhancing the pH of the microenvironment. RESEARCH HIGHLIGHTS: Kashmir cave inhabit potentially active bacteria in terms of biogeochemical processes. Cave bacteria significantly precipitated CaCO 3 . Calcite, aragonite, and nanosize vaterite were dominant in precipitates.
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