Abstract

The bacterium Sporosarcina pasteurii (SP) is known for its ability to cause the phenomenon of microbially induced calcium carbonate precipitation (MICP). We explored bacterial participation in the initial stages of the MICP process at the cellular length scale under two different growth environments (a) liquid culture (b) MICP in a soft agar (0.5%) column. In the liquid culture, ex-situ imaging of the cellular environment indicated that S. pasteurii was facilitating nucleation of nanoscale crystals of calcium carbonate on bacterial cell surface and its growth via ureolysis. During the same period, the meso-scale environment (bulk medium) was found to have overgrown calcium carbonate crystals. The effect of media components (urea, CaCl2), presence of live and dead in the growth medium were explored. The agar column method allows for in-situ visualization of the phenomena, and using this platform, we found conclusive evidence of the bacterial cell surface facilitating formation of nanoscale crystals in the microenvironment. Here also the bulk environment or the meso-scale environment was found to possess overgrown calcium carbonate crystals. Extensive elemental analysis using Energy dispersive X-ray spectroscopy (EDS) and X-ray powder diffraction (XRD), confirmed that the crystals to be calcium carbonate, and two different polymorphs (calcite and vaterite) were identified. Active participation of S. pasteurii cell surface as the site of calcium carbonate precipitation has been shown using EDS elemental mapping with Scanning transmission electron microscopy (STEM) and scanning electron microscopy (SEM).

Highlights

  • Biomineralization of calcium carbonate (CaCO3) or its precipitation due to chemical alteration of the environment induced by the microbial activity is known as microbiologically induced calcium carbonate precipitation (MICP) [1,2,3,4]

  • A comparison of NBUC-7SPdead and NBUC-7SPlive, suggests that bacterial activity led to change in pH; precipitation was observed for NBUC-7SPlive

  • Ureolytic S. pasteurii cells were found to possess cell surface CaCO3 and it was prominent deposited on the cell surface

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Summary

Introduction

Biomineralization of calcium carbonate (CaCO3) or its precipitation due to chemical alteration of the environment induced by the microbial activity is known as microbiologically induced calcium carbonate precipitation (MICP) [1,2,3,4]. Bacteria can participate in the MICP phenomenon by means of various mechanisms such as urea hydrolysis [1, 2], photosynthesis [5, 6], sulfate reduction [7, 8], anaerobic sulfide oxidation [9], biofilm formation [10] and mineral adsorption to extracellular polymeric substances [11, 12].

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