Sporosarcina Pasteurii Can Form Nanoscale Crystals on Cell Surface
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bioRxiv preprint doi: https://doi.org/10.1101/184184; this version posted September 4, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. Sporosarcina pasteurii can form nanoscale crystals on cell surface Swayamdipta Bhaduria1,Tanushree Ghosha1, Carlo Montemagnob and Aloke Kumarcd* aDepartment of Mechanical Engineering, University of Alberta, Edmonton AB T6G 2G8, Canada bDepartment of Chemical and Materials Engineering, University of Alberta, Edmonton AB T6G 2G8, Canada cDepartment of Earth and Environmental Engineering, Columbia University, New York NY 10027, USA dDepartment of Mechanical Engineering, Indian Institute of Science, Bangalore KA 560012, India *Corresponding author email: [email protected] Abstract: Using a semi-solid 0.5% agar column, we study the phenomenon of microbially induced mineral (calcium carbonate) by the bacteria Sporosarcina pasteurii. Our platform allows for in-situ visualization of the phenomena, and we found clear evidence of bacterial cell surface facilitating formation of nanoscale crystals. Moreover, in the bulk agar we found the presence of microspheres, which seem to arise from an aggregation of nanoscale crystals with needle like morphology. Extensive chemical characterization confirmed that the crystals to be calcium carbonate, and two different polymorphs (calcite and vaterite) were identified. 1 Equal contributions 1 bioRxiv preprint doi: https://doi.org/10.1101/184184; this version posted September 4, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. Introduction Biomineralization refers to the process of mineral precipitation due to chemical alteration of the environment induced by the microbial activity1-4. For unicellular organisms such as bacteria4, the biomineralization process can be either extracellular5 or intracellular6. Microbially induced calcite precipitation (MICP) is an excellent example of an extracellular mineral deposition. Several microbial species take part in MICP by means of various mechanisms such as photosynthesis7,8, urea hydrolysis1,5, sulfate reduction9,10, anaerobic sulfide oxidation11, biofilm and extracellular polymeric substances12,13. There has been significant interest in microorganisms that can produce urease (urea amidohydrolase; EC 3.5.1.5) and hence are able to hydrolyze urea to induce calcite precipitation14. Sporosarcina pasteurii (formerly Bacillus pasteurii) is a non-pathogenic, endospore producing soil bacteria that also produces urease and can tolerate highly basic environments. S. pasteurii has attracted significant attention from researchers for its unique feature of calcium carbonate precipitation, which can be easily controlled10,15-19. S. pasteurii is being investigated for the possibility of its utilization towards a multitude of applications including underground storage of carbon, healing masonry structures of archaeological importance and long-term sealing of geologic cracks in large-scale structures3,5,20- 24. Hammes and Verstraete (2002) reported the four very important parameters for MICP as pH, dissolved organic carbon, calcium concentration and available nucleation site14. The saturation 2− rate of carbonate ions concentration (CO3 ) is controlled by the first three parameters and it is believed that bacterial cell wall as the nucleation site facilitate the stable and continuous calcium carbonate deposition20. However the bacteria-free solution loaded with urease enzyme can also induce calcium carbonate precipitation. Mitchell and Ferris (2006) studied the influence of bacteria on the nucleation of MICP. The bacteria-free enzyme solution was compared to the bacteria induced environment. Authors reported significant positive effect of bacterial presence (referred as “bacteria-inclusive”) on the increase of size and growth rate of the precipitated crystal though the idea of bacterial control of MICP was rejected. The bacteria-free urease solution showed similarities with the bulk chemical precipitation whereas differences were observed for aqueous microenvironment of bacteria16. It has been suggested that the bacterial cell walls can serve as nucleation sites3,14,23,25 as bacterial cell surfaces carry negatively charged groups at neutral pH26-28. These negative charges can 2 bioRxiv preprint doi: https://doi.org/10.1101/184184; this version posted September 4, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. influence the binding of cations (e.g. Ca2+) on the cell surface and eventually act as nucleation sites when reacting with carbonate anions from the solution to form insoluble calcium carbonate1,26,29. Definitive proofs of involvement of bacterial cell walls in complex environments on the nucleation process are rare. Ghashghaei and Emtiazi reported the presence of nanocrystals of calcium carbonate on cell walls of the bacteria E. ludwigii for experiments performed with a liquid culture30. While the data is suggestive of the role of cell wall, a more definite proof is desirable. In a contrasting study, Bundeleva et al. reported on MICP by the anoxygenic Rhodovulum sp. Their TEM analyses failed to show the existence of CaCO3 on or near live cells31. The authors claim the existence of certain cell protection mechanisms against mineral incrustation at the vicinity of live bacteria and they invoke the idea of mineral precipitation at a certain distance from the cell surface31. Thus, we see that the issue of role of cell wall on mineral precipitation in MICP remains controversial and detailed studies delineating the exact mechanism leading to the nucleation of crystals in in-situ conditions are required to resolve this important biophysical conundrum. To the best of our knowledge, no conclusive reports of the role of cell wall in MICP in complex environments have been reported. Applications of S. pasteurii’s MICP often include their activity in porous media such as concrete and rocks3,20,32-34, where in-situ visualization is often challenging. In order to the address the fundamental mechanism of MICP by S. pasteurii in complex environments, we designed an agar column setup, which allows us to investigate mineral precipitation by direct observation. Our setup consists of a 0.5% agar-column that is stab-inoculated and MICP proceeds in the setup as downward travelling conspicuous mineral trails. We investigate the morphology of precipitated crystals and conclusively demonstrate that the presence of nano-crystals of calcite on the bacterial cell wall. While this can be considered as definitive evidence that the cell wall does serve as a nucleation site, other mechanisms of nucleation are not ruled out. Results and Discussion: Agar Column: To understand growth of S. pasteurii is a porous environment, an agar column with stab culture was observed for a period of one week. Figure 1(a) shows the original culture tubes containg growth spans after day-1 and day-7. Extensive calcite deposition can be 3 bioRxiv preprint doi: https://doi.org/10.1101/184184; this version posted September 4, 2017. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. prominently seen in Figure 1(b) after 7 days of incubation. The agar media acted as soft, porous and transperant nutrient riched environment to monitor the bacterial motility and calcite precipitation. Figure 1c depicts a scanning electron microscopy image of the agar column, where porous structures can clearly be seen. S. pasteurii bacterium possesses flagellum (see Figure S1b) which likely allows it to navigate the porous structure of the agar column. The agar column was sectioned at a depth of 1.25 cm after 4 days, and the bacterial motion observed through optical microscopy. Figure S2 a,b show a motile bacteria within the agar column and the corresponding velocity historgram. The histogram indicates within the agar matrix the bacterium can travel at velocities ~10−7 m/s and hence it can be expected that bacterial cells can travel approximately 1 cm of agar column per day. This ‘seeping speed’ is also corroborated through macroscale observations (Figure 1b). Figure 1d also shows the presence of deposits in the agar column after 7 days of bacterial activity. Calcite micro-spheres: The primary advantage of the agar-column experimental setup is in-situ visualization and easy access for supporting characterizations. The agar column was section at a depth of 2.5 cm after a period of 7 days and crystalline depositions were characterized by other forms of microscopy. Specifically, the agar colunm was characterized using optical microsopy, transmission electron microscopy (TEM), selected area diffraction pattern (SAED) and elemental characteization was determined by powder XRD and energy-dispersive X-ray spectroscopy (EDS). Optical microscopy of ultrathin (~80 nm) sections of the agar medium revealed depositions of crystalline mircrospheres profusely