Carbon dioxide sequestration is an essential component of climate change mitigation, including geologic sequestration the underground storage CO2, and surface sequestration. Carbonate minerals are stable forms of CO2 storage, but their geologic formation is slow. Many microbes alter carbonate mineral morphology; however mechanisms of such mineralization are largely unknown. Hypothesized mechanisms include metabolic processes that alter pH and supersaturation, as well as cell surface properties that induce mineral nucleation. This work systematically investigates these mechanisms by allowing calcium carbonate (CaCO3) formation in the presence or absence of microbes with various native surfaces features including lipopolysaccharides, surface layer proteins (S-layers) and engineered surface features.Surprisingly, formation of stable crystalline CaCO3 was accelerated by the presence of all microbes relative to abiotic solutions. This rate acceleration also occurred for metabolically inactive bacteria, indicating that metabolic activity was not necessary. Rather, since CaCO3 crystals increased in number as the cell density increased, results indicate that many bacterial species accelerate the nucleation of CaCO3 crystals. To understand the role of specific biomolecules on nucleation, we engineered variants of surface layer proteins (S-layers), which are tractable models to evaluate surface interfaces through peptide display. Bacterial surface charge and cation binding was assessed and correlated to bacterial surface chemistry and biomineralization experiments. From these results, we propose that the S-layer surfaces that can selectively attract Ca2+ ions, serve as nucleation sites for CaCO3, thereby accelerating crystal formation, and that engineered variants with selective cation binding enhance this effect. These observations provide substantive evidence for a non-specific nucleation mechanism, and stress the importance of microbes, on the rate of formation of carbonate minerals. This work also indicates that microbes with tuned S-layer surfaces could be used to enhance the sequestration of CO2 as stable mineral carbonates. http://foundry.lbl.gov/afgroup/index.html
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