Biomimetic Mineralization of Ca-Mg Carbonates: Relevance to Microbial Cells and Extracellular Polymeric Substances

Research on Ca-Mg carbonate crystallization and phase transition regulated by microbial cells and extracellular polymeric substances (EPS) is significant for carbon sequestration, remediation of polluted soil and water, and synthesis of functional biomaterials. This study focused on the mineralogical transformation from amorphism to crystal, and interaction among cells, EPS, and minerals. By tracing the law of mineral growth and morphological evolution, the influences of cells and EPS on mineral formation were investigated. The results revealed that calcification and the template of rod-shaped cells of strain HJ-1 were the basis for the formation of dumbbell-shaped particles, and directional aggregation and differential growth were the keys to the development and stability of dumbbells. Cell participation had a noticeable impact on mineral prototypes, instead of determining the polymorphism. EPS contributed to aragonite formation and stability. The acidic amino acids or proteins in EPS were likely to cause an increase in MgCO3 content in Mg-calcite. EPS promoted aggregation of particles and induced spherical formation. Exopolysaccharides and proteins were the main components of EPS that can affect carbonate mineralization. EPS could influence the morphology and polymorphism by providing nucleation sites, interacting with Mg2+, adsorbing or incorporating mineral lattices, and inducing particle aggregation.