Raguin, E. | bioRxiv Science

bioRxiv2023

Logistics of Bone Mineralization in the Chick Embryo Studied by 3D Cryo FIB-SEM Imaging

During skeletal development, bone growth and mineralization require transport of substantial amounts of calcium, while maintaining very low concentration. How an organism overcomes this major logistical challenge remains mostly unexplained. To shed some light on the dynamics of this process, we use cryogenic Focused Ion Beam-Scanning Electron Microscopy (cryo-FIB/SEM) to image forming bone tissue at day 13 of a chick embryo femur. We visualize both cells and matrix in 3D and observe calcium-rich intracellular vesicular structures. Counting the number of these vesicles per unit volume and measuring their calcium content based on the electron back-scattering signal, we are able to estimate the intracellular velocity at which these vesicles need to travel to transport all the calcium required for the mineral deposited in one day within the collagenous tissue. We estimate this velocity at 0.27 m/s, which is too large for a diffusion process and rather suggests active transport through the cellular network. We conclude that calcium logistics is hierarchical and based on several transport mechanisms: first through the vasculature using calcium-binding proteins and the blood flow, then active transport over tens of micrometers through the network of osteoblasts and osteocytes and, finally, diffusive transport over the last one or two microns.

systems biology↗

bioRxiv2022

Induced mineralization in Escherichia coli biofilms: the key role of bacterial alkaline phosphatase

Biofilms appear when bacteria colonize a surface and synthesize and assemble extracellular matrix components. In addition to the organic matrix, some biofilms precipitate mineral particles such as calcium phosphate. While calcified biofilms induce diseases like periodontitis in physiological environments, they also inspire the engineering of living composites. Understanding mineralization mechanisms in biofilms will thus provide key knowledge for either inhibiting or promoting mineralization in these research fields. The enzyme alkaline phosphatase (ALP) plays a key role in calcium phosphate precipitation in mammalian bone tissue. Produced by eukaryotic cells, ALP catalyzes the hydrolysis of monophosphates starting from different precursors (e.g., alkaloids, proteins) and makes phosphate ions readily available for the precipitation with calcium. Bacterial ALPs are expressed by the well-characterized gram-negative and gram-positive bacteria E. coli and S. aureus as well as a large number of marine and soil bacteria. While it was recently proposed that bacterial ALPs induce mineral precipitation, their role in biofilm mineralization is not fully understood. In this work, we address this question using the biofilm-forming E. coli K-12 strain W3110, which expresses periplasmic ALP from the phoA gene. We first identify the mineralization conditions of biofilms grown on nutritive agar substrates supplemented with calcium ions and {beta}-glycerophosphate. We then localize the mineral phase at different scales, using light and scanning electron microscopy as well as X-ray microtomography. Wide-angle X-ray scattering enables us to further identify the mineral as being hydroxyapatite. Finally, growing E. coli cells on mineralizing medium supplemented with an ALP inhibitor demonstrates that ALP is essential for biofilm mineralization. This is confirmed with a bacteria-free model, where the deposition of a drop of bacterial ALP solution on calcium and {beta}-glycerophosphate containing agar substrate is sufficient to induce mineralization. Overall, these results will benefit the development of strategies against diseases involving calcified biofilms as well as the engineering of biofilm-based living composites.

microbiology↗