Innate Biomineralization

Exploring the Link Between Autophagy-Lysosomal Dysfunction and Early Heterotopic Ossification in Tendons

Heterotopic ossification (HO), the pathological formation of bone within soft tissues such as tendon and muscle, is a notable complication resulting from severe injury. While soft tissue injury is necessary for HO development, the specific molecular pathology responsible for trauma-induced HO remains a mystery. The previous study detected abnormal autophagy function in the early stages of tendon HO. Nevertheless, it remains to be determined whether autophagy governs the process of HO generation. Here, trauma-induced tendon HO model is used to investigate the relationship between autophagy and tendon calcification. In the early stages of tenotomy, it is observed that autophagic flux is significantly impaired and that blocking autophagic flux promoted the development of more rampant calcification. Moreover, Gt(ROSA)26sor transgenic mouse model experiments disclosed lysosomal acid dysfunction as chief reason behind impaired autophagic flux. Stimulating V-ATPase activity reinstated both lysosomal acid functioning and autophagic flux, thereby reversing tendon HO. This present study demonstrates that autophagy-lysosomal dysfunction triggers HO in the stages of tendon injury, with potential therapeutic targeting implications for HO.

Enhanced osteogenic differentiation potential of Arnica montana and Bellis perennis in C3H10T1/2 multipotent mesenchymal stem cells

BACKGROUND

Arnica montana and Bellis perennis are two medicinal plants that are thought to accelerate bone repair in homoeopathic literature. Mesenchymal stem cells (MSCs) are multipotent stem cells with the ability to differentiate and regenerate bone or osteogenesis. Hence, we aimed to determine the role of Arnica montana and Bellis perennis on the osteogenic differentiation of the C3H10T1/2 stem cell line.

METHODS AND RESULTS

The cell proliferation of Arnica montana and Bellis perennis was evaluated by MTT assay. Osteogenic differentiation of C3H10T1/2 was induced by the addition of β-glycerophosphate, ascorbic acid and dexamethasone in the differentiation medium over 3 weeks. Cells were treated with Arnica montana and Bellis perennis individually as well as in combination. The osteogenic differentiation potential of Arnica montana and Bellis perennis to differentiate C3H10T1/2 into osteoblasts was measured by alkaline phosphatase activity, alizarin red staining and the expression of Osteocalcin using immunostaining and qRT-PCR. Arnica montana and Bellis perennis could enhance C3H10T1/2 cell proliferation at 1600 µg. Further, the compound showed the ability to augment osteogenesis as confirmed by increased expression of alkaline phosphatase and enhanced calcium accumulation as seen by the Alizarin Red staining and quantification. Enhanced osteogenesis was further supported by the increased expression of osteocalcin in the treated cells with individual and combined doses of Arnica montana and Bellis perennis. Therefore, the findings provide additional support for the positive impact of Arnica montana and Bellis perennis on bone formation.

CONCLUSIONS

Our findings suggest that homoeopathic compounds Arnica montana and Bellis perennis can augment osteogenesis individually as well as in combination.

Biomimetic mineralization based on self-assembling peptides

Biomimetic science has attracted great interest in the fields of chemistry, biology, materials science, and energy. Biomimetic mineralization is the process of synthesizing inorganic minerals under the control of organic molecules or biomolecules under mild conditions. Peptides are the motifs that constitute proteins, and can self-assemble into various hierarchical structures and show a high affinity for inorganic substances. Therefore, peptides can be used as building blocks for the synthesis of functional biomimetic materials. With the participation of peptides, the morphology, size, and composition of mineralized materials can be controlled precisely. Peptides not only provide well-defined templates for the nucleation and growth of inorganic nanomaterials but also have the potential to confer inorganic nanomaterials with high catalytic efficiency, selectivity, and biotherapeutic functions. In this review, we systematically summarize research progress in the formation mechanism, nanostructural manipulation, and applications of peptide-templated mineralized materials. These can further inspire researchers to design structurally complex and functionalized biomimetic materials with great promising applications.

Phylogeny and chemistry of biological mineral transport

Three physiologically mineralizing tissues - teeth, cartilage and bone - have critical common elements and important evolutionary relationships. Phylogenetically the most ancient densely mineralized tissue is teeth. In jawless fishes without skeletons, tooth formation included epithelial transport of phosphates, a process echoed later in bone physiology. Cartilage and mineralized cartilage are skeletal elements separate from bone, but with metabolic features common to bone. Cartilage mineralization is coordinated with high expression of tissue nonspecific alkaline phosphatase and PHOSPHO1 to harvest available phosphate esters and support mineralization of collagen secreted locally. Mineralization in true bone results from stochastic nucleation of hydroxyapatite crystals within the cross-linked collagen fibrils. Mineral accumulation in dense collagen is, at least in major part, mediated by amorphous aggregates - often called Posner clusters - of calcium and phosphate that are small enough to diffuse into collagen fibrils. Mineral accumulation in membrane vesicles is widely suggested, but does not correlate with a definitive stage of mineralization. Conversely mineral deposition at non-physiologic sites where calcium and phosphate are adequate has been shown to be regulated in large part by pyrophosphate. All of these elements are present in vertebrate bone metabolism. A key biological element of bone formation is an epithelial-like cellular organization which allows control of phosphate, calcium and pH during mineralization.