Chondroitin sulfate is involved in the hypercalcification of the organic matrix of bovine peritubular dentin.

Apatitic mineral of dentin forms within the collagenous matrix (intertubular dentin, ITD) secreted from the odontoblastic processes (OP). Highly calcified mineral (peritubular dentin, PTD) is deposited at the interface between the ITD and each process membrane, creating a tubular system penetrating the dentin that extends from the dentino-enamel junction to the predentin-dentin junction. We focus on determining the composition of the PTD both with regard to its organic matrix and the inorganic phase.

Peritubular dentin, a highly mineralized, non-collagenous, component of dentin: isolation and capture by laser microdissection.

We demonstrate the capability and technique to perform microdissection and isolation of select regions of untreated, mineralized dentin using laser capture. Dentin is a complex, non-homogeneous tissue comprised of a mineralized collagenous matrix (intertubular dentin [ITD]), odontoblastic processes (ODPs), a void space (tubules) that forms within the ITD left behind by the retraction of ODPs during dentin maturation, and a highly mineralized non-collagenous component that exists at the interface between the tubules and ITD known as peritubular dentin (PTD). PTD forms as the dentin matures.

Water in the formation of biogenic minerals: peeling away the hydration layers.

Minerals of biogenic origin form and crystallize from aqueous environments at ambient temperatures and pressures. The in vivo environment either intracellular or intercellular, contains many components that modulate both the activity of the ions which associate to form the mineral, as well as the activity and structure of the crowded water. Most of the studies about the mechanism of mineralization, that is, the detailed pathways by which the mineral ions proceed from solution to crystal state, have been carried out in relatively dilute solutions and clean solutions.

Biomineralization mechanisms: a new paradigm for crystal nucleation in organic matrices.

There is substantial practical interest in the mechanism by which the carbonated apatite of bone mineral can be initiated specifically in a matrix. The current literature is replete with studies aimed at mimicking the properties of vertebrate bone, teeth, and other hard tissues by creating organic matrices that can be mineralized in vitro and either functionally substitute for bone on a permanent basis or serve as a temporary structure that can be replaced by normal remodeling processes. A key element in this is mineralization of an implant with the matrix and mineral arranged in the proper orientations and relationships.

Rediscovering Hydrogel-Based Double-Diffusion Systems for Studying Biomineralization.

For those seeking to model biomineralization in vitro, hydrogels can serve as excellent models of the extracellular matrix (ECM) microenvironment. A major challenge posed in implementing such systems is the logistics involved, from fundamental engineering to experimental design. For the study of calcium phosphate (e.

Sea urchin tooth mineralization: calcite present early in the aboral plumula.

In both vertebrate bone, containing carbonated hydroxyapatite as the mineral phase, and in invertebrate hard tissue comprised of calcium carbonate, a popular view is that the mineral phase develops from a long-lived amorphous precursor which later transforms into crystal form. Important questions linked to this popular view are: when and where is the crystallized material formed, and is amorphous solid added subsequently to the crystalline substrate? Sea urchin teeth, in which the earliest mineral forms within isolated compartments, in a time and position dependent manner, allow direct investigation of the timing of crystallization of the calcite primary plates. Living teeth of the sea urchin Lytechinus variegatus, in their native coelomic fluid, were examined by high-energy synchrotron X-ray diffraction.

Hydroxyapatite nanoparticle-containing scaffolds for the study of breast cancer bone metastasis.

Breast cancer frequently metastasizes to bone, where it leads to secondary tumor growth, osteolytic bone degradation, and poor clinical prognosis. Hydroxyapatite Ca(10)(PO(4))(6)(OH)(2) (HA), a mineral closely related to the inorganic component of bone, may be implicated in these processes. However, it is currently unclear how the nanoscale materials properties of bone mineral, such as particle size and crystallinity, which change as a result of osteolytic bone remodeling, affect metastatic breast cancer.

Digital microfluidics and delivery of molecular payloads with magnetic porous silicon chaperones.

Digital microfluidics involves the manipulation of molecules and materials in discrete packages. This paper reviews our work using amphiphilic magnetic microparticles constructed from porous silicon. An individual porous particle can be used to carry a nanomole or smaller quantities of a reagent, and assemblies of the particles can encapsulate and transport microliter droplets of liquid containing inorganic, organic, or biological molecules.

Manipulation of liquid droplets using amphiphilic, magnetic one-dimensional photonic crystal chaperones.

The controlled manipulation of small volumes of liquids is a challenging problem in microfluidics, and it is a key requirement for many high-throughput analyses and microassays. One-dimensional photonic crystals made from porous silicon have been constructed with amphiphilic properties. When prepared in the form of micrometre-sized particles and placed in a two-phase liquid such as dichloromethane/water, these materials will accumulate and spontaneously align at the interface.