The circularly causal
orchestration of bone production and destruction
is a part of the standard model of bone remodeling, but the crystallinity
of the bone mineral, which naturally alternates during this process,
has not had a steady place in it. Here we show that osteoclasts and
osteoblasts, the cells resorbing and building bone, respectively,
can sense the crystallinity of the bone mineral and adjust their activity
thereto. Specifically, osteoblastic MC3T3-E1 cells secreted mineral
nodules more copiously when they were brought into contact with amorphous
calcium phosphate (ACP) nanoparticles than when they were challenged
with their crystalline, hydroxyapatite (HAp) analogues. Moreover,
the gene expressions of osteogenic markers BGLAP, ALP, BSP-1, and RUNX2 in
MC3T3-E1 cells were higher in the presence of ACP than in the presence
of HAp. At the same time, the dental pulp stem cells differentiated
into an osteoblastic phenotype to a degree that was inversely proportional
to the amount and the crystallinity of the mineral added to their
cultures. In contrast, the resorption of HAp nanoparticles was more
intense than the resorption of ACP, as concluded by the greater retention
of the latter particles inside the osteoclastic RAW264.7 cells after
10 days of incubation and also by the time-dependent free Ca2+ concentration measurements in the cell culture media at early incubation
time points (<1 week), prior to the spontaneous crystallization
of the amorphous phase. A detailed morphological, compositional, and
microstructural characterization of ACP and HAp is provided too, and
it is shown that although ACP transforms to HAp in the cell culture
media, some microstructural properties are retained in the powder
following this transformation, influencing the resorption rate. On
the basis of these findings, a model of bone remodeling at the level
of individual biogenic apatite nanoparticles was proposed, taking
into account the effects of hydration and lattice strain. According
to this model, apatite is a “living” mineral, undergoing
fluctuations in crystallinity within a closed ossifying/resorptive
feedback loop in a way that buffers against potential runaway effects.
A finite degree of amorphousness of every apatite crystal in bone
is seen as a vital prerequisite for a healthy, dynamic bone remodeling
process, and the best bone mineral, from this standpoint, is the living
mineral, the one undergoing a constant process of structural change
in response to biochemical stimuli thanks to its partially amorphous
microstructure and unique interfacial dynamics.