The fossil record shows that osteocytes were present in bones of jawless fish 400 to 250 million years ago. Osteocyte size has been shown to
covary with genome size; and this relationship has been used in paleogenomic research. During bone formation, an
osteoblast is left behind and buried in the bone matrix as an "osteoid osteocyte", which maintains contact with other osteoblasts through extended cellular processes. Although recently it was shown that vascular smooth muscle cells drive osteocyte differentiation, most aspects of osteocytogenesis remain largely unknown. Various molecules have been reported to be involved. Examples include matrix metalloproteinases (MMPs),
dentin matrix protein 1 (DMP-1), osteoblast/osteocyte factor 45 (OF45),
Klotho, TGF-beta inducible factor (TIEG),
lysophosphatidic acid (LPA), E11 antigen, and oxygen. Palumbo et al. (1990) distinguish three cell types from osteoblast to mature osteocyte: type I preosteocyte (osteoblastic osteocyte), type II preosteocyte (osteoid osteocyte), and type III preosteocyte (partially surrounded by mineral matrix). The cell undergoes a dramatic transformation from a polygonal shape to a cell that extends dendrites toward the mineralizing front, followed by dendrites that extend to either the vascular space or bone surface. As the osteoblast transitions to an osteocyte, alkaline phosphatase is reduced, and casein kinase II is elevated, as is
osteocalcin. Oxygen tension may regulate the differentiation of osteoblasts into osteocytes, and osteocyte hypoxia may play a role in disuse-mediated bone resorption. ==Function==