Regulacin de la mineralizacin sea por factores inorgnicos y peptdicos / Regulation of Bone Mineralization by inorganic and peptide factors

RESUMEN

La mineralizacin ortotpica comienza con la produccin de las vesculas de matriz, por brotacin polarizada de la superficie de condrocitos, osteoblastos y odontoblastos. Esta transcurre en dos etapas. La primera es la formacin de cristales de hidroxiapatita dentro de las vesculas de matriz, seguido por la propagacin de la hidroxiapatita a travs de la membrana de la vescula dentro de la matriz extracelular. En la regulacin de la mineralizacin ortotpica, aparte de las clulas tejido especficas, intervienen un gran nmero de enzimas, factores inorgnicos y peptdicos, que tienen complejas interacciones. Para que la mineralizacin normal contine se necesita un ajustado balance entre los niveles de fosfato inorgnico (Pi) y de pirofosfato inorgnico (PPi) extracelular. El PPi antagoniza la habilidad del Pi para cristalizar con el calcio y formar hidroxiapatita y por lo tanto suprime su propagacin. Se han identificado tres molculas reguladoras centrales de los niveles extracelulares de PPi: la fosfatasa alcalina tejido-no especfica (TNAP), que hidroliza el PPi, la nucletido pirofosfato fosfodiesterasa 1 (NPP1), que genera PPi de nuclesidos trifosfato y la protena transmembrana de mltiples-pasos ANK, que media la transferencia intracelular al extracelular de PPi. A su vez existen dos protenas SIBLING llamadas DMP1 y MEPE reguladoras de la mineralizacin. La expresin de DMP1 por el osteocito se induce en forma marcada en respuesta a la carga mecnica incrementando la mineralizacin sea. La protena MEPE contiene un motivo peptdico proteasa resistente llamado ASARM, que se cree es un candidato a ser un inhibidor de la mineralizacin (minhibina). La osteropontina es otro inhibidor de la mineralizacin en su forma fosforilada y su secrecin est marcadamente reducida en los ratones "knockout" para NPP1. Los datos actuales parecen sostener la hiptesis que estas molculas podran ser las transductoras del "strain" seo y participar en la regulacin de la mineralizacin del espacio osteoctico perilacunar.

ABSTRACT

Orthotopic mineralization begins with the production of matrix vesicles that are produced by polarized budding of the surface of condrocytes, osteoblasts and odontoblasts. It occurs in two steps: The first one is the formation of hydroxiapatite crystals within the matrix vesicles, followed by the propagation of the hydroxiapatite crystals through the membrane vesicle into the extra cellular matrix. In the regulation of orthotopic mineralization, apart from tissue-specific cells, a great number of enzymes, inorganic and peptide factors participate, that have complex interactions among them. Inorganic pyrophosphate (PPi) antagonizes the ability of phosphate (Pi) to crystallize with calcium and to form hydroxiapatite, thus suppressing its propagation. For the normal mineralization to continue, an adjusted balance of the extra cellular Pi and PPi levels is needed. Three molecules have been identified that have a central role in the regulation of extra cellular PPi levels: tissue non-specific alkaline phosphatase (TNAP), which hydrolyzes PPi, the nucleotide pyrophosphatase phosphodiesterase 1 (NPP1), which generates PPi from triphosphate nucleosides, and the multiple-steps transmembrane protein ANK which transfers PPi from the intracellular to the extracellular compartment. There are, in turn, two SIBLING proteins called DMP1 and MEPE that regulate mineralization. The expression of DMP1 by the osteocyte is dramatically induced in response to mechanical loading increasing bone mineralization. MEPE protein contains a protease resistant motif called ASARM, which is believed to be the candidate for the mineralization inhibitor (minhibin). Osteopontin is another mineralization inhibitor in its phosphorilated form and its secretion is markedly reduced in knockout mice for NPP1. Present data seem to support the hypothesis that these molecules could be the translators of bone strain and participate in the regulation of mineralization of the perilacunar osteocytic space.