Glimcher M J, Lefteriou B, Kossiva D
Calcif Tissue Int. 1979 Aug 24;28(1):83-6. doi: 10.1007/BF02441222.
O-phosphoserine [Ser(P)], O-phosphothreonine [Thr(P)], and gamma-carboxyglutamic acid (Gla) have been identified in native, calcified cementum and in non-collagenous proteins which can be extracted from the tissue in EDTA at neutral pH. The concentrations of Ser(P) and Thr(P) and the amino acid composition of the EDTA extractable proteins are more similar to those found in bone than in dentin or enamel. The concentration of Gla in cementum is lower than it is in bone and higher than it is in enamel, which contains essentially no Gla. Based on the contents of Gla in these mineralized tissues and the distribution of alkaline and acid phosphatases in these tissues, it is speculated that Gla may be part of these or other proenzymes rather than being involved directly and structurally with the deposition of the mineral phase.
O-磷酸丝氨酸[Ser(P)]、O-磷酸苏氨酸[Thr(P)]和γ-羧基谷氨酸(Gla)已在天然钙化牙骨质以及可在中性pH值的乙二胺四乙酸(EDTA)中从该组织提取的非胶原蛋白中被鉴定出来。Ser(P)和Thr(P)的浓度以及EDTA可提取蛋白的氨基酸组成与在骨中发现的更为相似,而与牙本质或牙釉质中的不同。牙骨质中Gla的浓度低于骨中的浓度,但高于牙釉质中的浓度,牙釉质中基本不含Gla。基于这些矿化组织中Gla的含量以及这些组织中碱性和酸性磷酸酶的分布,推测Gla可能是这些或其他酶原的一部分,而不是直接在结构上参与矿质相的沉积。