Buhi W C, Ducsay C A, Bazer F W, Roberts R M
J Biol Chem. 1982 Feb 25;257(4):1712-23.
Uteroferrin, a purple-colored, iron-containing phosphatase which is induced by progesterone in the porcine uterus, has been proposed to be an intermediary in iron transfer between the mother and conceptus in the pig. Along with a number of other uterine proteins of maternal origin, it accumulates in the allantoic fluid during mid-pregnancy. When [59Fe]uteroferrin was introduced into the allantoic sacs of five fetuses at Day 60 of pregnancy, its iron was transferred to another protein, identified as transferrin. The half-life of iron loss from uteroferrin was approximately 24 h and the kinetics suggested an approximately second order process. 59Fe was also distributed to the fetus and was recovered at high specific activity in the fetal red blood cells (as hemoglobin), liver, and spleen. Introduction of [59Fe] transferrin to allantoic fluid resulted in an almost identical distribution of isotope in the fetus as was observed with [59Fe]uteroferrin. Whereas [125I]transferrin has been shown to be capable of leaving the allantoic sac in intact form, [125I]uteroferrin either has only a limited capacity to exit or else is almost immediately degraded upon entering the fetal circulation. Following loss of its iron to transferrin in allantoic fluid, uteroferrin rapidly loses immunological reactivity and is cleaved proteolytically into small peptides. The transfer of iron between uteroferrin and transferrin has also been followed in vitro. Iron on uteroferrin is relatively stable to pH and is not readily lost to transferrin at around neutral pH unless low molecular iron chelators such as citrate, pyrophosphate, ATP, or ascorbate are present. Iron transfer was promoted at ascorbate concentrations (approximately 50 microM) and at pH values (approximately 6.8) approximating those found in allantoic fluid. Results are consistent with a model in which maternal uteroferrin can transfer its iron to fetal transferrin via a low molecular weight intermediary in the allantoic sac. Transferrin is then responsible for iron distribution to the fetus.
子宫铁蛋白是一种紫色含铁磷酸酶,由猪子宫中的孕酮诱导产生,有人提出它是猪母体与胎儿之间铁转运的中间介质。与许多其他母体来源的子宫蛋白一起,它在妊娠中期积聚在尿囊液中。当在妊娠第60天将[59Fe]子宫铁蛋白引入5个胎儿的尿囊中时,其铁被转移到另一种蛋白质上,该蛋白质被鉴定为转铁蛋白。子宫铁蛋白中铁损失的半衰期约为24小时,动力学表明这是一个近似二级过程。59Fe也分布到胎儿体内,并在胎儿红细胞(作为血红蛋白)、肝脏和脾脏中以高比活度被回收。将[59Fe]转铁蛋白引入尿囊液导致胎儿体内同位素分布与[59Fe]子宫铁蛋白观察到的几乎相同。虽然[125I]转铁蛋白已被证明能够以完整形式离开尿囊,但[125I]子宫铁蛋白要么只有有限的能力离开,要么在进入胎儿循环后几乎立即降解。在尿囊液中其铁转移给转铁蛋白后,子宫铁蛋白迅速失去免疫反应性,并被蛋白水解切割成小肽。子宫铁蛋白和转铁蛋白之间的铁转移也在体外进行了跟踪。子宫铁蛋白上的铁对pH相对稳定,在接近中性pH时不容易转移给转铁蛋白,除非存在柠檬酸盐、焦磷酸盐、ATP或抗坏血酸盐等低分子铁螯合剂。在抗坏血酸盐浓度(约50 microM)和pH值(约6.8)接近尿囊液中的值时,铁转移得到促进。结果与一个模型一致,即母体子宫铁蛋白可以通过尿囊中一种低分子量中间介质将其铁转移给胎儿转铁蛋白。然后转铁蛋白负责将铁分配给胎儿。