CEA Marcoule, Fundamental Research Division, 30207 Bagnols sur Céze, France.
Metallomics. 2019 Feb 20;11(2):496-507. doi: 10.1039/c8mt00272j.
Uranium is widespread in the environment, resulting both from natural occurrences and anthropogenic activities. Its toxicity is mainly chemical rather than radiological. In the blood it is transported as uranyl UO22+ cation and forms complexes with small ligands like carbonates and with some proteins. From there it reaches the skeleton, its main target organ for accumulation. Fetuin is a serum protein involved in biomineralization processes, and it was demonstrated to be the main UO22+-binder in vitro. Fetuin's life cycle ends in bone. It is thus suspected to be a key protagonist of U accumulation in this organ. Up to now, there has been no effective treatment for the removal of U from the body and studies devoted to the interactions involving chelating agents with both UO22+ and its protein targets are lacking. The present work aims at studying the potential role of 3,4,3-LI(1,2-HOPO) as a promising chelating agent in competition with fetuin. The apparent affinity constant of 3,4,3-LI(1,2-HOPO) was first determined, giving evidence for its very high affinity similar to that of fetuin. Chromatography experiments, aimed at identifying the complexes formed and quantifying their UO22+ content, and spectroscopic structural investigations (XAS) were carried out, demonstrating that 3,4,3-LI(1,2-HOPO) inhibits/limits the formation of fetuin-uranyl complexes under stoichiometric conditions. But surprisingly, possible ternary complexes stable enough to remain present after the chromatographic process were identified under sub-stoichiometric conditions of HOPO versus fetuin. These results contribute to the understanding of the mechanisms accounting for U residual accumulation despite chelation therapy after internal contamination.
铀在环境中广泛存在,既有自然产生的,也有人为活动造成的。其毒性主要是化学性质的,而非放射性的。在血液中,它以铀酰UO22+阳离子的形式运输,并与小分子配体(如碳酸盐)和一些蛋白质形成复合物。从那里它到达骨骼,这是其主要的蓄积靶器官。胎球蛋白是一种参与生物矿化过程的血清蛋白,已被证明是体外UO22+的主要结合物。胎球蛋白的生命周期在骨骼中结束。因此,它被怀疑是该器官中 U 蓄积的关键主角。到目前为止,还没有有效的方法从体内去除 U,并且缺乏涉及与 UO22+及其蛋白质靶标相互作用的螯合剂的研究。本工作旨在研究 3,4,3-LI(1,2-HOPO)作为一种有前途的螯合剂与胎球蛋白竞争的潜在作用。首先确定了 3,4,3-LI(1,2-HOPO)的表观亲和力常数,证明了它与胎球蛋白相似的非常高的亲和力。进行了色谱实验,旨在鉴定形成的复合物并定量其 UO22+含量,并进行了光谱结构研究(XAS),证明 3,4,3-LI(1,2-HOPO)在化学计量条件下抑制/限制了胎球蛋白-铀酰复合物的形成。但令人惊讶的是,在 HOPO 与胎球蛋白的亚化学计量条件下,即使在螯合治疗后,仍能鉴定出足够稳定以在色谱过程后仍然存在的可能的三元复合物。这些结果有助于理解尽管进行了内部污染后的螯合治疗,但仍存在 U 残留蓄积的机制。