Department of Pathology, Immunology and Laboratory Medicine, Center for the Study of Lithiasis, University of Florida, Gainesville, Florida 32610-0275, USA.
J Urol. 2011 Sep;186(3):1107-13. doi: 10.1016/j.juro.2011.04.109. Epub 2011 Jul 23.
Idiopathic Ca oxalate stones may develop with attachment to renal interstitial Ca phosphate deposits (Randall's plaques). Sodium phosphate cotransporter (Npt2a) null mice have hypercalciuria and hyperphosphaturia, and produce tubular and interstitial Ca phosphate deposits. To determine whether this mouse is suitable for Randall's plaque investigations we chronologically studied Ca phosphate deposit sites, structure and composition.
The kidneys of Npt2a null mice 2 days to 1 year old were examined by light, scanning and transmission electron microscopy. Electron diffraction and energy dispersive x-ray microanalyses were done to determine mineral composition.
Poorly crystalline, biological apatite deposits were seen in collecting duct lumina. Deposits consisted of aggregates approximately 5 μm in diameter appearing as microspheres of concentrically organized needle or plate-like, matrix rich crystals. Epithelium/crystal interfaces were filled with membrane bound vesicles. Some tubules were completely occluded by crystals and occasionally lost the epithelium while crystals moved into the interstitium.
Ca phosphate crystals formed in the tubular lumina and were organized as microspheres. The aggregation of Ca phosphate crystals produced nuclei, which grew by adding crystals at the periphery. They eventually became large enough to occlude the tubular lumina and obliterate the tubular epithelium, leading to the relocation of microliths into the interstitium. The pathogenesis of interstitial deposits in Npt2a null mice appears different from that proposed for Randall's plaques. Since Npt2a null mice purge the renal crystal deposits, these mice may serve as a model in which to investigate the elimination of crystal deposits in children and adults with nephrocalcinosis.
特发性草酸钙结石可能在与肾间质钙磷酸盐沉积(兰德尔斑块)附着的情况下形成。钠磷协同转运蛋白(Npt2a)缺失小鼠有高钙尿和高磷酸盐尿,并产生管状和间质钙磷酸盐沉积。为了确定这种小鼠是否适合兰德尔斑块的研究,我们按时间顺序研究了钙磷酸盐沉积部位、结构和成分。
对 2 天至 1 岁的 Npt2a 缺失小鼠的肾脏进行了光镜、扫描和透射电镜检查。进行电子衍射和能量色散 X 射线微分析以确定矿物成分。
在集合管腔中可见结晶不良的生物磷灰石沉积。沉积物由直径约 5μm 的聚集物组成,呈同心排列的针状或板状、基质丰富的晶体微球体。上皮/晶体界面充满了膜结合的小泡。一些小管完全被晶体阻塞,偶尔失去上皮,而晶体进入间质。
钙磷酸盐晶体在管状腔中形成,并以微球体的形式排列。钙磷酸盐晶体的聚集产生了核,核通过在边缘添加晶体而生长。它们最终变得足够大,以至于阻塞了管状腔并使管状上皮消失,导致微石转移到间质中。Npt2a 缺失小鼠间质沉积的发病机制似乎与兰德尔斑块提出的机制不同。由于 Npt2a 缺失小鼠会清除肾脏的晶体沉积,因此这些小鼠可能成为研究儿童和成人肾钙质沉着症中晶体沉积消除的模型。