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胆结石形成过程中胆汁脂质和胆囊离子转运的顺序变化。

Sequential changes in biliary lipids and gallbladder ion transport during gallstone formation.

作者信息

Giurgiu D I, Saunders-Kirkwood K D, Roslyn J J, Abedin M Z

机构信息

Philadelphia VAMC, Pennsylvania, USA.

出版信息

Ann Surg. 1997 Apr;225(4):382-90. doi: 10.1097/00000658-199704000-00007.

Abstract

OBJECTIVE

This study sought to correlate gallbladder (GB) Na+ and Cl-) fluxes with biliary lipid composition during the various stages of gallstone (GS) formation.

SUMMARY BACKGROUND DATA

GS formation is associated with altered GB ion transport and increased biliary lipid and Ca2+ concentrations. Nonetheless, the longitudinal relationship between ion transport and biliary lipid changes during GS formation has not been defined.

METHODS

Prairie dogs were fed standard (n = 18) or 1.2% cholesterol-enriched (n = 30) diets for 4 to 21 days. Hepatic and GB bile were analyzed for lipids and Ca2+. Animals were designated either Pre-Crystal, Crystal, or GS based on absence or presence of crystals or GS, respectively. GBs were mounted in Ussing chambers, electrophysiologic parameters were recorded, and unidirectional Na+ and Cl- fluxes measured.

RESULTS

Short-circuit current and potential difference were similar during Pre-Crystal and Crystal stages but significantly reduced during GS stage compared to controls and Pre-Crystals. Transepithelial resistance was similar in all groups. Net Na+ absorption was increased during Pre-Crystal but decreased during GS stage due to increased mucosa-to-serosa and serosa-to-mucosa flux, respectively. Increased serosa-to-mucosa flux of both Na+ and Cl- characterized the Crystal stage. Biliary lipids and Ca2+ increased progressively during various stages of GS formation and correlated positively with unidirectional fluxes of Na+ and Cl-.

CONCLUSION

GB epithelial ion transport changes sequentially during GS formation, with the early Pre-Crystal stage characterized by increased Na+ absorption, and the later Crystal stage accompanied by prosecretory stimuli on Na+ and Cl- fluxes, which may be due to elevated GB bile Ca2+ and total bile acids.

摘要

目的

本研究旨在探究在胆结石(GS)形成的各个阶段,胆囊(GB)的钠(Na⁺)和氯(Cl⁻)通量与胆汁脂质成分之间的相关性。

总结背景数据

GS的形成与GB离子转运改变以及胆汁脂质和钙离子(Ca²⁺)浓度升高有关。然而,GS形成过程中离子转运与胆汁脂质变化之间的纵向关系尚未明确。

方法

将草原犬鼠分为两组,分别给予标准饮食(n = 18)或富含1.2%胆固醇的饮食(n = 30),持续4至21天。分析肝胆汁和GB胆汁中的脂质和Ca²⁺。根据是否存在晶体或GS,将动物分别指定为晶体前期、晶体期或GS期。将GB置于Ussing室中,记录电生理参数,并测量单向Na⁺和Cl⁻通量。

结果

晶体前期和晶体期的短路电流和电位差相似,但与对照组和晶体前期相比,GS期显著降低。所有组的跨上皮电阻相似。晶体前期净Na⁺吸收增加,但在GS期由于黏膜到浆膜和浆膜到黏膜通量增加而降低。Na⁺和Cl⁻的浆膜到黏膜通量增加是晶体期的特征。在GS形成的各个阶段,胆汁脂质和Ca²⁺逐渐增加,并与Na⁺和Cl⁻的单向通量呈正相关。

结论

在GS形成过程中,GB上皮离子转运依次发生变化,早期晶体前期以Na⁺吸收增加为特征,后期晶体期伴随着对Na⁺和Cl⁻通量的促分泌刺激,这可能是由于GB胆汁Ca²⁺和总胆汁酸升高所致。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d99d/1190746/5fa1817c61bc/annsurg00026-0054-a.jpg

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