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Black and brown pigment gallstones differ in microstructure and microcomposition.
Hepatology (Baltimore, Md.)
|March 1, 1984
Summary
Black and brown pigment gallstones form through distinct mechanisms, differing in microstructure and chemical composition. These findings support different formation pathways for these common gallstone types.
Area of Science:
- Gastroenterology
- Biochemistry
- Materials Science
Background:
- Pigment gallstones are broadly classified into black and brown subtypes.
- These subtypes exhibit variations in chemical makeup and the processes leading to their formation.
Purpose of the Study:
- To investigate the microstructural and microchemical differences between black and brown pigment gallstones.
- To determine if these differences correlate with distinct formation mechanisms.
Main Methods:
- Scanning electron microscopy (SEM) was employed to analyze stone surfaces and cross-sections.
- Microchemical techniques, including electron probe microanalysis and plasma/argon ion etching, were used to identify elemental and chemical composition.
- Specific attention was paid to the distribution of calcium bilirubinate, calcium palmitate, and protein structures.
Main Results:
- Black bilirubinate and black phosphate stones displayed smooth, homogenous surfaces, while brown stones were rough with lamellated bands.
- Black stones showed high sulfur and copper concentrations, with sulfur in a low valence state, suggesting protein disulfide linkages.
- Brown stones contained significant calcium palmitate in lighter bands and calcium bilirubinate in darker bands.
- Protein networks were observed in black stones but not brown stones; calcium bilirubinate had a rod-shaped arrangement in black stones.
Conclusions:
- Structural and compositional disparities between black noncarbonate and brown pigment gallstones support divergent formation mechanisms.
- The layered structures in black carbonate and brown stones indicate that biliary composition fluctuations influence gallstone growth.