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Gall Bladder Pathology Online
;
Cholelithiasis ;
Pigment stones (calcium bilirubinate)
;
"Mixed" stones.
A cholesterol
stone is usually solitary (the cholesterol 'solitaire').
It is oval
or rounded in shape, and vary from 1 to 4 cm in diameter, or larger.
It is light in weight as well as in color.
In its
absolutely pure state it is very pale yellow in colour and feebly translucent.
More often
bile pigments are deposited within it.
On section
it has a radiating crystalline interior.
Cholesterol
stones, which make up some 6% of all gallstones, are believed to
be formed primarily in aseptic static bile (in a "stasis" gallbladder). They tend to
reside in Hartmann’s pouch.
The stone is
composed of 50 to 100% cholesterol, the rest consists of calcium
salts and mucin.
Cholesterol
stones are often detected at autopsy. During their
reproductive period, women are three times more likely to develop
cholesterol gallstones than men.The incidence is higher in users of
oral contraceptives and in women with several pregnancies.
Interestingly, cholesterol gallstones are exceedingly common in Pima
Indian women in the American Southwest, among whom three-quarters
are affected by age 25, and 90% above the age of 60 years. This may
be due to the genetic factors.
Blacks in
the US have a lower incidence of gallstones than whites, but a
higher incidence than blacks in Africa. This difference probably
reflects environmental influence, although a role of genetic
admixtures is also possible.
A brood of
mixed (secondary or inflammatory) gallstones may be formed later, or
a mixed covering of pigment and cholesterol may form around the
primary cholesterol stone. This is known as combination stone.
Pathogenesis:
Diagram showing Pathogenesis of Cholesterol
stone: click here
Pathogenesis of
cholesterol stones relates mainly to the composition of the bile.
Normally,
cholesterol, a compound highly insoluble in water, is secreted by
the hepatocytes into the bile, where it is held in solution by the
combined action of the bile acids and lecithin and carried in the form of mixed lipid micelles. If
the bile contains excess cholesterol or is deficient in bile acids,
the bile becomes supersaturated, and under some circumstances the
cholesterol precipitates as solid crystals.
The bile of
persons afflicted with cholesterol gallstones has more cholesterol
as it leaves the liver than that of normal individuals, pointing to the liver, rather than gallbladder as the culprit in the genesis of
cholesterol stones.
The hepatocytes
of patients with cholesterol gallstones are deficient in
7alpha-hydroxylase, the enzyme involved in the rate-limiting step
by which bile salts are formed from cholesterol.
As a result,
the total size of the bile salt pool is reduced.
The resulting
decrease in bile salt secretion contributes to the stone-forming (lithogenic)
properties of the bile.
Furthermore, in
obese people, cholesterol secretion by the liver is augmented,
further adding to the supersaturation of the bile with cholesterol.
Although
cholesterol supersaturation of the bile is apparently required for
gallstone formation , additional factors are also required.
Cholesterol
does not precipitate from saturated bile obtained from patients
without gallstones.
On the other
hand , bile from persons without gallstones, but with properties
similar to those in the bile of patients with gallstones,
crystallizes without difficulty.
It is
thought that the mucinous glycoproteins secreted by the gallbladder
epithelium provide the necessary nidus for crystallization.
Risk
factors:
The higher
prevalence of gallstones in premenopausal women has been attributed
to the fact that estrogens stimulate the formation of
lithogenic bile by the liver.
Estrogens
increase the hepatic secretion of cholesterol and may decrease
the secretion of bile acids.
These effects
are augmented during pregnancy, because the gallbladder empties more
slowly in the last trimester, thereby causing stasis and increasing
the opportunity for precipitation of cholesterol crystals.
Progesterone has been shows to inhibit discharge of bile from the
gallbladder. These mechanisms are also invoked to explain the
increased incidence of gallstones in users of oral contraceptives.
Other risk
factors for the development of cholesterol gallstones can be divided
into those that relate to increased biliary cholesterol secretion,
those that relate to decreased secretion of bile salts and lecithin,
and those that relate to combination of the two.
Risk factors associated with increased biliary cholesterol secretion
include the following:
Increasing age
; Obesity ; Membership of certain ethnic groups (e.g. Chilean women,
some northern European groups) ; Familial predisposition ;
Diets high in calories and cholesterol ; Certain metabolic
abnormalities associated with high blood cholesterol levels, for
instance diabetes ; Some genetic hyperlipoproteinemias, and Primary biliary cirrhosis.
Decreased
secretion of bile salts and lecithin occurs in nonobese Caucasians
who develop gallstones.
Gastrointestinal absorptive disorders that interfere with the
enterohepatic circulation of bile acids - for instance pancreatic
insufficiency secondary to cystic fibrosis and Crohn's disease also decrease secretion of bile acids and favour gallstone formation.
Cholesterol
synthesis is increased while that of bile salt and lecithin is
reduced in American Pima Indians and in those who take certain drugs
(e.g. clofibrate). |