Skin Glands
Sebaceous Glands
- also known as "Oil
Glands"
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Most
are associated with hair
follicles.
They secret either into the neck of a hair follicle, or directly onto the surface of the skin via a pore. |
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Location
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Sebaceous
glands are located over most of the surface of the skin/body but not in the
palms of the hands or the soles of the feet.
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Secretion(s):
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Importance
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Sebum
helps to protect skin and hair by:
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preventing
hairs from becoming too dry and brittle
preventing
the skin from becoming too dry (by preventing excessive evaporation of water from the
surface of the skin), hence also helping to keep the skin soft and effective
restricting
the growth/development of certain bacteria.
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Sudoriferous Glands
- also known as "Sweat
Glands"
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Different Types:
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Location
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Apocrine Glands :-
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Eccrine Glands :-
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Secretion(s):
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Sudoriferous glands secret sweat, which is
also called "perspiration". Apocrine glands secret a sticky viscous
secretion while the secretion from eccrine glands is thinner; watery by
comparison.
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Importance:
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The main functions of the secretion of
sweat are to help regulate body temperature and to help eliminate from the
body some of the waste products of metabolism (i.e.
metabolic reactions).
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Ceruminous
Glands
- the "Wax
Glands" of the ear
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Ducts open either directly onto the surface
of the external auditory canal or into the ducts of
sebaceous glands.
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Location
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The external auditory canal, also known
(colloquially) as simply the "outer ear"
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Secretion(s):
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The prefix "cer-" means
"wax".
The secretions from ceruminous glands combines with sebum secreted by nearby or associated sebaceous glands to form cerumen which is also known colloquially as "ear wax". |
Importance
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Cerumen, assisted by the hairs in the outer
ear, protects the ear from particles originating outside of the body e.g. of
dust, fine sand, or similar in the air getting into the ear itself. Cerumen
provides a sticky barrier that prevents many such particles from going
further into the ear.
Scent gland
Scent glands are exocrine
glands found in most mammals.
They produce semi-viscous secretions which
contain pheromones and other semiochemical compounds. These odor-messengers indicate
information such as status ,territorial marking,
mood, and sexual power. The odor may be subliminal—not consciously
detectable. Though it is not their primary function, the salivary
glands may also function as scent glands in some
animals.
How we determine the age of a rock?
RADIOMETRIC AGE-DATING
Radiometric
dating or radioactive dating is a technique used to date materials such as rocks or carbon, in which
trace radioactive impurities were selectively incorporated when they formed.
The method compares the abundance of a naturally occurring radioactive isotope within
the material to the abundance of its decay products, which form at a known constant
rate of decay. The use of radiometric dating was first published in 1907
by Bertram Boltwood and is now the principal source of
information about the absolute age of rocks and other geological features,
including the age of the Earth itself, and can be used to date a wide range
of natural and man-made materials.
Some elements have forms (called isotopes)
with unstable atomic nuclei that have a tendency to change, or decay. For
example, U-235 is an unstable isotope of uranium that has 92 protons and 143
neutrons in the nucl eus of each atom. Through a series of changes within the
nucleus, it emits several particles, ending up with 82 protons and 125
neutrons. This is a stable condition, and there are no more changes in the
atomic nucleus. A nucleus with that number of protons is called lead
(chemical symbol Pb). The protons (82) and neutrons (125) total 207. This
particular form (isotope) of lead is called Pb-207. U-235 is the parent
isotope of Pb-207, which is the daughter isotope.
Many rocks contain small amounts of
unstable isotopes and the daughter isotopes into which they decay. Where the
amounts of parent and daughter isotopes can be accurately measured, the ratio
can be used to determine how old the rock is.
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