BODY TEMPERATURE CONCEPT MAP

At the extremes in the animal world are what in the
popular language are referred to as warm-blooded and cold-blooded animals. The
more precise scientific terminology is:
In this chaotic
world, the temperature is always changing, so there are two basic issues in
temperature regulation,
The core temperature (at deep sites within the
body) of the living vertebrate is a balance between thermal inputs and thermal
losses. Heat transfer occurs with the same basic principles as diffusion, e.g.
heat moves from regions of high temperature to low temperature. There are
several sources of heat which include:
In the more primitive reptiles which do not have
complex physiologic mechanisms for thermal regulation, behaviour patterns
permit a crude regulation of body temperature. Thus if air temperature is low,
the lizard or Iguana will search out sunny areas to heat their body to optimum
temperature and will engage in vigourous muscle activity to assist in elevation
of core temperature. On the other hand, if local temperature is high they will
seek shady spots or cool damp locations and avoid physical activity. These
critters have very low capacity of the circulatory, nervous systems and other
more subtle physiologic mechanisms to independently regulate core body
temperature. At a seminar many years ago, I heard a researcher describe a model
for temperature regulation in iguanas: It was an aluminium beer can half full
of water. If he moved it from sun to shade when the iguanas he was observing
moved, the temperature of the water in the beer can was a very good
approximation of the core temperature of the live iguanas. Iguanas are poikilotherms!
While humans, at least some humans, will seek shady spots during hot sunny
conditions, this is not the prime means for regulating our core body
temperature. We have a variety of sophistic ated physiologic mechanisms to
enhance heat loss allowing a human to bask in the sun and absorb sufficient
amount of external heat, to produce a lethal effect in an iguana, but obviously
most humans survive. Humans are homeotherms!
Other mammals have dense fur or hair which acts as
an effective layer of insulation to reduce heat loss through the skin. Man has
residual amounts of body hair and retains the reflex which is present in truly
hairy mammals to improve the insulating properties. That is a neurogenic reflex
of the sympathetic nervous system to activate the pilo-erector muscles. This
results in the body hairs being pulled to a position more nearly perpendicular
to the skin surface, instead of lying flat to the skin, and thus increasing the
thickness of the trapped layer of insulating air. In humans the amount of body
hair is usually trivial, so all we see is the appearance of 'goose bumps' in
response to cold stress as an evolutionary memory of when we had enough ha ir
to do something useful in reducing heat loss.
All mammals have a superficial layer of fat
associated with the skin which serves as an insulating layer. In marine mammals
this 'blubber' is very thick and provides the means for their survival in a
very cold environment. Humans who are cold adapted for long periods will
develop thicker superficial fat layer to reduce heat loss. These differences
have been measured in Inuit and others living and working in the arctic.
Analysis of the skeletal remains of Neanderthal
humans who prospered during a period when ice ages were a dominant feature of
the climatic pattern is interesting from the point of view of temperature
regulation issues. While Neanderthals were larger and taller than modern man,
the key difference appears to be a very thick hugely muscular body. This was
beneficial in two ways, 1) a reduced surface to volume ratio, with reduced heat
loss a consequence, and 2) a huge muscle mass with the capability of a
similarly large thermogenesis capacity. Since we only have skeletal remains,
one can only hypothesize that they probably also had large amounts of brown
adipose tissue to assist their survival. It didn't hurt that this level of
physical strength was useful in the hunting of mega-mammals dominant in that
period. In addition the morphology of the skull with the sloping forehead and
long nose, provided a heat and water conservation mechanism, exhaled air had a
larger portion of its heat recaptured by the vascular bed of the long
naso-pharynx, and more of the water vapour was recaptured as well. A good
evolutionary adaptation to a harsh cold climate.
Thermal
receptors exist in the skin, deep organs and in the central nervous system.
They send their signals to the autonomic nervous system. The key site for
determining perceived core temperature appears to be in the hypothalamus, but a
variety of temperature adaptive responses can be triggered by peripheral
receptors. When the thermal receptors indicate excessive loss of heat through
the skin, the autonomic nervous system produces vasoconstriction of peripheral
circulation to the skin, with shunting of most blood flow to the deeper tissue
thus reducing heat loss. In man vasoconstriction can reduce heat loss by 1/6 to
1/3. One of the consequences of this adaptation is an increase in central
arterial pressure as the resistance in the superficial vascular beds increases
dramatically.
The diving
reflex is a specialized version of this with protective potential that is most
sensitive in human neo-nates. That is cold stimulus of the face will trigger
reduced heart-rate (bradycardia) and shunting of the blood flow from the
periphery t o the CNS and vital organs. This reflex is responsible for the
survival without CNS damage of children falling through ice in very cold water
with recovery occurring at a time when by usual criteria they should be brain
dead.
Cold also
triggers release of adrenaline and nor-adrenaline from the adrenal medulla. In
addition there is a neurally regulated increase in thyroxine release. All of
these result in increased metabolic activity. The net result is a neurally
regulated non-shivering thermogenesis.
CNS perception
of cold can induce reflex shivering to increase contractile thermogenesis.
What are the
mechanisms for coping when there is too much heat and there is a threat of
increasing core temperature?