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Thermoregulation

From Simple English Wikipedia, the free encyclopedia
(Redirected from Body temperature)

Thermoregulation is the ability of an organism to control its body temperature within certain limits, even when the surrounding temperature is different.[1] This is an aspect of homeostasis: the keeping of a constant internal environment.

Endotherms

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So-called warm-blooded animals control the temperature of their body at quite a high level. This ability is called endothermy. All mammals and birds are endotherms (homeotherms or homoiotherms). The basic source of the heat is chemical energy from the body's metabolism. They have a number of temperature-control devices:

  1. When they are cold they can do things to make themselves warmer. For example, they "shiver", or shake, or run about, or move into a warmer place. This is because all movement by animals creates heat from the chemical reactions of respiration. So polar bears do not freeze because their metabolism produces heat, and movement produces more heat. During hibernation bears exist several degrees lower that they do in active life. Of course, warm-blooded animals have thermal insulation: hair, feathers, or in water blubber (thick fat). These adaptations help keep heat energy inside the animal.
  2. When they are warm they sweat to become cooler, or pant, or open their feathers, or move to a less hot place and lie down.

Hibernation

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In the colder climates many mammals hibernate or aestivate. This means they have a two-level metabolism. Their temperature is held at a high level when they are active, and at a lower level when they are hibernating. This has the advantage of saving energy during times when they cannot get enough food to keep up the higher temperature.

The human body has automatic responses to help regulate temperature.[1] When the external environment heats up, arterioles leading to the capillary loops in the dermis dilate (widen).[2] This increases blood flow to the surface of the skin where its heat can more easily radiate away.[2] This process is called vasodilation. Sweat glands also produce greater amounts of sweat. This liquid is secreted onto the surface of the skin. Sweat needs energy to turn from a liquid into a gas and evaporate. This energy is called the latent heat of vaporisation.[2] The body supplies this heat and so it cools down as the sweat evaporates.[2]

If the body is unable to maintain a normal temperature and it increases significantly above normal, a condition known as hyperthermia occurs. This occurs when the body is exposed to temperatures of approximately 55 °C; any exposure longer than a few hours at this temperature or up to around 70 °C kills. The opposite condition, when body temperature decreases below normal levels, is known as hypothermia.

Fossil groups

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Palaeontologists are fairly certain that some fossil groups were endotherms. Obvious examples are pterosaurs, whose bodies were covered by hair (or hair-like filaments),[3] and the smaller carnivorous dinosaurs which evolved feathers ("dinobirds").[4][5] It is thought that feathers originally functioned to keep body temperature higher. They appear on bird-like dinosaurs before there were any flying birds (Anchiornis huxlei), and they appear on dinosaurs which are too heavy to fly at all.

Heterotherms

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Heterothermy is a term for animals that have features of both ectothermy and endothermy. They can switch between strategies.

Basic physiology

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The fundamental idea is that smaller endothermic animals have, relative to their mass, a larger body surface. "Heat loss takes place from the surface, and in order to keep warm, an animal must produce heat at a rate equal to its loss".[6]

Animals 'make' heat by the metabolism inside their bodies, but lose heat through their surface (mostly their skin). Now, their bodies are three-dimensional, whereas their surface is two-dimensional. So, if an animal of length X doubles its length, then its surface area increases by about X2, but its body mass increases by about X3. Example:

A three-inch-long animal doubles its length to six inches. As a result, its surface area increases in proportion 3x3 = 9 square inches. Its body mass increases in proportion 3x3x3 = 27 cubic inches. Since energy production is related to body mass, the animal is better off in its energy balance.

Thus larger animals are much more "energy efficient" than smaller animals. Large animals lose heat relatively slower than small animals because their surface area is smaller in proportion.

Strategies for small animals

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Small warm-blooded animals have three main tactics for overcoming this problem of heat loss. First, they have a higher metabolic rate than large animals. This is universal in birds and mammals: only the details differ. A higher metabolic rate affects the whole of their lives, and is the main reason why they have shorter lives than large animals.[7]p58/9 The smallest mammals (shrews) and the smallest hummingbirds are about the same size and weight. They have fast heartbeats, up to 1,200 per minute,[6]p129 and they use up more calories per gram than any other endotherms. The rate of oxygen use is similarly high. As a result of the metabolism running at such a high rate, they do produce more heat per gram than any other living things.

Second, many allow their temperature to drop at night. Many hummingbirds go into a trance-like torpor at night.

"One bird... increased its heart rate [in the morning] from about 150 beats per minute at 21 degrees C to over 1000 beats per minute at 36 degrees C".[7]

In that state, they are less aware and less able to take flight, so there is a greater risk of predators. However, when they are asleep they cannot feed, and at their normal rate of metabolism they need sugar regularly. The torpor is their way of saving energy which they cannot replace until the next day.

Thirdly, almost all endotherms are insulated to reduce heat loss. Obviously that is true of birds (which have feathers) and land mammals (which have fur). Marine mammals have thick layers of fat under their skin, which is better insulation than wet fur. The exceptions are some very large mammals such as elephants, which have almost no fur. Their problem is how to get rid of heat, and that is a problem for all really large land animals. The African elephant's solution is to have large ears, which are well supplied with blood vessels, and to wallow in water if that is available. It is very likely that the same problem affected large dinosaurs. After all, the largest titanosaurs were far larger than any land animal alive today.[7]

Ectotherms

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Pseudemys turtles (shown here basking for warmth) are ectothermic.
Junonia lemonias is basking under the sun.

Ectotherms are what is often called "cold-blooded". To function properly they need some heat, and usually this is heat from their surroundings.[8] Many need heat in order to digest their food.[9][10]

Many supposedly cold-blooded animals do things to keep their temperature higher than the surrounding air or water. Fast-moving fish, like tunny, and some sharks, keep their temperature above the level of the surrounding water. Reptiles such as lizards and snakes sit in the sun when they are cold and in the shade when they are hot. Some insects control their temperature, especially colonial insects. Termite mounds have 'air conditioning': their system of openings and galleries allows currents of air to flow through the mound. Honey bees fan their wings to cool their colony. However, many smaller invertebrates do not control their body temperature at all.

Variable temperature

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An animal whose internal temperature varies considerably. is a poikilotherm (noun), poikilothermic (adjective). The term is preferred to cold-blooded by some scientists.

References

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  1. 1.0 1.1 "What is thermoregulation?", How it Works, no. 40, Imagine Publishing, p. 36, 2012-11-01
  2. 2.0 2.1 2.2 2.3 Bradfield, Phil; Potter, Steve (2009). Edexcel IGCSE Biology: Student Book. Pearson Education. pp. 92-93. ISBN 9780435966881.
  3. The discovery is discussed by Wellnhofer P. Pterosaurs of the Triassic, in Norman D. & Wellnhofer P. The illustrated encyclopedia of dinosaurs. London: Salamander. p281/2. ISBN 1-84065-204-7
  4. Dong Zhiming 1988. Dinosaurs from China. transl. Angela Milner, BM(NH)/China Ocean.
  5. Benton M.J. et al. 2008. The remarkable fossils from the Early Cretaceous Jehol biota of China and how they have changed our knowledge of Mesozoic life. Proceedings of the Geological Association 119, p209–228.
  6. 6.0 6.1 Schmidt-Nielsen, Knut 1984. Scaling: why is animal size so important?. Cambridge University Press, p77. ISBN 0-521-31987-0
  7. 7.0 7.1 7.2 McGowan, Christopher 1994. Diatoms to dinosaurs: the size and scale of living things. London: Penguin, p27. ISBN 0-14-028104-5
  8. Davenport, John. Animal life at low temperature. Springer 1991. ISBN 978-0412403507
  9. Jay M. Savage ; with photographs by Michael Fogden and Patricia Fogden. (2002). The amphibians and reptiles of Costa Rica : a herpetofauna between two continents, between two seas. Chicago, Ill.: University of Chicago Press. p. 409. ISBN 0-226-73538-9.{{cite book}}: CS1 maint: multiple names: authors list (link)
  10. Hildebrand, Milton & Goslow G.E.Jr. (2001). Analysis of vertebrate structure. New York: Wiley. p. 429. ISBN 0-471-29505-1.

Further reading

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  • Schmidt-Nielsen, Knut 1972. How animals work. Cambridge University Press. ISBN 0-521-09692-8. Basic information on heat balance and heat exchange in animals.