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Invertebrate circulatory systems. Basic physicochemical considerations.

Invertebrate circulatory systems. Basic physicochemical considerations.

To maintain optimum metabolism, all living cells require a suitable environment, which must be maintained within relatively narrow limits. An appropriate gas phase (i.e., suitable levels ofoxygen and other gases), an adequate and suitable nutrient supply, and a means of disposal of unwanted products are all essential.

Direct diffusion through the body surface supplies the necessary gases and nutrients for small organisms, but even some single-celled protozoa have a rudimentary circulatory system. Cyclosis in many ciliates carries food vacuoles—which form at the forward end of the gullet (cytopharynx)—on a more or less fixed route around the cell, while digestion occurs to a fixed point of discharge.

For most animal cells, the supply of oxygen is largely independent of the animal and therefore is a limiting factor in its metabolism and ultimately in its structure and distribution. The nutrient supply to the tissues, however, is controlled by the animal itself, and, because both major catabolic end products of metabolism—ammonia (NH3) and carbon dioxide (CO2)—are more soluble than oxygen (O2) in water and the aqueous phase of the body fluids, they tend not to limit metabolic rates. The diffusion rate of CO2 is less than that of O2, but its solubility is 30 times that of oxygen. This means that the amount of CO2 diffusing is 26 times as high as for oxygen at the same temperature and pressure.

The oxygen available to a cell depends on the concentration of oxygen in the external environment and the efficiency with which it is transported to the tissues. Dry air at atmospheric pressure contains about 21 percent oxygen, the percentage of which decreases with increasing altitude. Well-aerated water has the same percentage of oxygen as the surrounding air; however, the amount of dissolved oxygen is governed by temperature and the presence of other solutes. For example, seawater contains 20 percent less oxygen than fresh water under the same conditions.

The rate of diffusion depends on the shape and size of the diffusing molecule, the medium through which it diffuses, the concentration gradient, and the temperature. These physicochemical constraints imposed by gaseous diffusion have a relationship with animal respiration. Investigations have suggested that a spherical organism larger than 0.5 millimetre (0.02 inch) radius would not obtain enough oxygen for the given metabolic rate, and so a supplementary transport mechanism would be required. Many invertebrates are small, with direct diffusion distances of less than 0.5 millimetre. Considerably larger species, however, still survive without an internal circulatory system.

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