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An Introduction to the Invertebrates, Second Edition - tiera.ru

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TRANSPORT SYSTEMS113Oxygen dissociation curvesGraphs showing oxygen dissociation (see diagram) express <strong>the</strong> relationshipbetween <strong>the</strong> amount of oxygen available and <strong>the</strong> amounttaken up by <strong>the</strong> blood.They are informative about <strong>the</strong> haemoglobins in different animals or in differentcircumstances. The characteristic sigmoid curve may be shifted ei<strong>the</strong>r <strong>to</strong> <strong>the</strong>left, when oxygen can more easily be taken up, or <strong>to</strong> <strong>the</strong> right, when oxygen ismore easilygiven off in<strong>the</strong> tissues.The‘Bohr shift’exemplifies <strong>the</strong>se two positionsof <strong>the</strong> curve within most animals: in diagram (a) curve A represents conditionsat <strong>the</strong> respira<strong>to</strong>ry surface and <strong>the</strong> shift <strong>to</strong> <strong>the</strong> right (<strong>to</strong> curve B) is caused by <strong>the</strong>higher CO 2 concentration (causing greater acidity) at <strong>the</strong> tissues, enabling moreoxygen <strong>to</strong> be given off from <strong>the</strong> haemoglobin molecule. <strong>An</strong>imals living in placeswith low oxygen tensions, where ease of oxygen uptake is paramount, havecurves well <strong>to</strong> <strong>the</strong> left see diagram (b), curve C, for <strong>the</strong> polychaete Arenicolain its burrow.O<strong>the</strong>r fac<strong>to</strong>rs affecting <strong>the</strong> balance of advantage between ease ofuptake and ease of release of oxygen are temperature (see curves D and E for<strong>the</strong> earthworm Lumbricus) and high altitude, where <strong>the</strong>re is less <strong>to</strong>tal oxygendue <strong>to</strong> low atmospheric pressure and <strong>the</strong> curve moves <strong>to</strong> <strong>the</strong> left.Countercurrent systemsWhere <strong>the</strong> direction of flow is opposite in closely apposed channels,countercurrent systems increase <strong>the</strong> uptake of oxygen at respira<strong>to</strong>ry surfaces.With countercurrent flow <strong>the</strong>re is a concentration gradient of oxygen (or anyo<strong>the</strong>r substance, or heat) along <strong>the</strong> whole surface in contact, allowing verymuch more diffusion than can occur in parallel (‘co-current’) flow, where <strong>the</strong>reis a high initial gradient progressively decreasing see diagrams (c) and (d).(c) Co-current and(d) countercurrent flow of waterand blood at a gill, showinggradients of oxygen content as<strong>the</strong> water passes along <strong>the</strong> gill.The transport systems of different invertebratesNo transport systemNo transport system occurs in sponges or in most cnidarians, where everycell is close <strong>to</strong> <strong>the</strong> ambient medium. None is present in platyhelminths, acoelomorphs,gnathos<strong>to</strong>mula, gastrotrichs, nema<strong>to</strong>des (where fluid under high pressureis moved in <strong>the</strong> body cavity), nema<strong>to</strong>morphs, rotifers, acanthocephala,kinorhynchs, priapulids (though <strong>the</strong>re are cells containing haemerythrin in <strong>the</strong>body cavity), en<strong>to</strong>procts, sipuncula, bryozoa or chae<strong>to</strong>gnaths.

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