Marine Mussels. Elizabeth Gosling
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Название: Marine Mussels

Автор: Elizabeth Gosling

Издательство: John Wiley & Sons Limited

Жанр: Техническая литература

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isbn: 9781119293934

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СКАЧАТЬ and retina that produce a low‐contrast image (Colicchia et al. 2009). The inner mantle fold, or velum, the largest of the three folds, has small sensory tentacles or papillae that usually fringe the fold. There is also a large muscular component, especially on the inhalant opening. The velum plays an important role in controlling the flow of water into and out of the mantle cavity.

Photos depict exhalant (white and smooth) and inhalant (fringed with tentacles) openings in the mantle of the mussel Mytilus edulis.

      Source: Photo courtesy of John Costelloe, Aquafact International Services Ltd., Galway, Ireland.

      Filter feeding is believed to have evolved in some group of early protobranch molluscs, giving rise to the Autobranchia, the dominant subclass of modern bivalves. These feed by filtering the incoming current as a source of food, the gills having replaced the palps as the feeding organs. One important development in the evolution of filter feeding was movement of the site of water intake to the posterior of the animal (see Chapter 1).

      Structure

Schematic illustration of (A) the section of a lamellibranch gill showing the ctenidial axis and four W-shaped filaments. (B) (i) section of a fillibranch gill in the mussel, Mytilus edulis. Adjacent filaments are joined together by ciliary junctions. (ii) Transverse section through one fillibranch gill filament (shaded in Bi), showing pattern of ciliation.

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      Functions

      Cilia on the gill filaments have specific arrangements and functions (Figure 2.8Bii). Lateral cilia are set along the sides of the filaments in fillibranch gills and in the ostia of eulamellibranch gills. These cilia are responsible for drawing water into the mantle cavity and passing it through the gill filaments or the ostia, and then upward to the exhalant chamber and on to the exhalant opening. Lying between the lateral and frontal cilia (see later) are the large feather‐like latero‐frontal cilia, which are unique to bivalves. When the incoming current hits the gill surface, these cilia flick particles from the water and convey them to the frontal cilia. The frontal cilia, which are abundantly distributed on the free outer surface of the gill facing the incoming current, convey particles aggregated in mucous – secreted by the filaments – downward toward the ciliated food grooves on the ventral side of each lamella. The movement of cilia is under nervous control. Each gill axis is supplied with a branchial nerve from a visceral ganglion, which subdivides to innervate individual groups of filaments. The general architecture and fine structure of the gill vary little from one mussel species to the next, even when rock (e.g. Lithophaga lithophaga; Akşit & Falakali Mutaf 2014) and sediment (e.g. Mytella falcate; David & Fontanetti 2005) burrowing species are considered. See Chapter 4 for a detailed description of the role of the gill in water pumping and particle capture.

      In bivalves, the gills have a respiratory as well as a feeding role. Their large surface area and rich haemolymph supply make them well suited for gas exchange. Deoxygenated haemolymph is carried from the kidneys to the gills by way of the afferent gill vein. Each filament receives a small branch of this vein. The filaments are essentially hollow tubes within which the haemolymph circulates. Gas exchange takes place across the thin walls of the filaments. The oxygenated haemolymph from each filament is collected into the efferent gill vein, which goes to the kidney and on to the heart. It is likely that gas exchange also occurs over the general mantle surface.

      The gills perform an additional function in hydrothermal vents mussels, which depend almost entirely on endosymbiont chemosynthetic bacteria in the gill filaments as an energy source. The bacteria use the energy obtained from the oxidation of reduced sulphur compounds and methane from hydrothermal fluid for the fixation of the CO2 required for primary production (Duperron et al. 2016 and references therein; see also Chapter 4).