Marine Mussels. Elizabeth Gosling

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2008) (see further details in Chapter 3). This type of research is particularly relevant in the light of observed and potential climate change impacts on marine organisms (see Chapter 3). Another use of shells is in trace elemental fingerprinting, which assesses larval origins or trajectories based on the elemental composition of their shells, which in turn reflects the chemistry of the water in which they were formed (see Chapter 5). The technique has also been used to identify population sources and thus redistribution potentials in adult M. edulis (Sorte et al. 2013).

Schematic illustration of shell morphological characters used to distinguish between different Mytilus taxa.

      Source: From McDonald et al. (1991). Reproduced with permission from Springer.

      Finally, mussel shells are extensively used to assess environmental contamination (Bellotto & Miekeley 2007; Pereira et al. 2012; see Chapter 8). Radionucleotides (e.g. uranium) and metals such as Cu, Cd, Cr, Pb, U, V and Zn will be highly concentrated in contaminated shells (Widdows & Donkin 1992; Boisson et al. 1998; Avelar et al. 2000; Richardson et al. 2001).

      Structure

      Function

      The mantle plays a crucial role in the formation of the shell, a process that has already been covered in some detail. Also, the mantle is the site of gametogenesis and the main location for the storage of nutrient reserves, especially glycogen. In M. edulis, reserves are laid down in summer and utilised in autumn and winter in the formation of gametes (see Chapter 5). For a full discussion of energy metabolism in the mantle and other tissues, see de Zwann & Mathieu (1992).

Photos depict inner anatomy of Mytilus edulis. The white posterior adductor muscle is visible in the upper image but has been cut in the lower image to allow the valves to open fully.

      Source: Photograph by Rainer Zenz. (See colour plate section for colour representation of this figure).

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