Marine Mussels. Elizabeth Gosling
et al. 2002; see Chapter 7 for salinity tolerance values in marine mussels).
Tomanek et al. (2012) examined the proteomic responses to hyposaline stress in M. trossulus and M. galloprovincialis, whose ranges overlap on the west coast of N. America (see earlier). Mussels were exposed to short time periods (4 hr) of hyposaline stress, followed by a recovery period to mimic conditions typical for bays and coastal areas experiencing heavy freshwater input, with a quick return to full salinity with incoming tides and mixing with full‐strength seawater. The differences in protein abundances in gill tissue suggested that M. trossulus was able to respond to a greater hyposaline challenge (24.5 psu) than M. galloprovincialis (29.8 psu). These differences, in a scenario of reduced coastal salinities, may enable M. trossulus to cope with greater hyposaline stress and outcompete M. galloprovincialis in the southern part of the M. trossulus range, thereby preventing M. galloprovincialis from expanding northward. Interestingly, Lockwood & Somero (2011b), in a transcriptomic analysis of gill tissue of Mytilus specimens from the same experiment (but limited to 29.8 and 35.0 psu), found no major differences in salinity stress tolerance between the two congeners at the level of transcriptional regulation.
P. viridis and Mytella charruana are two species of non‐native marine mussels that have recently invaded Florida, United States; as they are now well established, they are potential causes of concern along SE‐US coasts. Both species have been documented on intertidal oyster reefs in Florida (Spinuzzi et al. 2013), where they have a negative impact on the commercially important eastern oyster Crassostrea virginica (Yuan et al. 2016a). The simultaneous effects of salinity and temperature on the two species were investigated to get a better understanding of their respective invasion potentials (Yuan et al. 2016b). Survival at three salinity ranges (5–9, 20–22.5 and 35–40 psu) in both cold and warm water was estimated for juveniles and adults of both species. Yuan et al. (2016b) found that P. viridis can survive at a wide range of temperatures (9–35 °C) when the salinity is 35–37 psu, but as salinity decreases, the thermal survival range for P. viridis becomes narrower. The data for M. charruana indicate that juvenile and adult individuals can survive at a wide range of salinities (5–40 psu) at 20 °C, but the salinity tolerance range narrows as the temperature decreases or increases. Also, temperature rapidly impacts survival of both species (within hours), while salinity impacts are more gradual (days to weeks). As the species are tolerant of many salinity–temperature combinations found in SE‐US, they should be able to both persist in their present invaded range and expand into new estuaries and bays along the Atlantic coastline of Florida and west within the Gulf of Mexico. Freezing weather, however, could impede expansions into colder waters. Given that both species have a detrimental effect on C. virginica and possibly on many other native species, the abiotic variables could be used to help predict successful introductions and future biogeographic expansions.
In 2004, Berge et al. (2005) were the first to report the presence of settled mussels (M. edulis), for the first time since the age of the Vikings (793–1066 AD), in the high Arctic Archipelago of Svalbard – a Norwegian archipelago between mainland Norway and the North Pole. Their data indicated that most mussels settled at a single site as spat in 2002 and that larvae were transported by the West Spitsbergen Current northward from the Norwegian coast to Svalbard the same year. The extension of the mussel’s distribution range was made possible by the unusually high northward mass transport of warm Atlantic water resulting in elevated sea surface temperatures in the North Atlantic and along the west coast of Svalbard. This was suggested to be a one‐time event as all mussels were of similar age. Recently, Leopold et al. (2019) carried out a detailed field survey with scientific divers to map the Mytilus spp. distribution along the west coast of Svalbard, with a focus on the west coast of Spitsbergen, the largest island of the Svalbard archipelago, where strong Atlantification (transition from cold, fresh Arctic waters to a warm, salty Atlantic regime) has been documented over the last few decades. Low densities (<0.5 individuals m−2) of live Mytilus were recorded at 21 locations on the west coast of Svalbard and Spitsbergen. Using genetic markers, the authors found that these were mainly M. edulis, although some samples were classified as M. galloprovincalis or as hybrids of both M. edulis/M. galloprovincalis and M. edulis/M. trossulus. However, Leopold et al. (2019) regarded the three species as one complex, referring to them as ‘Mytilus spp.’ throughout their publication. The oldest mussel collected settled around the year 2000, indicating, despite low mussel densities at all sites, that settlement of blue mussels is a recurring event, with evidence of recruitment every year since 2000. The presence of Mytilus on Svalbard is the probable outcome of at least two distinct dispersal vectors: natural larval advection4 by ocean currents and human introduction by ship traffic. Based on the estimated year of settlement of mussels found in non‐harbour locations, Leopold et al. (2019) concluded that the settlement of Mytilus spp. is an annual event, rather than the unique one suggested by Berge et al. (2005), which implies that current environmental conditions are favourable for continued persistence of Svalbard’s Mytilus spp. populations.
The coast of South Africa comprises three broad biogeographic regions: the cool‐temperate western coast, the warm‐temperate southern coast and the subtropical eastern coast; these are aligned with two globally important currents and characterised by a clear decrease of upwelling intensity and frequency and by primary production from west to east (McQuaid et al. 2015 and references therein). The two currents are the upwelling‐driven Benguela Current (BC) on the southwestern coast and the warm, temperate Agulhas Current (AC), which follows the eastern and southern coasts (Figure 3.3). Upwelling is believed to have strong effects on the advection of larvae between coastal waters and the intertidal. In southern Africa, the indigenous mussel, P. perna, dominates the subtropical and warm‐temperate bioregions from central Mozambique to the Cape of Good Hope, west of Cape Agulhas on the southwest coast of S. Africa. The species is absent from there to central Namibia due to the cold, upwelling waters of the Benguela system – a distributional gap of more than 1000 km. From there, P. perna extends northward along the west coast of Africa to the Mediterranean Sea, as far as the Gulf of Tunis (Van Erkom Schurink & Griffiths 1990; Zardi et al. 2015). The invasive M. galloprovincialis is considered to have arrived on the western coast of South Africa via shipping in the 1970s (Grant & Cherry 1985). The species subsequently spread both north and south, with its northerly spread being more rapid under the influence of the north‐flowing BC, which flows from the Cape of Good Hope to Lüderitz, after which it is deflected away from the coast to the northwest. The northern limit of M. galloprovincialis on the west coast is in central Namibia, where conditions may represent the limit of the species’ temperature tolerance (Zardi et al. 2007a). The second distributional limit for M. galloprovincialis occurs on the SE southern African coast. There, the warm AC, which flows to the southwest, diverges away from the coast, thereby reducing SST significantly. And because warm waters tend to have fewer nutrients than cold waters, the distributional limits of M. galloprovincialis may also be affected by unfavourable trophic conditions beyond these boundaries, in addition to prohibitive thermal conditions (Assis et al. 2015).
Figure 3.3 Map of the Benguela Current region bordering Namibia and South Africa, showing the 500 m depth contour (dashed line) and the approximate locations of the Lüderitz upwelling cell (which separates the northern and southern Benguela Current subsystems) and the Agulhas Current.
Source: From Roux et al. (2013). Reproduced with permission from the Bulletin