4; Supplementary data Fig 9) Most of the percentage variation i

4; Supplementary data Fig. 9). Most of the percentage variation in the original data (fitted) could be explained Navitoclax cell line by the two axes (76.6%). Thirty-eight morpho-species of foraminifera were recovered from samples collected at the two sites along the SW coast of South Africa. Although this number is higher than has previously been reported

from around Africa (Murray, 2007), it is in general agreement with observations of other workers in shallow water sites from around the world (Yanko et al., 1994, Rathburn et al., 2000, du Châtelet et al., 2004, Ferraro et al., 2006 and Mojtahid et al., 2008). Discrepancies with respect to the African datasets probably reflect the paucity of studies conducted in Africa. That a greater number of taxa were collected from TB than SHB could be indicative of both the less stressed environment there (see below) and the slightly warmer temperatures experienced (Jury and Bain, 1989). Three main biogeographic provinces have been identified around South Africa (Bustamante and Branch, 1996): a sub-tropical province that extends southwards along the east coast to approximately East London, a warm temperate province that extends westwards to Talazoparib solubility dmso Cape Point, and a cold temperate Namaqua province that ranges northwards

along the west coast of South Africa. This schema has been identified for vertebrates (Turpie et al. 2000) and a wide variety of invertebrate taxa (Day, 1967, Griffiths, 1974 and Millard, 1975) and algae (Bolton and Stegenga, 2002), but is modified by life-history strategy (Gibbons et al., 2010). Species richness tends to be higher at the boundaries to these provinces (Awad et al., 2002 and Scott et al., 2012) and as TB is adjacent Adenosine triphosphate to Cape Point it likely contains an admixture of warm- and cold-temperate taxa (Stephenson,

1944). As noted in other studies (Yanko et al., 1994; Rathburne et al., 2000; Ruiz et al., 2004, Bergin et al., 2006 and Mojtahid et al., 2008), foraminiferal assemblages tended to be dominated by a handful of species and most were relatively uncommon. A. parkinsoniana was present in greatest abundance throughout SHB but was rare in TB, whilst E. articulatum was predominant in TB. Species of the genus Ammonia have previously been reported as opportunistic and are found in most types of environments. Even those experiencing chemical stress ( Seiglie, 1971, Nagy and Alve, 1987, Yanko et al., 1994, Scott et al., 2001, Bergin et al., 2006 and Ferraro et al., 2006), so their dominance of assemblages in SHB is hardly surprising given the fairly stressed nature of the system there (see below).

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