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State of the Bay Report 2011-Final.pdf - Anchor Environmental

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<strong>State</strong> <strong>of</strong> Saldanha <strong>Bay</strong> & Langebaan Lagoon <strong>2011</strong><br />

Intertidal invertebrates<br />

8.3 RESULTS AND DISCUSSION<br />

8.3.1 Species Diversity and Zonation<br />

The survey <strong>of</strong> <strong>the</strong> eight rocky shores yielded a total <strong>of</strong> 84 species/taxa, <strong>of</strong> which 50 taxa were<br />

invertebrates (59.5%) and 34 (40.5%) algae. The faunal component was represented by 16<br />

species <strong>of</strong> grazers, 3 trappers, 7 predators and scavengers, 6 anemones, and 18 filter-feeders. The<br />

algal component comprised 22 corticated (foliose) seaweeds, 6 ephemerals, 1 kelp, 4 crustose (or<br />

encrusting) corallines and 1 articulated coralline (it has to be pointed out that this is a gross<br />

underestimation <strong>of</strong> coralline taxa as most species are not identifiable in <strong>the</strong> field and are thus<br />

lumped into larger groups).<br />

The overall taxa count has remained relatively constant over <strong>the</strong> years with most taxa<br />

having also been recorded during one or more <strong>of</strong> <strong>the</strong> previous monitoring years (<strong>Anchor</strong><br />

<strong>Environmental</strong> Consultants 2006, 2009, 2010, <strong>2011</strong>). Fur<strong>the</strong>rmore many <strong>of</strong> <strong>the</strong> species are also<br />

listed by o<strong>the</strong>r studies conducted in <strong>the</strong> Saldanha <strong>Bay</strong> area (e.g. Simons 1977, Schils et al. 2001,<br />

Robinson et al. 2007). The species are generally common to <strong>the</strong> South African West Coast (e.g.<br />

Day 1974, Branch et al. 2010a), including <strong>the</strong> two alien invasive species, <strong>the</strong> Mediterranean<br />

mussel Mytilus galloprovincialis and <strong>the</strong> acorn barnacle, Balanus glandula. The former was<br />

introduced from Europe sometime in <strong>the</strong> 1970’s, but is now <strong>the</strong> dominant west coast mussel,<br />

forming a dense mid- to low shore band in wave-exposed areas (Hockey & van Erkom Schurink<br />

1992). The presence <strong>of</strong> B. glandula, originating from <strong>the</strong> Pacific coast <strong>of</strong> North America, has only<br />

been recognized more recently (Simon-Blecher et al. 2008), but it seems that <strong>the</strong> species has been<br />

in South Africa since at least <strong>the</strong> early 1990s and it is now <strong>the</strong> most abundant intertidal barnacle<br />

along <strong>the</strong> sou<strong>the</strong>rn west coast (Laird & Griffiths 2008). The alien’s presence was overlooked for<br />

many years as it was mistaken for <strong>the</strong> indigenous species Chthamalus dentatus. Apparently as a<br />

result <strong>of</strong> <strong>the</strong> invasion by B. glandula, <strong>the</strong> formerly abundant C. dentatus is now very rare on South<br />

African west coast shores (Laird & Griffiths 2008). At <strong>the</strong> Saldanha <strong>Bay</strong> monitoring study sites, <strong>the</strong><br />

alien barnacle was first confidently identified in 2008. It is, however, assumed that it had been<br />

present during <strong>the</strong> baseline survey in 2005 but was confused with <strong>the</strong> indigenous barnacle.<br />

Consequently, in all analyses involving <strong>the</strong> 2005 dataset, C. dentatus abundances are converted to<br />

B. glandula.<br />

The composition and distribution <strong>of</strong> <strong>the</strong> rocky intertidal biota is strongly influenced by <strong>the</strong><br />

prevailing wave exposure at a shore as well as substratum topography. Within a site, however,<br />

shore height is <strong>the</strong> critical factor as <strong>the</strong> interface between air and water along with <strong>the</strong> action <strong>of</strong><br />

tides and waves result in a vertical emersion gradient <strong>of</strong> increasing exposure to air from low shore<br />

to high shore. Clear, well studied, patterns <strong>of</strong> zonation <strong>of</strong> flora and fauna thus exist on rocky<br />

shores (Stephenson & Stephenson 1972). The effects <strong>of</strong> wave action are generally attenuated upshore<br />

and superseded by <strong>the</strong> uniformly severe desiccation stress experienced high on <strong>the</strong> shore.<br />

Consequently <strong>the</strong> high shores were relatively similar among <strong>the</strong> sites being mostly barren with<br />

few species. At <strong>the</strong> very sheltered boulder shores Dive School and Jetty, considerable amounts <strong>of</strong><br />

sand and gravel had also accumulated amongst <strong>the</strong> boulders. Typical high shore species,<br />

particularly at <strong>the</strong> sheltered sites, included <strong>the</strong> winkle Oxystele variegata and towards <strong>the</strong> more<br />

exposed sites <strong>the</strong> small periwinkle Afrolittorina knysnaensis with average densities <strong>of</strong>ten<br />

exceeding 100 individuals per 0.5 m 2 (Figure 8.4). The alien B. glandula occurred at almost all high<br />

shores but with very low cover (on average 95% at most high<br />

shores. The exceptions were Schaapen East, which had occasional patches <strong>of</strong> blue-green algae,<br />

and Marcus Island were a dense low carpet <strong>of</strong> <strong>the</strong> ephemeral algae Ulva spp. with occasional tufts<br />

<strong>of</strong> ano<strong>the</strong>r ephemeral, Porphyra capensis, covered >70% <strong>of</strong> <strong>the</strong> high shore (Figure 8.4).<br />

Ephemerals are opportunistic algae that have short life cycles and are usually <strong>the</strong> first settlers on<br />

168<br />

ANCHOR<br />

e n v i r o n m en t a l

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