State of the Bay Report 2011-Final.pdf - Anchor Environmental
State of the Bay Report 2011-Final.pdf - Anchor Environmental
State of the Bay Report 2011-Final.pdf - Anchor Environmental
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Dive School<br />
Jetty<br />
Schaapen East<br />
Schaapen West<br />
Iron Ore Jetty<br />
Lynch Point<br />
North <strong>Bay</strong><br />
Marcus Island<br />
<strong>State</strong> <strong>of</strong> Saldanha <strong>Bay</strong> & Langebaan Lagoon <strong>2011</strong><br />
Intertidal invertebrates<br />
Figure 8.15. Temporal changes <strong>of</strong> evenness and Shannon-Wiener diversity indices (mean ± SE) from 2005 to<br />
<strong>2011</strong> at <strong>the</strong> eight rocky shore sites. (DS = Dive School, J = Jetty, SE = Schaapen East, SW =<br />
Schaapen West, IO = Iron Ore Terminal, L = Lynch Point, NB = North <strong>Bay</strong>, M = Marcus Island).<br />
2D Stress: 0.19<br />
2005<br />
2008<br />
2009<br />
2010<br />
<strong>2011</strong><br />
Figure 8.16. Multi-dimensional scaling (MDS) plot <strong>of</strong> <strong>the</strong> rocky shore communities at <strong>the</strong> eight study sites<br />
from 2005 to <strong>2011</strong>. The circles delineate a 40% similarity level.<br />
Ano<strong>the</strong>r seaweed that had declined in abundance was Gigartina polycarpa at Dive School<br />
and Iron Ore Terminal, whereas Sarcothalia stiriata increased at <strong>the</strong> latter site. Changes in barnacle<br />
cover had also contributed to dissimilarities, specifically at <strong>the</strong> two very sheltered boulder beaches<br />
Dive School and Jetty, where B. glandula was absent in 2010 but present in <strong>2011</strong>, while <strong>the</strong> striped<br />
barnacle Amphibalanus amphitrite occurred in 2010 at Jetty and Iron Ore Terminal but not in <strong>2011</strong>.<br />
In general though, average dissimilarities between <strong>the</strong> years per site were low, indicating that<br />
temporal differences in rocky shore communities were small (Table 8.2).<br />
Temporal variations in abundance <strong>of</strong> functional groups at <strong>the</strong> eight study sites are illustrated<br />
in Figure 8.17. At <strong>the</strong> two sheltered boulder beaches Dive School and Jetty, filter feeders and<br />
ephemerals had slightly decreased while corticated algae and grazers had increased with time. In<br />
<strong>2011</strong>, however, algae o<strong>the</strong>r than encrusting were sparse. At Schaapen East, filter feeders depicted<br />
an increasing and ephemerals a decreasing trend, while encrusting corallines fluctuated strongly. At<br />
Schaapen West, biotic cover had steadily increased until 2010, especially encrusting corallines and<br />
ephemerals. The latter group had drastically declined by <strong>2011</strong>, reducing <strong>the</strong> overall cover. Iron Ore<br />
Terminal and Lynch Point remained relatively constant over time, with only minor variations in<br />
encrusting coralline and ephemeral cover at Lynch Point. At North <strong>Bay</strong>, <strong>the</strong>re was a drastic increase<br />
in filter feeders until 2010, remaining at <strong>the</strong> same level in <strong>2011</strong>. Corallines and ephemerals again<br />
showed slight temporal fluctuations. At Marcus Island, ephemeral algae had greatly increased from<br />
2005 to 2009 while at <strong>the</strong> same time corticated algae and filter feeders declined. The substantial<br />
ephemeral cover resulted in an overall greater biotic cover in 2009. In 2010, ephemerals had<br />
somewhat reduced but returned again <strong>2011</strong>.<br />
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ANCHOR<br />
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