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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<strong>State</strong> <strong>of</strong> Saldanha <strong>Bay</strong> & Langebaan Lagoon <strong>2011</strong><br />
Benthic macr<strong>of</strong>auna<br />
increase are not clear given that, based on <strong>the</strong> increases in o<strong>the</strong>r taxonomic groups, <strong>the</strong> ecosystem<br />
did not appear to have been negatively disturbed by anthropogenic or natural perturbations. The<br />
increase in small polychaete species (predominantly detritivores) is likely to be a result <strong>of</strong> biological<br />
interactions.<br />
Big <strong>Bay</strong><br />
Crustaceans and polychaetes have dominated <strong>the</strong> benthic macr<strong>of</strong>auna community in Big <strong>Bay</strong> in<br />
terms <strong>of</strong> abundance in all surveys conducted since 1999, while crustaceans and tongue worms<br />
(Echiuroidea) have dominated in terms <strong>of</strong> biomass. The overall biomass and abundance <strong>of</strong> benthic<br />
macr<strong>of</strong>auna in Big <strong>Bay</strong> increased between 1999 and 2004. This is an indication that benthic<br />
environment in Big <strong>Bay</strong> had been recovering since <strong>the</strong> dredging events <strong>of</strong> 1997/8. A dramatic<br />
decrease in both <strong>the</strong> abundance and biomass <strong>of</strong> benthic macr<strong>of</strong>auna in Big <strong>Bay</strong> was seen between<br />
2004 and 2008. It is likely that this was a response to <strong>the</strong> dredging events in Small <strong>Bay</strong> (maintenance<br />
dredging <strong>of</strong> <strong>the</strong> Multi Purpose Terminal) in 2007/8 and <strong>of</strong>f north beach at <strong>the</strong> nor<strong>the</strong>rn end <strong>of</strong><br />
Langebaan Lagoon. Much <strong>of</strong> <strong>the</strong> reduction in biomass and abundance could be attributed to <strong>the</strong> loss<br />
<strong>of</strong> crustaceans. There was also a dramatic reduction in <strong>the</strong> density <strong>of</strong> polychaetes between 2004<br />
and 2008.<br />
There was a substantial increase in <strong>the</strong> abundance and biomass <strong>of</strong> benthic macr<strong>of</strong>auna in Big<br />
<strong>Bay</strong> between 2008 and 2009. Much <strong>of</strong> <strong>the</strong> increase in abundance was attributed to <strong>the</strong> increase in<br />
polychaetes. This was however not reflected in <strong>the</strong> biomass, indicating that <strong>the</strong> community had<br />
become dominated in terms <strong>of</strong> abundance by small polychaetes. The increase in <strong>the</strong> overall biomass<br />
<strong>of</strong> <strong>the</strong> benthic community between 2008 and 2009 was principally attributed to an increase in<br />
crustacean biomass. The results <strong>of</strong> <strong>the</strong> 2010 survey revealed that <strong>the</strong> abundance <strong>of</strong> benthic<br />
macr<strong>of</strong>auna had decreased while <strong>the</strong> biomass had increased. This indicates that fewer, larger<br />
organisms were dominating, and possibly leading to a reduction in <strong>the</strong> number <strong>of</strong> smaller organisms<br />
through predatory or competitive community interactions. This is a typical sign <strong>of</strong> <strong>the</strong> succession <strong>of</strong><br />
a system following a disturbance. Interestingly, <strong>the</strong> abundance <strong>of</strong> polychaetes and crustaceans<br />
increased dramatically between 2010 and <strong>2011</strong>. This result was not reflected in <strong>the</strong> biomass results<br />
indicating that small crustaceans and polychaetes had colonised <strong>the</strong> Big <strong>Bay</strong> area by <strong>2011</strong>. The<br />
reason for <strong>the</strong> dramatic increase in <strong>the</strong> abundance <strong>of</strong> small polychaetes and crustaceans in Big <strong>Bay</strong> is<br />
not clear. A similar increase in <strong>the</strong> abundance <strong>of</strong> small polychaetes was also seen in Small <strong>Bay</strong>. It is<br />
likely that a natural <strong>Bay</strong>-wide fluctuation, possibly based on nutrient availability and productivity,<br />
may have occurred between 2010 and <strong>2011</strong>, which supported an increase in <strong>the</strong> abundance <strong>of</strong> small<br />
polychaetes. The stability <strong>of</strong> o<strong>the</strong>r taxonomic groups and <strong>of</strong> <strong>the</strong> proportions <strong>of</strong> functional groups<br />
suggests that <strong>the</strong> system has not been subject to a negative disturbance and remains in a state <strong>of</strong><br />
recovery following dredge events<br />
The biomass <strong>of</strong> <strong>the</strong> benthic community in Big <strong>Bay</strong> has been dominated by detritivores in all<br />
years except 2008 when scavengers became dominant. The increased proportion <strong>of</strong> scavengers was<br />
not reflected in terms <strong>of</strong> abundance suggesting that few, large scavenging species and many, small<br />
opportunistic detritivores colonised <strong>the</strong> benthic habitat following dredging. Since 2008, <strong>the</strong> benthic<br />
community has shifted back to one dominated by detritivores both in terms <strong>of</strong> abundance and<br />
biomass, indicating that larger detritivores had re-established. Filter feeding organisms are more<br />
abundant and make a greater contribution to <strong>the</strong> biomass <strong>of</strong> benthic macr<strong>of</strong>auna in Big <strong>Bay</strong> than in<br />
Small <strong>Bay</strong>.<br />
Langebaan Lagoon<br />
Langebaan Lagoon generally supports a much lower abundance and biomass <strong>of</strong> benthic macr<strong>of</strong>auna<br />
than Saldanha <strong>Bay</strong>. This may be due to <strong>the</strong> fast water movements and high levels <strong>of</strong> tidal variation<br />
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ANCHOR<br />
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