Patterns in subtidal seaweed communities on coral-dominated reefs at Sodwana Bay on the KwaZulu-Natal coast,South Africa

Subtidal seaweed communities of the northern coast of KwaZulu-Natal (KZN) have not been studied before. At Sodwana Bay, we tested the hypotheses that the seaweed communities would (1) differ floristically with depth, (2) be more species-rich in shallower water, (3) show similar biomasses within the depth range sampled and (4) be affected (biomass and/or species composition) by sand. Samples were collected (using SCUBA) from reefs ('sites') at depths of about 1m, 7m, 10m, 15m and 26m. Each sample comprised all macroscopic (non-crustose) seaweeds within a 25cm × 25cm quadrat (five quadrats per depth). Environmental factors, including percentage sand cover and depth, were recorded. The seaweed communities were mainly compact turfs; a total of 82 Rhodophyta, 14 Chlorophyta and eight Phaeophyta were recorded. Ordination (canonical correspondence analysis) and classification (Twinspan) of the data showed clear differences in the floristic composition (either as species biomass or presence/absence) with depth, mainly between shallow subtidal communities (0.5–1.0m depth) and those at intermediate depths (5.5–15.0m), followed by the deepest communities (25.7–29.0m) and those at intermediate depths. The shallow samples showed the greatest species diversity. Total seaweed biomass decreased significantly with depth and percentage bare (seaweed-free) substratum increased significantly with depth, possibly because of lower wave action, light penetration, or different grazing patterns. Sand (as percentage sand cover) also affected seaweed community composition, but this showed no pattern with depth. The algal communities on these reefs at Sodwana Bay showed exceptional α-diversity, with 104 taxa (>20% of the recorded KZN flora) occurring in the total sample area of only 1.56m². The seaweed communities of northern KZN are structurally and floristically similar to those of other tropical coral reefs around the world.     

The colonization of artificial substrata by marine sessile organisms in False Bay. 1. Community development

Marine sessile communities developing on stainless steel test panels set 10 and 20 m deep in False Bay over periods ranging from a month to a year were examined. The establishment of communities was characterized by seasonal succession, colonization rates being lowest during winter. Community development differed between depths. At 10 m, barnacles appeared first but numerous mussels settled on them, eventually smothering them. Later, secondary settlement of barnacles on the mussels increased the bulk of the layer. Initial development was slower at the 20 m site, progressing from barnacle dominance to a more complex community including barnacles, serpulids, hydrozoans and compound ascidians. The settlement of solitary ascidians during summer led to their final dominance alongside barnacles. It is suggested that solitary ascidians and barnacles would normally dominate at sublittoral depths up to 20 m in False Bay, except where mussel dominance develops first.     

Geomorphological and managerial implications of fish trapping in the Kosi Bay Estuary,KwaZulu-Natal,South Africa

The tidal basin of the Kosi Bay lagoonal-lacustrine complex is dominated by fish traps that line the intertidal and subtidal environments. These have been considered significant sediment sinks, responsible for transformation of parts of the system from subtidal and intertidal sand-flat settings to mangrove habitats. Mangrove progradation has been attributed to sediment retention within the trap structures. Fish-trap counts since 1942 indicate no significant increase in trap number prior to 1980, but thereafter trap numbers have increased exponentially. Historical GIS analysis indicates a linear growth rate of mangrove areas since 1942, a trend not mirrored in the numbers of fish traps. Modelling of mangrove progradation indicates lateral extension rates per annum much lower than global figures for choked systems elsewhere. Modelling of choking thresholds for the Kosi Bay system yields a minimum date of ～2500 AD. By including sea-level rise within the model, newly formed mangrove communities may either be drowned or remain in step with predicted sea-level rises within the next 150–200 years. The role of fish traps in the conversion of subtidal environments to sedimentary environments dominated by mangroves is negligible, and this shallowing would not be of concern in light of the short-term nature of managerial timescales.