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Parks Victoria Technical Series No. 79<br />

Flinders and Twofold Shelf Bioregions Marine Natural Values Study<br />

Intertidal<br />

Soft sediment<br />

The intertidal soft sediment is in the north-west of Point Hicks MNP as sand beach fronting<br />

an extensive dune system (Ball and Blake 2007). As noted by Plummer et al. (2003) no<br />

specific data on the biota on sandy beaches are available in the MNP or nearby. Intertidal<br />

soft sediment flora is restricted to macroalgae drift and macroalgal epiphytes. Beach-washed<br />

materials in sandy beach habitats are a significant source of food for many shore birds, and<br />

contribute to the detrital cycle that nourishes many of the invertebrates, such as bivalves,<br />

living in the sand (Parks Victoria 2006c).<br />

Reef<br />

Rocky intertidal reefs, also called rocky reefs or intertidal platforms, are generally found in<br />

Victoria on and near headlands with stretches of sandy beaches either side. Along with<br />

beaches, intertidal reefs are one of the most accessible components of the <strong>marine</strong><br />

environment as they are the interface between the ocean and the land (Power and Boxshall<br />

2007). As such they are valued as important habitats by people and tend to be visited more<br />

than other sections of the coast (Carey et al. 2007a; Carey et al. 2007b). This means they<br />

are often subjected to human pressures like harvesting, fossicking and trampling as well as<br />

pressures from pollution sources on land and in the sea (Power and Boxshall 2007).<br />

Intertidal reef biota are exposed to large changes in physical conditions such as temperature<br />

and desiccation. There is great spatial and temporal variability in the life histories of the<br />

organisms and the environmental processes in reef habitats (Underwood and Chapman<br />

2004). The recruitment of new biota onto the reef, from the plankton, strongly influences the<br />

ecological patterns for individual species and assemblages. Interactions between biota on<br />

the reef also influence biota distribution. Resources which are often in short supply on<br />

intertidal reefs are space on which to live and the food itself (Underwood and Chapman<br />

2004).<br />

The composition of invertebrate assemblages living on the intertidal reefs at Point Hicks are<br />

more similar to those found at Mallacoota, Merimbula and Bermagui than to assemblages<br />

found further west along the Victorian coast (Hidas et al. 2007). East coast species<br />

contributing to these differences have lower densities at Point Hicks than in NSW (Hidas et<br />

al. 2010).<br />

The MNP has a relatively narrow band rock platform around the base of Point Hicks itself<br />

(Ball and Blake 2007). The remote location of the MNP means that human threats to the<br />

intertidal reef such as biota collection and trampling is low, due to this there is has been no<br />

intertidal reef monitoring program in Point Hicks MNP. As noted by Plummer et al. (2003) no<br />

specific data on the biota on intertidal reefs are available in Point Hicks MNP or nearby.<br />

Subtidal<br />

Soft sediment<br />

Between Whaleback Rock and the isolated reef directly off Point Hicks biogenic gravel,<br />

consisting of whole and broken shells often encrusted in pink algae, covers the ocean floor<br />

(Holmes et al. 2007a). Shell areas tend to have many small orange ball sponges Tethya in<br />

amongst the shells (Holmes et al. 2007a). Sometimes vertical sponges are also present,<br />

attached to larger shells (Holmes et al. 2007a). Areas with rippled sand also contains shells<br />

in the ripple troughs. These shells are usually covered in pink encrusting algae, possibly<br />

indicating the presence of rhodoliths in these areas (Holmes et al. 2007a). Sand areas tend<br />

to be bare, although if vegetation is present, it is usually clumps of Caulerpa. Some areas of<br />

sand are inhabited by sessile invertebrates; however, as the species of invertebrates<br />

observed must attach to a hard substrate, it is assumed that the sand forms a thin veneer<br />

over the reef (Holmes et al. 2007a).<br />

53

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