the reef biota at bunurong marine national park - Parks Victoria
the reef biota at bunurong marine national park - Parks Victoria
the reef biota at bunurong marine national park - Parks Victoria
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<strong>Parks</strong> <strong>Victoria</strong> Technical Series No. 84<br />
Bunurong Subtidal Reef Monitoring<br />
3 RESULTS<br />
3.1 Biodiversity<br />
3.1.1 Community Structure<br />
Macroalgae<br />
The canopy algae assemblages <strong>at</strong> Bunurong were characterised by a diverse range of<br />
medium-sized brown algal species. The predominant brown algal species included S.<br />
axillaris, C. pl<strong>at</strong>ylobium, C. moniliformis, C. retorta, C. retroflexa, A. panicul<strong>at</strong>a and<br />
Sargassum fallax. O<strong>the</strong>r larger brown species such as E. radi<strong>at</strong>a and P. comosa were<br />
generally absent or in very low abundances. O<strong>the</strong>r dominant components of <strong>the</strong> algal<br />
assemblages included <strong>the</strong> seagrass A. antarctica, coralline algae such as Haliptilon roseum<br />
and Metagoniolithon radi<strong>at</strong>um, as well as <strong>the</strong> red algae Phacelocarpus peperocarpos,<br />
Areschougia congesta and Plocamium angustum. The dominant green algae were; Caulerpa<br />
brownii, Caulerpa scalpelliformis and Caulerpa flexilis, however were rel<strong>at</strong>ively low in<br />
abundance.<br />
The MDS plots indic<strong>at</strong>ed <strong>the</strong>re was an overall east-west gradient in changes in algal<br />
assemblage structure (Figure 3.1a - b). This change in site algal assemblage can be largely<br />
<strong>at</strong>tributed to an increasing predominance of <strong>the</strong> seagrass A. antarctica, as well as <strong>the</strong> brown<br />
algae S. axillaris and C. pectin<strong>at</strong>a in <strong>the</strong> far eastern sites. The eastern sites also had much<br />
lower abundances of A. panicul<strong>at</strong>a and P. peperocarpos than <strong>the</strong> western sites.<br />
The sites within <strong>the</strong> Bunurong Marine N<strong>at</strong>ional Park (MNP) were rel<strong>at</strong>ively similar in<br />
structure, however a distinction between Shack Bay sites (Sites 5, 6 and 12) and o<strong>the</strong>r sites<br />
was evident (Figure 3.1a). Amphibolis antarctica was absent or in very low percentage cover<br />
<strong>at</strong> Twin Reefs (Site 4), Oaks East (Site 3) and The Oaks Beach (Site 12), with prevalence<br />
much higher <strong>at</strong> Shack Bay sites.<br />
Amongst <strong>the</strong> western reference sites, Cape P<strong>at</strong>erson (site 1) was quite different in<br />
assemblage structure and was reasonably isol<strong>at</strong>ed <strong>at</strong> <strong>the</strong> top of <strong>the</strong> MDS plot (Figure 3.1b).<br />
This can be explained by a higher abundance of A. antarctica, C. retorta and C. retroflexa,<br />
lower abundance of P. peperocarpos and an absence of S. axillaris. This algal assemblage is<br />
more similar to <strong>the</strong> far eastern sites (Sites 7, 8 and 13) and this is reflected in its rel<strong>at</strong>ive<br />
position in <strong>the</strong> MDS plot. There was considerable overlap in assemblage structure for <strong>the</strong><br />
three eastern reference sites (Figure 3.1b).<br />
The algal assemblage control charts indic<strong>at</strong>ed an increase in devi<strong>at</strong>ion from both <strong>the</strong> prior<br />
times and baseline centriods for all sites except Bo<strong>at</strong> Ramp East (Site 15) and Petrel Rock<br />
West (Site 13; Figure 3.2a - d). Sites <strong>at</strong> Shack Bay (Site 5, 6 and 12) showed significant<br />
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