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Kirsten Benkendorff*, Ryan Baring, Tom Stewart and Tanith Ramsdale. *Author for correspondence, School of Biological Sciences, Email: [email protected] .au Ph: 8201 3959; Fax: 8201 3015 IMPACTS OF SAND DREDGING: O’SULLIVANS BEACH DECEMBER 2009 O’Sullivans Beach intertidal reef in April, 2009 after sand dredged from the O’Sullivans - Beach Marina was deposited on the adjacent shore. - 1| Page

IMPACTS OF SAND DREDGING: O’SULLIVANS BEACH · flushed lower intertidal areas, much of the sand appeared to have dispersed within a couple of weeks. This indicates that the long-term

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Kirsten Benkendorff*, Ryan Baring, Tom Stewart and Tanith Ramsdale.

*Author for correspondence, School of Biological Sciences,

Email: [email protected] .au

Ph: 8201 3959; Fax: 8201 3015

IMPACTS OF SAND�DREDGING: O’SULLIVANS�

BEACH�DECEMBER 2009

O’Sullivans Beach intertidal reef in April, 2009 after sand dredged from the O’Sullivans­Beach Marina was deposited on the adjacent shore.­

1 | P a g e

Summary­In April 2009 sand dredged from the O’Sullivans Beach Marina was dumped on the adjacent

intertidal reef at O’Sullivans Beach. This report documents the outcomes of a monitoring

program to assess any immediate impacts of the sand deposition (May 2009) relative to

control sites, as well as the recovery of intertidal communities six months later (October,

2009). Where possible, comparisons are also made to pre-impact surveys undertaken in

November 2007. Overall there was minimal evidence of any substantial impacts on the

intertidal reefs as a result of sand dumping. Most of the sand had cleared from the intertidal

zone by May 2009 and although some large anoxic patches of sand were observed in the

higher intertidal zone, these had all cleared by October, 2009. Transect surveys of the

percent cover of intertidal habitat revealed a relatively high proportion of bare substrate

and less algal cover in May 2009 relative to November 2007. However, this occurred across

all sites, including controls and had mostly recovered by October 2009, thus indicating

natural seasonal variability. The diversity and abundance of invertebrates from quadrat

surveys was found to vary in both space and time, with the impact sites surveys generally

falling within the range of control sites post-impact. The abundance of molluscs increased

substantially in October relative to May, 2009, most likely as a result of the corresponding

increase in algal cover. Multivariate analyses revealed no significant different in invertebrate

community composition between impact and control sites. The macrofaunal communities

were observed to change significantly over time at all sites. Dispersion also varied between

sites but with no consistent effect over time according to proximity to the sand deposition

(i.e. impact vs. control sites). Surveys for the whelk Dicathais orbita also revealed no

evidence for negative impacts associated with sand accumulation in the shallow subtidal

area subsequent to the dredging. Overall these surveys indicate that intertidal reefs such as

O’Sullivans Beach may be relatively resilient to one-off sand dumping events at the

beginning of Winter. Nevertheless, caution should be taken before extrapolating these

results to other any locations, times or larger scale dredging activities.

2 | P a g e

Contents

Summary .................................................................................................................................................2

Introduction ............................................................................................................................................4

Aims ....................................................................................................................................................6

Methods.................................................................................................................................................. 7

Study sites & surveys ..........................................................................................................................7

Substrate Percent cover& sand depth................................................................................................9

Sand accumulation..............................................................................................................................9

Intertidal gastropod abundance & sessile organism cover ................................................................9

Abundance and size frequency of Dicathais orbita ............................................................................9

Statistical Analyses............................................................................................................................10

Results...................................................................................................................................................10

Video Transect Data..........................................................................................................................10

Sand Accumulation ...........................................................................................................................12

Species Richness ...............................................................................................................................15

Species Diversity ...............................................................................................................................15

Photo Quadrat Abundances and Percent Cover of Sessile Invertebrates ........................................18

Invertebrate Community Composition .............................................................................................21

Dicathais orbita abundance and size ................................................................................................23

Discussion..............................................................................................................................................24

References ............................................................................................................................................26

Appendix ...............................................................................................................................................28

3 | P a g e

Introduction­Coastal marine habitats in South Australia can be essentially divided into soft sediment

habitats (e.g. sandy beaches) and rocky reefs. Distinct ecological communities have evolved

to live in, or on, these vastly different substrata (Benkendorff et al., 2008). In particular,

rocky intertidal shores are highly productive environments with large visible populations of

a range of invertebrates, predominantly molluscs. The hard substratum is coated with a

microbial biofilm that provides a source of food for micrograzers, such as limpets and snails.

In the mid-to-lower intertidal zones the hard substrate also provides suitable attachment

sites for macroalgae and sessile invertebrates, including barnacles, mussels and other filter

feeding organisms. On the other hand, sandy marine habitats often resemble a desert

(Benkendorff et al., 2008). Whilst many invertebrates are adapted to live in the sand, they

are mostly microscopic or burrowing organisms that hide beneath the sand surface.

Consequently, the deposition of sand on rocky reefs is expected to result in detrimental

impacts to rocky shore adapted organisms.

Previous studies on the effects of sedimentation on rocky intertidal and subtidal reefs have

revealed a range of effects due to scour and smothering. These include reduction of light

availability for juvenile plants, interference with the recruitment and survival of algae

(Airoldi and Cinelli, 1997; Littler et al., 1983; Scheil et al., 2006; Yanez et al., 2008), changes

in the zonation patterns (Littler et al., 1983) and species diversity (Huff and Jarett, 2007;

Pulfrich et al., 2003), as well as the unstabilisation of communities (Prathep et al., 2003).

Sand smothering can also interfere with respiration and feeding activity of intertidal

organisms (Airoldi and Hawkins, 2007) and interfere with settlement and recruitment

patterns (Taylor and Littler, 1982; Pineda, 1994). Consequently, if sand persists on rocky

shores, it may lead to long-term shifts in the local ecological communities and ultimately a

reduction in the productivity of the area.

Periodically, sand dredging activities are required along the South Australian coast in order

to maintain boat access in harbours and marinas. For practicality, the excess sand is often

disposed locally at adjoining coastal areas, as off-shore disposal or trucking the sand away

would have significant cost implications. However, these economic costs need to be

weighed up against potential long-term environmental impacts. To date no studies have

investigated the effects of sand dumping on rocky reefs in South Australia. Recently,

community concerns have been raised over the deposition of sand on O’Sullivans Reef, as a

result of dredging the local marina. Personal observations at the site a few weeks after the

dredging event indicate that significant areas of the reef were smothered by sand (Figure 1).

Large sand patches remained in the mid-high intertidal areas extending north of the marina

and beyond the Port Stanvac fence, up towards the Port Stanvac Jetty. However, in well

flushed lower intertidal areas, much of the sand appeared to have dispersed within a couple

of weeks. This indicates that the long-term effects of sand deposition on rocky reefs may

depend on a combination of factors, including the topography of the reef, water movement

and sand dispersal, as well as the scale and frequency of the sand deposition. The recent

dredging event in early 2009 at the O’Sullivans Beach site offers a good opportunity to

4 | P a g e

investigate the short term impacts on local rocky reef communities and some of the factors

that may influence longer-term change.

a) b)

c) d)

Figure 1: The intertidal reef at O’Sullivans Beach pre- (left panels) and post-(right panels)

impact from sand dumping on the rocky shore. Pre-impact photos (a & c) were taken in

November 2007, whereas post-impact photos (b & d) were taken in April 2009. The top

panels (a & b) show the view towards the O’Sullivans Beach Marina which was dredged in

April 2009, where as the lower panels (c & d) show the view toward Port Stanvac, with the

Port Stanvac jetty visible in the background.

5 | P a g e

Assessing impacts to ecological communities can often be complicated by a lack of baseline

data before the impact. Ideally, ecological impacts should be assessed using replicated

studies at the both the impact site and several control sites, both before and after the

impact event (Underwood, 2001). Recent surveys of the shallow subtidal whelk Dicathais

orbita have been undertaken at the impacted O’Sullivans Beach site and potential controls

sites (Noble et al., 2009). As an invertebrate predator, this species can be considered a good

indicator for reef health. Furthermore, in 2007, intertidal surveys were undertaken in the

O’Sullivans Beach & Port Stanvac area for the Adelaide and Mt Lofty Natural Resource

Management Board (Dutton and Benkendorff, 2008). Through the application of

standardised methodology, this data can be used for pre- and post impact comparisons. The

Dutton and Benkendorff (2008) surveys include baseline data at the main impact site, a

more distant impacted site north of the Port Stanvac fence, as well as suitable control sites

at various distances from O’Sullivans Beach (one on the northern side of the Port Stanvac

Jetty, one at Hallett Cove and another at Marino Rocks; refer to Figure 2 and Figure 3).

Useful baseline data from the Dutton and Benkendorff (2008) surveys include standardised

transects for the percent composition of the substrate. Notably, no sand was recorded at

the O’Sullivans Beach main impact site (Figure 1) in the 2007 survey, whilst ~15% of the

habitat was recorded as sand along transects at the Northern impact site at Port Stanvac

(Dutton and Benkendorff, 2008). High species richness and particularly high percent covers

were recorded for turf and foliose algae at O’Sullivans Beach, in comparison to the Port

Stanvac area. Percent cover of sessile invertebrates and mobile gastropods were similar.

By applying standardised methodologies at the previously surveyed impact and control

sites, it should be possible to gain insight into any changes in the rocky reef communities

that have occurred at these sites since the recent sand deposition in early 2009. To fully

assess the scale of impact of the 2009 sand deposition episode, additional sites without

baseline data were implemented in the southern impact zone and a control site south of the

O’Sullivans Beach Marina (Figure 2). All sites were surveyed in May and six months later in

October, 2009, to assess possible recovery. Additional data parameters on sand patches and

topography were recorded at the main impacts sites to gain insight into the nature of sand

persistence on rocky reefs.

Aims

The aim of this project was to assess the impacts of sand deposition at O’Sullivans Beach,

S.A. This was done using previous data and a short term case study of intertidal reefs in the

region. The application of before, after control, impact studies of the rocky reef ecological

communities along the Adelaide Metropolitan coast will provide a model system for future

monitoring programs. Specific objectives are to:

1) Provide a detailed assessment of the percent cover and depth of sand overlying the

rocky substrate along transects at varying distances from the sand deposition site.

2) Characterise the topography where sand has accumulated on the intertidal rocky

reefs.

6 | P a g e

3) Assess the percent cover of sessile intertidal organisms at impact and reference

locations, in comparison to previously collected data.

4) Assess the invertebrate abundance and community composition at control and

impact surveys in May and six months later in October, 2009.

5) Assess the abundance and size frequency distribution of shallow subtidal Dicathais

orbita at one control and one impact site, in comparison to previous data.

Methods

Study sites & surveys

This study focused on the O’Sullivans Beach area (Figure 2), with several reference sites

located at varying distances to the north (Figure 2& 3). In total the study included the main

impact site at O’Sullivans beach, as well as two mild impacted locations (<200m to the north

and South). Nearby control locations were sited < 1km to the north and south side of the

impact zones, both on the other side of large rock groynes preventing indirect sand drift

from the dredges. Two additional sites to the North at Hallett Cove and Marino Rocks were

chosen as secondary control sites located greater than 10 km from the impact zone (Figure

3). Each site was surveyed once in May - June and again in October-November (Table 1). All

intertidal surveys were undertaken in calm weather at low tide. It should be noted that the

first May surveys occurred several weeks after the dredged sand was dumped at O’Sullivans

Beach and subsequent to a major storm event.

Table 1: Sites and sampling dates for the intertidal reef sand dredging impact survey at O’Sullivans

Beach during May and October 2009.

Site GPS Coordinates Sampling Date Tide Height Tide Time

South East May October May October May October

Marino Rocks 35o02’45.6” 138

o30’27.6” 13/05/09 6/11/09 0.61m 0.32 11:40am 1:30pm

Hallett Cove 35o05’06.2’’ 138

o29’31.5” 13/05/09 6/11/09 0.61m 0.32 11:40am 1:30pm

North Control 35o06’28.4” 138

o28’20.0” 14/05/09 5/11/09 0.67m 0.21m 12:06pm 1:00pm

North Impact 35o06’48.8” 138

o28’13.5” 14/05/09 5/11/09 0.67m 0.21m 12:06pm 1:00pm

Main Impact 35o06’57.5” 138

o28’11.2” 12/05/09 2/11/09 0.58m 0.21m 11:12am 11:35am

South Impact 35o07’07.05” 138

o28’06.72” 11/05/09 2/11/09 0.57m 0.21m 10:45am 11:35am

South Control 35o07’16.10” 138

o28’02.36” 29/05/09 22/10/09 0.83m 0.35 12:06pm 1:10pm

7 | P a g e

Figure 2: Intertidal reef survey and whelk sites at O’Sullivans Beach surveyed in May and

October, 2009.

Figure 3: Intertidal reef control sites (>10km from O’Sullivans beach main impact zone)

surveyed in May and October 2009.

8 | P a g e

Substrate Percent cover& sand depth

Ten randomly spaced, 20 m shore-normal line transects were located within each study site

using a 50 m fibreglass tape. To enable rapid survey of substrate types during low tide,

transects were recorded using an Olympus (Model Tough8000) camera. Substrate video

footage was subsequently analysed for percent cover using VLC media player. Substrate

types were recorded in patches greater than 5 cm in length using the line intercept method.

In addition to sand and bare rock, sessile organism cover were recorded along the transects

categorised as; foliose algae, turfing algae, encrusting algae/lichen, seagrass, mussels,

galeolaria crust, mixed community and barnacles according to Dutton and Benkendorff

(2008). The extent of each substrate was recorded in centimetres, summed and divided by

the total length (20m) to obtain the percent cover.

Sand accumulation

The O’Sullivans Beach impact sites were visually assessed for areas of persistent sand

accumulation. 15 sand patches were marked and mapped using GPS. For each sand patch,

the volume of the sand patch was calculated by the surface area X depth (averaged from 10

random depth measurements). The average colour of the sand was recorded by comparison

to numbered paint colour charts in the sandy through grey to black colour scheme, where

darker coloured sand provides an indication of anoxic conditions. The topographical

characteristics of the sand patches were recorded based on distance from the low water

mark and on the average height of the surrounding rock on the seaward side.

Intertidal gastropod abundance & sessile organism cover

At each site, 10 replicate 0.25 m2

quadrats were randomly places in the mid-low intertidal

area and a further 10 in the mid-high intertidal zone. For each quadrat, 5 photographs were

taken using an Olympus digital camera (Model µ1030SW/Tough8000). Quadrats were

divided into quarters, with one photo taken of each quarter, as well as one encompassing

the whole quadrat. Photos were subsequently analysed using imaging software. All visible

mobile fauna were identified and counted. Colonial sessile biota such as Limnoperna pulex

and Galeolaria caespitosa were also assessed for percent cover from the photographs.

Abundance and size frequency of Dicathais orbita

Timed search surveys were undertaken in the shallow subtidal areas for Dicathais orbita at

Marino Rocks and O’Sullivans Beach (main impact site, Table 2). All animals located in a

30min search period were collected then measured using callipers, then returned to the

subtidal area.

Table 2: Sites and sampling dates for the subtidal whelk surveys at O’Sullivans Beach.

Survey Date Location GPS

13-03-08 O’Sullivans Beach Reef - South Control 35 07'15.82"S, 138 28'01.50"E

09-05-09 O’Sullivans Beach Reef - South Control 35 07'15.82"S, 138 28'01.50"E

17-05-09 O’Sullivans Beach Reef - Main Impact Zone 35 07'02.35"S, 138 28'08.32"E

14-11-09 O’Sullivans Beach Reef - Main Impact Zone 35 07'02.35"S, 138 28'08.32"E

9 | P a g e

Statistical Analyses

To determine the diversity and evenness of invertebrate species composition at all sites, three

different diversity indices were calculated (Shannon-Wiener index, Pielou’s evenness and Simpson’s

index) based on the total number of individuals (N) of each taxa (S). The Shannon-Wiener index

identifies greater species diversity with an index number closer to one. Pielou’s index identifies the

equitability of species presence at each site where a larger number indicates less evenness.

Simpson’s index is a measure of ecological diversity with infinite diversity decreasing from zero to

one, indicating dominance of single species (Clarke and Warwick 2001).

Multivariate data on changes in the invertebrate community composition across time and space

were analysed using PRIMER v.6 +PERMANOVA. Square-root transformed, Bray Curtis similarity

(with dummy variable = 1) data were used for the analysis. PERMANOVA was used to investigate

differences in the macrofaunal community among sites and months, using a three-way, nested

design, with Sites (a random factor with 7 levels) nested in Types (a fixed-factor with 2 levels;

impacted versus control) both fully-crossed with Months (a fixed factor with 2 levels; May and

October). PERMANOVA detects significant differences in both community structure and variability.

To separate these, PERMDISP was used to test for significant differences in dispersion (i.e.

variability) among samples and a multidimensional scaling (MDS) plot constructed to investigate

differences in the macrofaunal community structure. Either an increase or decrease in dispersion

can be an indicator of disturbance in marine communities (Anderson et al. 2008).

Results

Video Transect Data

Transect data from the pre-impact sampling period in November 2007 revealed a relatively high

cover of sand at the Northern Impact site (>20%), over 10% sand at Marino and < 2% at Hallet Cove,

but no sand at the Main impact or North Controls in the O’Sullivans Beach/Port Stanvac area (Figure

4a). The percent of bare substrate ranged from <50% at the Main Impact site to 80% at Hallet Cove.

After the sand dumping in May 2009 the video transects revealed a large percent cover of bare

substrate (> 70%) at most sites except the Southern Control site (Figure 4b). In comparison the

percent cover of sand was minimal (< 1%) and only present at the Hallett Cove, Main Impact, South

Impact and South Control sites. In October 2009 the percent cover of bare substrate reduced to

below 70% at all sites, and a low percent cover of sand (< 5%) was recorded at the Marino, Main

Impact, South impact and South Control sites (Figure 4c).

10 | P a g e

November 2007�

(a)

0

10

20

30

40

50

60

70

80

90

100

Pe

rce

nt

cov

er

(%)

sand

bare substrate

Marino Rocks Hallett Cove North Control North Impact Main Impact

(b)

0

10

20

30

40

50

60

70

80

90

100

Pe

rce

nt

Co

ve

r (%

)

May 2009

Sand

Bare Substrate

Marino Rocks Hallett Cove North Control North Impact Main Impact South Impact South Control

100 October 2009 90

80 (c)

Pe

rce

nt

Co

ve

r (%

) 70

Sand

60 Bare Substrate

50

40

30

20

10

0

Marino Hallett Cove North Control North Impact Main Impact South Impact South Control

Figure 4: Mean percent cover of bare substrate and sand cover from video transects at O’Sullivans

Beach impact and controls sites during (a) November 2007 (pre-impact), (b) May 2009 and (c)

October 2009 (post impact).

11 | P a g e

The transect data from the pre-impact November , 2007 surveys is not directly comparable to the

post-impact surveys due finer detail on the algal composition in the 2009 surveys (Figure 5).

Nevertheless, it is clear that higher pre-impact algal cover was found in the Port Stanvac/O’Sullivans

Beach area compared to the more northern sites at Marino and Hallet Cove (Figure 5a). In May,

2009 the total percent cover of flora and sessile fauna dropped at all previously surveyed sites, but

was substantially higher the South Control site, which was strongly influenced by the presence of the

foliose green algae Ulva australis and mixed algal communities (Figure 5b). The percent cover of

mixed algal community was also well represented at the North Control and Main Impact sites.

Compared to May, video transects from October 2009 identified an increase in percent cover of

flora and fauna at all sites except the South Control site which had similar percentages for each

category in both months (Figure 5c). All sites were represented by large percentages of mixed algal

communities, while the North Control and North Impact sites also had large percentages of mixed

invertebrate communities. Encrusting red algae was also well represented at the Main Impact site

with a large contribution to the overall percent cover of flora and fauna for this site (Figure 5c).

Sand Accumulation

Sand accumulation patches on the intertidal reef were only recorded within the Main Impact and

North Impact sites during May, 2009. The sand patches recorded at both sites were limited to the

mid to high tide zones behind rock ledges of > 1 metre in height (Table 3). The overall accumulation

across all sand patches indicated that the mean dimensions of patches were generally large (>1m

width and > 2m length) but with small volumes (< 0.25m3) and appeared to be partially anoxic

according to colouration (Table 3, Figure 6). In October there was no indication of persistent sand

accumulation with zero sand patches were recorded within the Main Impact and North Impact sites.

12 | P a g e

Impact

November 2007�

Perc

ent C

over

(%)

Pe

rce

nt

Co

ve

r (%

) Pe

rcen

t Cov

er (%

)

80

70

60

50

40

(b) 30

20

10

0

80

70

60

50

40

30

20

10

0

0

Marino Hallett Cove North North Main Impact

Rocks Control

May 2009

Mussel

Lichen

Nerita

Mixed Algal /Invertebrate

Mixed Invertebrate Community

Mixed Algal community

Encrusting Green

Foliose Green

Turfing Green

Encrusting Red

Foliose Red

Turfing Red

Foliose Brown

Encrusting Brown

Turfing Brown

Barnacle

Tube Worms

Marino Rocks Hallett Cove North Control North Impact Main Impact South Impact South Control

October 2009

Mussel

Lichen

Mixed Algal /Invertebrate

Mixed Invertebrate Community

Mixed Algal community

Encrusting Green

Foliose Green

Turfing Green

Encrusting Red

Foliose Red

Turfing Red

Foliose Brown

Encrusting Brown

Turfing Brown

Barnacle

Tube Worms

Marino Hallett Cove North Control North Impact Main Impact South Impact South Control

Mussels

Lichen

80

70

Mixed Algae/Invertebrates 60

Foliose Algae (a)

50 Encrusting Algae

40 Turfing Algae

Barnacles 30

Tube worms 20

10

Figure 5: Mean percent cover of flora and sessile fauna from video transects at O’Sullivans Beach

impact and controls sites during (a) November 2007 (pre-impact), (b) May 2009 and (c) October

2009 (post impact).

13 | P a g e

Table 3: Presence of sand accumulation for the Main Impact and North Impact sites recorded during

May 2009. Sand patch colour code for potential oxygen content and quality of sand. N = Normal (1-

3), PA = Partially Anoxic (4-5), HA = Highly Anoxic (6-7), EA = Extremely Anoxic (8).

Site Sand Patch Number GPS position Distance from Low Tide (m) Rock Height (m) Mean Width (m) Mean Depth (m) Length (m) Volume (m3) Sand Patch Colour

Main Impact Zone

Main Impact Zone

Main Impact Zone

Main Impact Zone

Main Impact Zone

Main Impact Zone

Main Impact Zone

Main Impact Zone

Main Impact Zone

Main Impact Zone

1

2

3

4

5

6

7

8

9

10

S35o06’59” E 138

o28’10”

S35o06’58.7” E138

o28’10.6”

S35o06’58.5” E138

o28’11.0”

S35o06’59.0" E138

o28’10.0”

S35o06’58.9” E138

o28’10.4”

S35o06’58.8” E138

o28’10.5”

S 35o06’58.9” E 138

o28’10.3”

S35o06’58.9” E 138

o28’10.5”

S35o06’59.1 E 138

o28’10.4

S 35o07’00.0” E 138

o28’10.2”

21

18

21

23

14

15

12

11

13

13

1 − 2

1 − 2

1 − 2

1 − 2

1 − 2

1 − 2

1 − 2

1 − 2

3

< 1

1.46

1.63

1.30

1.90

0.85

0.65

0.85

0.40

1.80

0.67

0.02

0.02

0.02

0.05

0.02

0.03

0.04

0.06

0.03

0.03

5.00

1.80

2.20

3.40

1.20

0.70

1.54

1.20

2.65

1.80

0.15

0.07

0.05

0.29

0.02

0.01

0.05

0.03

0.13

0.03

3

3

4

4

4

4

4

5

4

4

North Impact Zone

North Impact Zone

North Impact Zone

North Impact Zone

North Impact Zone

1

2

3

4

5

S 35o06’50.1” E 138

o28’13.0”

S 35o06’50.2” E 138

o28’13.2”

S 35o06’50.6” E 138

o28’13.0”

S 35o06’50.7” E 138

o28’12.9”

S 35o06’50.8” E 138

o28’13.2”

15

14

15

13

13

2

3

3

3

1

4.50

3.85

1.25

1.70

1.00

0.06

0.07

0.06

0.06

0.03

2.95

2.18

3.40

1.70

2.90

0.76

0.59

0.26

0.18

0.08

4

4

4

4

4

Mean − − 15.4 − 1.37 0.04 2.31 0.18 3.93

Sand Patch Code

1

2 N

3

4

5 PA

6 HA

7

8 EA

Figure 6: An example of a sand patch showing grey colouration indicative of anoxia in the

sediment dredged from O’Sullivans Beach marina and deposited on the adjacent intertidal reef.

14 | P a g e

Species Richness

Invertebrate species richness recorded from quadrat surveys on the intertidal reefs was highest at

the North Impact and Main Impact sites during May, which was attributed to the large number of

gastropod species (Figure 7a, Appendix 1). Control sites held similar species numbers and mainly

consisted of gastropods, except Marino which had very low species numbers in comparison. The

presence of crustaceans at most sites was represented by two species of barnacles (Chthamalus

antennatus and Chamaesipho tasmanica). In comparison, bivalves and annelids were only

represented by ones species for each taxa (Limnoperna pulex and Galeolaria caespitosa respectively)

(Figure 7a). In October species richness remained highest at the North Impact and Main Impact, as

well as the South Impact site, due to the large number of gastropod species (Figure 7b). However, in

comparison to the May survey the numbers of gastropod species was much lower, while the

presence of bivalves and annelid tubeworms increased overall. In addition, a new species of annelid

tubeworm was recorded at the North Impact and South Control Sites (Pomatoceros taenita) in the

October survey (Figure 7b).

In comparison to the November 2007 pre-impact surveys, species richness was higher at all sites in

the May 2009 surveys, with a maximum of 17 species recorded at two sites within the impact zone

(Table 4). By October 2009, the species richness dropped to similar numbers as recorded in the pre-

impact 2007 surveys, with a maximum of 14 species at O’Sullivans Beach.

Species Diversity

Pre-impact diversity indexes were only available for the North Impact and northern control sites

(Dutton and Benkendorff, 2009). Comparison of the Shannon-Weiner diversity index at the north

impact site showed a decrease in diversity from 1.5 in November 2007 to 0.6 in May 2009m then

recovering to 1.5 in October 2009 (Table 4). A drop in Pielou’s eveness values at the North Impact

site in May 2009 (Table 4) indicates corresponding increase in the eveness between species

abundances immediately post impact. A drop in the diversity and increase in the eveness values was

also observed at the Northern control site in the May 2009 survey in comparison to November 2007,

although the magnitude of change was much smaller than at the main impact site. The diversity and

evenness at the more northern control sites at Hallet Cove and Marino remained relatively constant

over time (Table 4)

The May survey 2009 recorded the highest Shannon-Weiner diversity values at the Main Impact and

Hallett Cove sites (Table 5a), which also had uneven species composition due to the dominance of

the gastropod Nerita atramentosa at both sites and the barnacle Chthamalus antennatus at the

Main Impact site (Appendix 1). Most of the other sites also recorded relatively high species diversity

in May except the North Impact site which had very low Shannon-Weiner diversity values in

comparison (Table 5a). In October 2009, the Hallett Cove, Marino and Main Impact sites decreased

in diversity (Table 5b), while all other sites increased in species diversity when compared to

Shannon-Weiner values recorded in May. The highest Shannon-Weiner diversity values in October

were identified for the South Impact and South Control sites with relatively even species

composition (Table 5b). However, a high Simpson’s Index indicated that there was some species

15 | P a g e

dominance due to the gastropod Siphonaria diamenensis at both the South Impact and South

Control sites and C. antennatus at the South Impact site.

(a)

0

2

4

6

8

10

12

14

16

18

20

Spe

cie

s N

um

be

r

May 2009

Crustacea

Bivalvia

Gastropoda

Annelida

Marino Rocks Hallett Cove North Control North Impact Main Impact South Impact South Control

18

16

(b)

Spe

cie

s N

um

be

r�

Crustacea

14 Bivalvia

12 Gastropoda

October 2009

Marino Hallett Cove North Control North Impact Main Impact South Impact South Control

10 Annelida

8

6

4

2

0

Figure 7: Total species richness recorded from quadrat surveys at the O’Sullivans Beach impact and

control sites during (a) May and (b) October 2009.

16 | P a g e

Table 4: Temporal comparison of the total species richness (S), Shannon-Weiner diversity index (H’)

and Pielou’s evenness (J’) from photoquadrats at the O’Sullivans Beach impact site and northern

controls. The November 2007 surveys were conducted by Dutton and Benkendorff (2008) prior to

the sand impact, where as the May and October 2009 represent post-impact surveys undertaken as

part of this study.

Site November 2007 May 2009 October 2009

S H’ J’ S H’ J’ S H’ J’

Marino 7 1.4 0.6 9 1.3 0.6 6 0.6 0.4

Hallet Cove 12 1.7 0.7 15 1.6 0.6 11 1.2 0.5

North Control 13 1.5 0.6 16 1.0 0.4 12 1.1 0.5

North Impact 14 1.5 0.5 17 0.6 0.2 13 1.4 0.4

Main Impact 14 NA NA 17 1.8 0.6 14 1.1 0.6

Table 5: Diversity Indices for the intertidal reefs survey during (a) May and (b) October 2009.

S = number of taxa; N = total number of individuals.

(a)

Site S N Shannon-Weiner Pielou's evenness Simpson

Marino 9 123 1.300 0.592 0.588

Hallett Cove 15 244 1.622 0.599 0.69

North Control 16 1958 1.028 0.371 0.484

North Impact 17 3584 0.553 0.195 0.244

Main Impact 17 448 1.790 0.632 0.767

South Impact 12 843 1.390 0.559 0.675

South Control 12 407 1.312 0.528 0.615

(b)

Site S N Shannon-Weiner Pielou's evenness Simpson

Marino 6 471 0.627 0.350 0.297

Hallett Cove 11 608 1.199 0.500 0.549

North Control 12 2722 1.140 0.459 0.570

North Impact 13 3208 1.354 0.528 0.648

Main Impact 14 1052 1.125 0.426 0.457

South Impact 14 1526 1.628 0.617 0.751

South Control 11 754 1.488 0.621 0.655

17 | P a g e

Photo Quadrat Abundances and Percent Cover of Sessile Invertebrates

In the May 2009 survey, abundances of all phyla in photo quadrats were highest at the North Impact

and North Control sites and comparatively low at all other sites (< 200 individuals m-2

) (Figure 8a).

The higher abundances of crustaceans at both the North Impact and North Control sites were

attributed to the large numbers of the C. antennatus barnacle (Figure 8b). In comparison, the

abundances of molluscs were highest at the North Impact and North Control sites, but were

comparatively low across all sites (< 110 individuals m-2

) (Figure 8c). In October 2009, the total

abundance of all phyla was greatest at the North Impact, North Control and South Impact sites,

while abundances at all other sites were comparably low (< 300 individuals per m3) (Figure 8a). The

abundances of crustaceans were low at all sites and substantially lower at the North Control, North

Impact and South Impact sites compared to the abundances recorded in the May survey (Figure 8b).

However, the abundances of molluscs increased across all sites in October, and were greatest at the

North Control and North Impact sites (Figure 8c).

Some pre-impact data was available for the percent cover of colonial sessile invertebrates from

Dutton and Benkendorff (2008). However, the percent cover was very low at all sites during the

2007 surveys (Figure 9). In the post-impact surveys of May 2009, percent cover was highest at the

South Control site for the Mytilidae mussels (Figure 9b), while the North Impact and Main Impact

sites were highest for the polychaete worms (Figure 9a). All other sites had very low percent cover of

sessile organisms or they were nonexistent. Colonial sessile invertebrates were recorded at all sites

in October 2009 with the greatest percent cover recorded for Mytilidae mussels at the South Control

site (Figure 9b). In comparison, the percent cover of polychaete worms was comparably low at all

sites (< 15% cover, Figure 9a).

18 | P a g e

All Phyla�

(a)

0

200

400

600

800

1000

1200

Ind

ivid

ual

s m

-2 (+

SD)

May

October

Marino Hallett North North Main South South

Cove Control Impact Impact Impact Control

Crustacea (b)

1000

900

May

October

Ind

ivid

ual

s m

-2 (+

SD)

Ind

ivid

ual

s m

-2 (+

SD)

800

700

600

500

400

300

200

100 (c)

0

Marino Hallett North North Main South South

Cove Control Impact Impact Impact Control

Mollusca 900

May

800

700

600

500

400

300

200

100

0

October

Marino Hallett North North Main South South

Cove Control Impact Impact Impact Control

Figure 8: Abundances of (a) All Phyla (b) Crustacea (c) Molluscs recorded from photo quadrats the

O’Sullivans Beach impact and control sites during May and October 2009.

19 | P a g e

Polychaeta�(a)

0

10

20

30

40

50

60

70

Pe

rce

nt

Co

ve

r m

-2 (

+S

D)

Nov-07

May-09

Oct-09

Marino Hallett North North Main South South

Cove Control Impact Impact Impact Control

(b) Mytilidae�

0

20

40

60

80

100

120

140

160

180

Pe

rce

nt

Co

ve

r m

-2 (

+S

D)

Nov-07

May-09

Oct-09

Marino Hallett North North Main South South

Cove Control Impact Impact Impact Control

Figure 9: Percent cover of sessile colonial invertebrates (a) Galeolaria tube worms and (b) Mytilidae

mussels recorded from photo quadrats the O’Sullivans Beach impact and control sites pre (Nov

2007) and post-impact (May and October 2009) from sand deposition. The pre-impact surveys were

only undertaken at Mario, Hallet cove, the North Control and the main impact sites.

20 | P a g e

Invertebrate Community Composition�

PERMANOVA results showed there was no significant difference based on site Types (impact vs

control). Only small-scale spatial and temporal effects were significant (Table 6). PERMANOVA also

shows that the community structure at all seven sites was significantly different between the two

sampling occasions (Table 7). The MDS plot shows a separation of samples based on sampling

occasions and sites (Figure 10), with replicates tending to clump into groups based on sites and

months, as expected based on the results of the PERMANOVA.

Table 6: PERMANOVA results for the invertebrate community composition on intertidal reefs along

the Fleurieu Peninsula surveyed at two time points after the sand deposition at O’Sullivans Beach

reef. Type shows the effect of grouping for control versus impact sites (refer to Figure 2 & 3). Bold

values for P (permutations-based) indicate significant differences.

Source d.f. SS MS Pseudo-F P (perm)Month 1 103070 103070 15.249 0.0002

Type 1 15380 15380 1.1409 0.2775

Site(Type) 5 67403 13481 7.0279 0.0001

Month x Type 1 9295.7 9295.7 1.3754 0.2618

Month x Site(Type) 5 33794 6758.7 3.5235 0.0001

Residual 266 510230 1918.2

Table 7: PERMANOVA pair-wise tests showing the difference at each site between months (October

v. May, 2009).

Site d.f. T P (perm)

Hallett Cove 38 3.947 0.001

Marino Rocks 38 4.607 0.001

Northern Control 38 3.628 0.001

Northern Impact 38 4.281 0.001

Main Impact 38 2.160 0.011

Southern Impact 38 2.265 0.001

Southern Control 38 2.368 0.005

PERMDISP showed there were significant differences in dispersion (i.e. variability) among replicates

for the seven sites (n = 280; F6,273 = 6.689; P (perm) = 0.001) but not between sampling occasions (n =

280; F1,278 = 0.002; P (perm) = 0.996). There were no consistent trends for changes in variability

between sampling occasions, with both control and impact sites showing increases and decreases in

variability (Table 8). Overall, these multivariate analyses indicate that are no significant differences

in community structure among sites based on proximity to the area of presumed impact by sand

deposition at O’Sullivans Beach in 2009. Instead, small-scale spatial (i.e. site) and temporal (i.e.

seasonal) effects seem to be driving differences in community structure among sites.

21 | P a g e

Table 8: PERMDISP pair-wise comparisons of the dispersion during each sampling occasion for each

site. Bolded text indicates significant differences in dispersion (i.e. variability) between sampling

occasions (May and October).

Type Site May October F1,38 P(perm)

Control Hallett Cove 34.041 < 45.249 20.616 0.0004

Control Marino Rocks 26.638 < 39.917 14.182 0.0016

Control Northern Control 47.155 > 40.086 3.63 0.0994

Impact Northern Impact 47.112 > 31.667 23.83 0.0002

Impact Main Impact 41.129 < 46.970 4.268 0.0562

Impact Southern Impact 44.511 < 48.447 1.5797 0.2319

Control Southern Control 45.831 > 36.331 10.674 0.0027

Hallett Cove

Marino Rocks

Northern Control

Northern Impact

Main Impact

Southern Impact

Southern Control

Stress = 0.19

Figure 10: Multidimensional scaling (MDS) plot showing sites (see key) and sampling occasions (May:

solid-fill; October: no fill). MDS plots highlight the relative similarity of replicate samples to each

other, using relative distances between points to represent high-dimensional relationships, in this

case, for community structure (i.e. multiple species and their abundances). Essentially, two points

that plot close to each other represent macrofaunal communities with a similar structure, two points

plotting far apart represent dissimilar communities.

22 | P a g e

Dicathais orbita abundance and size

Timed search surveys of the subtidal environment were undertaken both north and south of the

O’Sullivans beach boat harbour (main impact zone and southern control respectively). Preliminary

observations of the control site south of the boat harbour appear to reveal no major differences in

size and abundance of D. orbita between survey dates March 2008 – April 2009. Consistent with the

intertidal observations of sediment deposition, preliminary observations of the subtidal environment

in the area north of the O’Sullivans beach boat harbour indicate a higher proportion of sediment

accumulation. Field observations revealed that the occurrence of sediment engulfed D. orbita on

rock surfaces with potential implications for survivorship of buried individuals via means of

starvation or asphyxiation if sedimentation remains for extended periods. The November 2009

sampling indicated a lower total abundance (Figure 11a), but a similar mean shell length of whelks at

both the control and impacted sites (Figure 11b).

(a)

(b)

Figure 11 D. orbita (a) abundance, and (b) mean shell length from shallow subtidal surveys

undertaken on a rocky reef at the control (South of O’Sullivans Beach boat ramp) and the impacted

(North of O’Sullivans Beach boat ramp) sites from March 2008 to November 2009

23 | P a g e

Discussion­

Monitoring of the intertidal zone at the O’Sullivans Beach, Port Stanvac and northern control sites

revealed no evidence for persistent impacts from sand dumping on the intertidal reefs. Overall the

variation in percent cover of sand and sessile organisms, as well as the abundance and diversity of

invertebrates appears to be within the range of natural temporal and spatial variability within this

region. The highest percent sand cover was actually recorded at the Northern Impact site in

November 2007 prior to the sand dredging event. Although substantial sand cover was anecdotally

observed in the main impact area immediately after the sand dumping at O’Sullivans Beach (Figure

1), it appears that the storm event prior to the May 2009 was successful in rapidly clearing the

majority of accumulated sand. Nevertheless, some fairly large and partially anoxic sand patches

were recorded in the main impact area during May 2009. These occurred behind rock ledges > 1m

tall and at distances between 12-23 m from low tide. However, by October 2009, all of these sand

patches had completely cleared from the intertidal reef.

The most noticeable effect of the sand dumping at O’ Sullivan Beach appears to be a substantial

increase in the percent cover of bare substrate at the main and north impacts sites between

November 2007 and May 2009 (> 25%). Correspondingly there is a drop in the percent cover of

algae. However, some reduction in the algal cover and increases in bare substrate were also

observed at the control sites and most likely represents a seasonal effect, as photosynthetic alga are

less prolific in the winter months. By October 2009, the algal and sessile invertebrate cover had

increased at all sites, most likely due to increased light availability and rising water temperatures in

spring. The organismal cover remained relatively low at the main and south impact sites when

compared to the pre-impact 2007 surveys, which could indicate slower recovery due to residual

effects from the sand accumulation. However, these sites still showed greater cover that the

northern metropolitan controls sites and generally appeared to be recovering well. As reported

previously from studies on the Isle of Mann, season appears to be the over-riding factor influencing

rocky shore communities (Prathep et al., 2002). The productivity of algae can vary seasonally, in

addition to the supply and movement of sediment, thus providing a naturally heterogeneous

environment.

The high sand cover at the North impact site may have influenced the relatively low diversity of

invertebrates found at this site in the May 2009 surveys, relative to the pre-impact surveys by

Dutton and Benkendorff (2008). Nevertheless, as the sand cleared in October, 2009, the diversity

recovered at this site, indicating no long-term detrimental effects. The main impact site was actually

found to have the highest diversity immediately after the sand dumping in May 2009 and whilst this

decreased in the October 2009 surveys, the diversity still remained within the range of all non-

impacted control sites. However, the relatively high number of barnacles at the impact sites in the

May 2009 surveys is of potential interest. Pineda (1994) have reported higher settlement of the

barnacle Chthamalus spp. at sites where rocks are surrounded by unsuitable sandy substrate,

possibly because settlement is intensified when suitable habitat is scare. Thus it is is possible that

24 | P a g e

barnacle recruitment during the sand dumping at O’Sullivans Beach resulted in unusually high

settlement in the remaining exposed rocks.

The abundance of invertebrates generally showed a lot of variability between sites and survey

periods. The molluscs showed particularly low abundance at all sites in May, relative to the October

2009 surveys, which is likely due to the lower algal cover in May, as these are mostly herbivorous

gastropods. The May surveys were also conducted on higher tides than the October 2009 surveys

(Table 1), which might also influence the observed differences in abundance. Conversely, surveys of

the whelk Dicathais orbita in the shallow subtidal region indicated a drop in abundance from April to

November 2009. The lower abundances of this predatory gastropod at both the impact and control

sites may be indirectly attributable to algal cover. Algal proliferation is normal for spring time in

metropolitan waters and this cover can inhibit the timed search surveys for whelks, as more time is

required to search through algal fronds that were not in such profusion during the April surveys.

Additional observations indicate that there is greater algal diversity and cover at the impact site,

which receives less human traffic than the control site. This may have resulted in fewer whelks

recorded at the control site in the October surveys. Overall, this data provides no evidence for

significant impacts on the intertidal or subtidal mollusc populations at O’Sullivans Beach as a result

of the sand dumping. These results are consistent with previous experimental sand manipulations on

rocky shores, which indicated recovery on intertidal communities one month after sand addition had

ceased (Huff and Jarett, 2007).

Sand fluctuation and sand scour is a natural event that occurs on many intertidal reefs (Tyler et al.,

1982; Littler et al., 1983). As a consequence intertidal communities might have adapted to rapidly

recover from temporary sand inundation. Many intertidal organisms will opportunistically colonise

and recruit into any suitable habitat that has been opened up by sand-stress (Littler et al., 1983).

Consequently, these systems may be naturally resilient to one-off sand deposition events, such as

occurred at O’Sullivans Beach. Intertidal systems along the Fleurieu Peninsula, South Australia may

recover particularly well over the winter period, during which high tides and substantial wave action

can clear away the accumulated sand prior to spring recruitment and colonisation events.

Nevertheless, the scale of impact is likely to depend on the amount of sand dumped, the duration of

sand retention, any repeated occurrence and the timing of these events. Experimental studies on

Mediterranean rocky shores have shown that the impacts of sedimentation and recolonisation of

the bare rock are dependent on the time at which succession is initiated (Airoldi and Cinelli, 1997).

Furthermore, studies in New Zealand have illustrated the importance of time and space in relation to

sand impacts regulating the interaction between invasive and indigenous species of rocky shore

mussels (Zardi et al., 2008). Consequently, caution should be taken before extrapolating these

results to other situations, including different times of the year and locations.

In conclusion, this study provides useful baseline data that could be used in future monitoring

programs to assess intertidal impacts associated with on-going activities in the O’Sullivans Beach and

Port Stanvac area. Additional dredging activities have been undertaken more recently in this area for

the O’Sullivans Beach waste water treatment plant. Furthermore, the construction of a

breakwater/jetty on O’Sullivans beach may lead to long term changes in the siltation and erosion

pattern along this coast. Future monitoring efforts should preferably commence with replicated

surveys undertaken in advance of the impact. Replicated surveys should occur pre-, during and post

25 | P a g e

dredging at control and impact sites to account for natural seasonal variation. The local community

should also be informed in advance of any proposed dredging events, with descriptions of their likely

duration and potential impacts. This report may help alleviate community concerns with respect to

the recovery of intertidal communities at O’Sullivans Beach subsequent to the sand dumping event

in April 2009. However, it should not be used to predict the impacts of sand dumping on intertidal

reefs at other locations and times.

References

Airoldi, L., & Cinelli, F., 1997. Effects of Sedimentation on subtidal macroalgal assemblages: an

experimental study from a Mediterranean rocky shore, Journal of Experimental Marine Biology and

Ecology, vol. 215: 269-288.

Airoldi, L., & Hawkins, SJ., 2007. Negative effects of sediment deposition on grazing activity and

survival of the limpet Patella vulgate, Marine Ecology Progress Series, vol. 332: 235-240.

Anderson, M.J., Gorely, R.N., Clarke, K.R., 2008. Permanova+ for PRIMER: Guide to Software and

Statistical Methods. Plymouth Marine Laboratory, United Kingdom.

Benkendorff, K. Fairweather, P. and Dittmann, S. (2008) Intertidal Ecosystems. Ch 10 In Natural

History of the Gulf St Vincent. Ed. S. Shepherd, S. Bryars, Kirkegaard, I., Harbison, P. and Jennings J.T.

Royal Society of S.A. Adelaide, Australia.

Clarke, K.R. Warwick, R.M. (2001) Change in Marine Communities – An Approach to Statistical

Analysis and Interpretation, 2nd

Edition. PRIMER-E, Plymouth.

Clarke , K.R. Gorley, R.N. (2006) PRIMER v6: User Manual/Tutorial. PRIMER-E, Plymouth.

Dutton, A. and Benkendorff, K. (2008) Biodiversity Assessment and Monitoring of the Port Stanvac

Intertidal Reef. Report to the Adelaide and Mt Lofty Natural Resource Management Board. (Flinders

University, Adelaide).

Huff, T.M., & Jarett, J.K., 2007. Sand addition alters the invertebrate community of intertidal

coralline turf, Marine Ecology Progress Series, vol. 345: 75-82.

Littler, M.M., Martz, D.R., Littler, D.S., 1983. Effects of recurrent sand deposition on rocky intertidal

organisms: importance of substrate heterogeneity in a fluctuating environment, Marine Ecology

Progress Series, vol. 11: 129-139.

Noble, W.J., Cocks, R.R., Harris, J., Benkendorff, K., 2009. Application of anaesthetics for sex

identification and bioactive compound recovery from wild Dicathais orbita, Journal of Experimental

Marine Biology and Ecology, vol. 380:1-2: 53-60.

Pineda, J., 1994. Spatial and temporal patterns in barnacle settlement rate along a southern

California rocky shore, Marine Ecology Progress Series, vol. 107: 125-138.

26 | P a g e

Prathep, A., Marrs, R.H., Norton, T.A., 2003. Spatial and temporal variations in sediment

accumulation in an algal turf and their impact on associated fauna, Marine Biology, vol. 142: 381-

390.

Pulfrich, A., Parkins, C.A., Branch, G.M., Bustamante, R.H., Velasquez, C.R., 2003. The effects of

sediment deposits from Namibian diamond mines on intertidal and subtidal reefs and rock lobster

populations, Aquatic Conservation: Marine and Freshwater Ecosystems, vol. 13: 257-278.

Schiel, D.R., Wood, S.A., Dunmore, R.A ., Taylor, D.I., 2006. Sediment on rocky intertidal reefs: Effects

on early post-settlement stages of habitat-forming seaweeds, Journal of Experimental Marine

Biology and Ecology, vol. 2006: 158-172.

Taylor, P.R., Littler, M.M., 1982. The roles of compensatory mortality, physical disturbance, and

substrate retention in the development and organisation of a sand-influenced, rocky-intertidal

community, Ecology, vol. 1982: 135-146.

Thompson, R.C. Crowe, T.P. and Hawkins, S.J. (2002). ‘Rocky intertidal communities: past

environmental changes, present status and predictions for the next 25 years’, Environmental

Conservation, vol. 29, pp. 168-191

Trowbridge, C.D., 1996. Demography and phenology of the intertidal green alga Codium setchellii:

the enigma of local scarcity on sand-influenced rocky shores, Marine Biology, vol. 127: 341-351.

Trott, T.J., 2004. Late 20th

-Century Qualitative Intertidal Faunal Changes in Cobscook Bay, Maine,

Northeastern Naturalist, vol. 11 (2): 325-354.

Underwood, A.J. (1991) Beyond BACI: Experimental designs for detecting human impacts on

temporal variation in natural populations. Aust. J. Mar. Freshw. Res. 42: 569-587.

Yanez, B., Carballo, J.L., Olabarria, C. Barron, J.J., 2008. Recovery of macrobenthic assemblages

following experimental sand burial, Oceanologia, vol. 50 (3): 391-420.

Zardi, G.I., Nicastro, K.R., McQuaid, C.D., Erlandsson , 2008. Sand and wave induced mortality in

invasive Mytilus galloprovinvialis) and indigenous (Perna perna) mussels, Marine Biology, vol. 153:

853-858.

27 | P a g e

Appendix

Table 1: Species list of summed total of individuals for each sampling site for (a) May and (b) October

2009.

(a)

(b)

Phylum Species

Marino Rocks Hallett Cove North Control North Impact

Sites

Main Impact South Impact South Control

Annelida Galeolaria caespitosa

Notoacmea flammea

Notoacmea petterdi

5

0

X

17

1

X

16

5

X

7

0

15

0

Mollusca Notoacmea spp.

Patelloida alticostata

Patelloida latistrigata

Patelloida spp.

Cellana tramoserica

Cellana solida

Nerita atramentosa

Montfortula rugosa

Chlorodiloma adelaidae

Diloma concamerata

Austrocochlea constricta

Austrocochlea porcata

Herpetopoma aspersa

Phasianella ventricosa

Austrolittorina unifasciata

Bembicium nanum

Bembicium vittatum

Neogastropoda spp.1

Siphonaria diemenensis

Siphonaria zelandica

Unidentified gastropod

Limnoperna pulex

Chtalamus antennatus

0

0

5

0

2

2

62

4

0

8

0

1

0

0

385

5

59

0

2

0

1

1349

0

0

1

0

0

5

80

0

0

6

0

1

1

0

339

8

11

3

3

3

3

3097

2

2

0

4

0

0

109

0

1

8

0

1

0

0

14

6

7

0

96

13

4

X

159

0

0

3

0

0

0

44

0

0

2

1

8

0

0

81

7

0

0

23

2

0

356

0

0

11

0

79

0

3

0

0

1

3

0

0

1

0

1

0

0

234

1

6

X

52

Crustacea Chamaesipho tasmanica

Eliminus modestus

62

6

0

5

0

1

309

0

0

0

Phylum Species

Marino Hallett Cove North Control North Impact

Site

Main Impact South Impact South Control

Annelida Galeolaria caespitosa

Pomatoceros taeniata

X

X

X

X

X

X

X

X

X

Mollusca Notoacmea flammea

Notoacmea spp.

Patella chapmani

Patelloida alticostata

Patelloida latistrigata

Patelloida spp.

Cellana tramoserica

Cellana solida

Cellana radiata

Nerita atramentosa

Diloma concamerata

Austrocochlea rudis

Austrocochlea constricta

Austrocochlea porcata

Austrolittorina unifasciata

Bembicium auratum

Bembicium nanum

Bembicium vittatum

Onchidella nigricans

Siphonaria diemenensis

Siphonaria zelandica

Unidentified gastropod

Limnoperna pulex

3

0

0

0

0

0

0

6

0

0

0

0

0

0

0

0

0

0

0

391

3

14

X

33

0

8

0

4

0

0

109

0

6

0

0

0

2

10

1

4

0

0

390

0

0

X

154

0

3

0

133

0

0

12

0

4

1

1

0

0

104

0

0

0

0

1640

1

2

X

52

0

0

0

268

0

21

272

1

11

6

0

0

0

97

0

3

4

0

1692

0

0

X

2

3

0

0

88

0

26

16

0

15

1

0

4

0

0

0

0

11

1

766

0

39

X

1

1

0

11

63

0

23

91

0

4

0

0

0

1

258

0

2

6

0

501

0

0

X

8

4

0

0

67

9

82

46

0

0

0

0

0

0

2

0

0

0

1

419

0

34

X

Crustacea Chtalamus antennatus

Chamaesipho tasmanica

Catomerus polymerus

54

0

0

41

0

0

667

0

0

780

0

1

61

19

0

497

67

0

82

0

0

28 | P a g e