Return to search

Responses in estuarine macrobenthic invertebrate assemblages to trace metal contaminated sediments

Three approaches were employed to examine the effects of elevated sediment trace
metal concentrations on estuarine/marine macrobenthic invertebrate assemblages. The
initial study examined macroinvertebrate communities along a known polymetallic
gradient, Lake Macquarie, NSW (gradient study). The second study experimentally
tested if sediments sourced from different locations within Lake Macquarie
differentially influenced the recolonisation of benthic invertebrates. The third study
investigated the different recolonisation patterns of benthic invertebrates into
sediments spiked with increasing concentrations of sediment-bound cadmium.
In the Lake Macquarie gradient study, four locations (Cockle Bay, Warner's Bay,
Kooroora Bay and Nord's Wharf) were sampled in winter 2000 and summer 2003
using a hierarchical design (location > site > plot). On both sampling occasions, the
sediments showed strong gradients in lead, cadmium and zinc concentrations
emanating from the Cockle Bay industrialised region in the lake's north, with
concentrations being significantly lower in the most southern and less urbanised
location (Nord's Wharf). In general, concentrations of lead, cadmium and zinc in the
sediments increased among locations in the following order: Nord's Wharf >
Kooroora Bay > Warner's Bay > Cockle Bay. AVSJSEM analyses indicated that in
some sites in Cockle Bay, and to a lesser extent Warner's Bay, SEM concentrations
exceeded their molar equivalence of AVS, indicating the potential for trace metals to
be labile within the porewaters. Granulometry also changed along the gradient, with a


higher proportion of silt/clay occurring in the locations with high metal
concentrations. Conversely, the percentage of total organic carbon was higher in the
less contaminated locations.
In winter 2000, changes in benthic communities along the gradient supported the a
priori hypotheses, with diversity and richness being greater in locations with lower
concentrations of metals. Polychaetes were most numerous in Cockle Bay and
Warner's Bay, whilst bivalves and gastropods were more abundant in Nord's Wharf
and Kooroora Bay. Crustaceans were more numerous in Nord's Wharf; with all other
locations having similar, lower, abundances. Ordination maps of the assemblages
provided relatively clear separation of the assemblages among locations, with nonparametric
multivariate analysis of variance (NPMANOVA) and subsequent pair-wise
comparisons finding significant differences among the assemblages from all locations.
SIMPER analyses found the highest level of dissimilarity was between the Nord's
Wharf and Cockle Bay assemblages - primarily attributable to differences in the
relative contributions of isopods; tellenid bivalves; and the polychaete families
Spionidae, Opheliidae and Nephytidae. Weighted Spearman rank correlations (BIOENV)
identified cadmium (Pw =0.74) as the strongest environmental (single or
combination) variable to correlate with biotic assemblages.
Benthic patterns along the gradient were less defined in summer 2003 due to a
dramatic reduction in the abundance and diversity of fauna in Nord's Wharf. This
decline was possibly attributable to a sustained reduction in salinity caused by a
prolonged rainfall event. With the exception of Nord's Wharf, trends in the
community indices and abundances of key taxa among the other locations were
similar to those reported in winter 2000. Multivariate analyses discriminated the
benthic assemblages from the four locations, with the findings from the NPMANOVA
pair-wise comparisons indicating that the assemblages from all four locations were
significantly different. SIMPER analyses showed the highest level of dissimilarity
was between Nord's Wharf and Warner's Bay, with these differences being primarily
attributable to their relative abundances of amphipods and polychaetes from the
families Spionidae, Cirratulidae, Opheliidae and Capitellidae. BIOENV found that the
combination of the sedimentary concentrations of cadmium and iron provided the best
correlation (Pw =0.73) with biotic patterns, with similar correlations occumng with
the addition of lead and its covariate, zinc (Pw =0.72).
The combined findings from the gradient study established a strong correlation
between trace metal concentrations within the sediments and suite of univariate and
multivariate measurements. The low abundance and diversity of fauna in Nord's
Wharf in the summer of 2003 highlighted the dynamic changes which can occur in the
distributions of macrobenthic invertebrates. Although the study indicated that there
was a strong relationship between trace metal concentrations and benthic community
structure, the study was correlative, and requires subsequent experimental testing to
confirm the causality of the observed relationships.
The second component of the research was a translocation experiment using benthic
recolonisation as an end-point. The experiment was performed to identify if the
sediments, and not location, were influencing the composition of benthic assemblages
in Lake Macquarie. Sediments were collected from three locations (Cockle Bay,
Warner's Bay and Nord's Wharf), defaunated, and transplanted in three new locations
along the south-east edge of the lake. At each location, 10 containers of each
treatment were randomly placed in the sediment and allowed to recolonise for 22
weeks. Upon retrieval, the benthic communities were sampled and enumerated in
conjunction with a variety of chemical and sedimentary measurements. Ten replicate
invertebrate samples were also collected in the sediments adjacent to the experiment
(ambient samples) at the completion of the experiment. Due to human interference,
the containers from only two locations were analysed.
Upon retrieval, pH and redox profiles of the sediments were similar to those expected
in natural sediments. In general, concentrations of metals were low in the porewaters;
however, iron precipitation on the porewater collection devices may have artificially
increased the diffusion of metals, increasing concentrations near the sediment-water
interface. Concentrations of SEM exceeded their AVS equivalence in some samples
taken from the Cockle Bay and Warner's Bay treatments.
Two-way ANOVAs found significant interactions between location and sediment
treatments in diversity, evenness and the number of polychaetes, as well as significant
differences in the number of capitellids and crustaceans among locations. Post-hoc
comparisons of means found the Nord's Wharf sediment contained a higher mean
number of individuals than the other treatments, including the ambient samples.
nMDS ordination plots for both locations provided poor graphical discrimination of
the assemblages among treatments; however, NPMANOVA detected significant
location and treatment interactions. In both locations, pair-wise comparisons indicated
that the assemblages within the Nord's Wharf treatments were significantly different
to the Cockle Bay, Warner's Bay and ambient assemblages. No significant differences
were detected between the Cockle Bay and Warner's Bay assemblages at either
location. SIMPER analyses found the highest level of dissimilarity occurred between
the ambient assemblages in Location 2 and the Nord's Wharf treatment, primarily due
to the relative difference in the abundances of Capitellidae, Spionidae, Oweniidae,
Nereididae and isopods among the assemblages.
The findings from the translocation experiment suggest that the sediments are
influencing the recolonisation of benthos. However, because differences were not
detected between the Cockle Bay and Warner's Bay treatments, the approach used in
the study shows potential as an in situ technique which could be used to assess the
potential ecological risks of sediments fiom specific locations. Excluding cost and
time considerations, the technique's primary disadvantage is the lack of a true control.
As a result, the technique can only identify if the sediments are modifying benthic
recolonisation, and not causality.
The final component of the research experimentally tested if elevated concentrations
of sediment-bound cadmium affected benthic invertebrate recolonisation. Sediments
from the south coast of New South Wales (Durras Lake) were defaunated, and spiked
with cadmium under anaerobic conditions to obtain three targeted cadmium
concentrations: control (<O.1 ug/g), Low-Cd (15 Cd ug/g) and High-Cd (150 Cd
ug/g). The physio-chemical properties of the waters and porewater concentrations of
cadmium were monitored over a 28-day equilibration period, with declines in pH
mediated with the addition of NaOH(aq). At the end of the equilibration period,
porewater concentrations of cadmium were low in the Low-Cd and High-Cd
treatments (maximum <l.5 ug/L in High-Cd), and below the detection limit in the
control. Cadmium was not detected in the control sediments, with concentrations in
the Cd-Low and Cd-High sediments exceeding their targeted concentrations, with
final mean concentrations of 17 ug/g and 183 ug/g, respectively.
The experimental design was similar to that employed in the translocation experiment,
with 10 containers from each treatment transplanted into the sediments at three
locations within Lake Macquarie. After 20 weeks, the containers were collected,
along with benthic invertebrate samples from the ambient sediments. Data was not
used from Location C due to extensive sediment deposition on the transplanted
treatments. Significant declines occurred in the concentrations of cadmium in both the
Low-Cd and High-Cd sediments, with the greatest loss occumng in the surficial
sediments. The loss of cadmium was probably due to the differential loss of the fine

fraction through physical means (hydrodynamic) rather than fluxing, as it assumed
that the cadmium was primarily sediment-bound and relatively insoluble under anoxic
conditions. Mean porewater concentrations of cadmium were below the detection
limit in the control treatments; < 1 ug/L in the Low-Cd treatment, and generally <
2ug/L in the High-Cd, with the exception of some samples in Location B (maximum
5.6 ug/L) Concentrations of ammonia were low in the porewaters from the surficial
sediments, with concentrations being significantly higher, and potentially toxic, in the
anoxic porewaters (7 cm depth).
In comparison to the previous recolonisation experiment, the number of individuals
which recolonised the cadmium-spiked treatments was low, and significantly lower
than the mean number of individuals sampled in the ambient sediments. No
significant differences were detected among the treatments or locations (and their
interactions) in diversity (H'), richness (d) or evenness (J). The number of polychaetes
and molluscs significantly differed among the treatments, with post-hoc analyses
indicating these differences were not among the cadmium-spike treatments, but were
due to a greater mean abundance of these taxa in the ambient sediments. A significant
interaction between treatment and location was detected in the mean abundance of
crustaceans, with the ambient sediments having significantly lower mean abundances
in both Location A and B. Ordination plots of the experiments in Location A and B
provided poor graphical discrimination among the spiked treatments, although the
ambient assemblages appear to be separated from the cadmium-spiked assemblages.
NPMANOVA detected a significant interaction between treatments and locations, as
well as among treatments. In both Location A and B, pair-wise analyses found the
assemblages in the ambient sediments to be significantly different to the assemblages
in all three cadmium treatments, with no differences being detected among the latter.
SIMPER analyses found the highest levels of dissimilarity occurred between the
spike-treatments and the ambient sediments, with these differences being primarily

due to the relatively higher abundance of decapods in the spiked treatments, and
capitellids in the ambient sediments.
The cadmium-spiking component of the experiment clearly illustrated that artificially
increasing the trace metal concentrations of metals in estuarine sediments is a
complex process which needs to be performed in a methodological manner in order to
obtain homogenous treatments with low porewater concentrations, and minimal
artefacts. Furthermore, the results confirmed that the equilibration time for sediments
can be extensive (several weeks), even in the case of organically rich sediments. The
timing of the experiment (commenced late summer, February, 2003) appears to the
major factor for the relatively low recolonisation rates, with the experiment missing
the main larval recolonisation period between spring and early summer. Even in the
highest treatment, elevated concentrations of cadmium did not appear to affect benthic
recolonisation. This finding is supported by other experimental studies which suggest
that concentrations of a single isolated metal must considerably exceed current
guideline values (or contain high porewater concentrations) in order to elicit a
biological effect. Nevertheless, as trace metals generally co-occur with other
contaminants - with the response of multiple contaminants being possibly additive or
synergistic - a conservative guideline value may be suitable in the interim as a
precautionary measure.
The findings of this thesis suggest that elevated concentrations of trace metal mixtures
in estuarine sediments can affect the structure and composition of benthic
communities; however, identifying causality is difficult. Although there has been an
increase in the use of manipulative field experiments as a means of reducing the
confounding influence of covariables found in field studies, this approach also has
limitations, e.g. spatial and temporal scale issues, container effects, cost and
biogeochemical changes to the sediments. Measuring stress at a community level is a

fundamental component of estuarine risk assessment programs; and in isolation this
approach can produce subjective and confounded findings. In order to accurately
assess the risks associated with trace metal contaminated sediments, an integrated
approach (e.g. weight of evidence) is required, one which uses multiple lines of
evidence sourced from various chemical, environmental biological measurements.

Identiferoai:union.ndltd.org:ADTP/218732
Date January 2005
CreatorsChariton, Anthony A., n/a
PublisherUniversity of Canberra. Resource, Environmental & Heritage Sciences
Source SetsAustraliasian Digital Theses Program
LanguageEnglish
Detected LanguageEnglish
Rights), Copyright Anthony A. Chariton

Page generated in 0.0022 seconds