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Research > Core research
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Research: Core research projects
Project two: Coastal Ecosystem and Biodiversity
Investigators
CSIRO Marine Research, Floreat, WA: Russ Babcock (Project Leader),
Geordie Clapin, Paul Dean, Peter Fearns, Tim Harriden, Matt Kleczkowski,
Martin Lourey, Nicole Murphy, Alan Pearce, Julia Phillips, Alison
Sampey, Mat Vanderklift, Mark Westera
CSIRO Marine Research, Hobart, TAS: Lesley Clementson, Andy Revill, Peter Thompson
Curtin University: Wojciech Klonowski
University of Western Australia: Marion Cambridge
Flinders University: Tim N. Moore
Executive summary
The
aim of the SRFME Coastal project is to characterize the coastal
benthic ecosystems of southwestern WA, with particular focus on
benthic reef ecosystems, their productivity and dynamics, and
the physical, chemical and biological factors driving variability
along dominant spatial and temporal scales. To achieve this, we
undertook 3-monthly seasonal sampling from 2003 – 2005 at
a series of coastal sites situated between Cape Naturaliste in
the south and Jurien Bay in the north. Benthic Sampling was integrated
with satellite observations of SST, ocean colour and subsurface
measurements of other water column properties, as well as sediment
biogeochemical sampling. Within this region benthic sampling was
nested at Regional (100s km) Local (10s km) and Site (1 km) scales
and within each of the regions additional sites were sampled to
incorporate site scale variability along cross-shore gradients.
The program involved nine core research components:
1) Correlate patterns with physical environmental variables
(e.g. light, nutrients, wave energy, transport)
2) Describe biogeographic patterns in benthic community structure
3) Quantify seasonal and inter-annual variability at key sites
4) Determine the effects of nutrient availability in benthic reef
communities
5) Describe patterns in community structure determined by ecological
interactions
6) Determine principal sources of nitrate supply to the shelf
7) Determine the role of biogeochemical nutrient cycling in pelagic
ecosystems
8) Characterise spatial and temporal variability in coastal ocean
water column productivity using chlorophyll concentration as a
proxy, and SST using remote sensing technology
9) Characterise spatial and temporal variability in coastal sediment
transport and benthic habitat distribution using remote sensing
technology
Standard
protocols included sampling to obtain data on: benthic algal species
diversity and biomass, benthic invertebrate diversity, abundance
and biomass, substratum physical characteristics, depth, invertebrate
recruitment, light attenuation, TSS, chlorophyll a, particulate
organic carbon, nutrient concentrations, salinity, as well as
CTD casts with concurrent measurement of in situ fluorescence,
dissolved oxygen and subsurface irradiance; discrete water column
samples for analysis of salinity, dissolved nutrients (nitrate+nitrite,
ammonium, phosphate and silicate), chlorophyll a, HPLC pigments,
particulate organic carbon, phytoplankton and microzooplankton
species composition and abundance. Biogeochemical sampling protocols
include sampling of sediment cores, and interstitial waters, sampling
for microphytobenthos, in situ O2
microprobe sediment measurements and in situ benthic
respirometry chamber deployments.
The coastal ecology program’s ocean colour group has developed
the capability to routinely download, archive and process remote-sensed
data from a number of applications. This capacity feeds into all
aspects of the SRFME program, and has been extensively validated
by a field sampling program including both case 1 and case 2 waters.
The remote sensing and concurrent validation have produced time
series of SST and chl a for the study area that indicate a clear
seasonality in coastal chl a with summer minima and winter maxima
in May-August. This seasonal trend in phytoplankton biomass is
attributable to an overall increase in phytoplankton rather than
to the abundance of any particular taxon. Winter chl a trends
are paralleled by a seasonal trend in total suspended solids (likely
to be mainly algal detritus) and CDOM. The parallel trends in
phytoplankton biomass as well as in re-suspended matter and CDOM
suggest that an important seasonal source of N in coastal waters
is indeed likely to be from sources in or near the bottom or sediments.
Analysis of broad scale spatial and temporal data sets suggests
that further offshore an additional source of nutrients is likely
to be deeper mixing related to a deepening of the mixed layer
mixing nutrients into the euphotic zone. These trends in phytoplankton
biomass are relative and WA coastal waters are very low in phytoplankton
productivity compared with other coastal waters around the world.
Algal
and invertebrate communities both display latitudinal trends in
community structure between the northern most sites at Greenhead,
and the southern most sites at Cape Naturaliste, though this pattern
is most clear in the algae. To date over 400 species of algae
and seagrasses and 530 taxa of invertebrates have been recorded.
There was significant variation in algal community structure within
the three study regions of Jurien, Perth and Geographe Bay, as
well as among sites within locations. Preliminary analysis suggests
that reef topography plays some role in this variation, though
further analysis including a wider range of physical variables
is still to be completed. The study of this variability holds
significant prospects for informing our understanding of physical
factors important to algal assemblage structure. Initial analysis
of the trends for invertebrates suggests these may follow a similar
pattern of variability at small scales.
Seasonal trends were apparent in benthic algal biomass, and
these appear to stem from both seasonal changes in the physical
environment and intrinsic life history attributes of some key
brown algal species. Sargassum spp. undergo a seasonal growth,
reproduction and senescence with maximum biomass in winter and
spring, and sites dominated by this genus showed overall trends
in keeping with this. Most sites however were dominated by either
the kelp Ecklonia radiata or mixed red and brown algal assemblages,
and these sites showed a minimum biomass in winter and spring,
correlating with decreased light penetration through the water
column and increased storm activity. Thus there appears to be
an inverse seasonal relationship between overall benthic algal
biomass and phytoplankton biomass, ultimately linked to the same
seasonal weather factors of storm activity and wave shear on the
inner shelf.
Studies
of spatial subsidies between reefs and seagrass habitats have
established that detached reef algae are exported to adjacent
seagrass beds, and are consumed by seagrass-associated fauna.
The large quantities of detached algae suggest that this might
form a considerable trophic link between reefs and adjacent seagrass
habitats. In some places the spatial extent of this trophic link
extends more than 300m away from the reefs. The biomass of detached
reef algae increased with increasing proximity to the shore, with
large accumulations occurring at some inshore reefs. Transport
of drift macrophytes (reef algae and seagrass) to inshore reefs
is considerable, and forms an important trophic link between inshore
reefs and habitats further offshore. The spatial extent of the
inshore-offshore linkages appears to be at least several kilometres.
Similar trophic linkages are likely to exist between reef predators
and prey species found in seagrasses. Studies to date have focused
on establishing the existence of gradients in predator density
and population structure that can be used to examine the influence
of reef-associated predators on seagrass fauna. At the Kingston
Reef Sanctuary area on Rottnest Island the population of rock
lobster greater than minimum legal size has been shown to be more
than ten times greater than in areas outside the sanctuary subjected
to recreational fishing. Sampling to assess the relative abundance
of prey items has been undertaken at sites across this gradient
and holds the potential to increase our understanding of important
trophic relationships in Western Australia’s coastal benthic
ecosystems.
Over the next year the coastal project will concentrate on completing
the processing of samples and analysis of data as well as preparing
results for publication in refereed scientific journals, though
significant amounts of data collection remain in the area of sediment
nutrient flux sampling. Plans are being made for follow-up projects
to investigate the roles of physical disturbance and recruitment
on benthic communities on the temperate west coast and to determine
the relative importance of linkages between water column and benthic
processes among different regions. Remote sensing of ocean colour
may play an important role in this, as well as in more extensive
application of remote sensing to mapping of shallow water coastal
habitat types. Plans are also underway to experimentally assess
the role of both physical (nutrients and sediment) and ecological
(herbivory and predation) disturbances to existing ecological
processes. The potential for similar research programs at Ningaloo
is also under development and may offer the opportunity to better
integrate our understanding of ecological processes between the
tropics and temperate areas.
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