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Effects of Sabella spallanzanii physical structure on soft sediment...
School of BioSciences, The University of Melbourne
The introduced European polychaete Sabella spallanzanii has become a dominant feature of sub-tidal habitats in south-eastern Australia. This study examines the physical effects... -
Effects of Sabella spallanzanii physical structure on soft sediment...
School of BioSciences, The University of Melbourne
The introduced European polychaete Sabella spallanzani has become a dominant feature of sub-tidal habitats in south-eastern Australia. This study examines the physical effects... -
Effects of periodic trampling on rocky intertidal algal beds: Hormosira banksii cover
School of BioSciences, The University of Melbourne
This study examines the effects of trampling on rocky intertidal platforms dominated by the brown algae Hormosira banksii. This dataset gives the percent cover of Hormosira... -
Determining the grainsize of sediment with increasing depth in core GC14,...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size... -
Determining the grainsize of sediment with increasing depth in core GC13,...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC13) was collected from a depth of 1482 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size... -
Determining the grainsize of sediment with increasing depth in core GC12,...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size... -
Determining the grainsize of sediment with increasing depth in core GC11,...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size... -
Determining the grainsize of sediment with increasing depth in core GC10,...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC10) was collected from a depth of 335 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size... -
Determining the grainsize of sediment with increasing depth in core GC09,...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC09) was collected from a depth of 166m within the Capricorn Channel, southern Great Barrier Reef (GBR). Samples were separated into different size fractions to... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC10) was collected from a depth of 335 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC13) was collected from a depth of 1482 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC09) was collected from a depth of 166m within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last Glacial... -
Determining main carbonate mineralogy, and the primary components of the non...
National Institute of Water and Atmosphere (NIWA)
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Analysis of other parameters revealed the Last... -
Denitrification measurements of sediments using cores and chambers:...
School of BioSciences, The University of Melbourne
Denitrification is a microbial process that takes place on and within sediment and results in the transformation of dissolved inorganic nitrogen to nitrogen gas (N2), which is... -
Current values collected through the water column using an Acoustic Doppler...
Australian Defence Force Academy (ADFA)
The record describes data collected from a winter deployment of an Acoustic Doppler Current Profiler (ADCP) moored in the central part of Jervis Bay, New South Wales (35o 05'S,... -
Current values collected through the water column using an Acoustic Doppler...
Australian Defence Force Academy (ADFA)
The record describes data collected from a summer deployment of an Acoustic Doppler Current Profiler (ADCP) moored in the central part of Jervis Bay, New South Wales (35o 05'S,... -
Current meter data obtained from a mooring off Point Perpendicular, Jervis...
Australian Defence Force Academy (ADFA)
A current meter mooring was installed at the entrance of Jervis Bay, off Point Perpendicular. This mooring housed 2 current meters, at 12m and 34m. Over a period of approx. 1yr... -
Current meter and tide gauge data obtained from an off-shore mooring near...
Australian Defence Force Academy (ADFA)
A current meter mooring was installed in 100m of water, approximately 2km offshore of Point Perpendicular, Jervis Bay. This mooring housed 3 current meters (at 30m, 55m and 90m...