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The percentage of calcium carbonate in samples taken from various depths in...
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). The percentage of calcium carbonate in samples... -
The percentage of calcium carbonate in samples taken from various depths in...
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). The percentage of calcium carbonate in samples... -
The percentage of calcium carbonate in samples taken from various depths in...
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). The percentage of calcium carbonate in samples... -
The percentage of CaCO3 in samples taken from various depths 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). The percentage of CaCO3 in samples collected from... -
The percentage breakdown of carbonate/non-carbonate fractions in core GC04,...
Australian National University
Core GC04, was collected from the southeastern side of the New Caledonian Basin (22.99965 S, 166.150716 E). Carbonate percent in the curve has an average value of ~79% and... -
The age versus depth profile for core GC04, located off the coast of New Caledonia
Australian National University
Core GC04, was collected from the southeastern side of the New Caledonian Basin (22.99965 S, 166.150716 E). The age of the sediment at each sample depth was determined by... -
Surface Sediment Broken Bay to Abyssal Plain
The major accomplishments of this research are the collection and analysis of data concerning surface sediment and shelf sedimentation in South East Australia, in 1992. -
Herbert River along the Jetty Grab Sampling 11 February 2004
Ocean Technology Group (OTG), The University of Sydney (USYD)
The objective of the research reported in this thesis was to develop a technique to monitor the dynamics of sediments and nutrients entering the coastal ocean with river plumes... -
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... -
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...