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Hawkesbury River Temperature Salinity Data 1986
Temperature and salinity data were collected at 8 station locations by students on a field trip to the Hawkesbury River during August 1986. -
Georges River CTD Data 17 October 1985
Nine samples were collected at Georges River using a conductivity-temperature-depth (CTD) device on the 17th October 1985, for collection of salinity data. -
Georges River CTD Data 11 October 1985
Nine samples were collected at Georges River using a conductivity-temperature-depth (CTD) device on the 11th October 1985, for collection of salinity data. -
Georges River CTD Data 10 September 1988
Twenty samples were collected at Georges River using a conductivity-temperature-depth (CTD) device on the 10th September 1988, for collection of water temperature and salinity... -
Dutton Bay CTD Data 7 December 1998
Ten samples were collected at Dutton Bay using a conductivity-temperature-depth (CTD) device on 7th December 1998, for analysis of water temperature and salinity data. -
DOF - Long Term Benthic Monitoring Locations at the Houtman Abrolhos Islands
This data comprises of three polygons outlining the shallow water (30m) areas of the three island groups of the Houtman Abrolhos Islands. Since 2007 Department of Fisheries has... -
Diatom recovery from core MD88-787: Raw counts
Department of Biological Sciences, Macquarie University
Core MD88-787 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,... -
Diatom recovery from core MD88-784: Raw counts
Department of Biological Sciences, Macquarie University
Core MD88-784 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,... -
Diatom recovery from core MD88-779: Raw counts
Department of Biological Sciences, Macquarie University
Core MD88-779 was taken during the 1988 French ASPARA IV cruise in the South East Indian Ocean aboard the Marion Dufresne. The core is situated on the South Tasman Rise... -
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...