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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... -
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... -
Department of Environment Protected Areas WMS
This Web Map Service contains three protected areas data layers sourced from the Australian Commonwealth Department of Environment: World Heritage Areas (2007), and the... -
Cyclone Summaries 1900-2015
CSIRO Marine and Amospheric Research
This dataset is a summary of global cyclone frequency. Data on the tracks of cyclones since 1900 was sourced from the International Best Track Archive for Climate Stewardship... -
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,...