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Ecological studies on seagrasses of SW Australia - Cockburn Sound - Field...
School of Plant Biology (SPB) / UWA Oceans Institute (OI), The University of Western Australia (UWA)
Two field experiments were carried out on seagrass in the Cockburn Sound area to assess the effect of water quality on seagrass growth. Leaf area was measured before and after... -
eAtlas Web Mapping Service (WMS) - Legacy MTSRF Server (AIMS)
Australian Institute of Marine Science
The eAtlas delivers its mapping products via two Web Mapping Services, a legacy server (from 2008-2011) and a newer primary server (2011+) to which all new content it added.... -
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. -
Do the assemblages of benthic macroinvertebrates in nearshore waters of...
Centre for Fish and Fisheries Research (CFFR), Murdoch University
Benthic macroinvertebrates were sampled seasonally in the subtidal and upper and lower swash zones at two sites in each of six nearshore habitat types on the lower west coast of... -
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... -
Distributions of rainforest vertebrates in the Australian Wet Tropics (MTSRF, JCU)
Centre for Tropical Biodiversity & Climate Change, James Cook University (CTBCC/JCU)
The purpose of this data set was to compile distributional, general life-history characteristics and phylogenies for Australian tropical rain forest vertebrates to inform a wide... -
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...