Northern Australia's seabed environments were mapped in a survey between 27 August and 24 September, 2009. The survey, conducted by Geoscience Australia and the Australian Institute of Marine Sciences, collected geological and biological data on carbonate banks, channels, and sediment plains. This data aims to establish the late-Quaternary evolution of the region and investigate relationships between the physical environment and biota.
Use Cases
- Modeling late-Quaternary seabed evolution based on geological data
- Investigating relationships between physical seabed features and biological communities
- Predicting marine biodiversity patterns based on environmental variables
- Analyzing sedimentological and geochemical properties of carbonate banks
Strengths
- Survey conducted by authoritative institutions Geoscience Australia and the Australian Institute of Marine Sciences
- Data collection covers a specific time range from 27 August to 24 September, 2009
- Multidisciplinary data includes geological, biological, geochemical, and geophysical information
Limitations
- Column-level documentation is absent; field semantics must be inferred after download
- Row count and data scale are unknown, which may limit suitability assessment
- Data freshness should be verified as the survey was completed in 2009
Provenance
- Source
- Australian Ocean Data Network
- Collection Method
- Seabed mapping survey (SOL4934) obtaining detailed geological and biological data.
- Time Range
- Survey completed between 27 August and 24 September, 2009.
- Geography
- Eastern Joseph Bonaparte Gulf, Northern Australia, specifically the Van Diemen Rise.