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- Predicting habitat preferences for Anthometrina adriani (Echinodermata) on the East Antarctic continental shelf
- Morphology and controls on the evolution of a mixed carbonate-siliciclastic submarine canyon system, Great Barrier Reef margin, north-eastern Australia
- Geomorphology of submerged reefs on the shelf edge of the Great Barrier Reef: The influence of oscillating Pleistocene sea-levels
- Demersal ichthyofaunal shelf communities from the Dumont d'Urville Sea (East Antarctica)
- Mesophotic coral ecosystems on the walls of Coral Sea atolls
- Variability in mesophotic coral reef communities along the Great Barrier Reef, Australia
- Community structure and benthic habitats across the George V Shelf, East Antarctica: Trends through space and time
- Near-bottom current direction inferred from comatulid crinoid feeding postures on the Terre Adélie and George V shelf, East Antarctica
- Topography, substratum and benthic macrofaunal relationships on a tropical mesophotic shelf margin, central Great Barrier Reef, Australia
- A new high-resolution bathymetry model for the Terre Adélie and George V continental margin, East Antarctica
- Estimating the biodiversity of the East Antarctic shelf and oceanic zone for ecoregionalisation: Example of the ichthyofauna of the CEAMARC (Collaborative East Antarctic Marine Census) CAML surveys
- Autonomous Underwater Vehicle-assisted surveying of drowned reefs on the shelf edge of the Great Barrier Reef, Australia
- Physical controls on deep water coral communities on the George V Land slope, East Antarctica
- New evidence for drowned shelf edge reefs in the Great Barrier Reef, Australia
- From corals to canyons: The Great Barrier Reef margin
- Geology-benthos relationships on a temperate rocky bank, eastern Bass Strait, Australia
- Bioregionalisation of the George V Shelf, East Antarctica
- Seafloor morphology and acoustic facies of the George V Land shelf, Antartica
- Processes controlling the formation of the Mertz Drift, George Vth continental shelf, East Antarctica: evidence from 3.5 kHz sub-bottom profiling and sediment cores
- Continental shelf drift deposit indicates non-steady state Antarctic bottom water production in the Holocene
- New evidence for the Holocene sea-level high from the inner shelf, central Great Barrier Reef, Australia
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