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Lithofacies distribution in relation to the geomorphic provinces of Prydz...
Over the past 15 years, Japanese, Australian and Russian expeditions to Prydz Bay have collected about 30 000 kilometrs of bathymetric data, 6 000 kilometres of sidescan sonar... -
Sediment Core from Beneath the Amery Ice Shelf, East Antarctica, Suggests...
The stability of floating ice shelves is an important indicator of ocean circulation and ice-shelf mass balance. A sub-ice -shelf sediment core collected during the Austral... -
Leg 188 Sythesis: Transitions in the Glacial History of the Prydz Bay...
Drilling during Leg 119 (1988) and Leg 188 (2000; Sites 1165-1167) of the Ocean Drilling Program (ODP) provides direct evidence for long- and short-term changes in Cenozoic... -
Bottom currents, sedimentation and ice-sheet retreat facies successions on...
Measurements of water turbidity, currents, seafloor sediment samples and geophysical data document the sedimentary processes and the Late Quaternary sedimentary history of a... -
Sedimenary Processes in the Wilkes Land Margin: A Record of Cenozoic East...
Multichannel seismic data collected off Wilkes Land (East Antarctica) reveal four main units that represent distinct phases in the evolution of the Cenozoic depositional... -
Davis Coastal Seabed Mapping Survey, Antarctica (GA-4301 / AAS2201 / HI468)...
The Davis Coastal Seabed Mapping Survey, Antarctica (GA-4301 / AAS2201 / HI468) was acquired by the Australian Antarctic Division workboat Howard Burton during February-March... -
Processes controlling the formation of the Mertz Drift, George Vth...
Recently discovered drift deposits on the Antarctic continental shelf provide access to information on the Holocene palaeoceanography of the bottom current regime within deep... -
Geology of the Stillwell Hills
The Stillwell Hills region comprises granulite facies gneisses which record evidence for multiple periods of deformation and metamorphism spanning more than 2500 Million years.... -
History of benthic colonisation beneath the Amery Ice Shelf, East Antarctica
This study presents compelling evidence for a diverse and abundant seabed community which has developed over the course of the Holocene beneath the Amery Ice Shelf in East... -
Physical Controls on Deep Water Coral Communities on the George V Land...
Dense coral-sponge communities on the upper continental slope at 570 - 950 m off George V Land have been identified as a Vulnerable Marine Ecosystem in the Antarctic. The... -
Ice shelf grounding zone features of western Prydz Bay, Antarctica...
Several grounding zone wedges were left on the floor and flanks of Prydz Channel in western Prydz Bay by the Lambert Glacier during the last glacial cycle. Seismic profiles... -
Seismic Stratigraphy and Sediment Distribution on the Wilkes Land and Terre...
Seismic reflection data show the existence of two major sedimentary basins along the continental margin of Wilkes Land and Terre Adélie, East Antarctica, that contain more than... -
Estimating the biodiversity of the East Antarctic shelf and oceanic zone for...
Ecoregions are defined in terms of community structure in function of abiotic or even anthropogenic forcing. They are mesoscale structures defined on the potential habitat of... -
Late Neogene Ice Drainage Changes in Prydz Bay, East Antarctica and the...
During the late Neogene, the Lambert Glacier-Amery Ice Shelf drainage system flowed across Prydz Bay and showed several changes in flow pattern. In the Early Pliocene, the... -
Physical Controls on Coral Communities on the George V Land Slope: Some...
Dense coral-sponge communities on the upper continental slope off George V Land have been identified as a Vulnerable Marine Ecosystem in the Antarctic. The challenge is now to... -
What lies beneath the Antarctic Ice?
During the summer of 2003-2004, six scientists and technicians spent over a month camped on the Amery Ice Shelf in eastern Antarctica. The aim of their stay was to drill through... -
Topographic Controls on Post-Oligocene Changes in Ice-sheet Dynamics, Prydz...
Within the general trend of post-Eocene cooling, the largest and oldest outlet of the East Antarctic Ice Sheet underwent a change from ice-cliff to ice-stream and/or ice-shelf... -
Continental shelf drift deposit indicates non-steady state Antarctic bottom...
A late Quaternay, current-lain sediment drift deposit over 30 metres in thickness has been discovered on the continental shelf of East Antarctica in an 850 metre deep glacial... -
A Review of the Cenozoic Stratigraphy and Glacial History of the Lambert...
The Cenozoic glacial history of East Antarctica is recorded in part by the stratigraphy of the Prydz Bay-Lambert Graben region. The glacigene strata and associated erosion... -
Lithofacies distribution in relation to the geomorphic provinces of Prydz...
Over the past 15 years, Japanese, Australian and Russian expeditions to Prydz Bay have collected about 30 000 kilometrs of bathymetric data, 6 000 kilometres of sidescan sonar...