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Processes controlling the formation of the Mertz Drift, George Vth continental shelf, East Antarctica: evidence from 35 Khz sub-bottom profiling and sediment cores

Created 11/01/2026

Updated 11/01/2026

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Recently discovered drift deposits on the Antarctic continental shelf provide access to information on the Holocene palaeoceanography of the bottom current regime within deep shelf basins that were previously inaccessible. The George Vth Basin on the East Antarctic margin has been identified by oceanographers as an important source of Antarctic Bottom Water, hence the Holocene history of bottom current activity here may be relevant to variations in bottom water export.

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Field Value
Title Processes controlling the formation of the Mertz Drift, George Vth continental shelf, East Antarctica: evidence from 35 Khz sub-bottom profiling and sediment cores
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/dataset/b1e69077-0bd3-4238-9ee7-f2bd7eee8a1f
Contact Point
Australian Ocean Data Network
clientservices@ga.gov.au
Reference Period 22/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
{
  "coordinates": [
    [
      [
        139.0,
        -67.5
      ],
      [
        147.0,
        -67.5
      ],
      [
        147.0,
        -65.0
      ],
      [
        139.0,
        -65.0
      ],
      [
        139.0,
        -67.5
      ]
    ]
  ],
  "type": "Polygon"
}
Data Portal Australian Oceans Data Network

Data Source

This dataset was originally found on Australian Oceans Data Network "Processes controlling the formation of the Mertz Drift, George Vth continental shelf, East Antarctica: evidence from 35 Khz sub-bottom profiling and sediment cores". Please visit the source to access the original metadata of the dataset:
https://catalogue.aodn.org.au/geonetwork/srv/eng/csw/dataset/processes-controlling-the-formation-of-the-mertz-drift-george-vth-continental-shelf-east-antarc1