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Sediment Core from Beneath the Amery Ice Shelf, East Antarctica, Suggests Mid-Holocene Ice-shelf Retreat

Created 23/01/2026

Updated 23/01/2026

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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 summer of 2000-2001 from site AM02 on the Amery Ice Shelf, East Antarctica, contains a full and continuous record of glacial retreat.

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Additional Info

Field Value
Title Sediment Core from Beneath the Amery Ice Shelf, East Antarctica, Suggests Mid-Holocene Ice-shelf Retreat
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/en/dataset/e5ef4c96-ffb4-4ef3-9ffd-afd9c94dd808
Contact Point
Australian Ocean Data Network
clientservices@ga.gov.au
Reference Period 22/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
{
  "coordinates": [
    [
      [
        66.0,
        -74.0
      ],
      [
        78.0,
        -74.0
      ],
      [
        78.0,
        -66.0
      ],
      [
        66.0,
        -66.0
      ],
      [
        66.0,
        -74.0
      ]
    ]
  ],
  "type": "Polygon"
}
Data Portal Australian Oceans Data Network

Data Source

This dataset was originally found on Australian Oceans Data Network "Sediment Core from Beneath the Amery Ice Shelf, East Antarctica, Suggests Mid-Holocene Ice-shelf Retreat". Please visit the source to access the original metadata of the dataset:
https://catalogue.aodn.org.au/geonetwork/srv/eng/csw/dataset/sediment-core-from-beneath-the-amery-ice-shelf-east-antarctica-suggests-mid-holocene-ice-shelf-3