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

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Created 14/01/2025

Updated 14/01/2025

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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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Title Sediment Core from Beneath the Amery Ice Shelf, East Antarctica, Suggests Mid-Holocene Ice-shelf Retreat
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/893f5261-cb6e-437a-b314-bdc18290a0e9
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 22/04/2018
Geospatial Coverage {"type": "Polygon", "coordinates": [[[66.0, -74.0], [78.0, -74.0], [78.0, -66.0], [66.0, -66.0], [66.0, -74.0]]]}
Data Portal data.gov.au

Data Source

This dataset was originally found on data.gov.au "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://devweb.dga.links.com.au/data/dataset/sediment-core-from-beneath-the-amery-ice-shelf-east-antarctica-suggests-mid-holocene-ice-shelf-

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