Sediment Core from Beneath the Amery Ice Shelf, East Antarctica, Suggests Mid-Holocene Ice-shelf Retreat
Maintenance and Update Frequency: unknown Statement: Unknown 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 An...
Other Authors: | , , , , , , |
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Format: | Text |
Language: | unknown |
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Australian Ocean Data Network
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Online Access: | https://researchdata.edu.au/sediment-core-beneath-shelf-retreat/687993 https://pid.geoscience.gov.au/dataset/ga/61493 |
Summary: | Maintenance and Update Frequency: unknown Statement: Unknown 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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