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

• Other Authors: BASFAW (custodian), Commonwealth of Australia (Geoscience Australia) (owner), Commonwealth of Australia (Geoscience Australia) (pointOfContact), EGD (hasAssociationWith), Harris, P.T. (author), Hemer, M.A. (author), Manager Client Services (custodian)
• Format: Text
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: geoscientificInformation; External Publication; Scientific Journal Paper; marine; Antarctic data; AQ; EARTH SCIENCES; Published_External; Amery Ice Shelf; Antarc*; Antarctic; Antarctica; East Antarctica; Ice Shelf; Ice Shelves
• Online Access: https://researchdata.edu.au/sediment-core-beneath-shelf-retreat/687993; https://pid.geoscience.gov.au/dataset/ga/61493

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.