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...

Full description

Bibliographic Details
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
Antarctic
East Antarctica
Austral
Amery
Amery Ice Shelf
Antarc*
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
Description
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.

Similar Items