Ice stream reorganization and glacial retreat on the northwest Greenland shelf

Understanding conditions at the grounding-line of marine-based ice sheets is essential for understanding ice sheet evolution. Offshore northwest Greenland, knowledge of the Last Glacial Maximum (LGM) ice sheet extent in Melville Bugt was previously based on sparse geological evidence. This study use...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Newton, A. M.W., Knutz, P. C., Huuse, M., Gannon, P., Brocklehurst, S. H., Clausen, O. R., Gong, Y.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
deglaciation
geomorphology
Greenland Ice Sheet
ice stream
Last Glacial Maximum
megascale glacial lineations
Greenland
Melville Bugt
Ice Sheet
Melville bugt
Online Access:https://pure.au.dk/portal/da/publications/ice-stream-reorganization-and-glacial-retreat-on-the-northwest-greenland-shelf(4e32de6f-6c77-4d85-b2aa-c6c2b27ba5fb).html
https://doi.org/10.1002/2017GL073690
Description
Summary:Understanding conditions at the grounding-line of marine-based ice sheets is essential for understanding ice sheet evolution. Offshore northwest Greenland, knowledge of the Last Glacial Maximum (LGM) ice sheet extent in Melville Bugt was previously based on sparse geological evidence. This study uses multibeam bathymetry, combined with 2-D and 3-D seismic reflection data, to present a detailed landform record from Melville Bugt. Seabed landforms include mega-scale glacial lineations, grounding-zone wedges, iceberg scours, and a lateral shear margin moraine, formed during the last glacial cycle. The geomorphology indicates that the LGM ice sheet reached the shelf edge before undergoing flow reorganization. After retreat of ~80 km across the outer shelf, the margin stabilized in a mid-shelf position, possibly during the Younger Dryas (12.9–11.7 ka). The ice sheet then decoupled from the seafloor and retreated to a coast-proximal position. This landform record provides an important constraint on deglaciation history offshore northwest Greenland.

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