GEOSCAN Search Results: Fastlink

GEOSCAN Menu


TitleEvidence for an extensive ice shelf in northern Baffin Bay during the Last Glacial Maximum
 
AuthorCouette, P -O; Lajeunesse, P; Ghienne, J -FORCID logo; Dorschel, BORCID logo; Gebhardt, C; Hebbeln, DORCID logo; Brouard, EORCID logo
SourceCommunications Earth & Environment vol. 3, issue 1, 2022 p. 1-12, https://doi.org/10.1038/s43247-022-00559-7 Open Access logo Open Access
Image
Year2022
Alt SeriesNatural Resources Canada, Contribution Series 20220453
PublisherNature
Documentserial
Lang.English
Mediapaper; digital; on-line
File formatpdf
ProvinceNunavut; Northern offshore region
NTS16; 26; 36; 27; 37; 28; 38; 48
AreaBaffin Island; Baffin Bay
Lat/Long WENS -85.0000 -55.0000 75.0000 65.0000
Subjectssurficial geology/geomorphology; ice; glaciology; ice sheets; ice flow; deglaciation; Laurentide Ice Sheet; Innuitian Ice Sheet; Greenland Ice Sheet
Illustrationslocation maps; bathymetric profiles; 3-D images; lithologic logs
Released2022 12 01
AbstractThe glaciological significance of ice shelves is relatively well established for the stability of modern ice sheets of Antarctica. Past ice shelves of the Arctic, however, are poorly documented while their role for the stability of former ice sheets remains mostly unknown. Here we present swath bathymetry data and seismostratigraphic profiles that reveal a large moraine system extending along the continental slope off Baffin Island, demonstrating that a 500-m thick ice shelf covered northern Baffin Bay during the last glacial episode. We suggest that this ice shelf had a profound impact on the stability of a series of major ice streams that drained the interior of the Laurentide, Innuitian and Greenland ice sheets. Climate warming and global sea-level rise in the early stage of deglaciation possibly contributed to a large-scale break-up of the ice shelf, which led to the destabilisation and reorganisation of tributary ice streams from these three ice sheets.
Summary(Plain Language Summary, not published)
The importance of ice shelves for the stability of present-day ice sheets such as Antarctica is well established. However, pre-historic record of ice shelves in the Arctic is poorly documented. Here we present bathymetry and sub-seafloor profiles in Western Baffin Bay, that indicate the existence of a 500-m thick ice shelf in northern Baffin Bay during the last glacial episode. We suggest that this ice shelf had a profound impact on the stability of glaciers that drained the ice sheets around Baffin Bay at that time. Climate warming and global sea-level rise in the early stage of deglaciation possibly contributed to a large-scale break-up of the ice shelf, which led to the destabilisation and reorganisation of glaciers from these ice sheets.
GEOSCAN ID331280

 
Date modified: