Controls upon the Last Glacial Maximum deglaciation of the northern Uummannaq Ice Stream System, West Greenland

Timothy P. Lane*, David H. Roberts, Brice R. Rea, Colm Cofaigh, Andreas Vieli, Angel Rodés

*Corresponding author for this work

Research output: Contribution to journalArticle

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Abstract

The Uummannaq Ice Stream System (UISS) was a convergent cross-shelf ice stream system that operated in West Greenland during the Last Glacial Maximum (LGM). This paper presents new evidence constraining the geometry and evolution of the northern sector of the UISS and considers the factors controlling its dynamic behaviour. Geomorphological mapping, 21 new terrestrial cosmogenic nuclide (TCN) exposure ages, and radiocarbon dating constrain LGM warm-based ice stream activity in the north of the system up to 1400ma.s.l. Intervening plateaux areas either remained ice free, or were covered by cold-based icefields. Beyond the inner fjords, topography and bathymetry forced ice flow southwards into the Uummannaq Trough, where it coalesced with ice from the south, and formed the trunk zone of the UISS.Deglaciation of the UISS began at 14.9cal.kaBP. Rapid retreat from the LGM limit was forced by an increase in air temperatures and rising sea level, enhanced by the bathymetric over-deepening of the Uummannaq and Igdlorssuit Sund troughs. Ice reached the inner fjord confines in the northern Uummannaq area by 11.6ka and experienced an ice marginal stabilisation in Rink-Karrat Fjord for up to 5ka. This was a function of topographic constriction and bathymetric shallowing, and occurred despite continued climatic forcing. In the neighbouring Ingia Fjord this did not occur. Following this period of stability, ice within Rink-Karrat Fjord retreated, reaching the present ice margin or beyond after 5ka. The presence of a major ice stream within a mid-fjord setting, during the mid-Holocene and the Holocene Thermal Maximum (~11-5ka) is in direct contrast to records of other ice streams throughout West Greenland, which suggest ice had retreated beyond its present margin by 9-7ka. This demonstrates the potential importance of topographic control on calving margin stability, and its ability to override climatic forcing.

Original languageEnglish
Pages (from-to)324-344
Number of pages21
JournalQuaternary Science Reviews
Volume92
Early online date27 Nov 2013
DOIs
Publication statusPublished - 15 May 2014

Fingerprint

ice stream
Greenland
deglaciation
Last Glacial Maximum
ice
fjord
trough
present
Holocene
stabilization
geomorphological mapping
ice margin
ice flow
Hypsithermal
radiocarbon dating
air
bathymetry
mathematics
geography
air temperature

Keywords

  • Deglaciation
  • Greenland ice sheet
  • Ice stream
  • Topographic control

ASJC Scopus subject areas

  • Geology
  • Global and Planetary Change
  • Ecology, Evolution, Behavior and Systematics
  • Archaeology
  • Archaeology

Cite this

Controls upon the Last Glacial Maximum deglaciation of the northern Uummannaq Ice Stream System, West Greenland. / Lane, Timothy P.; Roberts, David H.; Rea, Brice R.; Cofaigh, Colm; Vieli, Andreas; Rodés, Angel.

In: Quaternary Science Reviews, Vol. 92, 15.05.2014, p. 324-344.

Research output: Contribution to journalArticle

Lane, Timothy P. ; Roberts, David H. ; Rea, Brice R. ; Cofaigh, Colm ; Vieli, Andreas ; Rodés, Angel. / Controls upon the Last Glacial Maximum deglaciation of the northern Uummannaq Ice Stream System, West Greenland. In: Quaternary Science Reviews. 2014 ; Vol. 92. pp. 324-344.
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