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The Holocene
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Dating of the Narssarssuaq stade in southern Greenland

Ole Bennike

Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark, obe{at}geus.dk

Charlotte J. Sparrenbom

Centre for GeoBiosphere Science, Quaternary Geology, Lund University, Sweden

Following the Holocene thermal maximum, the Greenland ice sheet began to expand, and many local glaciers formed. The maximum extent of most outlet glaciers from the Inland Ice was reached around 100 to 200 years ago. However, some exceptions have been recorded. In southern Greenland, the Neoglacial Narssarssuaq stade marks an older re-advance that exceeded the historical advance. The dating of the Narssarssuaq stade has been much debated. Here we present new radiocarbon dates from a sediment core collected from a small lake within the moraines formed during this stade. A minimum age for the Narssarssuaq stade of around 1200 yr BP is suggested from the dates.

Key Words: Holocene • Neoglacial • Narssarssuaq stade • Narssarssuaq • Greenland • ice sheet • glacier variations

The Holocene, Vol. 17, No. 2, 279-282 (2007)
DOI: 10.1177/0959683607075856
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