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Late-Holocene Atlantic bottom-water variability in Igaliku Fjord, South Greenland, reconstructed from foraminifera faunasGeological Survey of Denmark and Greenland,Østervoldgade 10, DK-1350 Copenhagen K, Denmark; sl{at}geus.dk
Geological Survey of Denmark and Greenland,Østervoldgade 10, DK-1350 Copenhagen K, Denmark
Geographic Institute, University of Copenhagen,Østervoldgade 10, DK-1350 Copenhagen K, Denmark
GEOMAR Research Center for Marine Geosciences, Wischhofstrasse 13, D-24148 Kiel, Germany
Geological Survey of Denmark and Greenland,Østervoldgade 10, DK-1350 Copenhagen K, Denmark A high-resolution record of late-Holocene subsurface water-mass characteristics in outer Igaliku Fjord, South Greenland, is presented based on benthic foraminifera faunas from core PO 243451 collected from a water depth of 304 m. Strati" cation with Atlantic water masses present in the lower part of the water-column is suggested to have prevailed during the last 3200 cal. years, except for a period referred to as theMediaeval Warm Period (MWP). During the MWP (c. ad 8851235) the outer part of Igaliku Fjord experienced enhanced vertical mixing and a high hydrodynamic energy level which we ascribe to increasing wind stress through this period, corresponding to the period of the Norse settlement. The transition from the MWP to theLittle Ice Age (LIA) shows a two-step pattern with a short climatic amelioration around AD 1520 before maximum cooling occurred. The intensified wind stress and the overall environmental change are suggested to have contributed to the loss of the Norse settlement in Greenland. Periods with strong stratification and marked in uence of Atlantic subsurface water masses around 2.6, 1.3 ka BP and during the LIA are correlated to North Atlantic Holocene ice-rafting events reported by Bond et al. (1997).
Key Words: Benthic foraminifera palaeoceanography hydrography climatic change Atlantic bottom water ocean currents Greenland Norse settlement late Holocene Little Ice Age Mediaeval Warm Period
The Holocene, Vol. 14, No. 2,
165-171 (2004) This article has been cited by other articles:
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