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Late-Holocene environment and climatic changes in Ameralik Fjord, southwest Greenland: evidence from the sedimentary record

Institute of Geography, University of Copenhagen, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark, hsm{at}geogr.ku.dk

K. G. Jensen

Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark

A. Kuijpers

Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark

S. Aagaard-Sørensen

Department of Earth Sciences, University of Aarhus, DK-8000 Århus C, Denmark

M.-S. Seidenkrantz

Department of Earth Sciences, University of Aarhus, DK-8000 Århus C, Denmark

M. Prins

Faculty of Earth and Life Sciences, Department of Paleoclimatology & Geomorphology, Vrije Universiteit Amsterdam, De Boelelaan 1085, NL-1081 HVAmsterdam, The Netherlands

R. Endler

Baltic Sea Research Institute, Seestrasse 15, D-18119, Rostock-Warnemünde, Germany

N. Mikkelsen

Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark

Sedimentological and geochemical (XRF) data together with information from diatom and benthic foraminiferal records of a 3.5 m long gravity core from Ameralik Fjord, southern West Greenland, is used for reconstructing late-Holocene environmental changes in this area. The changes are linked to large-scale North Atlantic ocean and climate variability. AMS ¹⁴C-dating of benthic foraminifera indicates that the sediment core records the last 4400 years and covers the termination of the Holocene Thermal Maximum (HTM). The late HTM (4.4-3.2 ka BP) is characterized by high accumulation rates of fine (silty) sediments related to strong meltwater discharge from the Inland Ice. The HTM benthic foraminiferal fauna demonstrates the presence of well-ventilated, saline bottom water originating from inflow of subsurface West Greenland Current water of Atlantic (Irminger Sea) origin. The hydrographic conditions were further characterized by limited sea ice probably related to a mild and relatively windy winter climate. After 3.2 ka BP lower fine-grained sedimentation rates, but a larger input from sea-ice rafted or aeolian coarse material prevailed. This can be related to colder atmospheric conditions with a decreased meltwater discharge and more widespread sea-ice cover in the fjord.

Key Words: Climate change • fjords • sedimentary environment • diatoms • benthic foraminifera • AmeralikFjord • Greenland • late Holocene

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