Radiocarbon dates, grain size measurements and selected foraminifera analysis from sediment cores AvH248260-2 and AvH248260-1, Ameralik Fjord, SW Greenland

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-...

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Bibliographic Details
Main Authors: Møller, H S, Jensen, Sven, Kuijpers, Antoon, Aagaard-Sørensen, Steffen, Seidenkrantz, Marit-Solveig, Prins, Maarten Arnoud, Endler, Rudolf, Mikkelsen, Naja
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
Ameralik Fjord
AvH248260-2
GC
Gravity corer
Greenland
Irminger Sea
Ameralik
Ameralik fjord
North Atlantic
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.785444
https://doi.org/10.1594/PANGAEA.785444
Description
Summary: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.

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