Duration and Ice Thickness of a Late Holocene Outlet Glacier Advance near Narsarsuaq, South Greenland
Greenland Ice Sheet (GrIS) outlet glaciers are currently losing mass leading to sea level rise. Reconstructions of past outlet glaciers through the Holocene help us better understand how they respond to climate change. Kiattuut Sermiat, a south Greenland outlet glacier near Narsarsuaq, is known to h...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Copernicus Publications
2023
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| Online Access: | https://doi.org/10.5194/egusphere-2023-440 https://noa.gwlb.de/receive/cop_mods_00065560 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00064079/egusphere-2023-440.pdf https://egusphere.copernicus.org/preprints/2023/egusphere-2023-440/egusphere-2023-440.pdf |
| Summary: | Greenland Ice Sheet (GrIS) outlet glaciers are currently losing mass leading to sea level rise. Reconstructions of past outlet glaciers through the Holocene help us better understand how they respond to climate change. Kiattuut Sermiat, a south Greenland outlet glacier near Narsarsuaq, is known to have experienced an anomalously small Little Ice Age advance compared with a larger Holocene advance that culminated at ~1600 cal yr BP. We report sedimentary records from two lakes at slightly different elevations in an upland valley adjacent to Kiattuut Sermiat, which reveal when the outlet glacier was significantly larger than its Little Ice Age size and constrain the associated outlet glacier surface elevation. We use bulk sediment geochemistry, magnetic susceptibility, color, texture, and the presence of aquatic plant macrofossils to distinguish between till, glaciolacustrine sediments, and organic lake sediments. Our 14C results above basal till recording regional deglaciation skew slightly old due to a hard water effect but are generally consistent with regional deglaciation occurring ~11,000 cal yr BP. Neoglacial advance of Kiattuut Sermiat is recorded by deposition of glaciolacustrine sediments in the lower-elevation lake, which was subsumed by an ice-dammed lake that formed along the glacier’s margin just after ~3900 cal yr BP. This timing is consistent with several other glacial records in Greenland showing Neoglacial cooling driving advance between ~4500–3000 cal yr BP. Given that glaciolacustrine sediments were deposited only in the lower-elevation lake, combined with glacial geomorphological evidence in the valley containing these lakes, we estimate the former ice margin’s elevation to have been ~670 m, compared with ~420 m today. The ice-dammed lake persisted until glacier retreat at ~1600 cal yr BP. That retreat timing contrasts with overall evidence for cooling and glacier advance in the region at that time, so we infer that retreat may have resulted from reduced precipitation amounts and/or local ... |
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