Late Quaternary sedimentation in Kejser Franz Joseph Fjord and the continental margin of East Greenland

• Main Authors: Evans, Jeff, Dowdeswell, Julian A, Grobe, Hannes, Niessen, Frank, Stein, Ruediger, Hubberten, Hans-Wolfgang, Whittington, R J
• Format: Dataset
• Language: English
• Published: PANGAEA 2002
• Subjects: ARK-X/2; AWI_Paleo; East Greenland Sea; Gravity corer (Kiel type); Kaiser-Franz-Josef-Fjord; East Greenland; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS2627-7; PS2628-1; PS2629-4; PS2630-5; PS2631-5; PS2632-5; PS2633-2; PS2641-4; PS31; PS31/135; PS31/136; PS31/137; PS31/138; PS31/140; PS31/141; PS31/142; PS31/154; Quaternary Environment of the Eurasian North; QUEEN; SL; Greenland; Kejser Franz Joseph Fjord; east greenland current; glacier; Greenland Sea; Ice Sheet; Kejser Franz Joseph fjord; Sea ice
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.728151; https://doi.org/10.1594/PANGAEA.728151

The marine sedimentary record in Kejser Franz Joseph Fjord and on the East Greenland continental margin contains a history of Late Quaternary glaciation and sedimentation. Evidence suggests that a middle-shelf moraine represents the maximum shelfward extent of the Greenland Ice Sheet during the last glacial maximum. On the upper slope, coarse-grained sediments are derived from the release of significant quantities of iceberg-rafted debris (IRD) and subsequent remobilization by subaqueous mass-flows. The middle-lower slope is characterized by hemipelagic sedimentation with lower quantities of IRD (dropstone mud and sandy mud), punctuated episodically by deposition of diamicton and graded sand/gravel facies by subaqueous debris flows and turbidity currents derived from the mass failure of upper slope sediments. The downslope decrease of IRD reflects either the action of the East Greenland Current (EGC) confining icebergs to the upper slope, or to the more ice-proximal setting of the upper slope relative to the LGM ice margin. Sediment gravity flows on the slope are likely to have fed into the East Greenland channel system, contributing to its formation in conjunction with the cascade of dense brines down the slope following sea-ice formation across the shelf. Deglaciation commenced after 15,300 14C years, as indicated by meltwater-derived light oxygen isotope ratios. An abrupt decrease in both IRD deposition and delivery of coarse-grained debris to the slope at this time supports ice recession, with icebergs confined to the shelf by the EGC. Glacier ice had abandoned the middle shelf before 13,000 14C years with ice loss through iceberg calving and deposition of diamicton. Continued retreat of glacier-ice from the inner shelf and through the fjord is marked by a transition from subglacial till/bedrock in acoustic records, to ice-proximal meltwater-derived laminated mud to ice-distal bioturbated mud. Ice abandoned the inner shelf before 9100 14C years and probably stabilized in Fosters Bugt at 10,000 14C years. ...