| Summary: | While the Holocene history of the eastern Fram Strait is well investigated, only little is known about the past climate and the oceanographic conditions of the western part near Greenland. To fill this knowledge gap, a high-resolution Holocene sediment record from the outermost NE Greenland shelf, obtained during expedition PS93.1 (2015) of RV Polarstern, was investigated using micropaleontological and geochemical methods. Used proxies allow a profound assessment of Atlantic Water advection, bioproductivity, sea-ice coverage, water mass properties (e.g., temperature, salinity, ventilation) and stratification, while also indicating possible cold events and their cyclicity. The 264 cm long sediment record (80.5°N, 8.5°W, 290 m water depth) was radiocarbon-dated and investigated at high resolution for sediment composition, foraminifer contents, grain size variations (sortable silt, grain size distribution), contents of ice-rafted debris, element ratios and the isotopic composition of planktic and benthic foraminifers. Planktic and benthic foraminifer flux rates show highest values between 10.6 and 8.0 cal. ky BP, marking the maximum in bioproductivity and indicating either ice-free conditions or a reduced sea-ice cover during this time interval. Correlating high planktic foraminifer fragmentation values are likely related to dissolution through organic carbon oxidation due to an increased accumulation of organic matter. The subpolar planktic foraminifer species T. quinqueloba appears continuously until ca. 5.6 cal. ky BP and can be linked to an increased advection of warmer Atlantic Water (AW). Low shares of rounded IRD and quartz grains before 5.0 cal. ky BP are characteristic for low amounts of sea-ice sediments and therefore display a lower degree of sea-ice coverage, possibly also due to the mentioned AW advection. Between 10.0 and 5.0 cal. ky BP, the IRD-corrected sortable silt curve tends towards coarse grains, reflecting stronger currents. Afterwards, a trend to finer grains implies weaker currents and thus ...
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