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Age model Anaerobic oxidation Antarctica Aquatic biota Arctic Ocean Bathymetry Benthic foraminifera Biogenic Bloom Biogeochemistry Biomarker Biomarkers Bulk marine sediment Bulk sediment Carbon Carbon and Oxygen isotopes Carbon isotopes Chironomids Climate indicator Climate indicator plant species Climate reconstruction Climate variability Climate warming Coccolithophores Concentration Cooloola Sand Mass Cryostratification Dating Deep water Deglaciation Diatoms Diffusion Dissociation Dunes East Siberian Margin Eastern equatorial Pacific Ebullution Eemian Eocene Fennoscandia Finland Flux Foraminifera Fraser Island Gas hydrate Geochemical proxy data Geochemistry Geochronology Geophysics Grain size Greenhouse Herald Canyon Holocene Hydrogen isotopes ISSS-2020 Icebreaker Oden Java Jämtland Lake Lake Tarfala Lake ice Lake ice phenology Lake sediments Last Interglacial Late Miocene Lateglacial Les Echets Lomonosov Ridge MIS 5e MIS2 MIS3 Marine Geology Marine Heat Flow Marine geology Marine sediment Maritime continent Matuyama/Bruhnes boundary Meteorology Methane Methane emissions Methane isotopes Mg/Ca Micrometeorology Middle Pleistocene Transition Mineral magnetics Multi-proxy Multibeam Nitrogen North Atlantic Northern hemisphere OSL OSL dates Observations Ocean circulation Oceanography Oligocene Optically stimulated luminescence Organic carbon Oxygen Palaeoceanography Palaeoclimate Paleoclimate Paleoenvironment Paleomagnetism Paleotemperature Planktic foraminifera Plant macrofossils Pleistocene Pollen RCS Reconstruction SWERUS-C3 SWERUS-C3 expedition Sample depth Scandinavia Scots pine Seafloor methane Seafloor morphology Seasonality changes Sediment properties Southern Sweden Stable isotopes Subarctic Summer temperature Sweden TOUGH+Hydrate TRW Tarfala Temperature Temperature proxy Temperature reconstruction Terrestial biota Trace gas Tree-rings Under-ice Volcanoes Warm-pool Water temperatures Weather station Younger Dryas ¹⁴C dates