Supporting data for "Changes in planktic foraminiferal distribution, productivity, and preservation in the Barents Sea during the last three millennia"

10.18710/16X6M9Anglada-Ortiz, GriseldaGriseldaAnglada-Ortiz0000-0001-5687-6683UiT The Arctic University of NorwayRasmussen, Tine L.Tine L.Rasmussen0000-0002-1625-2291UiT The Arctic University of NorwayChierici, MelissaMelissaChierici0000-0003-0222-2101Institute of Marine ResearchFransson, AgnetaAgnetaFransson0000-0003-1403-2110Norwegian Polar InstituteZiveri, PatriziaPatriziaZiveri0000-0002-5576-0301Institute of Environmental Science and Technology, Autonomous University of BarcelonaThomsen, ErikErikThomsen7005764780Department of Geosciences, Aarhus UniversityZamelczyk, KatarzynaKatarzynaZamelczyk0000-0002-9876-5807UiT The Arctic University of NorwayMeilland, JulieJulieMeilland0000-0001-8966-3115CEREGEEzat, Mohamed M.Mohamed M.Ezat0000-0002-9475-0974UiT The Arctic University of NorwayGarcia-Orellana, JordiJordiGarcia-Orellana0000-0002-0543-2641Institute of Environmental Science and Technology, Autonomous University of BarcelonaSupporting data for "Changes in planktic foraminiferal distribution, productivity, and preservation in the Barents Sea during the last three millennia"DataverseNO2025Earth and Environmental Sciencespaleoproductivitycalcium carbonate dissolutionlate HoloceneArctic OceanAnglada-Ortiz, GriseldaGriseldaAnglada-OrtizUiT The Arctic University of NorwayRasmussen, Tine L.Tine L.RasmussenUiT The Arctic University of NorwayUiT The Arctic University of NorwayUiT The Arctic University of Norway2025-03-242025-05-072013-05-30/2018-09-29observational data10.1029/2024PA00498955684402337527531145text/plaintext/comma-separated-valuestext/comma-separated-valuestext/comma-separated-valuestext/comma-separated-values1.1CC0 1.0Paleoproduction changes in the northern and southern Barents Sea based on changes of abundance (absolute and relative) of planktic foraminifers and stable isotopes. Data of total and organic carbon and calcium carbonate content in the sediment was measured. The age-depth model from sediment cores was built based on a combination of lead 210 and carbon 14. See "Changes in planktic foraminiferal distribution, productivity, and preservation in the Barents Sea during the last three millennia".Research Council of NorwayRCN#276730Research Council of NorwayRCN#216538Research Council of NorwayRCN#223259Tromsø Research Fundation#A31720