Biomarker, foraminiferal abundance, stable isotope and trace element data from sediment cores JM11-FI-19PC and LINK 16 from the southern Norwegian Sea during 130-110 kadoi:10.18710/3LCQJXDataverseNO2024-10-111Ezat, Mohamed Mahmoud; Fahl, Kirsten; Rasmussen, Tine L., 2024, "Biomarker, foraminiferal abundance, stable isotope and trace element data from sediment cores JM11-FI-19PC and LINK 16 from the southern Norwegian Sea during 130-110 ka", https://doi.org/10.18710/3LCQJX, DataverseNO, V1Biomarker, foraminiferal abundance, stable isotope and trace element data from sediment cores JM11-FI-19PC and LINK 16 from the southern Norwegian Sea during 130-110 kadoi:10.18710/3LCQJXEzat, Mohamed MahmoudFahl, KirstenRasmussen, Tine L.Ezat, Mohamed MahmoudFahl, KirstenRasmussen, Tine L.274429274429A31720DataverseNOUiT The Arctic University of NorwayEzat, Mohamed MahmoudEzat, Mohamed M.2024-09-21Earth and Environmental SciencesNordic SeasThe Last InterglacialForaminiferaStable isotopesBiomarkersFreshwater forcingThe Atlantic Meridional Overturning CirculationWe present biomarker, foraminiferal abundance, stable isotope and trace element data from sediment cores JM11-FI-19PC and LINK16 from the southern Norwegian Sea during 130-110 ka. Sediment core JM11-FI-19PC was retrieved from a water depth of 1179 m northwest of the Faroe Islands (62°49′N, 03°52′W). Sediment core LINK 16 was retrieved from a water depth of 773 from the northeast of the Faeroe–Shetland Channel (62°36′N, 3°31′W). For sediment core LINK16, brassicasterol (24-methylcholesta-5, 22E-dien-3β-ol), IP25 (a C25 Isoprenoid Lipid), benthic foraminiferal assembalges, and foraminiferal stable isotope data are provided. For sediment core JM-FI-19PC, brassicasterol , IP25 and foraminiferal Na/Ca and Ba/Ca are provided. The age models of both sediment cores M11-FI-19PC and LINK 16 are provided.2011-04-012022-04-01The Norwegian Sea-4-36263Observation data<a href="http://creativecommons.org/publicdomain/zero/1.0">CC0 1.0</a>Ezat, M.M; Fahl, K; Rasmussen, T.L. Arctic freshwater outflow suppressed Nordic Seas overturning and oceanic heat transport during the Last Interglacial. Accepted In Principle. Nature CommunicationsEzat, M.M; Fahl, K; Rasmussen, T.L. Arctic freshwater outflow suppressed Nordic Seas overturning and oceanic heat transport during the Last Interglacial. Accepted In Principle. Nature Communications00_README_Ezat et al..txtREAD ME filetext/plainAge models for sediment cores LINK 16 and JM11-FI-19PC.csvAge models for sediment cores LINK 16 and JM11-FI-19PC text/comma-separated-valuesData for sediment core LINK16.csvData from core LINK16:Plantkic and benthic foraminiferal stable isotope values, IP25, Brassicasterol, and P(B)IP25 Index. Abbreviations: - Age (ka), ka: thousands of years before present - N. pachyderma d18O: oxygen isotope values Neogloboquadrina pachyderma, unit pemille (‰) - M. barleeanus d18O: oxygen isotope values Neogloboquadrina pachyderma, unit pemille (‰) - M. barleeanus d13C: carbon isotope values Melonis barleeanus, unit permille (‰) - %M. barleanus: percentage of Melonis barleeanus of the total benthic foraminifera - %C. neoteretis: percentage of Cassidulina neoteretis of the total benthic foraminifera - %C. reniforme: percentage of Cassidulina reniforme of the total benthic foraminifera - IP25 (a C25 Isoprenoid Lipid), unit (nano gram/gram Sediments) - Brassicasterol, unit (nano gram/gram Sediments) - Sea ice index P(B)IP25 text/comma-separated-valuesData from sediment core JM11-FI-19PC.csvData from core JM11-FI-19PC: IP25, Brassicasterol, P(B)IP25 Index, and foraminiferal Na/Ca and Ba/Ca. Abbreviations: - Age (ka), ka: thousands of years before present - IP25 (a C25 Isoprenoid Lipid), unit (nano gram/gram Sediments) - Brassicasterol, unit (nano gram/gram Sediments) - Sea ice index P(B)IP25 - Na/Ca measured in Neogloboquadrina pachyderma, unit pemille (milli mol/mol) - Ba/Ca measured in Neogloboquadrina pachyderma, unit pemille (micro mol/mol) text/comma-separated-values