Stable isotopes (δ13C and δ18O) and Mg/Ca-based temperatures of Globorotalia truncatulinoides from a Holocene sediment core southwest off the Cabo Verde archipelago (MUC5)

10.1594/PANGAEA.972511Pérez-Rodríguez, IreneIrenePérez-RodríguezNürnberg, DirkDirkNürnbergGEOMAR - Helmholtz Centre for Ocean Research KielSchindlbeck-Belo, JulieJulieSchindlbeck-Belo0000-0001-5865-3272GEOMAR - Helmholtz Centre for Ocean Research KielWharton, JackJackWharton0009-0005-7401-651XHansteen, Thor HThor HHansteen0000-0003-1991-5107GEOMAR - Helmholtz Centre for Ocean Research KielHuvenne, Veerle A IVeerle A IHuvenne0000-0001-7135-6360National Oceanography Centre, SouthamptonThornalley, David J RDavid J RThornalley0000-0001-5885-5499Mosquera Giménez, ÁngelaÁngelaMosquera Giménez0000-0001-5509-7493Instituto Español de OceanografíaKutterolf, SteffenSteffenKutterolf0000-0002-0645-3399GEOMAR - Helmholtz Centre for Ocean Research KielBarnhill, Kelsey ArcherKelsey ArcherBarnhill0000-0001-6882-1209Orejas, CovadongaCovadongaOrejas0000-0002-2580-1002Centro Oceanográfico de Gijón, Spanish Institute of Oceanography (IEO-CSIC)Stable isotopes (δ13C and δ18O) and Mg/Ca-based temperatures of Globorotalia truncatulinoides from a Holocene sediment core southwest off the Cabo Verde archipelago (MUC5)PANGAEA2024Cabo Verde ArchipelagoForaminiferal stable isotopesHolocenemicrofossilsplanktonic foraminifera Mg/CaEvent labelSample code/labelDEPTH, sediment/rockDepth, top/minDepth, bottom/maxAGEMagnesium/Calcium ratioStrontium/Calcium ratioAluminium/Calcium ratioIron/Calcium ratioManganese/Calcium ratioδ13Cδ18OSub-surface temperatureMultiCoreriMirabilis2_Leg1Sarmiento de GamboaIntegrated Assessment of Atlantic Marine Ecosystems in Space and Time (iAtlantic)2021-08-10T00:00:00Dataset10.1029/2007PA001505385 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalData access is restricted (moratorium, sensitive data, license constraints)This dataset presents combined stable isotopes (δ13C and δ18O) and Mg/Ca ratios for the sub-thermocline dwelling planktonic foraminifer Globorotalia truncatulinoides. Al/Ca, Fe/Ca, and Mn/Ca ratios are also included to assess potential contamination of the foraminiferal tests. The microfossils were obtained from the 315-400 μm sediment fraction of a core collected at a water depth of 4394 m off the Cabo Verde archipelago, which covers most of the Holocene Epoch.-25.5015114.63284Horizon 2020 of the European Commissionhttps://doi.org/10.13039/501100007601818123Integrated Assessment of Atlantic Marine Ecosystems in Space and Time