10.1594/PANGAEA.971729Wang, YiyunYiyunWangvon Dobeneck, TiloTilovon Dobeneck0000-0002-0087-4053Department of Geosciences, Bremen UniversityMARUM - Center for Marine Environmental Sciences, University BremenBukar, ShettimaShettimaBukar0000-0003-4154-6045Department of Geosciences, Bremen UniversityFrederichs, ThomasThomasFrederichs0000-0003-0976-0332Department of Geosciences, Bremen UniversityPANGAEA2025Geochemistrygrain size distributionGrand Banks MarginHeinrich eventsIce-Rafted DetritusRock magnetismDEPTH, sediment/rockHeinrich eventMagnetic susceptibilityIsothermal remanent magnetization, mass-normalizedAnhysteretic remanent magnetization, mass-normalizedHard isothermal remanent magnetizationSaturation isothermal remanent magnetization/kappa ratioS-ratioGravity corerMagnetic susceptibility meter, Bartington MS2B bulk sensor 460 HzMagnetometer, cryogenic, pass-through, 2G Enterprises 755 RMSM39Maria S. MerianProcesses and impacts of climate change in the North Atlantic Ocean and the Canadian Arctic (ArcTrain)2014-06-14T13:58:00Dataset10.1594/PANGAEA.97178510.1029/2024GC01193110.1594/PANGAEA.9712901968 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalStandard remanence-based dry-bulk rock magnetic parameters were determined in 2.3 cm steps along core GeoB18530-1 using an automated 2G Enterprises 755R DC SQUID Magnetometer with built-in AF, DC and pulse coils. The 6.2 cm³ large cube samples were measured in water-saturated state and subsequently dried and weighed in order to convert their magnetic moments to dry-mass-specific remanent magnetization, thereby eliminating the magnetic impact of porosity variations. The herein published data for IRM_20mT, IRM_100mT, ARM_100mT, HIRM, SIRM/χ and S_0.3T are diagnostic for magnetic mineral composition and were selected from a much larger raw data series based on 28 pulse field steps from 10 mT to 2.7 T. The chosen core depth range from 4.88 m to 10.60 m includes six Heinrich Event Layers and their surrounding interlayers.Corresponds to Figure 1-49.23483333333342.8395SE Grand Banks SlopeGerman Research Foundationhttps://doi.org/10.13039/501100001659221211316GRK/IRTG 1904: ArcTrain - Processes and impacts of climate change in the North Atlantic Ocean and the Canadian ArcticPetroleum Technology Development Fundhttps://doi.org/10.13039/501100009614Shettima BukarOverseas postgraduate scholarship to Shettima Bukar