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Holocene 231Pa/230Th ratios, Uranium isotopes and biogenic Opal concentration...
To investigate the variability of the Atlantic Meridional Overturning Circulation (AMOC) during the Holocene in the North Atlantic, we analyzed radioisotopes (230Th, 231Pa,... -
Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
14C data of three North Atlantic sediment cores during the Holocene
To examine the variability of the Atlantic Meridional Overturning Circulation (AMOC) during the Holocene in the North Atlantic, we developed new age models for three sediment... -
231Pa/230Th (Pa/Th) and related radioisotope concentrations from eleven Atlan...
231Pa/230Th and related radioisotope concentrations from eleven Atlantic sediment cores for the Holocene. The concentrations of sedimentary 231Pa, 238U, 230Th, and 232Th were... -
Principal Component Analysis (PCA) of IRD content in Heinrich Event layers (H...
The data matrix of 192 classified IRD count data from H1-H5a and I1-I5 (excluding I6 because of too low IRD counts) by 22 IRD lithologies... -
Nonlinear Mapping (NLM) analysis of IRD content in Heinrich Event layers (H1-...
This 3D data set represents the result of a Sammon projection (Sammon, 1969; https://doi.org/10.1109/T-C.1969.222678), where the mean relative proportions of all classified IRD... -
Extended age model of sediment core GeoB18530-1 by correlation of δ18O record...
The previously published 14C-AMS based chronology of GeoB18530-1 by Max et al. (2022; doi:10.1594/PANGAEA.943562), covering the upper 0 - 7.16 m core section down to Heinrich... -
Water column raw data (Kongsberg EM 122 entire dataset) of RV MARIA S. MERIAN...
Raw water-column data were collected using the ship's own Kongsberg EM122 multibeam echosounder during the RV MARIA S. MERIAN cruise MSM39 (Linking past and present in the North... -
Multibeam bathymetry raw data (Kongsberg EM 122 entire dataset) of RV MARIA S...
Raw bathymetry data were collected using the ship's own Kongsberg EM122 multibeam echosounder during the RV MARIA S. MERIAN cruise MSM39 (Linking past and present in the North... -
Isothermal Remanent Magnetization (IRM) acquisition curves for the unclassifi...
IRM acquisition curves (and their derivatives) resolve the cumulative coercivity distribution (and spectrum) of a magnetic mineral assemblage. Here we present IRM data for all... -
Relative and absolute abundance records of three IRD particle groups and six ...
As detailed in Bukar et al. (2024), the 22 classifiable IRD lithologies can be group according to their preferred affiliation to Heinrich Layers (HL) and Interlayers (IL). Group... -
Extended age model of sediment core GeoB18530-1 by correlation of Ca/Sr recor...
The previously published 14C-AMS based chronology of GeoB18530-1 by Max et al. (2022; doi:10.1594/PANGAEA.943562), covering the upper 0 - 7.16 m core section down to Heinrich... -
Light reflectance (RGB) of sediment core GeoB18530-1
This dataset has no description
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Physical oceanography, CFC-11 and CFC-12 measured on water bottle samples dur...
Temperature, salinity and CFCs measured on the RV Maria S. Merian Cruise MSM39 St. John's - St. John's 06/07 - 06/25/2014 Chief Scientist: Stefan MulitzaRegion: Northwestern... -
Physical oceanography during Maria S. Merian cruise MSM39
This dataset has no description
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Digital grain and thin section micrographs of petrologically representative I...
The micrographs of the representive IRD particles showcase the pristine physical appearances of the IRD and their mineralogical compositions. Digital images of the pristine IRD... -
Lithology-specific IRD counts of sediment core GeoB18530-1
Total and lithology-specific ice-rafted detritus (IRD) counts of sediment core GeoB18530-1 were determined by stereomicroscopically identifying, picking and counting all... -
IRD composition and accumulation rates of Heinrich Event layers (H1-H6) and i...
The cumulative classified count record (in percentages) over ~2 cm resolution of each petrologically identified IRD lithologies within the stratigraphic units of Heinrich Layers... -
Isothermal Remanent Magnetization (IRM) acquisition curves for petrologically...
IRM acquisition curves (and their derivatives) resolve the cumulative coercivity distribution (and spectrum) of a magnetic mineral assemblage. Here we present data of larger,... -
Radiocarbon ages in 14C conventional and calibrated ages
All ages are shown with 1 sigma uncertainty. Calibrated ages were determined with CALIB 7.1 (Stuiver et al., 2017) using the Marine13 (Reimer et al., 2013) database and a...
