Dataset - B2FIND

Rock magnetic, geochemical and sedimentological properties related to IRD com...

The IRD-rich Heinrich Event (HE) layers of gravity core GeoB18530-1, retrieved from the SE Grand Banks slope of Newfoundland, coincide with bulk magnetic susceptibility maxima....

Petrological classification and lithology-specific abundance analysis of ice-...

IRD-rich Heinrich Event (HE) layers are commonly used as stratigraphic markers of North Atlantic sediments. Gravity core GeoB18530-1, retrieved from the SE Grand Banks slope of...

Light reflectance (RGB) of 21 sediment cores from Maria S. Merian cruise MSM39

Spectral light reflectance is a measure of the relative amount of light reflected by a material under incident white light. It is expressed within an absolute range from 0...

Electrical conductivity, porosity and density of 21 sediment cores from Maria...

The electrical sediment conductivity σs (and reciprocal resistivity Rs) was determined using an inductive GEOTEK non-contact resistivity (NCR) sensor. The system applies...

Susceptibility of 21 sediment cores from Maria S. Merian cruise MSM39

The sediment series recovered during MERIAN Cruise MSM 39 by gravity coring were subject to routine magnetic susceptibility loggin, which was usually performed on the closed...

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...