Dataset - B2FIND

Element ratio proxy records for dolomitic and granitic IRD content in sedimen...

Because of its sensitivity for detrital dolomite, the Ca/Sr ratio of sediment core GeoB18530-1 was previously used to identify Heinrich Event layers (doi:10.1594/PANGAEA.943557...

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,...

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...

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....

Rock and paleomagnetic data from two sediment cores from the Black Sea for th...

Rock magnetic and paleomagnetic results covering the past 30 ka were constructed from two sediment cores MSM33_856-1 (MSM33-55-1) and MSM33_855-1 (54-3) from the Black Sea....

Paleomagnetic and rock magnetic data of SO202-33-4, North Pacific

Paleoceanography research is always limited by the accuracy of age-depth relationships. For sediments below carbonate compensation depth (CCD) where other dating methods could...

Paleomagnetic data from Black Sea, sediment core MSM33_851-1 (MSM33-53-1)

This data publication includes paleo and rock magnetic data from sediment core MSM33-53-1 recovered during the marine expedition MSM33 of the German research vessel RV Maria S....