Dataset - B2FIND

Replication Data for: Trapdoor viscous remanent magnetization

Jupyter notebooks to generate several Figures of "Trapdoor viscous remanent magnetization". The programs and functions in the notebooks can be used to vary model parameters and...

Six linear regression models for the magnetic susceptibility of sediment core...

Six linear regression estimates of magnetic susceptibility were empirically tested for their ability to predict distinct HLs and ILs signal patterns. As predictors, we used MD...

Grain-size distribution and grain-size dependent magnetic susceptibility of s...

Since the weight percentages of (classifiable) IRD particles > 1 mm and (unclassifiable, but separable) IRD particles > 125 µm both largely underestimate the total content...

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...

Bulk rock magnetic property records of sediment core GeoB18530-1

Standard 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...

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 properties of petrologically representative IRD particles in se...

In order to determine the bulk magnetic impact of all 22 classified IRD lithologies, the specific petromagnetic properties of each were investigated in detail. In order to...

Unclassified IRD susceptibility and content, porosity and grain density of se...

IRD content is commonly assessed by weighing the detrital particles of the >125µm or > 1mm sieve fractions or by counting the IRD particles of the latter. Here we present...

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....

Physical property data form the Wanihama section and the Khan Sahib section i...

Samples were taken in 2019 at the Wanihama loess-paleosol sequence to (a) assess the physical properties of loess-paleosol sequences in Kashmir, and to specifically test their...

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...

Rock magnetic, major element, siliciclastic grain-size data from sediment cor...

Magnetic signals in deep-sea sediments have the potential to unravel past continental environmental changes – via changes in primary terrigenous magnetic supply – but also...

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....