Dataset - B2FIND

Annual mean and mean summer/winter precipitation at weather station Vladivostok

Sediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur...

Annual mean and mean summer/winter air temperature at weather station Vladivo...

Sediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur...

Geochemical composition (corrected) of the Late Holocene sediments core LV66-...

Sediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur...

Geochemical composition (XRF SR uncorrected) of the Late Holocene sediments c...

Sediment core LV66-3 (43°07,473' N,131°49,622' E length of 466 cm; water depth 33 m) was collected in 2014 during the 66th cruise of the R/V Akademik M.A. Lavrentiev in the Amur...

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...