-
Ca/Sr ratios of sediment core GeoB18530-1
This dataset has no description
-
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... -
Mg/Ca temperature, d18O data, Sr/Ca ratio and radiocarbon ages from sediment ...
Sediment core GeoB18530-1 was collected during MSM39 cruise in 2014 in the subpolar western North Atlantic. X-ray fluorescence (XRF) core-scanning measurements of GeoB18530-1... -
Thresholds identified in the recurrence plot of NGRIP δ18O record and their c...
Thresholds identified in the recurrence plot of NGRIP δ18O record and their correspondence in the marine isotope stratigraphy of the last climate cycle stratigraphy (Bassinot et... -
Comparison of the main steps detected by Hodell and Channell (2016) from U130...
Comparison of the main steps detected by Hodell and Channell (2016) from U1308 marine record with those deduced from the Recurrence Plot of the benthic δ18O and bulk carbonate... -
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... -
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... -
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... -
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... -
Statistics of the recurrence rate analysis for U1308 benthic δ18O, U1308 bulk...
Statistics of the recurrence rate analysis for U1308 benthic δ18O, U1308 bulk carbonate δ18O (Hodell and Channell, 2016) and NGRIP δ18O (Rasmussen et al., 2014). The RR... -
Detection of abrupt climate changes over the past 3.2 Myr
The past 3.2 Myr have seen drastic climate changes with the development, waxing and waning of huge continental ice sheets over the Northern Hemisphere. These striking phenomena...
