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Silt and clay of marine sediment core GL-1090
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Major elements of marine sediment core GL-1090
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Magnetic susceptibility of marine sediment core GL-1090
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IRM, S-ratio, and HIRM of marine sediment core GL-1090
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Hysteresis parameters of marine sediment core GL-1090
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Bulk carbonate of marine sediment core GL-1090
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Anhysteretic remanent magnetization and magnetic susceptibility of marine sed...
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Age model and terrigenous accumulationrates of marine sediment core GL-1090
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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... -
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.... -
Paleo- and rock magentic data of core PS97/085-3
During Expedition PS97 of the Research Vessel POLARSTERN to the Drake Passage in 2016, three sediment cores, PS97/085-3, PS97/084-1, and PS97/079-2 were collected along the... -
Paleo- and rock magentic data of core PS97/084-1
During Expedition PS97 of the Research Vessel POLARSTERN to the Drake Passage in 2016, three sediment cores, PS97/085-3, PS97/084-1, and PS97/079-2 were collected along the...
