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Grain-size distribution of from different Holes of IODP Expedition 386
This dataset provides grain-size distributions for 278 sediment samples from 11 sediment cores targeting four event beds - Event Bed 1 (CE 2011 Tohoku-Oki), Event Bed 2 (CE 1456... -
Uranium-Thorium series of sediment core Arc7-E25
*230Thxs is calculated by the subtraction of mean activity value of 234U from the total 230Th. -
TOC and stable carbon isotopic composition of sediment core Arc7-E25
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Grain size distribution of sediment core Arc7-E25
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Bulk mineralogy measurements of sediment core Arc7-E25
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Radionuclides of sediment core Arc7-E25
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14C dates of sediment core Arc7-E25
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Sedimentology, mineralogy, and geochemistry results of core Arc7-E25 from sou...
The 320 cm long gravity core E25 (Arc7-E25, 179.4°E, 79.0°N; 1200 m) was retrieved from the southernmost Mendeleev Ridge during the 7th cruise of the Chinese Arctic expedition... -
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... -
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... -
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... -
Grain-size analysis obtained from sediment core RD04 (island of Sylt)
Core RD04 originates from a natural back-barrier marsh (island of Sylt). The marsh in Sylt is a low-energy, back-barrier marsh. Grain-size data were used to determine and... -
Grain-size analysis obtained from sediment core BT03 (Eiderstedt peninsula; s...
Core BT03 originates from a reinstated, former managed marsh (Eiderstedt peninsula). The marsh in Eiderstedt is exposed to storm waves from the open North Sea. Grain-size data... -
Grain-size analysis obtained from sediment core BT02 (Eiderstedt peninsula; s...
Core BT02 originates from a reinstated, former managed marsh (Eiderstedt peninsula). The marsh in Eiderstedt is exposed to storm waves from the open North Sea. Grain-size data... -
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....
