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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... -
Processed CT image of sediment core GeoB22315-2 from Hvalsund, northern Baffi...
Processed CT data of sediment core GeoB22315-2, performed using the ZIB edition of the Amira software (version 2021.08; Stalling et al., 2005), including CT image and... -
Processed CT image of sediment core GeoB22346-3 from Clyde Fjord, Baffin Isla...
Processed CT data of sediment core GeoB22346-3, performed using the ZIB edition of the Amira software (version 2021.08; Stalling et al., 2005), including CT image and... -
Processed CT image of sediment core GeoB22357-3 from western Baffin Bay, Mari...
Processed CT data of sediment core GeoB22357-3, performed using the ZIB edition of the Amira software (version 2021.08; Stalling et al., 2005), including CT image and... -
Processed CT image of sediment core GeoB22336-4 from northern Baffin Bay, Mar...
Processed CT data of sediment core GeoB22336-4, performed using the ZIB edition of the Amira software (version 2021.08; Stalling et al., 2005), including CT image and... -
Relative and absolute abundance records of three IRD particle groups and six ...
As detailed in Bukar et al. (2024), the 22 classifiable IRD lithologies can be group according to their preferred affiliation to Heinrich Layers (HL) and Interlayers (IL). Group... -
Lithology-specific IRD counts of sediment core GeoB18530-1
Total and lithology-specific ice-rafted detritus (IRD) counts of sediment core GeoB18530-1 were determined by stereomicroscopically identifying, picking and counting all... -
IRD composition and accumulation rates of Heinrich Event layers (H1-H6) and i...
The cumulative classified count record (in percentages) over ~2 cm resolution of each petrologically identified IRD lithologies within the stratigraphic units of Heinrich Layers... -
Coastal ice-rafted detritus of Black Sea sediment cores covering MIS 6 (184-1...
The amount of coastal ice-rafted detritus (IRDC) was determined by counting the detrital grains from 8.8 cm3 subsamples of the dried and wet-sieved sediment fraction >150 mm...
