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Differentiation index from Calypso core GS16-204-22CC-B, Eirik Drift, Labrado...
This dataset shows the relative abundance of the five most important open ocean and sea ice indicator ASVs for the time interval 5–45 kyr b2k in GS16-204-22CC-B, Eirik Drift,... -
Metabarcoding data from Calypso core GS16-204-22CC-B, Eirik Drift, Labrador Sea
This dataset consists of simplified metabarcoding data, including normalised ASV richness and the relative abundance of large taxonomic groups for the time interval 5–45 kyr b2k... -
Open ocean and sea ice indicator ASVs from Calypso core GS16-204-22CC-B, Eiri...
This dataset shows the relative abundance of the five most important open ocean and sea ice indicator ASVs for the time interval 5–45 kyr b2k in GS16-204-22CC-B, Eirik Drift,... -
Sedimentological data from Calypso core GS16-204-22CC-B, Eirik Drift, Labrado...
We counted ice rafted debris grains >150 µm across Heinrich Event 4 in GS16-204-22CC-B, Eirik Drift, Labrador Sea, and report on the grains per g dry sediment. -
Radiocarbon ages from Calypso core GS16-204-22CC-B, Eirik Drift, Labrador Sea
The dataset includes radiocarbon ages measured on the planktonic foraminifer Neogloboquadrina pachyderma from four Holocene samples in GS16-204-22CC-B, Eirik Drift, Labrador... -
Stable isotope data from Calypso core GS16-204-22CC-A, Eirik Drift, Labrador Sea
The dataset contains stable oxygen isotope data of the planktonic foraminifer Neogloboquadrina pachyderma for the interval 0-191 cm of GS16-204-22CC-A, Eirik Drift, Labrador... -
Colour data from Calypso core GS16-204-22CC-B, Eirik Drift, Labrador Sea
Sediment colour parameters (L* a b) measured using a spectrophotometer for the interval 0-857 cm in GS16-204-22CC-B, Eirik Drift, Labrador Sea, covering MIS 3 to the Holocene. -
Colour data from Calypso core GS16-204-22CC-A, Eirik Drift, Labrador Sea
This dataset includes the sediment colour parameters (L* a b) measured using a spectrophotometer for the interval 0-786 cm in GS16-204-22CC-A, Eirik Drift, Labrador Sea. Also... -
Colour, sedimentological, stable isotope, radiocarbon, and metabarcoding data...
The dataset contains colour parameters and sedimentological and paleogenomic data for two Calypso cores (giant piston cores), recovered at the same station on the Eirik Drift... -
IRD flux and supporting data on two cores in the western North Atlantic
A series of catastrophic iceberg discharges termed Heinrich events punctuated the last ice age in the North Atlantic. During Heinrich events, coarse terrigenous debris released... -
Extended age model of sediment core GeoB18530-1 by correlation of Ca/Sr recor...
The previously published 14C-AMS based chronology of GeoB18530-1 by Max et al. (2022; doi:10.1594/PANGAEA.943562), covering the upper 0 - 7.16 m core section down to Heinrich... -
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... -
Gravel petrology of Hudson strait sediments
Sediments from channel samples were weighed and sieved through a 2 mm mesh. Granules >2 mm were visually identified with a binocular microscope and dolomite was separated... -
Mineral composition of Heinrich events 8, 9, and 10 samples
Nine samples from Heinrich events 8, 9, and 10 were obtained from cores HU91020-074 and HU204024-042 which are located some 1900 km south of Hudson Strait in the area of the... -
Neogloboquadrina pachyderma abundances in sediment core EW9303-37JPC
This dataset has no description
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Neogloboquadrina pachyderma abundances in sediment core DY081_GVY01
This dataset has no description
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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...
