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(Table S1) Paleomagnetic declination and inclination for sediment core MD99-2322
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Non-clay and clay mineral composition of sediment core MD99-2236
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Non-clay and clay mineral composition of sediment core MD99-2246
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Non-clay and clay mineral composition of sediment core MD99-2237
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Age determinations on 4 sediment cores off Iceland
The north Icelandic shelf is partly distinguished by the Tjörnes Fracture Zone featuring numerous active basins in a mud-dominated shelf environment. Late Glacial and Holocene... -
Stable isotope ratios of foraminifera, grain-size distribution and magnetic s...
High-resolution grain size and magnetic susceptibility records from the eastern Gulf of Cadiz (site MD99-2339; 1170m water depth) reveal contourites formed by the Mediterranean... -
Ice-rafted debris, geochemistry and stable oxygen isotope record of sediment ...
Sediment proxy records from a continuous, 1.5 million year long deep-sea sediment core from a site in the western Norwegian Sea were used to obtain new insights into the nature... -
Age determination of sediment cores of the Golf of Lions
Siliciclastic turbidites represent huge volumes of sediments, which are of particular significance for (1) petroleum researchers, interested in their potential as oil reservoirs... -
Sea surface reconstruction of sediment cores off West Spitsbergen
Two sediment cores from the West Spitsbergen area, Euro-Arctic margin, MD99-2304 and MD99-2305, have been investigated for paleoceanographic proxies, including benthic and... -
Sedimentology and benthic foraminiferal assemblages of the late Younger Dryas...
A high-resolution study of palaeoenvironmental changes through the late Younger Dryas and early Holocene in the Skagerrak, the eastern North Atlantic, is based on multi-proxy... -
High-resolution marine record of sediment core MD99-2343 in the Balearic Sea
The IMAGES core MD99-2343, recovered from a sediment drift north of the island of Minorca, in the north-western Mediterranean Sea, holds a high-resolution sequence that is... -
Benthic foraminifera, stable isotope record and sedimentology of Holocene sed...
A high-resolution multi-proxy study of core MD99-2286 reveals a highly variable hydrographic environment in the Skagerrak from 9300 cal. yr BP to the present. The study includes... -
Radiocarbon ages, carbon and oxygen isotopes and Mg/Ca and Sr/Ca ratios of Gl...
This study presents high-resolution foraminiferal-based sea surface temperature, sea surface salinity and upper water column stratification reconstructions off Cape Hatteras, a... -
Physical properties of sediment cores from the Labrador Sea
Sediment core logs from six sediment cores in the Labrador Sea show millennial-scale climate variability during the last glacial by recording all Heinrich events and several... -
Ages and geochemical and geophysical characteristics of sediment core MD99-22...
A sediment core from the Lofoten Contourite Drift on the continental slope off Northern Norway, proximal to the former Vestfjorden-Trsnadjupet Ice Stream, details the... -
Age determination and foraminiferal faunas in sediment core MD99-2275
A high-resolution study of palaeoceanographic changes off North Iceland during the time period 8600-5200 cal year BP is based on benthic and planktonic foraminiferal... -
Isotope ratios, IRD and planktonic foraminifera content during marine isotope...
Variable climatic and oceanographic conditions characterized the last interglacial at high northern latitudes, probably related to changes in the strength of the Atlantic... -
Age determination of sediment core MD99-2201
A marine sediment core from the leeward margin of Great Bahama Bank (GBB) was subjected to a multiproxy study. The aragonite dominated core MD992201 comprises the past 7230... -
Holocene Mg/Ca, alkenones, and light stable isotope measurements on the outer...
We present new Holocene century to millennial-scale proxies for the well-dated piston core MD99-2269 from Húnaflóadjúp on the North Iceland Shelf. The core is located in 365 mwd... -
Paleoceanographic data from core MD99-2202
Paleorecords and modeling studies suggest that instabilities in the Atlantic Meridional Overturning Circulation (AMOC) strongly affect the low-latitude climate, namely via...
