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(Table 1) Stable isotope ratios of foraminifera in sediment core CH82-20
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Stable isotopes on foraminifera from sediment core HU72-021-3
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Ice rafted debris and sortable silt from sediment core MD99-2323
Weight (> 2 mm) and volume % of coarse sand fractions of laser-sized Malvern grain-size data and calculated % of the sortable silt fraction (10-63 µm) and the average size of... -
Interaction between warm Atlantic-sourced waters and the East Greenland Curre...
Changes in the Holocene interaction of the (i) cold/fresh East Greenland Current (EGC) and (ii) warm/saline Irminger Current (IC) in northern Denmark Strait have been... -
Occurrence of IRD in ODP Hole 151-909C
The Arctic cryosphere is changing and making significant contributions to 21st century sea level rise. The Pliocene epoch had similar CO2 levels to present and a warming... -
Stable isotope records, IRM, ARM, and relative abundance of planktic foramini...
The percentage of the formainifere is related to the total abundace of planktonic foraminifera -
Dinocyst-derived sea-surface characteristics, palynomorph abundances, ice-raf...
The last glacial millennial climatic events (i.e. Dansgaard-Oeschger and Heinrich events) constitute outstanding case studies of coupled atmosphere-ocean-cryosphere... -
Ice rafted debris content of sediment core MD99-2303
For method on "AGE" see Risebrobakken et al., 2005. For method on "Age model" see Risebrobakken et al., 2006 -
Occurrence of planktic foraminifera in Pliocene to Holocene sediments of DSDP...
A new planktic foraminifer transfer function (GSF18) related 5 North Atlantic assemblages to winter and summer sea surface temperature. GSF18, based on recombined and simplified... -
Sedimentology and stable isotopes of core OD96_9:11:1
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Sedimentology and stable isotopes of core OD96_31:3:1
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Sedimentology and stable isotopes of core OD96_10:4:1
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(Fig. 1) Ice rafted debris and planktic foraminifers of Hole 94-609
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