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Late Glacial/early Holocene benthic foraminifera assemblages, stable isotopes...
Lateglacial/early Holocene interval from the sediment core JM09-020GC recovered in Storfjordrenna (western Barents Sea) has been studied for benthic foraminifera assemblages,... -
Surface water properties and sea ice distribution proxies from sediment core ...
A marine sediment core (JM09-KA11-GC) from the Kveithola Trough at the western Barents Sea margin has been investigated in order to reconstruct sub-surface temperatures and sea... -
Element analysis of sediment core JM09-020GC
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Vivianit content of sediment core JM09-020GC
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Stable oxygen isotope record of sediment core JM09-020GC
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Magnetic susceptibility of sediment core JM09-020GC
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IRD flux of sediment core JM09-020GC
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Relative abundances of benthic foraminifera in sediment core JM09-020GC
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Benthic foraminifera counts of sediment core JM09-020GC
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Isotopes for sediment core JM09-KA11-GC
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Fragmentation for sediment core JM09-KA11-GC
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Shell weight measured for sediment core JM09-KA11-GC
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Subsurface temperature calculated for sediment core JM09-KA11-GC
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Sedimentation rate of sediment core JM09-KA11-GC
Age Model: Based on 8 AMC C14 dates. Linear interpolation between the dated levels. -
14C ages of sediment core JM09-KA11-GC
6 AMS C14 dates from D. Ruther et al (2012).Based on existing data from Near Bear Island (Mangerud and Gulliksen,1975) -
Biomarkers of sediment core JM09-KA11-GC
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Planktonic foraminifera of sediment core JM09-KA11-GC
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Organic biomarkers and derived sea ice concentrations in sediment core JM09-K...
This dataset has no description
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(Table 3) Accelerator mass spectrometry (AMS) radiocarbon dates and calibrate...
°From Rebesco et al. (2016a).*From Rüther et al. (2012).a Radiocarbon laboratory: Poz = Poznan Radiocarbon Laboratory (Poland); TRa = Angström Laboratory Uppsala (Norway).b... -
(Table 3) Radiocarbon dates of sediment cores obtained during a 2009 Jan Maye...
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