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(Table S4) Mineral composition of sediment core JM96-1210
This dataset has no description
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Principal component scores on XRD logratio mineralogy of sediment core JM07-W...
This dataset has no description
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XRD mineralogy of sediment core JM07-WP-174-GC
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
Age determination of sediment core JM07-WP-174-GC
This dataset has no description
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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... -
(Tab S3) Age determination of sediment core JM11-FI-19PC
Conventional and calibrated radiocarbon dates of core JM11-FI-19PC. Ages were first converted to calendar years before present (1950) using the CALIB Radiocarbon Calibration... -
(Table 1) Age determination of sediment profile JM96-1225, supplement to: Hag...
The paleoceanography in the Denmark Strait, North Atlantic, is reconstructed based on down core analysis of planktonic foraminifera, carbon and oxygen isotopes, carbonate, and... -
Fluxes of trap JM9_DRIFT1
This dataset has no description
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Fluxes of trap JM7_DRIFT1
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Fluxes of trap JM6_DRIFT1
This dataset has no description
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Fluxes of trap JM5_DRIFT1
This dataset has no description
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Fluxes of trap JM4_DRIFT1
This dataset has no description
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Fluxes of trap JM3_DRIFT1
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Fluxes of trap JM2_DRIFT1
This dataset has no description
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Fluxes of trap JM11_DRIFT1
This dataset has no description
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Fluxes of trap JM10_DRIFT2
This dataset has no description
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Fluxes of trap JM10_DRIFT1
This dataset has no description
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Particle flux of drift station JM9-1
This dataset has no description
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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...