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(Table 9) Stable oxygen isotope derived SST of surface sediments
This dataset has no description
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(Table 9) Alkenone and Mg/Ca derived SST of surface sediments
This dataset has no description
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(Table 5) Stable oxygen isotope and Mg/Ca ratios of foraminifera from surface...
This dataset has no description
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Coccolith species abundances in sediment core GeoB11035-1 from the NW Iberian...
Coccolithophore assemblage data from sediment core GeoB11035-1 from the NW Iberian continental margin for the past 55 ka. The assemblage data were used to assess changes in... -
Planktonic foraminiferaof surface sediments
This dataset has no description
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(Fig. 7) Coccolith species abundance of sediment core GeoB11035-1
This dataset has no description
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Downcore Florisphaera profunda
This dataset has no description
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(Table 2) Radiocarbon measurements and age calibration
Continental shelves represent areas of highest economical and ecological importance. Nevertheless, these sedimentary systems remain poorly understood due to a complex interplay... -
Apsorption units at wavenumbers of several samples
This dataset has no description
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Mineral content of several samples
This dataset has no description
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(Fig. 3) Inter-core correlation of Ca/Fe ratios and magnetic susceptibility s...
This dataset has no description
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(Table 4) Vegetation and soil ratios in all analyzed surface sediments from t...
Surface sediment samples were sampled from a depth interval of 0-2 cm. -
(Table 3) Concentrations of lipid biomarkers and lignin-derived phenols in al...
Surface sediment samples were sampled from a depth interval of 0-2 cm. -
(Table 1) Age model tie points of sediment cores GeoB11035-1, GeoB13071-1, an...
14C age at base of GeoB11035-1 (asterisk) is not considered because beyond radiocarbon limits. a Correlation with d18O record of GISPII. b Leibniz Laboratory, Kiel, Germany. c... -
(Table 2) Radiocarbon dates and age calibration
°1From Lantzsch et al. (2009a,b).*Age calibrationisbasedonthefunctionof Bard etal.(1998).Radiocarbon laboratory: KIA=Leibniz Laboratory in Kiel (Germany) and Poz=Poznan'... -
(Table 2) Radiocarbon dates and age calibration
The high-energy, low-accumulation NW Iberian shelf features three confined Holocene mud depocentres. Here, we show that the evolution of such depocentres follows successive... -
Sources, transport, and partitioning of organic matter from 40 surface sedime...
Continental shelves play a major role as transition zone during transport of multiply-sourced organic matter into the deep sea. In order to obtain a comprehensive understanding... -
X-ray diffraction analysis, binocular component analysis and radiocarbon dati...
Based on a well-established stratigraphic framework and 47 AMS-14C dated sediment cores, the distribution of facies types on the NW Iberian margin is analysed in response to the... -
(Table S1) Diatom abundance in coastal upwelling systems
Coastal upwelling systems account for approximately half of global ocean primary production and contribute disproportionately to biologically driven carbon sequestration.... -
(Table 1) Location and bulk properties of samples from the NW Iberian margin ...
Surface sediment samples were sampled from a depth interval of 0-2 cm.
