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(Table 5) Stable oxygen isotope and Mg/Ca ratios of foraminifera from surface...
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(Table 9) Alkenone and Mg/Ca derived SST of surface sediments
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(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... -
(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... -
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. -
(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. -
X-ray diffraction analysis of sediment samples from the NW Iberian shelf system
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Binocular component analysis performed on the grain-size fraction 250–500 µm ...
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Radiocarbon ages of sediment core GeoB11033-1
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TOC, Norg and CaCO3 content of sediment core GeoB11033-1
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Age model of sediment core GeoB11033-1
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(Table 9) Stable oxygen isotope derived SST of surface sediments
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Planktonic foraminiferaof surface sediments
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Controls of sediment dynamics on the Galician slope reconstructed from three ...
Controls of sediment dynamics at the Galician continental slope (NW Iberia) during the past 30 ka were reconstructed from three new gravity cores (GeoB11035-1, 130206-1,... -
(Fig. 3) Inter-core correlation of Ca/Fe ratios and magnetic susceptibility s...
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