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(Figure 4) Stable carbon isotopic records of sediment core GeoB6212-1
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(Figure 3) Age model and sedimentation rates for marine sediment core GeoB6212-1
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(Table 1) Accelerator mass spectrometer radiocarbon dates and calibrated ages...
Poz: Poznan Radiocarbon Laboratory, Poznan, Poland.** Beta Analytic Radiocarbon Dating Laboratory, Miami, USA.All radiocarbon ages were calibrated with the calibration curve... -
Age model, sedimentation rates and stable carbon isotopic rates of sediment c...
Abrupt millennial-scale climate change events of the last deglaciation (i.e. Heinrich Stadial 1 and the Younger Dryas) were accompanied by marked increases in atmospheric CO2... -
(Table S4c) Age control points used for calculation of sedimentation rates of...
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(Table S3b) 14C ages measured on Globigerinoides sacculifer of sediment core ...
Jaeschke et al.. 2007; 14C ages from GeoB 3910-2. depths are correlated based on tuned Ti/Ca ratios (see Table S2).14C ages, 14C plateaus, and age conversion into calendar ages... -
(Table S3a) 14C ages measured on Globigerina bulloides of sediment core GeoB1...
*KIA 555: conventional 14C age from Littlel et al. (1997); #KIA4109 and #KIA 4110: conventional 14C age from Vidal et al. (1999).14C ages, 14C plateaus, and age conversion into... -
(Table S1 b) Definition of planktic 14C plateaus for sediment core GeoB3910-1
Very low sedimentation rates below Plateau 3 suggest hiatus. -
(Table S1 a) Definition of planktic 14C plateaus for sediment core GeoB1711-4
Plateau No. 1 - 3: By comparison with Suigetsu Plateau 3 the short length of Plateau 3 may be explained by a ~200-yr drop in local 14C reservoir age over Plateau 3. Its actual... -
Compiled mass accumulation rates (MAR) of the n-alkanes-Biomarker data (Table 3)
Depth = composite depth / HPA-Index, Higher Plant Alkanes Index (n-alkanes with carbon number C23,C25,...,C33; n-alkanols with carbon number C22,C24,..,C32) -
Processed stable isotope (carbon and oxygen) data from epibenthic Cibicidoide...
To investigate deep ocean heat uptake variability, we measured Mg/Ca ratios of Uvigerina spp. on samples from site GeoB9508-5 off NW Africa. Bottom water temperatures (BWT) were... -
Bottom water temperatures (raw and processed including confidence intervals) ...
To investigate deep ocean heat uptake variability, we measured Mg/Ca ratios of Uvigerina spp. on samples from site GeoB9508-5 off NW Africa. Bottom water temperatures (BWT) were... -
Color measurements on sediment core GeoB10070-5
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Color measurements on sediment core GeoB10069-3
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Color measurements on sediment core GeoB10069-1
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Color measurements on sediment core GeoB10068-2
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Color measurements on sediment core GeoB10067-6
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Color measurements on sediment core GeoB10066-7
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Color measurements on sediment core GeoB10065-7
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Color measurements on sediment core GeoB10065-5
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