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(Table S1) Chronology of sediment core GeoB10065-9, sedimentation and accumul...
DBD: Calculated: Polynomial extrapolation from a parallel gravity core GeoB 10065-7, assuming 20 cm was lost during sampling at the top of the gravity core. -
(Table 1) Slope, accumulation rates and annual Cl-/Na+ values of sampling sit...
This dataset has no description
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(Table 1b) 210Pb chronology of bulk sediment samples from core JM05-G001 duri...
Accumulation rate was originally given in kg/m²/a and was recalculated to g/cm²/a by dividing by 10. -
(Table 1) 210Pb dates and sedimentation and accumulation rates from sediment ...
This dataset has no description
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(Table 1) 210Pb dates from sediment core JM99-1197/BC obtained during Jan May...
SECTION, height is slice depth. -
(Table 5) Element composition of snow samples from the New Byrd transect, Ant...
This dataset has no description
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(Table 3) Element composition of snow samples from the Dumont d'Urville-Dome ...
This dataset has no description
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(Table C1) 210Pb concentrations and age model of Baltic sea sediments
All sediment parameters corrected for salt dilution. Assumed background values: LF1 = 15.5 Bq/kg, LF1.5 = 16.0 Bq/kg, LF3 = 27.0 Bq/kg. -
(Table 2) Physical parameters of bottom sediments from the Laptev Sea
This dataset has no description
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Gamma emitting radionuclides and age model of sediment core SIS11-3 from Silb...
The chronology of the top part of the core SIS11-3 is based on excess 210Pb and anthropogenic gamma emitting radionuclides. The analyses of samples down to 66 cm depth were... -
(Table 1) Distribution of 210Pb in the surface layer of shelf sediments near ...
A constant concentration model was used in conjunction with the nonequilibrium 210Pb method in determining mean sedimentation rates of bottom sediments sampled during Cruise 20... -
Porosity and accumulation rates of sediments of lake Rotsee, Switzerland
This dataset has no description
