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Grain-size analysis obtained from sediment core RD04 (island of Sylt)
Core RD04 originates from a natural back-barrier marsh (island of Sylt). The marsh in Sylt is a low-energy, back-barrier marsh. Grain-size data were used to determine and... -
Radionuclide measurements (210Pb, 137Cs, 226Ra) obtained from sediment core B...
Sediment cores BT02 origins from a reinstated, former managed marsh (Eiderstedt peninsula). Data include radionuclide activity of 137Cs, 210Pb and 226Ra. Measurements of the... -
Grain-size analysis obtained from sediment core BT02 (Eiderstedt peninsula; s...
Core BT02 originates from a reinstated, former managed marsh (Eiderstedt peninsula). The marsh in Eiderstedt is exposed to storm waves from the open North Sea. Grain-size data... -
Radionuclide measurements (210Pb, 137Cs, 226Ra) obtained from sediment core B...
Sediment cores BT03 origins from a reinstated, former managed marsh (Eiderstedt peninsula). Data include radionuclide activity of 137Cs, 210Pb and 226Ra. Measurements of the... -
Grain-size analysis obtained from sediment core BT03 (Eiderstedt peninsula; s...
Core BT03 originates from a reinstated, former managed marsh (Eiderstedt peninsula). The marsh in Eiderstedt is exposed to storm waves from the open North Sea. Grain-size data... -
Radionuclide measurements (210Pb, 137Cs, 226Ra) obtained from sediment core R...
Core RD04 originates from a natural back-barrier marsh (island of Sylt). Data include radionuclide activity of 137Cs, 210Pb and 226Ra. Measurements of the radionuclides were... -
Grainsize analysis and radionuclide measurements (210Pb, 137Cs, 226Ra) obtain...
Three sediment cores were retrieved from marshes at the southern North Sea coast, recovering the past 100 years. Core RD04 originates from a natural back-barrier marsh (island...