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X-ray fluorescence (XRF) scanning data of sediment core EN21103 from Lake Ulu...
X-ray fluorescence (XRF) scanning data, scanned with an AvaaTech XRF core scanner at AWI in Potsdam. All elements were measured at X-ray voltages of 10 kV and 30 kV and currents... -
Stable carbon isotopes of organic matter of sediment core EN21103 from Lake U...
Stable carbon isotopes of organic matter (d13C), measured with a Delta V Advantage Mass Spectrometer at the ISOLAB Facility of AWI in Potsdam. All isotopic values are reported... -
Element composition of sediment core EN21103 from Lake Ulu, eastern Siberia
Element composition including total carbon (TC), total organic carbon (TOC), total inorganic carbon (TIC), and total nitrogen (TN), measured with a soli TOC cube (Elementar) and... -
Bacon age-depth model of sediment core EN21103 from Lake Ulu, eastern Siberia
This model was established based on the Bayesian method with a hiatus at 138 cm and calibrated using the IntCal20 dataset via the Bacon function in the R-package rbacon. A... -
Radiocarbon dating of sediment core EN21103 from Lake Ulu, eastern Siberia
Radiocarbon dating performed on the total organic carbon content of 40 bulk sediments, measured at the MICADAS (Mini Carbon Dating System) Laboratory of AWI in Bremerhaven. -
Geochemistry of sediment core EN21103 from Lake Ulu, eastern Siberia
Here are the bundled geochemical data of an 11-m-long sediment core EN21103 collected from Lake Ulu (63.34°N, 141.05°E) in the Oymyakon region (eastern Siberia) during the...