10.1594/PANGAEA.973035Lauer, TobiasTobiasLauerUniversity of TübingenZvara, EmaEmaZvara0009-0002-3762-4127Universität LeipzigPejdanović, SnježanaSnježanaPejdanovićUniversity of TübingenKühn, PeterPeterKühn0000-0002-4417-5633University of TübingenZielhofer, ChristophChristophZielhofer0000-0001-9551-4466Universität LeipzigFitzsimmons, Kathryn EKathryn EFitzsimmons0000-0002-9337-0793University of TübingenPANGAEA2025Eger floodplainEger Riverfloodplain depositsGeochronologyluminescence datingNördlingenoverbank silt-clay depositionSouthern GermanyEvent labelLatitude of eventLongitude of eventSample code/labelLaboratory code/labelDEPTH, soilUraniumUranium, errorThoriumThorium, errorPotassiumPotassium, errorDose rate, soil, totalDose rate, soil, total, errorEquivalent doseEquivalent dose, errorAge, datedAge, dated, errorHand-dug soil profileMeasuredCalculatedRadiation Instruments, DTU Physics, Risø TL/OSL-DA-20Nördlingen_NEP_20232023-04-03T09:00:00/2023-04-03T16:00:00Dataset10.1594/PANGAEA.972856110 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalWe established a luminescence based chronology by dating 7 samples collected from profiles NEP 1 and NEP 3. The methods allows to determine the last sunlight exposure of sediment grains (commonly quartz and feldspar). All measurements were conducted in the luminescence laboratory within the Geo-and Environmental research center in Tübingen. We used a so called pIR150 protocol on polyminerals. The results point to various periods of deposition between approximately 1-8 ka.10.51150510.51265348.86717348.868228Nördlingen, Bavaria, Southern GermanyDeutsche Forschungsgemeinschaft, Bonnhttps://doi.org/10.13039/501100001659460849764SPP 2361: On the Way to the Fluvial AnthroposphereDeutsche Forschungsgemeinschaft, Bonnhttps://doi.org/10.13039/501100001659509893043Local pathways to the Fluvial Anthroposphere at Echaz (Rhine) and Eger (Danube). A comparative analysis from c. AD 1100 to 1800