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This study focusses on dose rate determination in complex settings in two drill cores from the site of Niederweningen, northern Switzerland. A crosscheck with a certified standard material and neutron activation analyses (NAA) reveals an overall good performance of high-resolution gamma spectrometry (HR-GS) when determining dose rate-relevant elements. A second focus is on average water content during burial, by comparing measured sediment moisture with water uptake capability. Furthermore, layer models are used to investigate the impact of inhomogeneous stratification on dose rate. Finally, different scenarios to correct for radioactive disequilibrium in the uranium decay chain are investigated. While most of the applied corrections appear to have only a minor to moderate effect on age calculation, the results for one core are contradictory. Possibly, some of the applied correction scenarios are not reflecting the complex natural setting sufficiently, in particular average sediment moisture during burial and the timing of radioactive disequilibrium might be incorrectly estimated. While deposition in one core can be quite securely attributed to the period 100–70 ka, assigning the sediment sequence in the other core to the time between ca. 130 ka and 90 ka remains to some extent insecure.
Wydawca
Czasopismo
Rocznik
Tom
Strony
28--49
Opis fizyczny
Bibliogr. 48 poz., rys.
Twórcy
autor
- Institute of Earth and Environmental Science, University of Freiburg, Albertstraße 23b, 79104 Freiburg, Germany
autor
- ADD Ideas, Zum Erzengel Michael 19, 01723 Mohorn, Germany
autor
- Institute of Earth and Environmental Science, University of Freiburg, Albertstraße 23b, 79104 Freiburg, Germany
autor
- Institute of Earth and Environmental Science, University of Freiburg, Albertstraße 23b, 79104 Freiburg, Germany
- Energy and Sustainability Research Institute Groningen, University of Groningen, Nijenborgh 6, 9747 AG Groningen, The Netherlands
Bibliografia
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- 20. Heiri O, Lotter A and Lemcke G, 2001. Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. Journal of Paleolimnology 25(1): 101–110, DOI 10.1023/A:1008119611481.
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- 24. Juschus O, Preusser F, Melles M and Radtke U, 2007. Applying SAR-IRSL methodology for dating fine-grain sediments from Lake El’gygytgyn, northeastern Siberia. Quaternary Geochronology 2(1–4): 187–194, DOI 10.1016/j.quageo.2006.05.006.
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- 28. Lowick SE and Preusser F, 2009. A method for retrospectively calculating water content for desiccated core samples. Ancient TL 27(1): 9–14. http://ancienttl.org/ATL_27.htm.
- 29. Lukas S, Preusser F, Anselmetti FS and Tinner W, 2012. Testing the potential of luminescence dating of high-alpine lake sediments. Quaternary Geochronology 8: 23–32, DOI 10.1016/j.quageo.2011.11.007.
- 30. Murray AS and Wintle AG, 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32(1): 57–73, DOI 10.1016/S1350-4487(99)00253-X.
- 31. Murray AS, Buylaert JP and Thiel C, 2015. A luminescence dating intercomparison based on a Danish beach-ridge sand. Radiation Measurements 81: 32–38, DOI 10.1016/j.radmeas.2015.02.012.
- 32. Murton JB, 2021. What and where are periglacial landscapes? Permafrost and Periglacial Processes 32(2): 186–212, DOI 10.1002/ppp.2102.
- 33. Nathan R and Mauz B, 2008. On the dose-rate estimate of carbonate-rich sediments for trapped charge dating. Radiation Measurements 81(1): 14–25, DOI 10.1016/j.radmeas.2007.12.012.
- 34. Nelson MS and Rittenour TM, 2015. Using grain-size characteristics to model soil water content: Application to dose-rate calculation for luminescence dating. Radiation Measurements 81: 142–149, DOI 10.1016/j.radmeas.2015.02.016.
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- 38. Prescott JR and Hutton JT, 1994. Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations. Radiation Measurements 23(2–3): 497–500, DOI 10.1016/1350-4487(94)90086-8.
- 39. Prescott JR and Hutton JT, 1995. Environmental dose rates and radioactive disequilibrium from some Australian dating sites. Quaternary Science Reviews 14(4): 439–448, DOI 10.1016/0277-3791(95)00037-2.
- 40. Preusser F, 2004. Towards a chronology of the Late Pleistocene in the northern Alpine Foreland. Boreas 33(3): 195–210, DOI 10.1111/j.1502-3885.2004.tb01141.x.
- 41. Preusser F and Degering D, 2007. Luminescence dating of the Niederweningen mammoth site, Switzerland. Quaternary International 164/165: 106–112, DOI 10.1016/j.quaint.2006.12.002.
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- 43. Rittenour TM, 2018. Dates and rates of earth-surface processes revealed using luminescence dating. Elements 14(1): 21–26, DOI 10.2138/gselements.14.1.21.
- 44. Smedley RK and Pearce NJG, 2016. Internal U, Th and Rb concentrations of alkali-feldspar grains: Implications for luminescence dating. Quaternary Geochronology 35: 16–25, DOI 10.1016/j.quageo.2016.05.002.
- 45. Welten M 1988. Neue pollenanalytische Ergebnisse über das Jüngere Quartär des nördlichen Alpenvorlandes der Schweiz (Mittel- und Jungpleistozän). Beiträge zur geologischen Karte der Schweiz – Neue Folge: 162, 40 pp.
- 46. Wintle AG and Murray AS, 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41: 369–391, DOI 10.1016/j.radmeas.2005.11.001.
- 47. Zander A, Degering D, Preusser F, Kasper HU and Brückner H, 2007. Optically stimulated luminescence dating of sublittoral and intertidal sediments from Dubai, UAE.: Radioactive disequilibria in the uranium decay series. Quaternary Geochronology 2(1–4): 123–128, DOI 10.1016/j.quageo.2006.04.003.
- 48. Zimmerman DW, 1971. Thermoluminescent dating using fine grains from pottery. Archaeometry 13(1): 29–52, DOI 10.1111/j.1475-4754.1971.tb00028.x.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-717c686a-511a-44b3-b75e-b93b537b4dee