Articles | Volume 4, issue 1
https://doi.org/10.5194/gchron-4-297-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gchron-4-297-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Luminescence age calculation through Bayesian convolution of equivalent dose and dose-rate distributions: the De_Dr model
Norbert Mercier
CORRESPONDING AUTHOR
Archéosciences Bordeaux, UMR 6034 CNRS – Université
Bordeaux Montaigne, Esplanade des Antilles, 33600 Pessac, France
Jean-Michel Galharret
Laboratoire de Mathématiques Jean Leray, UMR 6629 CNRS – Nantes Université, 44000 Nantes, France
Chantal Tribolo
Archéosciences Bordeaux, UMR 6034 CNRS – Université
Bordeaux Montaigne, Esplanade des Antilles, 33600 Pessac, France
Sebastian Kreutzer
Geography & Earth Sciences, Aberystwyth University, Llandinam
Building, Penglais Campus, Aberystwyth, SY23 3DB, Wales, UK
Archéosciences Bordeaux, UMR 6034 CNRS – Université
Bordeaux Montaigne, Esplanade des Antilles, 33600 Pessac, France
Anne Philippe
Laboratoire de Mathématiques Jean Leray, UMR 6629 CNRS – Nantes Université, 44000 Nantes, France
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We present results of the Baix loess–palaeosol sequence, SE France. Reconstructed intense soil formation under warm, moist conditions before and into the last ice age and less intense soil formations in warm (temporarily moist) phases during the generally cold, dry ice age were validated with laboratory and dating techniques. This is particularly relevant as Baix is located in the temperate–Mediterranean climate transition zone, a sensitive zone that is susceptible to future climate changes.
Mathieu Bosq, Sebastian Kreutzer, Pascal Bertran, Philippe Lanos, Philippe Dufresne, and Christoph Schmidt
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During the last glacial period, cold conditions associated with changes in atmospheric circulation resulted in the deposition of widespread loess. It seems that the phases of loess accumulation were not strictly synchronous. To test this hypothesis, the chronology of loess deposition in different regions of Europe was studied by recalculating 1423 luminescence ages in a database. Our study discusses the link between the main loess sedimentation phases and the maximal advance of glaciers.
Sebastian Kreutzer, Steve Grehl, Michael Höhne, Oliver Simmank, Kay Dornich, Grzegorz Adamiec, Christoph Burow, Helen M. Roberts, and Geoff A. T. Duller
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The concept of open data has become the modern science meme. Funding bodies and publishers support open data. However, the open data mandate frequently encounters technical obstacles, such as a lack of a suitable data format for data sharing and long-term data preservation. Such issues are often community-specific and demand community-tailored solutions. We propose a new human-readable data format for data exchange and long-term preservation of luminescence data called XLUM.
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This paper demonstrates how to model optically stimulated luminescence (OSL) and radiocarbon ages in a Bayesian framework, using a dedicated software tool called BayLum. We show the effect of stratigraphic constraints, of modelling the covariance of ages when the same equipment is used for a series of OSL samples, and of including independent ages on a chronological inference. The improvement in chronological resolution is significant.
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Short summary
Dosimetric dating methods based on the analysis of luminescence signals emitted by granular minerals extracted from sedimentary deposits now play an important role in the study of the Quaternary. Here we propose a new approach in which the age of the deposit is calculated by combining the equivalent dose and dose-rate distributions. The underlying Bayesian mathematical model and its implementation via an R code are provided, together with the results obtained for a finite set of configurations.
Dosimetric dating methods based on the analysis of luminescence signals emitted by granular...