Evaluating post-glacial bedrock erosion and surface exposure duration by coupling in situ optically stimulated luminescence and 10Be dating

Assessing the impact of Quaternary glaciation at the Earth's surface implies an understanding of the long-term evolution of alpine landscapes. In particular, it requires simultaneous quantification of the impact of climate variability on past glacier fluctuations and on bedrock erosion. Here we...

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Bibliographic Details
Published in:Earth surface dynamics 2019-01, Vol.7 (3), p.633-662
Main Authors: Lehmann, Benjamin, Herman, Frédéric, Valla, Pierre G, King, Georgina E, Biswas, Rabiul H
Format: Article
Language:English
Subjects:
Alpine environments
Bedrock
Beryllium 10
Chronology
Climate variability
Dating
Duration
Earth
Earth surface
Environmental Sciences
Erosion
Erosion rates
Exposure
Glaciation
Glaciers
Glaciology
Luminescence
Quaternary
Variation
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Summary:Assessing the impact of Quaternary glaciation at the Earth's surface implies an understanding of the long-term evolution of alpine landscapes. In particular, it requires simultaneous quantification of the impact of climate variability on past glacier fluctuations and on bedrock erosion. Here we present a new approach for evaluating post-glacial bedrock surface erosion in mountainous environments by combining terrestrial cosmogenic nuclide 10Be (TCN) and optically stimulated luminescence (OSL) surface exposure dating. Using a numerical approach, we show how it is possible to simultaneously invert bedrock OSL signals and 10Be concentrations into quantitative estimates of post-glacial exposure duration and bedrock surface erosion. By exploiting the fact that OSL and TCN data are integrated over different timescales, this approach can be used to estimate how bedrock erosion rates vary spatially and temporally since glacier retreat in an alpine environment.
ISSN:2196-6311
2196-632X
DOI:10.5194/esurf-7-633-2019