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  Synchronizing 10Be in two varved lake sediment records to IntCal13 14C during three grand solar minima

Czymzik, M., Muscheler, R., Adolphi, F., Mekhaldi, F., Dräger, N., Ott, F., et al. (2018). Synchronizing 10Be in two varved lake sediment records to IntCal13 14C during three grand solar minima. Climate of the past, 14(5), 687-696. doi:10.5194/cp-14-687-2018.

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 Creators:
Czymzik, Markus, Author
Muscheler, Raimund, Author
Adolphi, Florian, Author
Mekhaldi, Florian, Author
Dräger, Nadine, Author
Ott, Florian1, Author              
Słowinski, Michał, Author
Błaszkiewicz, Mirosław, Author
Aldahan, Ala, Author
Possnert, Göran, Author
Brauer, Achim, Author
Affiliations:
1Archaeology, Max Planck Institute for the Science of Human History, Max Planck Society, ou_2074312              

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 Abstract: Timescale uncertainties between paleoclimate reconstructions often inhibit studying the exact timing, spatial expression and driving mechanisms of climate variations. Detecting and aligning the globally common cosmogenic radionuclide production signal via a curve fitting method provides a tool for the quasi-continuous synchronization of paleoclimate archives. In this study, we apply this approach to synchronize 10Be records from varved sediments of Tiefer See and Lake Czechowskie covering the Maunder, Homeric and 5500aBP grand solar minima with 14C production rates inferred from the IntCal13 calibration curve. Our analyses indicate best fits with 14C production rates when the 10Be records from Tiefer See were shifted for 8 (−12∕ + 4) (Maunder Minimum), 31 (−16∕ + 12) (Homeric Minimum) and 86 (−22∕ + 18) years (5500aBP grand solar minimum) towards the past. The best fit between the Lake Czechowskie 10Be record for the 5500aBP grand solar minimum and 14C production was obtained when the 10Be time series was shifted 29 (−8∕ + 7) years towards present. No significant fits were detected between the Lake Czechowskie 10Be records for the Maunder and Homeric minima and 14C production, likely due to intensified in-lake sediment resuspension since about 2800aBP, transporting "old" 10Be to the coring location. Our results provide a proof of concept for facilitating 10Be in varved lake sediments as a novel synchronization tool required for investigating leads and lags of proxy responses to climate variability. However, they also point to some limitations of 10Be in these archives, mainly connected to in-lake sediment resuspension processes.

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Language(s): eng - English
 Dates: 2018-05-312018-05
 Publication Status: Published in print
 Pages: 10
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.5194/cp-14-687-2018
Other: shh1199
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Title: Climate of the past
  Abbreviation : Clim. Past
Source Genre: Journal
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Publ. Info: Katlenburg-Lindau : Copernicus Ges.
Pages: - Volume / Issue: 14 (5) Sequence Number: - Start / End Page: 687 - 696 Identifier: ISSN: 1814-9332
CoNE: https://pure.mpg.de/cone/journals/resource/1814-9332