EGU21-7314
https://doi.org/10.5194/egusphere-egu21-7314
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

The First Holocene Varve Chronology for the UK: based on the integration of varve counting, radiocarbon dating and tephrostratigraphy from Diss Mere (UK).

Celia Martin-Puertas1, Amy A. Walsh1, Simon P.E Blockley1, Poppy Harding1, George E. Biddulph2, Palmer Adrian1, Ramisch Arne3, and Brauer Achim3,4
Celia Martin-Puertas et al.
  • 1Royal Holloway University of London, n/a, Geography, Egham, UK (celia.martinpuertas@rhul.ac.uk)
  • 2School of Geography and Sustainable Development, University of St Andrews, St. Andrews, UK (g.biddulph@hotmail.co.uk)
  • 3Climate Dynamics and Landscape Evolution, GFZ German Centre for Geosciences, Potsdam, Germany (aramisch@gfz-potsdam.de)
  • 4Institute of Geosciences, University of Potsdam, Potsdam, Germany (brau@gfz-potsdam.de)

This paper reports the first Holocene varved chronology for the lacustrine sediment record of Diss Mere in the UK. The record of Diss Mere is 15 m long, and shows 4.2 m of finely-laminated sediments, which are present between ca. 9 and 13 m of core depth. The microfacies analysis identified three major seasonal patterns of deposition, which corroborate the annual nature of sedimentation throughout the whole interval. The sediments are diatomaceous organic and carbonate varves with an average thickness of 0.45 mm. A total of 8473 varves were counted with maximum counting error of up to  40 varves by the bottom of the varved sequence. To tie the resulting floating varve chronology to the IntCal 2020 radiocarbon timescale, we used a Bayesian Deposition model (P_Sequencewith outlier detection) on all available chronological data from the core. The data included five radiocarbon dates, two known tephra layers (Glen Garry and OMH-185) with calendar ages based on Bayesian modelling of sequences of radiocarbon ages, and the relative varve counts between dated points. The resulting age-depth model (DISSV-2020) dates the varved sequence between ca. 2100 and 10,300 cal BP and age uncertainties are decadal in scale (95% confidence). 

How to cite: Martin-Puertas, C., Walsh, A. A., Blockley, S. P. E., Harding, P., Biddulph, G. E., Adrian, P., Arne, R., and Achim, B.: The First Holocene Varve Chronology for the UK: based on the integration of varve counting, radiocarbon dating and tephrostratigraphy from Diss Mere (UK)., EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-7314, https://doi.org/10.5194/egusphere-egu21-7314, 2021.