Articles | Volume 18, issue 16
Biogeosciences, 18, 4791–4816, 2021
https://doi.org/10.5194/bg-18-4791-2021
Biogeosciences, 18, 4791–4816, 2021
https://doi.org/10.5194/bg-18-4791-2021

Research article 24 Aug 2021

Research article | 24 Aug 2021

Sediment and carbon accumulation in a glacial lake in Chukotka (Arctic Siberia) during the Late Pleistocene and Holocene: combining hydroacoustic profiling and down-core analyses

Stuart A. Vyse et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on bg-2021-39', Anonymous Referee #1, 26 Mar 2021
    • AC2: 'Reply on RC1', Stuart Vyse, 30 May 2021
  • RC2: 'Comment on bg-2021-39', Daniel Nyvlt, 13 Apr 2021
    • AC1: 'Reply on RC2', Stuart Vyse, 30 May 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (31 May 2021) by Petr Kuneš
AR by Stuart Vyse on behalf of the Authors (02 Jul 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (02 Jul 2021) by Petr Kuneš
RR by Daniel Nyvlt (07 Jul 2021)
ED: Publish subject to technical corrections (08 Jul 2021) by Petr Kuneš
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Short summary
Lakes act as important stores of organic carbon and inorganic sediment material. This study provides a first investigation into carbon and sediment accumulation and storage within an Arctic glacial lake from Far East Russia. It shows that major shifts are related to palaeoclimate variation that affects the development of the lake and its surrounding catchment. Spatial differences to other lake systems from other regions may reflect variability in processes controlled by latitude and altitude.
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