Articles | Volume 18, issue 1
Clim. Past, 18, 103–127, 2022
https://doi.org/10.5194/cp-18-103-2022
Clim. Past, 18, 103–127, 2022
https://doi.org/10.5194/cp-18-103-2022

Research article 20 Jan 2022

Research article | 20 Jan 2022

Holocene palaeoceanography of the Northeast Greenland shelf

Teodora Pados-Dibattista 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 cp-2021-59', Anonymous Referee #1, 05 Jul 2021
    • AC1: 'Reply on RC1', Teodora Pados-Dibattista, 29 Oct 2021
  • RC2: 'Comment on cp-2021-59', Anonymous Referee #2, 11 Jul 2021
    • AC2: 'Reply on RC2', Teodora Pados-Dibattista, 29 Oct 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (11 Nov 2021) by Bjørg Risebrobakken
AR by Teodora Pados-Dibattista on behalf of the Authors (18 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (24 Nov 2021) by Bjørg Risebrobakken
AR by Teodora Pados-Dibattista on behalf of the Authors (02 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (02 Dec 2021) by Bjørg Risebrobakken
AR by Teodora Pados-Dibattista on behalf of the Authors (03 Dec 2021)  Author's response    Manuscript
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Short summary
We carried out foraminiferal, stable isotope, and sedimentological analyses of a marine sediment core retrieved from the Northeast Greenland shelf. This region is highly sensitive to climate variability because it is swept by the East Greenland Current, which is the main pathway for sea ice and cold waters that exit the Arctic Ocean. The palaeoceanographic reconstruction reveals significant variations in the water masses and in the strength of the East Greenland Current over the last 9400 years.