Articles | Volume 18, issue 8
https://doi.org/10.5194/cp-18-1867-2022
https://doi.org/10.5194/cp-18-1867-2022
Research article
 | 
16 Aug 2022
Research article |  | 16 Aug 2022

Heavy mineral assemblages of the De Long Trough and southern Lomonosov Ridge glacigenic deposits: implications for the East Siberian Ice Sheet extent

Raisa Alatarvas, Matt O'Regan, and Kari Strand

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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-2021-111', Ruediger Stein, 13 Oct 2021
    • AC1: 'Reply on RC1', Raisa Alatarvas, 05 Jan 2022
  • RC2: 'Comment on cp-2021-111', Leonid Polyak, 09 Dec 2021
    • AC2: 'Reply on RC2', Raisa Alatarvas, 05 Jan 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (07 Jan 2022) by Denis-Didier Rousseau
AR by Raisa Alatarvas on behalf of the Authors (11 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (25 Mar 2022) by Denis-Didier Rousseau
RR by Ruediger Stein (20 Apr 2022)
ED: Publish as is (05 Jul 2022) by Denis-Didier Rousseau
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Short summary
This research contributes to efforts solving research questions related to the history of ice sheet decay in the Northern Hemisphere. The East Siberian continental margin sediments provide ideal material for identifying the mineralogical signature of ice sheet derived material. Heavy mineral analysis from marine glacial sediments from the De Long Trough and Lomonosov Ridge was used in interpreting the activity of the East Siberian Ice Sheet in the Arctic region.