Articles | Volume 14, issue 5
https://doi.org/10.5194/bg-14-1261-2017
https://doi.org/10.5194/bg-14-1261-2017
Research article
 | 
15 Mar 2017
Research article |  | 15 Mar 2017

Yedoma Ice Complex of the Buor Khaya Peninsula (southern Laptev Sea)

Lutz Schirrmeister, Georg Schwamborn, Pier Paul Overduin, Jens Strauss, Margret C. Fuchs, Mikhail Grigoriev, Irina Yakshina, Janet Rethemeyer, Elisabeth Dietze, and Sebastian Wetterich

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (06 Dec 2016) by Alexey V. Eliseev
AR by Lutz Schirrmeister on behalf of the Authors (16 Jan 2017)
ED: Reconsider after major revisions (17 Jan 2017) by Alexey V. Eliseev
AR by Lutz Schirrmeister on behalf of the Authors (19 Jan 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (19 Jan 2017) by Alexey V. Eliseev
RR by Anonymous Referee #2 (19 Feb 2017)
ED: Publish subject to minor revisions (Editor review) (19 Feb 2017) by Alexey V. Eliseev
AR by Lutz Schirrmeister on behalf of the Authors (24 Feb 2017)
ED: Publish as is (28 Feb 2017) by Alexey V. Eliseev
AR by Lutz Schirrmeister on behalf of the Authors (01 Mar 2017)
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Short summary
We investigate late Pleistocene permafrost at the Buor Khaya Peninsula (Laptev Sea, Siberia) for cryolithological, geochemical, and geochronological parameters. The sequences were composed of ice-oversaturated silts and fine-grained sands with 0.2 to 24 wt% of organic matter. The deposition was between 54.1 and 9.7 kyr BP. Due to coastal erosion, the biogeochemical signature of the deposits represents the terrestrial end-member, and is related to organic matter deposited in the marine realm.
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