Articles | Volume 13, issue 4
https://doi.org/10.5194/bg-13-1179-2016
https://doi.org/10.5194/bg-13-1179-2016
Research article
 | 
26 Feb 2016
Research article |  | 26 Feb 2016

Sedimentological processes and environmental variability at Lake Ohrid (Macedonia, Albania) between 637 ka and the present

Alexander Francke, Bernd Wagner, Janna Just, Niklas Leicher, Raphael Gromig, Henrike Baumgarten, Hendrik Vogel, Jack H. Lacey, Laura Sadori, Thomas Wonik, Melanie J. Leng, Giovanni Zanchetta, Roberto Sulpizio, and Biagio Giaccio

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (16 Dec 2015) by Jack Middelburg
AR by Alexander Francke on behalf of the Authors (22 Jan 2016)  Author's response   Manuscript 
ED: Publish subject to technical corrections (04 Feb 2016) by Jack Middelburg
AR by Alexander Francke on behalf of the Authors (05 Feb 2016)  Manuscript 
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Short summary
Lake Ohrid (Macedonia, Albania) is thought to be more than 1.2 million years old. To recover a long paleoclimate record for the Mediterranean region, a deep drilling was carried out in 2013 within the scope of the Scientific Collaboration on Past Speciation Conditions in Lake Ohrid (SCOPSCO) project. Here, we present lithological, sedimentological, and (bio-)geochemical data from the upper 247.8 m composite depth of the overall 569 m long DEEP site record.
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