Articles | Volume 13, issue 4
Biogeosciences, 13, 1179–1196, 2016

Special issue: Integrated perspectives on biological and geological dynamics...

Biogeosciences, 13, 1179–1196, 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 et al.


Interactive discussion

Status: closed
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: 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
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.
Final-revised paper