Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12188/30856
DC FieldValueLanguage
dc.contributor.authorWagner, Bernden_US
dc.contributor.authorTauber, Paulen_US
dc.contributor.authorFrancke, Alexanderen_US
dc.contributor.authorLeicher, Niklasen_US
dc.contributor.authorBinnie, Steven A.en_US
dc.contributor.authorCvetkoska, Aleksandraen_US
dc.contributor.authorJovanovska, Elenaen_US
dc.contributor.authorJust, Jannaen_US
dc.contributor.authorLacey, Jack H.en_US
dc.contributor.authorLevkov, Zlatkoen_US
dc.contributor.authorLindhorst, Katjaen_US
dc.contributor.authorKouli, Katerinaen_US
dc.contributor.authorKrastel, Sebastianen_US
dc.contributor.authorPanagiotopoulos, Konstantinosen_US
dc.contributor.authorUlfers, Arneen_US
dc.contributor.authorZaova, Dušicaen_US
dc.contributor.authorDonders, Timme H.en_US
dc.contributor.authorGrazhdani, Andonen_US
dc.contributor.authorKoutsodendris, Andreasen_US
dc.contributor.authorLeng, Melanie J.en_US
dc.contributor.authorSadori, Lauraen_US
dc.contributor.authorScheinert, Mirkoen_US
dc.contributor.authorVogel, Hendriken_US
dc.contributor.authorWonik, Thomasen_US
dc.contributor.authorZanchetta, Giovannien_US
dc.contributor.authorWilke, Thomasen_US
dc.date.accessioned2024-06-29T16:18:52Z-
dc.date.available2024-06-29T16:18:52Z-
dc.date.issued2022-10-31-
dc.identifier.urihttp://hdl.handle.net/20.500.12188/30856-
dc.description.abstract<jats:p>Studies of the upper 447 m of the DEEP site sediment succession from central Lake Ohrid, Balkan Peninsula, North Macedonia and Albania provided important insights into the regional climate history and evolutionary dynamics since permanent lacustrine conditions established at 1.36 million years ago (Ma). This paper focuses on the entire 584‐m‐long DEEP sediment succession and a comparison to a 197‐m‐long sediment succession from the Pestani site ~5 km to the east in the lake, where drilling ended close to the bedrock, to unravel the earliest history of Lake Ohrid and its basin development. <jats:sup>26</jats:sup>Al/<jats:sup>10</jats:sup>Be dating of clasts from the base of the DEEP sediment succession implies that the sedimentation in the modern basin started at <jats:italic>c</jats:italic>. 2 Ma. Geophysical, sedimentological and micropalaeontological data allow for chronological information to be transposed from the DEEP to the Pestani succession. Fluvial conditions, slack water conditions, peat formation and/or complete desiccation prevailed at the DEEP and Pestani sites until 1.36 and 1.21 Ma, respectively, before a larger lake extended over both sites. Activation of karst aquifers to the east probably by tectonic activity and a potential existence of neighbouring Lake Prespa supported filling of Lake Ohrid. The lake deepened gradually, with a relatively constant vertical displacement rate of ~0.2 mm a<jats:sup>−1</jats:sup> between the central and the eastern lateral basin and with greater water depth presumably during interglacial periods. Although the dynamic environment characterized by local processes and the fragmentary chronology of the basal sediment successions from both sites hamper palaeoclimatic significance prior to the existence of a larger lake, the new data provide an unprecedented and detailed picture of the geodynamic evolution of the basin and lake that is Europe’s presumed oldest extant freshwater lake.</jats:p>en_US
dc.publisherWileyen_US
dc.relation.ispartofBoreasen_US
dc.titleThe geodynamic and limnological evolution of Balkan Lake Ohrid, possibly the oldest extant lake in Europeen_US
dc.typeArticleen_US
dc.identifier.doi10.1111/bor.12601-
dc.identifier.urlhttps://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12601-
dc.identifier.urlhttps://onlinelibrary.wiley.com/doi/full-xml/10.1111/bor.12601-
dc.identifier.urlhttps://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12601-
dc.identifier.volume52-
dc.identifier.issue1-
item.fulltextWith Fulltext-
item.grantfulltextopen-
crisitem.author.deptFaculty of Natural Sciences and Mathematics-
Appears in Collections:Faculty of Natural Sciences and Mathematics, Institute of Biology: Journal Articles
Files in This Item:
File Description SizeFormat 
2023 - Wagner et al. - Geodynamic and limnological evolution of Lake Ohrid .pdf3.84 MBAdobe PDFView/Open
Show simple item record

Page view(s)

19
checked on Oct 8, 2024

Download(s)

7
checked on Oct 8, 2024

Google ScholarTM

Check

Altmetric


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.