Articles | Volume 13, issue 7
https://doi.org/10.5194/bg-13-2093-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-2093-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
08 Apr 2016
Research article |
| 08 Apr 2016
Environmental control on the occurrence of high-coercivity magnetic minerals and formation of iron sulfides in a 640 ka sediment sequence from Lake Ohrid (Balkans)
Janna Just
CORRESPONDING AUTHOR
Institute of Geology and Mineralogy, University of Cologne, Cologne,
Germany
Collaborative Research Centre 806 – Our Way to Europe, University of
Cologne, Cologne, Germany
Norbert R. Nowaczyk
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences,
Potsdam, Germany
Leonardo Sagnotti
Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
Alexander Francke
Institute of Geology and Mineralogy, University of Cologne, Cologne,
Germany
Hendrik Vogel
Institute of Geological Sciences & Oeschger Centre for Climate Change
Research, University of Bern, Bern, Switzerland
Jack H. Lacey
NERC Isotope Geosciences Facilities, British Geological Survey,
Nottingham, UK
Bernd Wagner
Institute of Geology and Mineralogy, University of Cologne, Cologne,
Germany
Collaborative Research Centre 806 – Our Way to Europe, University of
Cologne, Cologne, Germany
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Cited
20 citations as recorded by crossref.
- Physical interpretation of isothermal remanent magnetization end‐members: New insights into the environmental history of Lake Hovsgul, Mongolia K. Fabian et al. 10.1002/2016GC006506
- Weak Influence of Paleoenvironmental Conditions on the Subsurface Biosphere of Lake Ohrid over the Last 515 ka C. Thomas et al. 10.3390/microorganisms8111736
- Tracing glacial-interglacial water mass changes in the Gulf of Corinth (IODP Expedition 381) using iron-sulphur geochemistry and magnetic susceptibility C. Mahoney & C. März 10.1016/j.margeo.2022.106801
- Centennial-scale vegetation dynamics and climate variability in SE Europe during Marine Isotope Stage 11 based on a pollen record from Lake Ohrid I. Kousis et al. 10.1016/j.quascirev.2018.04.014
- Greigite nanocrystals produced by hyperthermophilic archaea of Thermococcales order A. Gorlas et al. 10.1371/journal.pone.0201549
- Greigite formed in early Pleistocene lacustrine sediments from the Heqing Basin, southwest China, and its paleoenvironmental implications X. Qiang et al. 10.1016/j.jseaes.2018.01.033
- A High‐Resolution Paleosecular Variation Record for Marine Isotope Stage 6 From Southeastern Black Sea Sediments N. Nowaczyk et al. 10.1029/2020JB021350
- The environmental and evolutionary history of Lake Ohrid (FYROM/Albania): interim results from the SCOPSCO deep drilling project B. Wagner et al. 10.5194/bg-14-2033-2017
- Sample preparation for determination of comminution ages in lacustrine and marine sediments A. Francke et al. 10.1016/j.chemgeo.2018.01.003
- Magnetic mineral dissolution recorded in a lacustrine sequence from the Heqing Basin, SW China, and its relationship with changes in the Indian monsoon X. Xu et al. 10.1016/j.jseaes.2019.104081
- Polycrystalline texture causes magnetic instability in greigite B. Lesniak et al. 10.1038/s41598-020-80801-4
- Insights into the evolution of the young Lake Ohrid ecosystem and vegetation succession from a southern European refugium during the Early Pleistocene K. Panagiotopoulos et al. 10.1016/j.quascirev.2019.106044
- Assessment of the controls on (234U/238U) activity ratios recorded in detrital lacustrine sediments A. Francke et al. 10.1016/j.chemgeo.2020.119698
- Mercury records covering the past 90 000 years from lakes Prespa and Ohrid, SE Europe A. Paine et al. 10.5194/bg-21-531-2024
- Aligning and synchronization of MIS5 proxy records from Lake Ohrid (FYROM) with independently dated Mediterranean archives: implications for DEEP core chronology G. Zanchetta et al. 10.5194/bg-13-2757-2016
- Mediterranean winter rainfall in phase with African monsoons during the past 1.36 million years B. Wagner et al. 10.1038/s41586-019-1529-0
- The geodynamic and limnological evolution of Balkan Lake Ohrid, possibly the oldest extant lake in Europe B. Wagner et al. 10.1111/bor.12601
- The Marine Isotope Stage 12 pollen record from Lake Ohrid (SE Europe): Investigating short-term climate change under extreme glacial conditions A. Koutsodendris et al. 10.1016/j.quascirev.2019.105873
- Weathering trends in the Norian through geochemical and rock magnetic analyses from the Pignola–Abriola section (Lagonegro Basin, Italy) M. Maron et al. 10.5194/cp-20-637-2024
- Sedimentological processes and environmental variability at Lake Ohrid (Macedonia, Albania) between 637 ka and the present A. Francke et al. 10.5194/bg-13-1179-2016
19 citations as recorded by crossref.
- Physical interpretation of isothermal remanent magnetization end‐members: New insights into the environmental history of Lake Hovsgul, Mongolia K. Fabian et al. 10.1002/2016GC006506
- Weak Influence of Paleoenvironmental Conditions on the Subsurface Biosphere of Lake Ohrid over the Last 515 ka C. Thomas et al. 10.3390/microorganisms8111736
- Tracing glacial-interglacial water mass changes in the Gulf of Corinth (IODP Expedition 381) using iron-sulphur geochemistry and magnetic susceptibility C. Mahoney & C. März 10.1016/j.margeo.2022.106801
- Centennial-scale vegetation dynamics and climate variability in SE Europe during Marine Isotope Stage 11 based on a pollen record from Lake Ohrid I. Kousis et al. 10.1016/j.quascirev.2018.04.014
- Greigite nanocrystals produced by hyperthermophilic archaea of Thermococcales order A. Gorlas et al. 10.1371/journal.pone.0201549
- Greigite formed in early Pleistocene lacustrine sediments from the Heqing Basin, southwest China, and its paleoenvironmental implications X. Qiang et al. 10.1016/j.jseaes.2018.01.033
- A High‐Resolution Paleosecular Variation Record for Marine Isotope Stage 6 From Southeastern Black Sea Sediments N. Nowaczyk et al. 10.1029/2020JB021350
- The environmental and evolutionary history of Lake Ohrid (FYROM/Albania): interim results from the SCOPSCO deep drilling project B. Wagner et al. 10.5194/bg-14-2033-2017
- Sample preparation for determination of comminution ages in lacustrine and marine sediments A. Francke et al. 10.1016/j.chemgeo.2018.01.003
- Magnetic mineral dissolution recorded in a lacustrine sequence from the Heqing Basin, SW China, and its relationship with changes in the Indian monsoon X. Xu et al. 10.1016/j.jseaes.2019.104081
- Polycrystalline texture causes magnetic instability in greigite B. Lesniak et al. 10.1038/s41598-020-80801-4
- Insights into the evolution of the young Lake Ohrid ecosystem and vegetation succession from a southern European refugium during the Early Pleistocene K. Panagiotopoulos et al. 10.1016/j.quascirev.2019.106044
- Assessment of the controls on (234U/238U) activity ratios recorded in detrital lacustrine sediments A. Francke et al. 10.1016/j.chemgeo.2020.119698
- Mercury records covering the past 90 000 years from lakes Prespa and Ohrid, SE Europe A. Paine et al. 10.5194/bg-21-531-2024
- Aligning and synchronization of MIS5 proxy records from Lake Ohrid (FYROM) with independently dated Mediterranean archives: implications for DEEP core chronology G. Zanchetta et al. 10.5194/bg-13-2757-2016
- Mediterranean winter rainfall in phase with African monsoons during the past 1.36 million years B. Wagner et al. 10.1038/s41586-019-1529-0
- The geodynamic and limnological evolution of Balkan Lake Ohrid, possibly the oldest extant lake in Europe B. Wagner et al. 10.1111/bor.12601
- The Marine Isotope Stage 12 pollen record from Lake Ohrid (SE Europe): Investigating short-term climate change under extreme glacial conditions A. Koutsodendris et al. 10.1016/j.quascirev.2019.105873
- Weathering trends in the Norian through geochemical and rock magnetic analyses from the Pignola–Abriola section (Lagonegro Basin, Italy) M. Maron et al. 10.5194/cp-20-637-2024
Saved (preprint)
Latest update: 24 Apr 2024
Short summary
The magnetic record from Lake Ohrid reflects a strong change in geochemical conditions in the lake. Before 320 ka glacial sediments contain iron sulfides, while later glacials are dominated by siderite. Superimposed on this large-scale pattern are climatic induced changes in the magnetic mineralogy. Glacial and stadial sediments are characterized by relative increases of high- vs. low-coercivity minerals which relate to enhanced erosion in the catchment, possibly due to a sparse vegetation.
The magnetic record from Lake Ohrid reflects a strong change in geochemical conditions in the...
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