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Wagner, Bernd; Sulpizio, Roberto; Zanchetta, Giovanni; Wulf, Sabine; Wessels, Martin; Daut, Gerhard; Nowaczyk, Norbert R (2008): Geological investigations on sediment core Lz1120 from Lake Ohrid [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.760113, Supplement to: Wagner, B et al. (2008): The last 40 ka tephrostratigraphic record of Lake Ohrid, Albania and Macedonia: a very distal archive for ash dispersal from Italian volcanoes. Journal of Volcanology and Geothermal Research, 177, 71-80, https://doi.org/10.1016/j.jvolgeores.2007.08.018

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Abstract:
A 1075 cm long core (Lz1120) was recovered in the south-eastern part of the Lake Ohrid (Republics of Macedonia and Albania) and sampled for identification of tephra layers. Magnetic susceptibility investigations show rather high magnetic values throughout the core, with peaks unrelated to the occurrence of tephra layers but instead to the relative abundance of detrital magnetic minerals in the sediment. Naked-eye inspection of the core allowed us to identify of two tephra layers, at 896-897 cm and 1070-1075 cm. Laboratory inspection of the grain-size fraction >125 µm allowed for the identification of a third cryptotephra at 310-315 cm. Major element analyses on glass shards of the tephra layers at 896-897 cm and 1070-1075 cm show a trachytic composition, and indicate a correlation with the regionally dispersed Y-3 and Y-5 tephra layers, dated at ca 30 and 39 cal ka BP. The cryptotephra at 310-315 cm has a mugearitic- benmoreitic composition, and was correlated with the FL eruption of Mt. Etna, dated at 3370±70 cal yr BP. These ages are in agreement with five 14C AMS measurements carried out on plant remains and macrofossils from the lake sediments at different depths along the core.
The recognition of distal tephra from Italian volcanoes allows us to link the Lake Ohrid succession to other archives located in the Mediterranean area and in eastern Europe. The benmoreitic-mugearitic tephra layer at 310-315 cm is the first recognition in the Balkan area of a distal ash deposit from a mid-intensity explosive eruption of Mt. Etna, as far as 600 km from the source.
Coverage:
Latitude: 40.938000 * Longitude: 20.759000
Date/Time Start: 2005-03-16T00:00:00 * Date/Time End: 2005-03-16T00:00:00
Event(s):
Lz1120 * Latitude: 40.938000 * Longitude: 20.759000 * Date/Time: 2005-03-16T00:00:00 * Elevation: 693.0 m * Lake water depth: 105 m * Recovery: 1.08 m * Location: Lake Ohrid, Macedonian/Albanian border * Campaign: ohrid-exp * Basis: Sampling/drilling in lake * Method/Device: Piston corer, UWITEC (PCUWI)
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
5 datasets

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Datasets listed in this publication series

  1. Wagner, B; Sulpizio, R; Zanchetta, G et al. (2008): (Table 1) Radiocarbon measurements of charcoal and plant remains collected at different depths along core Lz1120. https://doi.org/10.1594/PANGAEA.760110
  2. Wagner, B; Sulpizio, R; Zanchetta, G et al. (2008): Grain size analysis of sediment core Lz1120. https://doi.org/10.1594/PANGAEA.760116
  3. Wagner, B; Sulpizio, R; Zanchetta, G et al. (2008): Susceptibility of sediment core Lz1120. https://doi.org/10.1594/PANGAEA.760115
  4. Wagner, B; Sulpizio, R; Zanchetta, G et al. (2008): (Table 3) Main characteristics of tephra layers recognised in core Lz1120. https://doi.org/10.1594/PANGAEA.760114
  5. Wagner, B; Sulpizio, R; Zanchetta, G et al. (2008): (Table 2) Major elements glass chemistry of the three tephra layers recognised in core Lz 1120. https://doi.org/10.1594/PANGAEA.760112