Wagner, Bernd; Sulpizio, Roberto; Zanchetta, Giovanni; Wulf, Sabine; Wessels, Martin; Daut, Gerhard; Nowaczyk, Norbert R (2008): (Table 3) Main characteristics of tephra layers recognised in core Lz1120 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.760114, In 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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Related to:
Coltelli, Mauro; Del Carlo, Paola; Vezzoli, Luigina (1998): The discovery of a Plinian basaltic eruption of Roman age at Etna volcano (Italy). Geology, 26(12), 1095-1098, https://doi.org/10.1130/0091-7613(1998)026%3C1095:DOAPBE%3E2.3.CO;2
De Vivo, B; Rolandi, G; Gans, P B; Calvert, A; Bohrson, W A; Spera, F J; Belkin, H E (2001): New constraints on the pyroclastic eruptive history of the Campanian volcanic Plain (Italy). Mineralogy and Petrology, 73(1-3), 47-65, https://doi.org/10.1007/s007100170010
Sulpizio, Roberto; Zanchetta, Giovanni; Paterne, Martine; Siani, Giuseppe (2003): A review of tephrostratigraphy in central and southern Italy during the last 65 ka. Il Quaternario - Italian Journal of Quaternary Sciences, 16(1), 91-108, https://amq.aiqua.it/index.php/amq/article/view/597
Wulf, Sabine; Kraml, Michael; Brauer, Achim; Keller, Jörg; Negendank, Jörg F W (2004): Tephrochronology of the 100 ka lacustrine sediment record of Lago Grande di Monticchio (southern Italy). Quaternary International, 122(1), 7-30, https://doi.org/10.1016/j.quaint.2004.01.028
Coverage:
Latitude: 40.938000 * Longitude: 20.759000
Date/Time Start: 2005-03-16T00:00:00 * Date/Time End: 2005-03-16T00:00:00
Minimum DEPTH, sediment/rock: 3.125 m * Maximum DEPTH, sediment/rock: 10.725 m
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)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Depth, top/min | Depth top | m | Wagner, Bernd | ||
3 | Depth, bottom/max | Depth bot | m | Wagner, Bernd | ||
4 | Age, dated | Age dated | ka | Wagner, Bernd | Age, 14C AMS | |
5 | Reference/source | Reference | Wagner, Bernd | |||
6 | Age, dated standard deviation | Age dated std dev | ± | Wagner, Bernd | ||
7 | Age, dated | Age dated | ka | Wagner, Bernd | calibrated | |
8 | Age, dated standard deviation | Age dated std dev | ± | Wagner, Bernd | calibrated | |
9 | Lithology/composition/facies | Lithology | Wagner, Bernd | of juvenile fragments | ||
10 | Area/locality | Area | Wagner, Bernd | inferred source |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
33 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Age dated [ka] (Age, 14C AMS) | 5 Reference | 6 Age dated std dev [±] | 7 Age dated [ka] (calibrated) | 8 Age dated std dev [±] (calibrated) | 9 Lithology (of juvenile fragments) | 10 Area (inferred source) |
---|---|---|---|---|---|---|---|---|---|
3.125 | 3.10 | 3.15 | 3.150 | Coltelli et al. (2000) | 0.060 | 3.370 | 0.070 | Dark-coloured glass fragments (5YR 2/2 dusky brown). Poorly vesicular, aphiric. Benmoreitic composition. | Mount Etna |
8.965 | 8.96 | 8.97 | 25.820 | Sulpizio et al. (2003) | 0.270 | 30.670 | 0.230 | Highly vesicular, aphiric, micropumice and colourless glass shards. Colour: 5Y 8/1-Yellowish grey. Trachytic composition. | Campi Flegrei |
8.965 | 8.96 | 8.97 | 27.256 | Wulf et al. (2004) | |||||
10.725 | 10.70 | 10.75 | 39.280 | De Vivo et al. (2001) | 0.110 | Light-coloured micropumice (5Y 7/2 yellowish grey to 5Y 5/2 Light olive grey), highly to extremely vesicular, almost aphiric (bt+san). Dark-coloured glass shards (5RP 2/2 very dusky red purple) are abundant. Trachytic composition. | Campi Flegrei | ||
10.725 | 10.70 | 10.75 | 36.670 | Wulf et al. (2004) |