Förster, Michael W; Sirocko, Frank (2016): Tephra-stack of combined sediment record ELSA [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.868671, Supplement to: Förster, MW; Sirocko, F (2016): The ELSA tephra stack: Volcanic activity in the Eifel during the last 500,000 years. Global and Planetary Change, 142, 100-107, https://doi.org/10.1016/j.gloplacha.2015.07.012
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
Tephra layers of individual volcanic eruptions are traced in several cores from Eifel maar lakes, drilled between 1998 and 2014 by the Eifel Laminated Sediment Archive (ELSA). All sediment cores are dated by 14C and tuned to the Greenland interstadial succession. Tephra layers were characterized by the petrographic composition of basement rock fragments, glass shards and characteristic volcanic minerals. 10 marker tephra, including the well-established Laacher See Tephra and Dümpelmaar Tephra can be identified in the cores spanning the last glacial cycle. Older cores down to the beginning of the Elsterian, show numerous tephra sourced from Strombolian and phreatomagmatic eruptions, including the 40Ar/39Ar dated differentiated tephra from Glees and Hüttenberg. In total, at least 91 individual tephra can be identified since the onset of the Eifel volcanic activity at about 500,000 b2k, which marks the end of the ELSA tephra stack with 35 Strombolian, 48 phreatomagmatic and 8 tephra layers of evolved magma composition. Many eruptions cluster near timings of the global climate transitions at 140,000, 110,000 and 60,000 b2k. In total, the eruptions show a pattern, which resembles timing of phases of global sea level and continental ice sheet changes, indicating a relation between endogenic and exogenic processes.
Related to:
Brunck, Heiko; Sirocko, Frank; Albert, Johannes (2016): The ELSA-Flood-Stack: A reconstruction from the laminated sediments of Eifel maar structures during the last 60000 years. Global and Planetary Change, 142, 136-146, https://doi.org/10.1016/j.gloplacha.2015.12.003
Sirocko, Frank (2016): The ELSA - Stacks (Eifel-Laminated-Sediment-Archive): An introduction. Global and Planetary Change, 142, 96-99, https://doi.org/10.1016/j.gloplacha.2016.03.011
Sirocko, Frank; Knapp, Hannes; Dreher, Frank; Förster, Michael W; Albert, Johannes; Brunck, Heiko; Veres, Daniel; Dietrich, Stephan; Zech, Michael; Hambach, Ulrich; Röhner, Marieke; Rudert, Saskia; Schwiebus, Klaus; Adams, Christel; Sigl, Petra (2016): The ELSA-Vegetation-Stack: Reconstruction of Landscape Evolution Zones (LEZ) from laminated Eifel maar sediments of the last 60,000years. Global and Planetary Change, 142, 108-135, https://doi.org/10.1016/j.gloplacha.2016.03.005
Coverage:
Latitude: 50.160000 * Longitude: 6.830000
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Age | Age | ka b2k | Förster, Michael W | ||
| 2 | Tephra or volcanic ash | Tephra | # | Förster, Michael W | Plinian | |
| 3 | Tephra marker | Tephra | Förster, Michael W | Plinian | ||
| 4 | Tephra or volcanic ash | Tephra | # | Förster, Michael W | Phreatomagmatic | |
| 5 | Tephra marker | Tephra | Förster, Michael W | Phreatomagmatic | ||
| 6 | Tephra or volcanic ash | Tephra | # | Förster, Michael W | Strombolian | |
| 7 | Tephra marker | Tephra | Förster, Michael W | Strombolian |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
325 data points
Data
| 1 Age [ka b2k] | 2 Tephra [#] (Plinian) | 3 Tephra (Plinian) | 4 Tephra [#] (Phreatomagmatic) | 5 Tephra (Phreatomagmatic) | 6 Tephra [#] (Strombolian) | 7 Tephra (Strombolian) |
|---|---|---|---|---|---|---|
| 1.000 | 0 | 0 | 0 | |||
| 10.999 | 0 | 0 | 0 | |||
| 11.000 | 0 | 1 | Ulmer Maar tephra | 0 | ||
| 11.001 | 0 | 0 | 0 | |||
| 12.899 | 0 | 0 | 0 | |||
| 12.900 | 1 | Laacher See tephra | 0 | 0 | ||
| 12.901 | 0 | 0 | 0 | |||
| 27.899 | 0 | 0 | 0 | |||
| 0 | 0 | 1 | Wartgesberg tephra | |||
| 27.901 | 0 | 0 | 0 | |||
| 30.199 | 0 | 0 | 0 | |||
| 30.200 | 0 | 0 | 1 | unknown tephra 1 | ||
| 30.201 | 0 | 0 | 0 | |||
| 40.999 | 0 | 0 | 0 | |||
| 41.000 | 0 | 1 | Dreiser Weiher tephra | 0 | ||
| 41.001 | 0 | 0 | 0 | |||
| 43.899 | 0 | 0 | 0 | |||
| 43.900 | 0 | 1 | unknown tephra 2 | 0 | ||
| 43.901 | 0 | 0 | 0 | |||
| 49.999 | 0 | 0 | 0 | |||
| 50.000 | 0 | 1 | 0 | |||
| 50.001 | 0 | 0 | 0 | |||
| 52.999 | 0 | 0 | 0 | |||
| 53.000 | 0 | 1 | 0 | |||
| 53.001 | 0 | 0 | 0 | |||
| 55.999 | 0 | 0 | 0 | |||
| 56.000 | 0 | 1 | 0 | |||
| 56.001 | 0 | 0 | 0 | |||
| 57.999 | 0 | 0 | 0 | |||
| 58.000 | 0 | 1 | 0 | |||
| 58.001 | 0 | 0 | 0 | |||
| 59.999 | 0 | 0 | 0 | |||
| 60.000 | 0 | 1 | Leucite tephra | 0 | ||
| 60.001 | 0 | 0 | 0 | |||
| 79.999 | 0 | 0 | 0 | |||
| 80.000 | 0 | 1 | 0 | |||
| 80.001 | 0 | 0 | 0 | |||
| 84.999 | 0 | 0 | 0 | |||
| 85.000 | 0 | 1 | 0 | |||
| 85.001 | 0 | 0 | 0 | |||
| 89.999 | 0 | 0 | 0 | |||
| 90.000 | 0 | 0 | 1 | |||
| 90.001 | 0 | 0 | 0 | |||
| 103.999 | 0 | 0 | 0 | |||
| 104.000 | 0 | 1 | 0 | |||
| 104.001 | 0 | 0 | 0 | |||
| 105.999 | 0 | 0 | 0 | |||
| 106.000 | 1 | Dümpelmaar tephra | 0 | 0 | ||
| 106.001 | 0 | 0 | 0 | |||
| 150.999 | 0 | 0 | 0 | |||
| 151.000 | 1 | Glees tephra | 0 | 0 | ||
| 151.001 | 0 | 0 | 0 | |||
| 151.999 | 0 | 0 | 0 | |||
| 152.000 | 0 | 1 | 0 | |||
| 152.001 | 0 | 0 | 0 | |||
| 153.499 | 0 | 0 | 0 | |||
| 153.500 | 0 | 0 | 1 | |||
| 153.501 | 0 | 0 | 0 | |||
| 174.999 | 0 | 0 | 0 | |||
| 175.000 | 0 | 1 | 0 | |||
| 175.001 | 0 | 0 | 0 | |||
| 175.999 | 0 | 0 | 0 | |||
| 176.000 | 0 | 0 | 1 | |||
| 176.001 | 0 | 0 | 0 | |||
| 180.999 | 0 | 0 | 0 | |||
| 181.000 | 0 | 1 | 0 | |||
| 181.001 | 0 | 0 | 0 | |||
| 182.999 | 0 | 0 | 0 | |||
| 183.000 | 0 | 1 | 0 | |||
| 183.001 | 0 | 0 | 0 | |||
| 184.999 | 0 | 0 | 0 | |||
| 185.000 | 0 | 1 | 0 | |||
| 185.001 | 0 | 0 | 0 | |||
| 214.999 | 0 | 0 | 0 | |||
| 215.000 | 1 | Hüttenberg tephra | 0 | 0 | ||
| 215.001 | 0 | 0 | 0 | |||
| 219.999 | 0 | 0 | 0 | |||
| 220.000 | 0 | 1 | 0 | |||
| 220.001 | 0 | 0 | 0 |