Relation between Central European Climate Change and Eifel Volcanism during the Last 130,000 Years
The Elsa-23-Tephra-Stack
Bibliographic Data
| ID | 15801899 |
|---|---|
| Authors | Frank Sirocko (0000-0002-3131-0613, Johannes Gutenberg University Mainz, corresponding author), Frederik Krebsbach (Johannes Gutenberg University Mainz), Johannes Albert (0009-0006-6508-6337, Johannes Gutenberg University Mainz), Sarah Britzius (0009-0003-1043-1787, Max Planck Institute for Chemistry), Fiona Schenk (0009-0008-2877-3204, Johannes Gutenberg University Mainz), Michael W Förster (Australian National University) |
| Year | 2024 |
| Volume | 7 |
| Issue | 2 |
| Pages | 21-21 |
| Publication date | 2024-04-25 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Quaternary (JOURNAL) |
| Journal identifiers | ISSN: 2571-550X • E-ISSN: 2571-550X |
| Publisher | Multidisciplinary Digital Publishing Institute (PUBLISHER • CH) |
| DOI | 10.3390/quat7020021 |
| OpenAlex | W4395466991 |
| Language | EN |
| Citations received | 5 |
| References cited | 42 |
The analysis of tephra layers in maar lake sediments of the Eifel shows 14 well-visible tephra during the last glacial cycle from the Holocene to the Eemian (0–130,000 yr b2k). These tephra were analyzed for their petrographic composition, which allows us to connect several tephra to eruption sites. All tephra were dated by application of the ELSA-20 chronology, developed using the late Pleistocene infilled maar lake of Auel and the Holocene lake Holzmaar (0–60,000 yr b2k). We extend the ELSA-20 chronology with this paper for the millennia of 60,000–130,000 yr b2k (ELSA-23 chronology), which is based on the infilled maar lake records from Dehner, Hoher List, and Jungferweiher. The evaluation of the tephra from the entire last glacial cycle shows that all 14 tephra were close to interstadial warming of the North Atlantic sea surface temperatures. In particular, phreatomagmatic maar eruptions were systematically associated with Heinrich events or C-events. These events represent times of warming of the Southern Hemisphere, global sea level rise, and CO2 increase, which predate the abrupt interstadial warming events of the Northern Hemisphere. This synchroneity indicates a physical relationship between endogenic and exogenic processes. Changes in the lithospheric stress field in response to changes in continental ice loads have already been suggested as a potential candidate to explain the exogenic forcing of endogenic processes. The chronology of volcanic activity in the Eifel demonstrates that intraplate mantle plumes are also affected by the exogenic forcing of endogenic processes
Climate change · Database · Earth science · Geochemistry · Geography · Physical geography · Relation (database · Stack (abstract data type · Tectonics · Tephra · Volcanism · Volcano · Archaeology and ancient environmental studies · Computer Science · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Geology · Oceanography · Paleontology
Holocene and Late Pleistocene Flood Events in Central Europe Reconstructed from Eifel Maar Lake Sediments
Fine-Tuning of Sub-Annual Resolution Spectral Index Time Series from Eifel Maar Sediments, Western Germany, to the NGRIP δ18O Chronology, 26–60 ka
Bioproductivity and vegetation changes documented in Eifel maar lake sediments (western Germany) compared with speleothem growth indicating three warm phases during the last glacial cycle
A Cryptotephra Layer in Sediments of an Infilled Maar Lake from the Eifel (Germany)
Vegetation Patterns during the Last 132,000 Years
A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ 18 O records
Insolation values for the climate of the last 10 million years
Sea-level fluctuations during the last glacial cycle
Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years
A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records
A new Greenland ice core chronology for the last glacial termination
A Cryptotephra Layer in Sediments of an Infilled Maar Lake from the Eifel (Germany)
Vegetation Patterns during the Last 132,000 Years
Bioproductivity and vegetation changes documented in Eifel maar lake sediments (western Germany) compared with speleothem growth indicating three warm phases during the last glacial cycle
Evidence of tephra reworking in loess based on 2D magnetic susceptibility mapping
Lateglacial calendar year chronology based on annually laminated sediments from Lake Meerfelder Maar, Germany
| Unique citing works | 5 |
|---|---|
| Citations per year | 1,67 |
| Citation span | 2023 - 2025 (3) |
| Citation velocity | recent |
| Highly cited | No |
| Citation types | Neutral: 5 |