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Cosmic-impact event in lake sediments from Central Europe postdates the Laacher See eruption and marks onset of the Younger Dryas
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SYSNO ASEP 0493827 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Cosmic-impact event in lake sediments from Central Europe postdates the Laacher See eruption and marks onset of the Younger Dryas Author(s) Kletetschka, Günther (GLU-S) RID, SAI, ORCID
Vondrák, D. (CZ)
Hrubá, J. (CZ)
Procházka, V. (CZ)
Nábělek, Ladislav (GLU-S) RID, SAI
Svitavská-Svobodová, Helena (BU-J) RID, ORCID
Bobek, Přemysl (BU-J) ORCID, SAI
Hořická, Zuzana (BC-A) RID
Kadlec, Jaroslav (GFU-E) ORCID, RID
Takáč, M. (CZ)
Stuchlík, Evžen (BC-A) RID, ORCIDSource Title Journal of Geology. - : University of Chicago Press - ISSN 0022-1376
Roč. 126, č. 6 (2018), s. 561-575Number of pages 15 s. Publication form Print - P Language eng - English Country US - United States Keywords biomass-burning episode ; 4 continents ; NE-Germany ; black mat ; boundary ; volcano ; tephra ; hypothesis ; spherules ; climate Subject RIV DB - Geology ; Mineralogy OECD category Geology Subject RIV - cooperation Biology Centre (since 2006) - Hydrology ; Limnology R&D Projects GA17-05935S GA ČR - Czech Science Foundation (CSF) Institutional support GLU-S - RVO:67985831 ; BU-J - RVO:67985939 ; BC-A - RVO:60077344 ; GFU-E - RVO:67985530 UT WOS 000449866400001 EID SCOPUS 85055477893 DOI 10.1086/699869 Annotation The Younger Dryas (YD) climate episode (similar to 12,850-11,650 calendar years before present [cal BP]) is an event recorded widely across the Northern Hemisphere. We conducted multiple analyses at high resolution of a YD-age sedimentary sequence from Stara Jimka, a paleolake in the Bohemian Forest, Czech Republic. Age-depth modeling indicates that a central European warming trend was interrupted at similar to 13,020 +/- 110 cal BP by the sudden onset of cooling (<20 y) known as the Gerzensee climate oscillation and marked by the deposition of fine-grained sediment at this location. That cooling episode ended at similar to 13,001 +/- 66 cal BP and was followed by a similar to 121-y-long warming trend. After that, the Laacher See tephra depositional event, dating to similar to 12,820 +/- 20 cal BP, continued an overall warming trend. The composition of Laacher See volcanic tephra in this section likely corresponds to the middle eruption sequence. Finally, the deposition of glassy microspherules marked the onset of the YD climate change at 12,755 +/- 92 cal BP. The sequence across the YD onset is marked by (1) a peak in glassy microspherules (117,000/kg), (2) a peak in framboidal spherules (14,000/kg), (3) significant changes in the lake's weathering proxies, and (4) major changes in fauna and flora, showing a shift to unfavorable environmental conditions (decrease in temperature and lake trophy status). Collectively, this evidence is consistent with the YD impact hypothesis and evidence of one or more cosmic airburst events occurring at this time. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2019
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