Reply to: Possible magmatic CO2 influence on the Laacher See eruption date

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F23%3A00131521" target="_blank" >RIV/00216224:14310/23:00131521 - isvavai.cz</a>
Result on the web
<a href="https://doi.org/10.1038/s41586-023-05966-0" target="_blank" >https://doi.org/10.1038/s41586-023-05966-0</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1038/s41586-023-05966-0" target="_blank" >10.1038/s41586-023-05966-0</a>

Result language
angličtina
Original language name
Reply to: Possible magmatic CO2 influence on the Laacher See eruption date
Original language description
We agree with Baldini et al.1 that the Laacher See tephra (LST) is a key Late Pleistocene chronostratigraphic unit across much of Europe. We also agree that the LST needs to be dated precisely to synchronize proxy archives and to better understand climate and environmental changes during the Late Glacial period. However, we disagree that our radiocarbon (14C) measurements from three subfossil trees killed and buried at different locations by the pyroclastic deposits of the Laacher See eruption (LSE)2 are possibly affected by outgassing magmatic carbon dioxide (CO2). Although the release of CO2 from active volcanic systems can influence 14C values3, we here provide both relict and modern radiocarbon evidence to demonstrate why our LSE date of 13,006 ± 9 calibrated years before present (BP; taken as AD 1950) is correct.
Czech name
—
Czech description
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Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10510 - Climatic research

Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2023
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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