Towards a dendrochronologically refined date of the Laacher See eruption around 13,000 years ago

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F20%3A00524309" target="_blank" >RIV/86652079:_____/20:00524309 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/20:00117038

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S0277379119304159?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0277379119304159?via%3Dihub</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quascirev.2019.106128" target="_blank" >10.1016/j.quascirev.2019.106128</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Towards a dendrochronologically refined date of the Laacher See eruption around 13,000 years ago

Popis výsledku v původním jazyce

The precise date of the Laacher See eruption (LSE), central Europe's largest Late Pleistocene volcanic event that occurred around 13,000 years ago, is still unknown. Here, we outline the potential of combined high-resolution dendrochronological, wood anatomical and radiocarbon (14C) measurements, to refine the age of this major Plinian eruption. Based on excavated, subfossil trees that were killed during the explosive LSE and buried under its pyroclastic deposits, we describe how a firm date of the eruption might be achieved, and how the resulting temporal precision would further advance our understanding of the environmental and societal impacts of this event. Moreover, we discuss the relevance of an accurate LSE date for improving the synchronization of European terrestrial and lacustrine Late Glacial to Holocene archives. (C) 2019 Elsevier Ltd. All rights reserved.

Název v anglickém jazyce

Towards a dendrochronologically refined date of the Laacher See eruption around 13,000 years ago

Popis výsledku anglicky

The precise date of the Laacher See eruption (LSE), central Europe's largest Late Pleistocene volcanic event that occurred around 13,000 years ago, is still unknown. Here, we outline the potential of combined high-resolution dendrochronological, wood anatomical and radiocarbon (14C) measurements, to refine the age of this major Plinian eruption. Based on excavated, subfossil trees that were killed during the explosive LSE and buried under its pyroclastic deposits, we describe how a firm date of the eruption might be achieved, and how the resulting temporal precision would further advance our understanding of the environmental and societal impacts of this event. Moreover, we discuss the relevance of an accurate LSE date for improving the synchronization of European terrestrial and lacustrine Late Glacial to Holocene archives. (C) 2019 Elsevier Ltd. All rights reserved.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2020

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Quaternary Science Reviews

ISSN

0277-3791

e-ISSN

—

Svazek periodika

229

Číslo periodika v rámci svazku

FEB 2020

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

6

Strana od-do

106128

Kód UT WoS článku

000514018700018

EID výsledku v databázi Scopus

2-s2.0-85076689028