Hot spring oases in the periglacial desert as the Last Glacial Maximum refugia for temperate trees in Central Europe

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F24%3A10136446" target="_blank" >RIV/00023272:_____/24:10136446 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985939:_____/24:00587624 RIV/00216208:11310/24:10480941 RIV/00216224:14310/24:00138546 RIV/00216208:11620/24:10480941

Výsledek na webu

<a href="https://www.science.org/doi/10.1126/sciadv.ado6611" target="_blank" >https://www.science.org/doi/10.1126/sciadv.ado6611</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1126/sciadv.ado6611" target="_blank" >10.1126/sciadv.ado6611</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Hot spring oases in the periglacial desert as the Last Glacial Maximum refugia for temperate trees in Central Europe

Popis výsledku v původním jazyce

Northern glacial refugia are a hotly debated concept. The idea that many temperate organisms survived the Last Glacial Maximum (LGM; ~26.5 to 19 thousand years) in several sites across central and northern Europe stems from phylogeographic analyses, yet direct fossil evidence has thus far been missing. Here, we present the first unequivocal proof that thermophilous trees such as oak (Quercus), linden (Tilia), and common ash (Fraxinus excelsior) survived the LGM in Central Europe. The persistence of the refugium was promoted by a steady influx of hydrothermal waters that locally maintained a humid and warm microclimate. We reconstructed the geological and palaeohydrological factors responsible for the emergence of hot springs during the LGM and argue that refugia of this type, allowing the long-term survival and rapid post-LGM dispersal of temperate elements, were not exceptional in the European periglacial zone.

Název v anglickém jazyce

Hot spring oases in the periglacial desert as the Last Glacial Maximum refugia for temperate trees in Central Europe

Popis výsledku anglicky

Northern glacial refugia are a hotly debated concept. The idea that many temperate organisms survived the Last Glacial Maximum (LGM; ~26.5 to 19 thousand years) in several sites across central and northern Europe stems from phylogeographic analyses, yet direct fossil evidence has thus far been missing. Here, we present the first unequivocal proof that thermophilous trees such as oak (Quercus), linden (Tilia), and common ash (Fraxinus excelsior) survived the LGM in Central Europe. The persistence of the refugium was promoted by a steady influx of hydrothermal waters that locally maintained a humid and warm microclimate. We reconstructed the geological and palaeohydrological factors responsible for the emergence of hot springs during the LGM and argue that refugia of this type, allowing the long-term survival and rapid post-LGM dispersal of temperate elements, were not exceptional in the European periglacial zone.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

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OECD FORD obor

10506 - Paleontology

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2024

Kód důvěrnosti údajů

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

Název periodika

Science Advances

ISSN

2375-2548

e-ISSN

—

Svazek periodika

10

Číslo periodika v rámci svazku

22

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

14

Strana od-do

1-14

Kód UT WoS článku

001266184600003

EID výsledku v databázi Scopus

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