Diatom responses to limnological and climatic changes at Ribains Maar (French Massif Central) during the Eemian and Early Würm

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985939%3A_____%2F07%3A00326971" target="_blank" >RIV/67985939:_____/07:00326971 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Diatom responses to limnological and climatic changes at Ribains Maar (French Massif Central) during the Eemian and Early Würm

Popis výsledku v původním jazyce

High-resolution diatom analysis was carried out to assess the limnological and climatic changes that took place at Ribains maar (French Massif Central) during the Late Pleistocene (131?105 ka BP), with a focus on the Eemian interglacial in particular. This study shows that at Ribains maar, the transition from the Riss (Saalian) Glacial to the Eemian interglacial was marked by a gradual increase in the contribution of spring-blooming diatom species, indicating a longer growing season and milder winter/ spring conditions at that time. A short cooling event interrupts this trend and may correspond to a stadial. The record ends with the Montaigu cold event. Variation in insolation throughout the Eemian may have been the driving factor behind the species succession observed in the diatom sequence.

Název v anglickém jazyce

Diatom responses to limnological and climatic changes at Ribains Maar (French Massif Central) during the Eemian and Early Würm

Popis výsledku anglicky

High-resolution diatom analysis was carried out to assess the limnological and climatic changes that took place at Ribains maar (French Massif Central) during the Late Pleistocene (131?105 ka BP), with a focus on the Eemian interglacial in particular. This study shows that at Ribains maar, the transition from the Riss (Saalian) Glacial to the Eemian interglacial was marked by a gradual increase in the contribution of spring-blooming diatom species, indicating a longer growing season and milder winter/ spring conditions at that time. A short cooling event interrupts this trend and may correspond to a stadial. The record ends with the Montaigu cold event. Variation in insolation throughout the Eemian may have been the driving factor behind the species succession observed in the diatom sequence.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EF - Botanika

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2007

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

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Svazek periodika

26

Číslo periodika v rámci svazku

11-12

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

53

Strana od-do

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Kód UT WoS článku

000248349700006

EID výsledku v databázi Scopus

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