Temperature oscillations over the last 10,000 years in western Europe estimated from terrestrial mollusc assemblages
Identifieur interne : 000486 ( France/Analysis ); précédent : 000485; suivant : 000487Temperature oscillations over the last 10,000 years in western Europe estimated from terrestrial mollusc assemblages
Auteurs : Denis-Didier Rousseau [États-Unis] ; Nicole Limondin [France] ; Frédéric Magnin [France] ; Jean-Jacques PuissegurSource :
- Boreas [ 0300-9483 ] ; 1994-03.
Descripteurs français
- Wicri :
- topic : Mollusque.
English descriptors
- KwdEn :
- Assemblage, Atlantic chronozone, Atlantic ocean, August, August temperatures, Boreas, British isles, Climatic, Correspondence analysis, Dryas, February, Fluctuation, Fossil, Fossil assemblages, Frederic magnin, General variability, Glacier, Hiatus, Holocene, Lake sediments, Last deglaciation, Last years, Lehman keigwin, Modern assemblages, Mollusc, Mollusc assemblages, Mollusc species, Molluscan, Molluscan assemblages, Multiple correlation coefficient, Nesje kvamme, Nicole limondin, Organic matter, Other proxy data, Past years, Pollen data, Quantitative reconstructions, Quaternary, Quaternary research, Quaternary science reviews, Rapid warming, Reconstructed values, Snail, Snail assemblages, Standard errors, Temperature boreas, Temperature estimates, Temperature oscillations, Terrestrial deposits, Terrestrial molluscs, Total number, Total variance, Transfer functions, Variance, Vertigo, Western europe, Western norway, Younger dryas, Younger dryas event.
- Teeft :
- Assemblage, Atlantic chronozone, Atlantic ocean, August, August temperatures, Boreas, British isles, Climatic, Correspondence analysis, Dryas, February, Fluctuation, Fossil, Fossil assemblages, Frederic magnin, General variability, Glacier, Hiatus, Holocene, Lake sediments, Last deglaciation, Last years, Lehman keigwin, Modern assemblages, Mollusc, Mollusc assemblages, Mollusc species, Molluscan, Molluscan assemblages, Multiple correlation coefficient, Nesje kvamme, Nicole limondin, Organic matter, Other proxy data, Past years, Pollen data, Quantitative reconstructions, Quaternary, Quaternary research, Quaternary science reviews, Rapid warming, Reconstructed values, Snail, Snail assemblages, Standard errors, Temperature boreas, Temperature estimates, Temperature oscillations, Terrestrial deposits, Terrestrial molluscs, Total number, Total variance, Transfer functions, Variance, Vertigo, Western europe, Western norway, Younger dryas, Younger dryas event.
Abstract
Snail assemblages are used to estimate February and August temperatures during the past 10,000 years in western Europe. We find that a strong warming occurred after the Younger Dryas event, followed by several rapid cooling and warming events. These observations are in agreement with insect and pollen proxy data from the European continent and with estimates of sea‐surface temperature from the North Atlantic Ocean as well as with fluctuations of glaciers in western Norway. This study also confirms that terrestrial molluscs can provide reliable climatic data in conjunction with other proxy data.
Url:
DOI: 10.1111/j.1502-3885.1994.tb00587.x
Affiliations:
- France, États-Unis
- Bourgogne-Franche-Comté, Franche-Comté, Languedoc-Roussillon, Occitanie (région administrative)
- Besançon, Montpellier
- Université Montpellier 2
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Assemblage</term>
<term>Atlantic chronozone</term>
<term>Atlantic ocean</term>
<term>August</term>
<term>August temperatures</term>
<term>Boreas</term>
<term>British isles</term>
<term>Climatic</term>
<term>Correspondence analysis</term>
<term>Dryas</term>
<term>February</term>
<term>Fluctuation</term>
<term>Fossil</term>
<term>Fossil assemblages</term>
<term>Frederic magnin</term>
<term>General variability</term>
<term>Glacier</term>
<term>Hiatus</term>
<term>Holocene</term>
<term>Lake sediments</term>
<term>Last deglaciation</term>
<term>Last years</term>
<term>Lehman keigwin</term>
<term>Modern assemblages</term>
<term>Mollusc</term>
<term>Mollusc assemblages</term>
<term>Mollusc species</term>
<term>Molluscan</term>
<term>Molluscan assemblages</term>
<term>Multiple correlation coefficient</term>
<term>Nesje kvamme</term>
<term>Nicole limondin</term>
<term>Organic matter</term>
<term>Other proxy data</term>
<term>Past years</term>
<term>Pollen data</term>
<term>Quantitative reconstructions</term>
<term>Quaternary</term>
<term>Quaternary research</term>
<term>Quaternary science reviews</term>
<term>Rapid warming</term>
<term>Reconstructed values</term>
<term>Snail</term>
<term>Snail assemblages</term>
<term>Standard errors</term>
<term>Temperature boreas</term>
<term>Temperature estimates</term>
<term>Temperature oscillations</term>
<term>Terrestrial deposits</term>
<term>Terrestrial molluscs</term>
<term>Total number</term>
<term>Total variance</term>
<term>Transfer functions</term>
<term>Variance</term>
<term>Vertigo</term>
<term>Western europe</term>
<term>Western norway</term>
<term>Younger dryas</term>
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<term>August temperatures</term>
<term>Boreas</term>
<term>British isles</term>
<term>Climatic</term>
<term>Correspondence analysis</term>
<term>Dryas</term>
<term>February</term>
<term>Fluctuation</term>
<term>Fossil</term>
<term>Fossil assemblages</term>
<term>Frederic magnin</term>
<term>General variability</term>
<term>Glacier</term>
<term>Hiatus</term>
<term>Holocene</term>
<term>Lake sediments</term>
<term>Last deglaciation</term>
<term>Last years</term>
<term>Lehman keigwin</term>
<term>Modern assemblages</term>
<term>Mollusc</term>
<term>Mollusc assemblages</term>
<term>Mollusc species</term>
<term>Molluscan</term>
<term>Molluscan assemblages</term>
<term>Multiple correlation coefficient</term>
<term>Nesje kvamme</term>
<term>Nicole limondin</term>
<term>Organic matter</term>
<term>Other proxy data</term>
<term>Past years</term>
<term>Pollen data</term>
<term>Quantitative reconstructions</term>
<term>Quaternary</term>
<term>Quaternary research</term>
<term>Quaternary science reviews</term>
<term>Rapid warming</term>
<term>Reconstructed values</term>
<term>Snail</term>
<term>Snail assemblages</term>
<term>Standard errors</term>
<term>Temperature boreas</term>
<term>Temperature estimates</term>
<term>Temperature oscillations</term>
<term>Terrestrial deposits</term>
<term>Terrestrial molluscs</term>
<term>Total number</term>
<term>Total variance</term>
<term>Transfer functions</term>
<term>Variance</term>
<term>Vertigo</term>
<term>Western europe</term>
<term>Western norway</term>
<term>Younger dryas</term>
<term>Younger dryas event</term>
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<front><div type="abstract" xml:lang="en">Snail assemblages are used to estimate February and August temperatures during the past 10,000 years in western Europe. We find that a strong warming occurred after the Younger Dryas event, followed by several rapid cooling and warming events. These observations are in agreement with insect and pollen proxy data from the European continent and with estimates of sea‐surface temperature from the North Atlantic Ocean as well as with fluctuations of glaciers in western Norway. This study also confirms that terrestrial molluscs can provide reliable climatic data in conjunction with other proxy data.</div>
</front>
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