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Holocene climate as reflected by a malacological sequence at Verrières, France

Identifieur interne : 000538 ( France/Analysis ); précédent : 000537; suivant : 000539

Holocene climate as reflected by a malacological sequence at Verrières, France

Auteurs : Nicole Limondin [France] ; Denis Idier Rousseau [France]

Source :

RBID : ISTEX:EEC8DA8B0266E546E50D20E6C3D7099D7B554886

Descripteurs français

English descriptors

Abstract

Though numerous analyses have been made of Holocene pollen sequences, they come from similar environmental contexts, mainly peat deposits. Land snails can provide good palaeoecological and palaeoclimatical data in different drier environmental settings. The Verrières deposits, located in the Seine Valley, southeast of Paris, provide rich and abundant malacofaunas. We compare the well–defined local biostratigraphy with other mollusc stratigraphies from Burgundy, the closet site to the studied region. Multivariate analysis of the malacofaunas indicates that temperature and moisture did not always vary in parallel during the Holocene. On the other hand, Verrières malacofaunas reflect the main Holocene changes, as observed in the classical pollen series, confirming the reliability of the local biostratigraphy. The younger Dryas in Verrières was cold and cry. This was followed by the Preboreal phase, which is not well preserved at Verrières, but shows cool and humid conditions. The Boreal and Subboreal both show a cold and moist event bounded by two temperature phases. The Atlantic is also divided into two temperate phases by a cool and moist event. The Subatlantic shows temperature oscillations with cool peaks, but moisture shows a continuous trend to dryness.

Url:
DOI: 10.1111/j.1502-3885.1991.tb00152.x


Affiliations:


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ISTEX:EEC8DA8B0266E546E50D20E6C3D7099D7B554886

Le document en format XML

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<term>Abida</term>
<term>Abida secale</term>
<term>Abida secale drap abida</term>
<term>Acanthinula aculeata</term>
<term>Acroloxus lacustris</term>
<term>Aegopinella nitidula drap cochlodina laminata mont cochlodina</term>
<term>Alluvial</term>
<term>Angustior</term>
<term>Anisus leucostomus millet aplexa hypnorum</term>
<term>Aquatic</term>
<term>Aquatic species</term>
<term>Aquatic taxa</term>
<term>Armiger crista</term>
<term>Assemblage</term>
<term>Boreal</term>
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<term>Bradybaena fruticum</term>
<term>Bythinia tentaculata</term>
<term>Candidula</term>
<term>Candidula unifasciata poiret pupilla muscorum</term>
<term>Carychium</term>
<term>Cecilioides acicula</term>
<term>Cepaea</term>
<term>Cepaea nemoralis</term>
<term>Chalky gravels</term>
<term>Chondrula</term>
<term>Chondrula tridens</term>
<term>Clausilia</term>
<term>Climatic</term>
<term>Climatic information</term>
<term>Climatic trends</term>
<term>Cochlicopa</term>
<term>Cochlodina</term>
<term>Coeurs</term>
<term>Coeurs section</term>
<term>Cold climate</term>
<term>Coordination archeologique autoroute</term>
<term>Correspondence analysis</term>
<term>Discus rotundatus</term>
<term>Drap</term>
<term>Dryas</term>
<term>Ecological</term>
<term>Ecological characteristics</term>
<term>Ecological group</term>
<term>Ecological groups</term>
<term>Elegans</term>
<term>Environmental variations</term>
<term>Euconulus</term>
<term>Forest taxa</term>
<term>Galba</term>
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<term>General data</term>
<term>Generalized inundation</term>
<term>Genesii</term>
<term>Gredler</term>
<term>Groups species</term>
<term>Gyraulus albus</term>
<term>Helicella</term>
<term>Helicella itala</term>
<term>Helicigona lapicida</term>
<term>Holocene</term>
<term>Holocene climate</term>
<term>Holocene land snaik</term>
<term>Holocene land snails</term>
<term>Holocene sequences</term>
<term>Human activity</term>
<term>Inundation</term>
<term>Itala</term>
<term>Jeffreys</term>
<term>Krier</term>
<term>Land snails</term>
<term>Limaces succinea oblonga drap carychium tridentatum risso vertigo angustior jeffreys euconulus alderi</term>
<term>Limnaea stagnalis</term>
<term>Limondin</term>
<term>Local biostratigraphy</term>
<term>Loess sequence</term>
<term>Lozek</term>
<term>Malacofaunas</term>
<term>Malacofaunas show</term>
<term>Malacological</term>
<term>Malacological analysis</term>
<term>Malacological assemblages</term>
<term>Malacological samples</term>
<term>Malacological sequence</term>
<term>Marshy environment</term>
<term>Miill</term>
<term>Moist event</term>
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<term>Mollusc</term>
<term>Molluscan assemblages</term>
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<term>Negative signs</term>
<term>Nicole</term>
<term>Nicole limondin</term>
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<term>Northern part</term>
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<term>Open environment</term>
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<term>Planorbis carinatus</term>
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<term>Planorbis contortus</term>
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<term>Right bank</term>
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<term>Rousseau boreas</term>
<term>Rousseau puisscgur</term>
<term>Rousseau puissegur</term>
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<term>Secale</term>
<term>Second phase</term>
<term>Seine</term>
<term>Seine valley</term>
<term>Significant erosion</term>
<term>Sphyradium doliolum brug helicodonta obuoluta</term>
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<term>Stratigraphical level</term>
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<term>Temperate climate</term>
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<term>Acroloxus lacustris</term>
<term>Aegopinella nitidula drap cochlodina laminata mont cochlodina</term>
<term>Alluvial</term>
<term>Angustior</term>
<term>Anisus leucostomus millet aplexa hypnorum</term>
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<term>Aquatic species</term>
<term>Aquatic taxa</term>
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<term>Boreal</term>
<term>Boreas</term>
<term>Bradybaena fruticum</term>
<term>Bythinia tentaculata</term>
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<term>Candidula unifasciata poiret pupilla muscorum</term>
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<term>Cepaea</term>
<term>Cepaea nemoralis</term>
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<term>Cochlicopa</term>
<term>Cochlodina</term>
<term>Coeurs</term>
<term>Coeurs section</term>
<term>Cold climate</term>
<term>Coordination archeologique autoroute</term>
<term>Correspondence analysis</term>
<term>Discus rotundatus</term>
<term>Drap</term>
<term>Dryas</term>
<term>Ecological</term>
<term>Ecological characteristics</term>
<term>Ecological group</term>
<term>Ecological groups</term>
<term>Elegans</term>
<term>Environmental variations</term>
<term>Euconulus</term>
<term>Forest taxa</term>
<term>Galba</term>
<term>Galba palustris</term>
<term>General data</term>
<term>Generalized inundation</term>
<term>Genesii</term>
<term>Gredler</term>
<term>Groups species</term>
<term>Gyraulus albus</term>
<term>Helicella</term>
<term>Helicella itala</term>
<term>Helicigona lapicida</term>
<term>Holocene</term>
<term>Holocene climate</term>
<term>Holocene land snaik</term>
<term>Holocene land snails</term>
<term>Holocene sequences</term>
<term>Human activity</term>
<term>Inundation</term>
<term>Itala</term>
<term>Jeffreys</term>
<term>Krier</term>
<term>Land snails</term>
<term>Limaces succinea oblonga drap carychium tridentatum risso vertigo angustior jeffreys euconulus alderi</term>
<term>Limnaea stagnalis</term>
<term>Limondin</term>
<term>Local biostratigraphy</term>
<term>Loess sequence</term>
<term>Lozek</term>
<term>Malacofaunas</term>
<term>Malacofaunas show</term>
<term>Malacological</term>
<term>Malacological analysis</term>
<term>Malacological assemblages</term>
<term>Malacological samples</term>
<term>Malacological sequence</term>
<term>Marshy environment</term>
<term>Miill</term>
<term>Moist event</term>
<term>Molesmes sample</term>
<term>Mollusc</term>
<term>Molluscan assemblages</term>
<term>Mollusques continentaux</term>
<term>Multivariate analysis</term>
<term>Negative pole</term>
<term>Negative signs</term>
<term>Nicole</term>
<term>Nicole limondin</term>
<term>Nitidus</term>
<term>Northern part</term>
<term>Obscura</term>
<term>Open environment</term>
<term>Open ground</term>
<term>Open ground species</term>
<term>Other ones</term>
<term>Oxychilus</term>
<term>Oxychilus cellarius</term>
<term>Paludal species</term>
<term>Peat deposits</term>
<term>Planorbis</term>
<term>Planorbis carinatus</term>
<term>Planorbis complanatus</term>
<term>Planorbis contortus</term>
<term>Planorbis corneus</term>
<term>Pollen series</term>
<term>Pomatias elegans</term>
<term>Positive pole</term>
<term>Puissegur</term>
<term>Pygmaeum</term>
<term>Right bank</term>
<term>Risso</term>
<term>Rousseau boreas</term>
<term>Rousseau puisscgur</term>
<term>Rousseau puissegur</term>
<term>Sand deposits</term>
<term>Secale</term>
<term>Second phase</term>
<term>Seine</term>
<term>Seine valley</term>
<term>Significant erosion</term>
<term>Sphyradium doliolum brug helicodonta obuoluta</term>
<term>Stratigraphic</term>
<term>Stratigraphic columns</term>
<term>Stratigraphic columns cpoo1</term>
<term>Stratigraphical</term>
<term>Stratigraphical level</term>
<term>Stratigraphy</term>
<term>Succinea</term>
<term>Taxon</term>
<term>Temperate</term>
<term>Temperate climate</term>
<term>Theoretical threshold</term>
<term>Tree line</term>
<term>Trichia</term>
<term>Trichia hispida</term>
<term>Upper part</term>
<term>Vallonia</term>
<term>Vallonia costata</term>
<term>Vallonia pulchella</term>
<term>Valuata piscinalis</term>
<term>Verrieres</term>
<term>Verrieres malacofaunas</term>
<term>Verrieres record</term>
<term>Verrieres site</term>
<term>Verrikres</term>
<term>Vertigo</term>
<term>Vertigo angustior</term>
<term>Younger dryas</term>
<term>Zonitoides</term>
<term>Zonitoides nitidus</term>
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<front>
<div type="abstract" xml:lang="en">Though numerous analyses have been made of Holocene pollen sequences, they come from similar environmental contexts, mainly peat deposits. Land snails can provide good palaeoecological and palaeoclimatical data in different drier environmental settings. The Verrières deposits, located in the Seine Valley, southeast of Paris, provide rich and abundant malacofaunas. We compare the well–defined local biostratigraphy with other mollusc stratigraphies from Burgundy, the closet site to the studied region. Multivariate analysis of the malacofaunas indicates that temperature and moisture did not always vary in parallel during the Holocene. On the other hand, Verrières malacofaunas reflect the main Holocene changes, as observed in the classical pollen series, confirming the reliability of the local biostratigraphy. The younger Dryas in Verrières was cold and cry. This was followed by the Preboreal phase, which is not well preserved at Verrières, but shows cool and humid conditions. The Boreal and Subboreal both show a cold and moist event bounded by two temperature phases. The Atlantic is also divided into two temperate phases by a cool and moist event. The Subatlantic shows temperature oscillations with cool peaks, but moisture shows a continuous trend to dryness.</div>
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