EdenteV2, France, Analysis, bibRecord, 000517

West-European terrestrial molluscs assemblages of isotopic stage 11 (Middle Pleistocene): climatic implications

Identifieur interne : 000517 ( France/Analysis ); précédent : 000516; suivant : 000518

West-European terrestrial molluscs assemblages of isotopic stage 11 (Middle Pleistocene): climatic implications

Auteurs : Denis-Didier Rousseau [États-Unis] ; Jean-Jacques Puisségur [France] ; François Lécolle [États-Unis, France]

Source :

Palaeogeography, Palaeoclimatology, Palaeoecology [ 0031-0182 ] ; 1992.

RBID : ISTEX:3BED487DA41A7115F26DCE81BF8E6B12A82624FB

Descripteurs français

Wicri :
- topic : Mollusque.

English descriptors

Abstract

Abstract: Tufa deposits in the Seine and the Avelasse Valleys have yielded numerous molluscsassemblages belonging to the Lyrodiscus Biome. These malacofaunas, primilarily indicative of forest which developed under a warm climate, have no present-day counterpart. The biostratigraphical study of several localities based on new investigations at Vernon (Seine Valley) and Arrest (Avelasse Valley) and a reexamination of the faunas from St Pierre-lès-Elbeuf suggests the allocation of a holsteinian age. This is supported by U/Th dates for Vernon and the stratigraphy of the loess sequence of St Pierre-lès-Elbeuf. Similar assemblages yielded by tufas of the same age in England and Germany indicate that the Lyrodiscus Biome was widespread. The warm climate recorded by the molluscs of the tufa deposits is aggreement with pollen and marine analyses for the isotopic stage 11 (362–423 kyr B.P.). In this way, the Lyrodiscus Biome appears as an interesting marker for the continental Quaternary in Western Europe. If the occurrence of these particular molluscan assemblages is due to climate, refuges from the declined Tertiary biota, from which i.e. R. (Lyrodiscus) could have emigrated, also needed to exist.

Url:

https://api.istex.fr/document/3BED487DA41A7115F26DCE81BF8E6B12A82624FB/fulltext/pdf

DOI: 10.1016/0031-0182(92)90132-O

Affiliations:

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ISTEX:3BED487DA41A7115F26DCE81BF8E6B12A82624FB

Le document en format XML

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<author><name sortKey="Puissegur, Jean Jacques" sort="Puissegur, Jean Jacques" uniqKey="Puissegur J" first="Jean-Jacques" last="Puisségur">Jean-Jacques Puisségur</name>
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<author><name sortKey="Lecolle, Francois" sort="Lecolle, Francois" uniqKey="Lecolle F" first="François" last="Lécolle">François Lécolle</name>
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<term>Skertchlyi</term>
<term>Species ecol</term>
<term>Species levels</term>
<term>Succinea</term>
<term>Taxon</term>
<term>Terrestrial molluscs assemblages</term>
<term>Tertiary biota</term>
<term>Total number</term>
<term>Travertine</term>
<term>Tufa</term>
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<term>Vallonia costata</term>
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<term>Assemblage</term>
<term>Autumn perihelion</term>
<term>Azeca goodalli</term>
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<term>Biological association</term>
<term>Biome</term>
<term>British quaternary studies</term>
<term>Canary archipelago</term>
<term>Carychium</term>
<term>Carychium tridentatum</term>
<term>Clausilia</term>
<term>Climatic</term>
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<term>Skertchlyi</term>
<term>Species ecol</term>
<term>Species levels</term>
<term>Succinea</term>
<term>Taxon</term>
<term>Terrestrial molluscs assemblages</term>
<term>Tertiary biota</term>
<term>Total number</term>
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<term>Vallonia costata</term>
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<front><div type="abstract" xml:lang="en">Abstract: Tufa deposits in the Seine and the Avelasse Valleys have yielded numerous molluscsassemblages belonging to the Lyrodiscus Biome. These malacofaunas, primilarily indicative of forest which developed under a warm climate, have no present-day counterpart. The biostratigraphical study of several localities based on new investigations at Vernon (Seine Valley) and Arrest (Avelasse Valley) and a reexamination of the faunas from St Pierre-lès-Elbeuf suggests the allocation of a holsteinian age. This is supported by U/Th dates for Vernon and the stratigraphy of the loess sequence of St Pierre-lès-Elbeuf. Similar assemblages yielded by tufas of the same age in England and Germany indicate that the Lyrodiscus Biome was widespread. The warm climate recorded by the molluscs of the tufa deposits is aggreement with pollen and marine analyses for the isotopic stage 11 (362–423 kyr B.P.). In this way, the Lyrodiscus Biome appears as an interesting marker for the continental Quaternary in Western Europe. If the occurrence of these particular molluscan assemblages is due to climate, refuges from the declined Tertiary biota, from which i.e. R. (Lyrodiscus) could have emigrated, also needed to exist.</div>
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West-European terrestrial molluscs assemblages of isotopic stage 11 (Middle Pleistocene): climatic implications

West-European terrestrial molluscs assemblages of isotopic stage 11 (Middle Pleistocene): climatic implications

Source :

Descripteurs français

English descriptors

Abstract

Links toward previous steps (curation, corpus...)

Links to Exploration step

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri