L'Eemien et le Pléistocène moyen récent fluvio-marin et continental de la vallée de la Seine de Cléon au Havre (Normandie)
Identifieur interne : 001531 ( Main/Exploration ); précédent : 001530; suivant : 001532L'Eemien et le Pléistocène moyen récent fluvio-marin et continental de la vallée de la Seine de Cléon au Havre (Normandie)
Auteurs : Jean-Pierre Lautridou [France] ; Patrick Auguste [France] ; Gérard Carpentier [France] ; Jean-Marie Cordy [France] ; Patrick Lebret [France] ; Claude Lechevalier [France] ; Dominique Lefebvre [France]Source :
- Quaternaire : (Paris) [ 1142-2904 ] ; 2003.
Descripteurs français
- Pascal (Inist)
- Corrélation stratigraphique, Dune, Estuaire, Eémien, France, Haute-Normandie, Interglaciaire, Paléobiogéographie, Paléontologie, Pléistocène, Périglaciaire, Quaternaire, Sable, Seine, Vallée Seine, Normandie, Seine-Maritime, Eémien, Pléistocène moyen, Donnée nouvelle, Altitude, Dune, Milieu fluviatile, Milieu marin, Milieu continental, Sédimentation estuaire, Période interglaciaire, Eustatisme.
- Wicri :
- geographic : France, Haute-Normandie.
- topic : Estuaire, Milieu marin.
English descriptors
- KwdEn :
- Dune, Eemian, Estuary, France, Haute-Normandie, Interglacial, Normandy, Palaeobiogeography, Palaeontology, Periglacial features, Pleistocene, Quaternary, Sand, Seine, Seine Valley, Seine-Maritime France, Stratigraphic correlation, altitude, dunes, estuarine sedimentation, eustacy, fluvial environment, interglacial periods, marine environment, middle Pleistocene, new data, terrestrial environment.
Abstract
New data and especially paleontological analysis allows the correlations between the formations of Rouen (upstream) and Le Havre (downstream) in the Seine Valley. The key formation is represented by a palaeoestuary of MIS 7 with an altitude that can reach 15 m O.D. Another formation, the "sables lités", alluvial (Tourville) or fluvio-marine (Tancarville), has been deposited just after, at the beginning of MIS 6. The Eemian is characterised by a dune (MIS 5e optimum) at Tancarville (4-14 m O.D.) and by a regressive palaeobeach (Le Havre) of the late MIS 5e, which altitude is lower than 0 m O.D. The beginning of the MIS 6 ("sables lités" formation) is in relation with a marine level identical to the level of the palaeostuary (MIS 7) below. So there was no marine regression during the early MIS 6 unlike the Early Weichselian (MIS substages 5 a-d).
Url:
Affiliations:
- France
- Basse-Normandie, Haute-Normandie, Hauts-de-France, Nord-Pas-de-Calais, Région Normandie, Île-de-France
- Caen, Mont Saint Aignan, Nanterre, Villeneuve D'Ascq
Links toward previous steps (curation, corpus...)
- to stream PascalFrancis, to step Corpus: 000295
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- to stream PascalFrancis, to step Corpus: 000300
- to stream PascalFrancis, to step Curation: 000415
- to stream PascalFrancis, to step Checkpoint: 000277
- to stream Main, to step Merge: 001568
- to stream Main, to step Curation: 001531
Le document en format XML
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wicri:level="3"><inist:fA14 i1="01"><s1>M2C Caen-Rouen, CNRS, Rue des Tilleuls</s1><s2>14000 Caen</s2><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>7 aut.</sZ></inist:fA14><country>France</country><placeName><region type="region" nuts="2">Région Normandie</region><region type="old region" nuts="2">Basse-Normandie</region><settlement type="city">Caen</settlement></placeName></affiliation></author><author><name sortKey="Auguste, Patrick" sort="Auguste, Patrick" uniqKey="Auguste P" first="Patrick" last="Auguste">Patrick Auguste</name><affiliation wicri:level="3"><inist:fA14 i1="02"><s1>CERP/EA 8018 Laboratoire de Préhistoire et Quaternaire, Université des Sciences et Technologies de Lillel, Géographie</s1><s2>59655 Villeneuve D'Ascq</s2><s3>FRA</s3><sZ>2 aut.</sZ></inist:fA14><country>France</country><placeName><region type="region" nuts="2">Hauts-de-France</region><region type="old region" nuts="2">Nord-Pas-de-Calais</region><settlement type="city">Villeneuve D'Ascq</settlement></placeName></affiliation></author><author><name sortKey="Carpentier, Gerard" sort="Carpentier, Gerard" uniqKey="Carpentier G" first="Gérard" last="Carpentier">Gérard Carpentier</name><affiliation wicri:level="3"><inist:fA14 i1="01"><s1>M2C Caen-Rouen, CNRS, Rue des Tilleuls</s1><s2>14000 Caen</s2><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>7 aut.</sZ></inist:fA14><country>France</country><placeName><region type="region" nuts="2">Région Normandie</region><region type="old region" nuts="2">Basse-Normandie</region><settlement type="city">Caen</settlement></placeName></affiliation></author><author><name sortKey="Cordy, Jean Marie" sort="Cordy, Jean Marie" uniqKey="Cordy J" first="Jean-Marie" last="Cordy">Jean-Marie Cordy</name><affiliation wicri:level="1"><inist:fA14 i1="03"><s1>Université Sart Tilman, Géologie, Place du xx août 7</s1><s2>4000 Liège</s2><s3>FRA</s3><sZ>4 aut.</sZ></inist:fA14><country>France</country><wicri:noRegion>4000 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Nanterre</s2><s3>FRA</s3><sZ>6 aut.</sZ></inist:fA14><country>France</country><placeName><region type="region" nuts="2">Île-de-France</region><settlement type="city">Nanterre</settlement></placeName></affiliation></author><author><name sortKey="Lefebvre, Dominique" sort="Lefebvre, Dominique" uniqKey="Lefebvre D" first="Dominique" last="Lefebvre">Dominique Lefebvre</name><affiliation wicri:level="3"><inist:fA14 i1="01"><s1>M2C Caen-Rouen, CNRS, Rue des Tilleuls</s1><s2>14000 Caen</s2><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>7 aut.</sZ></inist:fA14><country>France</country><placeName><region type="region" nuts="2">Région Normandie</region><region type="old region" nuts="2">Basse-Normandie</region><settlement type="city">Caen</settlement></placeName></affiliation></author></analytic><series><title level="j" type="main">Quaternaire : (Paris)</title><title level="j" type="abbreviated">Quaternaire : (Paris)</title><idno type="ISSN">1142-2904</idno><imprint><date when="2003">2003</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Quaternaire : (Paris)</title><title level="j" type="abbreviated">Quaternaire : (Paris)</title><idno type="ISSN">1142-2904</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Dune</term><term>Eemian</term><term>Estuary</term><term>France</term><term>Haute-Normandie</term><term>Interglacial</term><term>Normandy</term><term>Palaeobiogeography</term><term>Palaeontology</term><term>Periglacial features</term><term>Pleistocene</term><term>Quaternary</term><term>Sand</term><term>Seine</term><term>Seine Valley</term><term>Seine-Maritime France</term><term>Stratigraphic correlation</term><term>altitude</term><term>dunes</term><term>estuarine sedimentation</term><term>eustacy</term><term>fluvial environment</term><term>interglacial periods</term><term>marine environment</term><term>middle Pleistocene</term><term>new data</term><term>terrestrial environment</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Corrélation stratigraphique</term><term>Dune</term><term>Estuaire</term><term>Eémien</term><term>France</term><term>Haute-Normandie</term><term>Interglaciaire</term><term>Paléobiogéographie</term><term>Paléontologie</term><term>Pléistocène</term><term>Périglaciaire</term><term>Quaternaire</term><term>Sable</term><term>Seine</term><term>Vallée Seine</term><term>Normandie</term><term>Seine-Maritime</term><term>Eémien</term><term>Pléistocène moyen</term><term>Donnée nouvelle</term><term>Altitude</term><term>Dune</term><term>Milieu fluviatile</term><term>Milieu marin</term><term>Milieu continental</term><term>Sédimentation estuaire</term><term>Période interglaciaire</term><term>Eustatisme</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>France</term><term>Haute-Normandie</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Estuaire</term><term>Milieu marin</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">New data and especially paleontological analysis allows the correlations between the formations of Rouen (upstream) and Le Havre (downstream) in the Seine Valley. The key formation is represented by a palaeoestuary of MIS 7 with an altitude that can reach 15 m O.D. Another formation, the "sables lités", alluvial (Tourville) or fluvio-marine (Tancarville), has been deposited just after, at the beginning of MIS 6. The Eemian is characterised by a dune (MIS 5e optimum) at Tancarville (4-14 m O.D.) and by a regressive palaeobeach (Le Havre) of the late MIS 5e, which altitude is lower than 0 m O.D. The beginning of the MIS 6 ("sables lités" formation) is in relation with a marine level identical to the level of the palaeostuary (MIS 7) below. So there was no marine regression during the early MIS 6 unlike the Early Weichselian (MIS substages 5 a-d).</div></front></TEI><affiliations><list><country><li>France</li></country><region><li>Basse-Normandie</li><li>Haute-Normandie</li><li>Hauts-de-France</li><li>Nord-Pas-de-Calais</li><li>Région Normandie</li><li>Île-de-France</li></region><settlement><li>Caen</li><li>Mont Saint Aignan</li><li>Nanterre</li><li>Villeneuve D'Ascq</li></settlement></list><tree><country name="France"><region name="Région Normandie"><name sortKey="Lautridou, Jean Pierre" sort="Lautridou, Jean Pierre" uniqKey="Lautridou J" first="Jean-Pierre" last="Lautridou">Jean-Pierre Lautridou</name></region><name sortKey="Auguste, Patrick" sort="Auguste, Patrick" uniqKey="Auguste P" first="Patrick" last="Auguste">Patrick Auguste</name><name sortKey="Carpentier, Gerard" sort="Carpentier, Gerard" uniqKey="Carpentier G" first="Gérard" last="Carpentier">Gérard Carpentier</name><name sortKey="Cordy, Jean Marie" sort="Cordy, Jean Marie" uniqKey="Cordy J" first="Jean-Marie" last="Cordy">Jean-Marie Cordy</name><name sortKey="Lebret, Patrick" sort="Lebret, Patrick" uniqKey="Lebret P" first="Patrick" last="Lebret">Patrick Lebret</name><name sortKey="Lechevalier, Claude" sort="Lechevalier, Claude" uniqKey="Lechevalier C" first="Claude" last="Lechevalier">Claude Lechevalier</name><name sortKey="Lefebvre, Dominique" sort="Lefebvre, Dominique" uniqKey="Lefebvre D" first="Dominique" last="Lefebvre">Dominique Lefebvre</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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