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            <title xml:lang="en">Middle and Late Triassic radiolarians from northern Tibet: Implications for the Bayan Har Basin evolution § Radiolaires du Trias moyen et supérieur du Tibet septentrional : implications pour l'évolution du Basin Bayan Har</title>
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                <title xml:lang="en">Middle and Late Triassic radiolarians from northern Tibet: Implications for the Bayan Har Basin evolution § Radiolaires du Trias moyen et supérieur du Tibet septentrional : implications pour l'évolution du Basin Bayan Har</title>
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                <title level="j">Geobios</title>
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                <term xml:lang="fr">Triassic</term>
                <term xml:lang="fr">Radiolaria</term>
                <term xml:lang="fr">Bayan Har Group</term>
                <term xml:lang="fr">Biostratigraphy</term>
                <term xml:lang="fr">Paleogeography</term>
                <term xml:lang="fr">Hoh Xil Mots clés : Trias</term>
                <term xml:lang="fr">Radiolaires</term>
                <term xml:lang="fr">Groupe Bayan Har</term>
                <term xml:lang="fr">Biostratigraphie</term>
                <term xml:lang="fr">Paléogéographie</term>
                <term xml:lang="fr">Hoh Xil</term>
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              <p>During the Triassic, the Bayan Har Basin is a huge triangular basin surrounded by the North China Platform, South China Platform and Qingtang Terrane. It is filled by a Triassic turbidite sequence, the Bayan Har Group. For a long time, the series of Bayan Har Group in the eastern part of the basin were considered to be a Lower to Upper Triassic sequence, and in the western part, was attributed to the Upper Triassic. A well-preserved diversified radiolarian fauna was recovered from radiolarian chert and tuffite interbeds of the Bayan Har Group turbidites and adjacent stratigraphic units in the Hoh Xil area, northern Tibet. Sixty-seven species are identified and subdivided into two assemblages: late Anisian and early Carnian. Combined with the discovery of the Late Permian and Early Triassic turbidite in the Bayan Har Group in this area by Huang et al., it proves that all the Triassic is also present in the Bayan Har Group sequence in the western part. The evolution of the Bayan Har Basin may be traced back to the Late Permian. The massive sequence of the Bayan Har Group and its provenance indicate that the Kunlun and Qinling orogenic belts rapidly rise during the Middle-Late Triassic. The basin extended to the end of the Triassic, possibly locally to the Jurassic. # Résumé Durant le Trias, le basin Bayan Har est un large basin triangulaire entouré par la plate-forme de Chine du Nord, la plate-forme de Chine du Sud et le terrane Qingtang. Il est rempli d'une séquence de turbidites triasiques, le groupe Baya Har. Durant une longue période, les séries du groupe Baya Har dans la partie orientale du bassin ont été considérées comme étant une séquence du Trias inférieur à supérieur et dans la partie occidentale comme étant du Trias supérieur. Une faune bien conservée et diversifiée de radiolaires a été découverte dans des cherts radiolaritiques et des tuffites intercalées dans les turbidites du group Baya Har et dans les unités stratigraphiques adjacentes de la région Hoh Xil, Nord Tibet. Soixante sept espèces sont identifiées et subdivisées en deux assemblages : un Anisien supérieur et un Carnien inférieur. Associé avec la découverte par Huang et al. de turbidites du Permien supérieur et du Trias inférieur dans le groupe Baya Har dans cette région, cela prouve que la totalité du Trias est aussi présente dans le groupe Baya Har de la partie ouest du bassin. L'évolution du bassin Bayan Har peut être retracée depuis le Permien. La séquence massive du groupe Bayan Har et sa provenance indiquent que les ceintures orogéniques Qinling et Kunlun se soulèvent rapidement durant le Trias moyen et supérieur. Le bassin s'étend jusqu'à la fin du Trias, peut-être localement jusqu'au Jurassique. # 2009 Elsevier Masson SAS. Tous droits réservés.</p>
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