{"refrec":{"BRefID":220714,"RR":"<b>Hancock, J.M.; Kennedy, W.J.</b> (1993). The high Cretaceous ammonite fauna from Tercis, Landes, France. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 63</i>: 149-209","BEntID":212447,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 63</i>: 149-209","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Hancock, J.M.; Kennedy, W.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Hancock, J.M.; Kennedy, W.J.","Englishabstract":"The very high Cretaceous ammonite fauna from the area close to Tercis-les-Bains, south-west of Dax, Landes, France, has been revised. Even the lower (but not lowest) part of the Grande Carrière is already near the top of the Campanian, belonging to the Zone of <i>Nostoceras hyatti</i>. This assemblage- zone has yielded <i>Hauericeras fayoli</i> (DE GROSSOUVRE, 1894), <i>Pseudokossmaticeras brandti</i> (REDTENBACHER, 1873), <i>P. tercense</i> (SEUNES, 1892), <i>Pachydiscus (Pachydiscus) perfidus</i> (DE GROSSOUVRE, 1894), <i>P. (P.) subrobustus</i> (SEUNES, 1892), <i>P. (P.)</i> cf. <i>colligatus</i> (BINKHORST, 1861), <i>Nostoceras (Nostoceras) hyatti</i> STEPHENSON, 1941, <i>N. (N.) helicinum</i> (SHUMARD, 1861) and <i>Baculites leopoliensis</i> NOWAK, 1908. This assemblage is comparable to that found in the Zone of <i>Pseudokossmaticeras tercense</i> in the region of the Bay of Biscay, and to that found in the Zone of <i>Nostoceras pozaryskii</i> (here re-named the Zone of <i>Nostoceras hyatti</i>) of the Vistula Valley in Poland. The lowest occurrence of the overlying Zone of <i>Pachydiscus epiplectus</i>, and the lowest Maastrichtian recognisable in ammonite terms, is marked by the incoming of <i>Hoploscaphites constrictus</i> (J. SOWERBY, 1817). Other ammonite species from this zone are: <i>Pachydiscus (Pachydiscus) epiplectus</i> (REDTENBACHER, 1873) and <i>Pachydiscus (P.) neubergicus</i> (VON HAUER, 1858). A higher ammonite Zone of <i>Menuites</i> [<i>Anapachydiscus</i>] <i>fresviltensis</i> has been detected only from museum specimens from La Pointe to the north of the Grande Carrière. The ammonites known from this zone are: <i>Pachydiscus jacquoti jacquoti</i> (SEUNES, 1890a), <i>Pachydiscus (Pachydiscus) armenicus</i> ATABEKIAN & AKOPIAN, 1969, <i>Desmophyllites larteti</i> (SEUNES, 1892), <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816), <i>Glyptoxoceras rugatum</i> (FORBES, 1846). The highest Maastrichtian ammonite zone in the Biscay region is that of <i>Menuites</i> [<i>Anapachydiscus</i>] <i>terminus</i>. This has not been detected near Tercis.","AbstractOtherLang":"La faune d'ammonites de la fin du Crétacé récoltée dans la région de Tercis, au sud-ouest de Dax (Landes, France) est révisée. La partie inférieure (mais non les couches de base) de la Grande Carrière appartient déjà à la Zone à <i>Nostoceras hyatti</i>, ce qui indique un âge proche de la fin du Campanien. Cette zone d'assemblé réunit les espèces <i>Hauericeras fayoli</i> (DE GROSSOUVRE, 1894), <i>Pseudokossmaticeras brandti</i> (REDTENBACHER, 1873), <i>P. tercense</i> (SEUNES, 1892), <i>P. (P.)</i> cf. <i>colligatus</i> (BINKHORST, 1861), <i>Nostoceras (Nostoceras) hyatti</i> STEPHENSON, 1941, <i>N. (N.) helicinum</i> (SHUMARD, 1861) et <i>Baculites leopoliensis</i> NOWAK, 1908. Cet assemblage est comparable à celui de la Zone à <i>Pseudokossmaticeras tercense</i> dans la région du Golfe de Gascogne et à celui de la Zone à <i>Nostoceras pozaryskii</i> (dénommée ici de la Zone à <i>Nostoceras hyatti</i>) dans la vallée de la Vistule, en Pologne. La base de la Zone à <i>Pachydiscus epiplectus</i> sus-jacente et celle de l'étage Maastrichtien sont caractérisées par l'apparition d'<i>Hoploscaphites constrictus</i> (J, SOWERBY, 1817). D'autres espèces d'ammonites rencontrées dans cette zone sont: <i>Pachydiscus (Pachydiscus) epiplectus</i> (REDTENBACHER, 1873) et <i>Pachydiscus (P.) neubergicus</i> (VON HAUER, 1858). La Zone à <i>Anapachydiscus fresvillensis</i>, une zone d'ammonites plus élevée, n'a été identifiée que sur base de spécimens de collections provenant de La Pointe, au nord de la Grande Carrière. Les ammonites présentes dans cette zone sont: <i>Pachydiscus jacquoti jacquoti</i> (SEUNES, 1890a), <i>Pachydiscus (Pachydiscus) armenicus</i> ATABEKIAN & AKOPIAN, 1969, <i>Desmophyllites larteti</i> (SEUNES, 1892), <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816) <i>Glyptoxoceras rugatum</i> (FORBES, 1846). La zone d'ammonites la plus élevée du Maastrichtien dans la région de la Biscaye est celle à <i>Anapachydiscus terminus</i>. Elle n'a pas été observée aux environs de Tercis.","BibLvlCode":"AS","StandardTitle":"The high Cretaceous ammonite fauna from Tercis, Landes, France","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-02 08:58:19.190595","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Campanian, Maastrichtian, ammonites, zones, southwest France, Campanien, Maastrichtien, sud-ouest de la France. 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