{"refrec":{"BRefID":219975,"RR":"<b>Kennedy, W.J.</b> (1986). The ammonite fauna of the type Maastrichtian with a revision of Ammonites colligatus BINKHORST, 1861. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 56</i>: 151-268","BEntID":211708,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 56</i>: 151-268","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kennedy, W.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kennedy, W.J.","Englishabstract":"A revision of the ammonites from Maastricht and adjacent parts of Limburg and Liège based on the BINKHORST Collection in the Museum für Naturkunde, Berlin, the collections of the Institut Royal des Sciences naturelles de Belgique, Brussels, (including material described by A. DE GROSSOUVRE in 1908) and the Natuurhistorisch Museum, Maastricht, revealed the following sequence of faunas. The youngest Campanian ammonite from the Vaals Formation is a specimen of <i>Hopliloplacenticeras marroti</i> (COQUAND, 1859) from Vijlen, Cotessen (Zuid-Limburg, The Netherlands); this is a typical lower Upper Campanian species. The Zeven Wegen Chalk yields <i>Baculites</i> at several localities and upper Upper Campanian <i>Hopliloplacenticeras coesfeldiense</i> (SCHLUETER, 1867) and <i>Trachyscaphites spiniger</i> (SCHLUETER, 1872) at Vijlenerbosch (Zuid-Limburg, The Netherlands): these are <i>Bostrychoceras polyplocum</i> Zone species. An unspecified horizon within the Gulpen Formation of Schneeberg, north of Vaals yields the lower Lower Maastrichtian <i>Acanthoscaphites tridens</i> (KNER, 1848); the same species occurs at Vaals. No ammonites were seen from the Beutenaken Chalk, but the Vijlen Chalk yields phosphatised and unphosphatised <i>Baculites</i> at a number of localities, <i>Hoploscaphites tenuistriatus</i> (KNER, 1848) at Mesch (Zuid-Limburg, The Netherlands), and there is a record of <i>Pachydiscus</i> sp. from Hallembaye, Liège. No ammonites were seen from the Lixhe or Lanaye Chalks. The base of the Valkenburg Chalk yields phosphatised <i>Baculites anceps</i> LAMARCK, 1822, and phosphatised <i>Baculites</i> sp. at the Blankenberg Quarry, Cadier en Keer (Zuid-Limburg, The Netherlands). No ammonites were seen from the Gronsveld, Schiepersberg or Emael Chalks. Ammonites known to be from the Nekum Chalk, mostly from the environs of Maastricht, are <i>Anapachydiscus fresvillensis</i> (SEUNES, 1890). <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816), <i>Baculites vertebralis</i> LAMARCK, 1801, <i>B. anceps</i> LAMARCK, 1822 and <i>Hoploscaphites constrictus</i> (J. SOWERBY. 1817). There are two records of <i>Sphenodiscus binkhorsti</i> BOEHM, 1898 from this unit. Ammonites known to be from the Meerssen Chalk are <i>Nostoceras</i> sp., <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816), <i>Baculites vertebralis</i> LAMARCK, 1801, <i>B. anceps</i> LAMARCK, 1822 and <i>Hoploscaphites constrictus</i> (J. SOWERBY, 1817). The upper part of the Meerssen Chalk only yields frequent <i>Sphenodiscus binkhorsti</i> BOEHM, 1898 and the <i>crassus</i> form of <i>Hoploscaphites constrictus</i>. A single specimen of <i>Eubaculites lyelli</i> (d'ORBIGNY, 1847) from Maastricht is from either the Nekum of the Meerssen Chalk. Ammonites from the upper part of the \"Calcaire de Kunraed\" are <i>Saghalinites</i> sp., <i>Pachydiscus (Pachydiscus) gollevillensis</i> (d'ORBIGNY, 1850), <i>P. (P.)</i> cf. <i>jacquoti</i> SEUNES, 1890, <i>Anapachydiscus fresvillensis</i> (SEUNES, 1890), <i>Glyptoxoceras</i> cf. <i>subcompressum</i> (FORBES, 1846), <i>G</i>. cf. <i>circulare</i> SHIMIZU, 1935, <i>G</i>. sp., <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816), <i>Baculites vertebralis</i> LAMARCK, 1801, which is common, <i>B. anceps</i> LAMARCK, 1822, <i>Hoploscaphites constrictus</i> (J. SOWERBY, 1817), <i>H. felderi</i> sp. nov., <i>H. pungens</i> (BINKHORST, 1861). <i>Acanthoscaphites verneuilianus</i> (d'ORBIGNY, 1841) and <i>Acanthoscaphites</i> sp. These ammonites records are in accord with recent work on the belemnites of the region (SCHULZ and SCHMID, 1983) that has shown the Zeven Wegen to Beutenaken Chalk to be Lower Maastrichtian, the Vijlen to lower Meerssen Chalk to be Upper Maastrichtian, <i>Belemnitella junior</i> Zone and only the upper part of the Meerssen Chalk to be Upper Maastrichtian, <i>Belemnella casimirovensis</i> Zone. The upper part of the \"Calcaire de Kunraed\" yields Upper Maastrichtian ammonites that show it to be older than the upper part of the Meerssen Chalk, compatible with microfaunal work by VILLAIN (1977) and the presence of belemnites of the <i>Belemnitella junior</i> Zone but <i>not</i> of the <i>Belemnella casimirovensis</i> Zone. Also included in this work is a revision of the classic Maastrichtian ammonite <i>Pachydiscus colligatus</i> BINKHORST, 1861. The syntypes are shown to belong to two genera, <i>Pachydiscus</i> and <i>Anapachydiscus</i>, and to at least four species. The lectotype, herein designated in accordance with customary useage, is shown to be from the Upper Campanian of Jauche (Brabant, Belgium).","AbstractOtherLang":"La révision des Ammonites de Maastricht et des régions avoisinantes du Limbourg et de la province de Liège, basée sur la collection BINKHORST du Museum für Naturkunde, Berlin, sur les collections de l'Institut royal des Sciences naturelles de Belgique, Bruxelles (comprenant des spécimens décrits par A. DE GROSSOUVRE en 1908) et celles du Natuurhistorisch Museum, Maastricht, a permis d'établir la séquence de faunes ci-après. L'Ammonite la plus jeune du Campanien de la Formation de Vaals est un exemplaire d'<i>Hoplitoplacenticeras marroti</i> (CoQUAND, 1859) de Vijlen, Cotessen (Zuid-Limburg, Pays-Bas), une espèce typique de la partie inférieure du Campanien Supérieur. Le «Zeven Wegen Chalk» contient des spécimens de <i>Baculites</i> sp. à plusieurs endroits et <i>Hoplitoplacenticeras coesfeldiense</i> (SCHLUETER, 1867) et <i>Trachyscaphites spiniger</i> (SCHLUETER, 1872), de la partie supérieure du Campanien Supérieur, à Vijlenerbosch (Zuid-Limburg, Pays-Bas): il s'agit d'espèces de la Zone à <i>Bostrychoceras polyplocum</i>. Un horizon non spécifié de la Formation de Gulpen du Schneeberg, au nord de Vaals (Zuid-Limburg, Pays-Bas) livre <i>Acanthoscaphites tridens</i> (KNER, 1848), espèce connue de la partie inférieure du Maastrichtien Inférieur. La même espèce a été retrouvée à Vaals. Aucune Ammonite du «Beutenaken Chalk» n'a été étudiée, mais le «Vijlen Chalk» a produit des <i>Baculites</i> sp. phosphatés ou non dans plusieurs localités, <i>Hoploscaphites tenuistriatus</i> (KNER, 1848) à Mesch (Zuid-Limburg, Pays-Bas) et <i>Pachydiscus</i> sp. est connu à Hallembaye (Liège). Aucune Ammonite n'a été étudiée ni du «Lixhe Chalk», ni du «Lanaye Chalk». La base du «Valkenburg Chalk» produit des exemplaires phosphatés de <i>Baculites anceps</i> LAMARCK, 1822 et de <i>Baculites</i> sp. à la carrière Blankenberg, Cadier, en Keer (Zuid-Limburg, Pays-Bas). Aucune Ammonite n'a été étudiée du «Gronsveld Chalk». du «Schiepersberg Chalk» ou de l'«Emael Chalk». Les Ammonites du «Nekum Chalk », en majeure partie des environs immédiats de Maastricht, appartiennent aux espèces suivantes: <i>Anapachydiscus fresvillensis</i> (SEUNES, 1890), <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816), <i>Baculites vertebralis</i> LAMARCK, 1801, <i>B. anceps</i> LAMARCK, 1822 et <i>Hoploscaphites constrictus</i> (S. SOWERBY, 1817). Deux spécimens de <i>Sphenodiscus binkhorsti</i> BOEHM, 1898 sont mentionnés de cette unité. Les Ammonites connues comme étant du «Meerssen Chalk» sont: <i>Nostoceras</i> sp., <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816), <i>Baculites vertebralis</i> LAMARCK. 1801. <i>B. anceps</i> LAMARCK, 1822 et <i>Hoploscaphites constrictus</i> (J. SOWERBY, 1817). La partie supérieure du «Meerssen Chalk» contient seulement de nombreux <i>Sphenodiscus binkhorsti</i> BOEHM, 1898 et la forme <i>crassus</i> de <i>Hoploscaphites constrictus</i>. Un exemplaire unique d'<i>Eubaculites lyelli</i> (d'ORBIGNY, 1847) provient du «Nekum Chalk» ou du «Meerssen Chalk» à Maastricht. Les Ammonites de la partie supérieure du «Calcaire de Kunraed» sont les suivantes: <i>Saghalinites</i> sp., <i>Pachydiscus (Pachydiscus) gollevillensis</i> (d'ORBIGNY. 1850). <i>P. (P.)</i> cf. <i>jacquoti</i> SEUNES, 1890, <i>Anapachydiscus fresvillensis</i> (SEUNES. 1890), <i>Glyptoxoceras</i> cf. <i>subcompressum</i> (FORBES, 1846), <i>Gl</i>. cf. <i>circulare</i> SHIMIZU, 1935, <i>Gl</i>. sp., <i>Diplomoceras cylindraceum</i> (DEFRANCE, 1816), <i>Baculites vertebralis</i> LAMARCK, 1801, qui y est fréquent, <i>B. anceps</i> LAMARCK, 1822, <i>Hoploscaphites constrictus</i> (J. SOWERBY, 1817), <i>H. felderi</i> sp. nov., <i>H. pungens</i> (BINKHORST, 1861), <i>Acanthoscaphïtes verneuilianus</i> (d'ORBIGNY, 1841) et <i>Ac.</i> sp. Ces données concernant les Ammonites de Maastricht sont en accord avec les travaux récents sur les Belemnites de la région (SCHULZ et SCHMID, 1983). Ceux-ci ont démontré la présence du Maastrichtien Inférieur du «Zeven Wegen Chalk» au «Beutenaken Chalk», la présence du Maastrichtien Supérieur, Zone à <i>Belemnitella junior</i>, du «Vijlen Chalk» à la partie inférieure du «Meerssen Chalk», et qu'uniquement la partie supérieure du «Meerssen Chalk» appartient au Maastrichtien Supérieur, Zone à <i>Belemnella casimirovensis</i>. La partie supérieure du «Calcaire de Kunraed» contient des Ammonites du Maastrichtien Supérieur, plus ancien que celui de la partie supérieure du «Meerssen Chalk». Ceci est en accord avec les travaux micropaléontologiques de VILLAIN (1977), la présence de Bélemnites de la Zone à <i>Belemnites junior</i> et l'absence de celles de la Zone à <i>Belemnites casimirovensis</i>. Ce travail contient en outre une révision de <i>Pachydiscus colligatus</i> BINKHORST, 1861. Ammonite classique du Maastrichtien. L'étude des syntypes à démontré qu'ils appartiennent à deux genres différents, <i>Pachydiscus</i> et <i>Anapachydiscus</i>, et au moins à quatre espèces. Le lectotypes choisi ici est du Campanien Supérieur de Jauche (Brabant, Belgique).","BibLvlCode":"AS","StandardTitle":"The ammonite fauna of the type Maastrichtian with a revision of Ammonites colligatus BINKHORST, 1861","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":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1986,"MonPub":null,"DateUpdate":"2024-02-12","DateCreate":"2012-11-12","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":219975,"PubliDate":1986,"Pagination":"151-268","XtraPublOfAnaID":null,"ISBN":null,"Volume":"56","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":64308,"SerRR":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. 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