Revision Des Gastropoda Du Danien Et Du Montien De La Belgique

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Revision Des Gastropoda Du Danien Et Du Montien De La Belgique REVISION DES GASTROPODA DU DANIEN ET DU MONTIEN DE LA BELGIQUE I LES GASTROPODA DU CALCAIRE DE MONS Ordre ARCHAEOGASTROPODA Superfamillc FI URELLA EA. Sous-ordre PLEUROTOMARIINA Famill FI URELLIDAE. Superfamille PLEUROTOMARIACEA. Sous-famille EMARGl1 LINAE. Famille SCISSURELLIDAE. Genre EM RGI ULA LAMARCK, 1801. Genre SCISSURELLA ORBIGNY, 1823. Sous-genre EMARGIN LA. 1. - Scissurella corneti R UTOT in COSSMANN, 1915. 1. - Emarginula (s. .) corncti R TOT (Pl. I, fig. 1.) in COSSMANN, 19] 5. Scissurella Cometi CossMANN, M., 1915, p. 17, pl. I, fig. 53- (Pl. I, fig. 2.) 55 (holotype n ° 3076 I.R.Sc.N.B.). Emargi1111/a Cometi CosSMA N, M ., 1915, p. 14, pl. I, fi g. 39 (lectotype, ici désigné, n° 3024), fig. 40 (paralectotype G i s e m e n t . - Calcaire de Mons. n ° 3025 I.R.Sc.N.B.). L 0 c a 1 i t é s . - Mons (Puits GOFFINT et G i s e m e n t . - Calcaire de Mons. COPPÉE). Loc a 1 i té. - Mons (Puits OPPÉE). N o m b r e d ' e x e m p 1 a i r e s . - Trois. N o m b r e d ' e x e m p 1 a i r e s . - Deux. R em arque . - M. CossMANN a parfaitement décrit la sculpture de la large rampe suturale et de la R c m a r que . - Il n'est pas douteux que cette partie inférieure des tours, ainsi que la cicatrice du espèce appartient au même groupe que Emarginula sinus, mais il a omis de signaler une particularité de carezi D E LAUBRIÈRE, 1881 du Thanétien et en repré­ l'ornementation de la base. Entre la carène circaombi­ sente assez vraisemblablement un ancêtre direct. Il est licale et la carène circumbasale il existe, outre les plis intéressant à ce propos de comparer entre clics la transverses mentionnés dans la description originale, figure originale du lectotype n° 3024 et la représen­ une sculpture spirale délicate constituée par six fins tation par M. CosSMANN et G. PISSAR RO (1910-1913, cordonnets arrondis, presque jointifs. Cette sculpture pl. II, fig. 9-5) d'un spécimen de l'espèce de Châlons­ n'est nettement visible que sur l'un de nos trois exem­ sur-Vesle. plaires. Signalons aussi que les plis transverses de la Toutefois Emarginula carezi atteint une taille supé­ base se poursuivent sur la paroi interne de l'entonnoir rieure (CossMANN, M., 1888, p. 39) et se distingue, en ombilical. outre, du fossile montien par ses côtes spirales moin 7 M. GLIBERT. - REVISIO DES GASTROPODA nombreuses cl bi en plus saillantes, surtout en avant. Lo c a l i té . - Mons (Puits COPPÉE). D'autre part, le treill is qui résulte du croisement des côtes intercalaires par les cordonnets transverses est N o m b r e d ' e x e m p 1 a i r e s . - Troi beaucoup plus grossier chez l'espèce thanétienne que chez Enwrginula corneti. Genre RIMULA DEFRANCE, 1827. 2. - E marginula (s. s.) montensis RuTOT Sous-genre RIMULA. in CossMA NN, 1915. (Pl. f, fi g. 3.) l. Rimula (s. s.) praeintorta R uTOT 1.::11wrr.: i1111/a 111011te11sis COSSMANN, M ., l 9 15, p. 15, pl. l , fi g. 41 -42 (holotype n° 3026 I.R.Sc.N.B.). in CosSMANN, 1915. Ri111ula praei11torta CosSMANN, M., 1915, p. 14, pl. I, fig. G i s c m c n t . - Calcaire de Mons. 43-45. L 0 c a 1 i l é s . - Mons (Puits GOFFJNT et G i s c m c n t . - Calcaire de Mons. COPl'J:E). L 0 c al i t é . - Mons (Puits COPPÉE). N o m b r c d ' c x c m p l a i r c s . - Quatre. N o m b r e d ' e x e m p 1 a i r e s . - L'unique R c m a r q u c . - Cette espèce de Mons appar­ exemplaire connu a été détruit à une date inconnue. ti ent au même groupe que Emarginula clathrata DESllAYES du Lutéticn, mais M. CossMANN (loc. cit) a clairement indiqué les caractères différentiels de ces Sous-famille DIODORINAE. deux taxa, principalement la taille des mailles formées par l'entrccroiscmcnl des sculptures radiaire et trans­ Genre DIODORA GRAY, 1821. ve rse. Chez D11argi11ula 111011/ensis ces mailles sont réduites ù de simples cupules. En outre, la cicatrice 1. - Diodora concentrica (BRIART et CORNET, 1887). du sinus est plus large, moins saillante et les arcs (Pl. I, fig. 6.) d'accroissement du cal d'obturation de la fissure sont Fissure/la co11ce11trica BRIART, A. et C ORNET, F . L., l 870- bi en plus grossiers chez l'espèce de Mons. 1887, fasc. 4, 1887, p. 66, pl. XXIV, fig. 1, a-c. - Cos s~IANN, M., 1915, p. 11, pl. I, fig. 30, 32 (ex. fig. n° 3021), fig. 31 (ex. fig. n° 3020 I.R.Sc.N.B.). 3. - Emarginula (s. s.) bcclardi RuTOT i11 COSSMANN, 1915. G i s e m e n t . - Calcaire de Mons. (Pl. f, fi g. 4.) Localité. - Mons (Puits COPPÉE). /:'11 111ri:i1111/a IJ l'd (/ rdi Coss~ IA NN , M., J 9 15, p. l 6, pl. J, fi g. 46, 47 (lcctotypc, ici désigné, 11 ° 3027 l.R.Sc.N.B.). N o m b r e d ' e x e m p 1 a i r e s . - Quatre. G i s c m c n t. - Calcaire de Mons. D i s c us s i o n . - li est vrai qu'aucun des L o c a 1 i t é . - Mons (Puits COPPÉE). exemplaires préservés dans la collection de l'Institut n'est aussi complet que l'holotype, mais l'un des deux No m b r c d ' c x cm pl a i r c s . - Unique. individus figurés par M. CosSMANN (ex. n° 3021) est R e m a r q u c . - Le seul exemplaire retrouvé cependant intéressant en ce qu'il montre, avec une dans la collection est incomplet. L 'espèce diffère des grande netteté, les étroits sillons rayonnants ponctués précédentes par son contour étroitement ovale, sa qui recoupent les rides concentriques autour du som­ forme plus haute et l'étroitesse extrême de la fissure met et jusqu'à une distance de 6 mm environ de ce du sinus. Les arcs d'accroissement du cal d'obturation dernier (CossMANN, M., 1915, pl. I, fig. 32). Le même sont hauts et très minces, assez largement espacés. spec1men possède aussi une perforation apicale intacte. Elle est entourée intérieurement, surtout vers l'avant, des petits plis rayonnants déjà mentionnés Genre SCUTUS MONTFORT, 1810. dans la description originale. Un autre exemplaire plus jeune (diamètre antéro­ ous-gcnre PROSCUTUM FISCHER, 1885. postérieur 20 mm), provenant de la collection E. DEJAER, et qui apparemment n'a pas été vu par M. 1. - Scutus (Proscutum) montensis RuTOT CossMANN, montre un autre caractère important. Fixé i11 Co MANN, 1915. à un bloc de sédiment cet individu se présente par sa (Pl. l , fi g. 5.) face interne et son péritrème est constitué comme Sc11t11111 (Proscu/11111) 111 011te11se Cos ~IANN, M., 1915, p. 17, celui de l'exemplaire n° 3021 dont il a été question pl. 1, fi g. 50-52 (holotype n" 3028 1. R. c. .B.). ci-dessus. Mais ici l'on observe, au côté droit du bord G i s me n t . - alcairc de Mon . libre (le seul intact), la présence de crénelures margi- 8 DU DA IE ET DU MO TIE DE LA BELGIQ E nale assez gro sières analogues à celle de Diodoro mognifico (DESHAYES, 1861) du Lutétien du Bas in de Paris (CossMANN, M. et PISSARO, G., 1910-1913, pl. ou - rdr P T LU II, fig. 6-12). up rfamill P TELL EA. J ai pu dégager une portion suffi ante de la face externe de ce spécimen pour observer des rides con­ Famill" P TELLIDAE. centriques d'une fraîcheur parfaite et nettement plu saillantes que celles de l'individu n° 3021. Elles u -famille PATELLINAE. méritent le nom de crêtes concentriques ondulé . Leurs ondulations coïncident avec les crénulation G nre P ATELLA LINNÉ, 175 marginales dont il a été fait mention plus haut et qui, avec les sillons radiaires apicaux, sont pour cette 1. - Patella vincenti BRIART t , l 7. espèce les seuls vestiges de la sculpture rayonnante (Pl. I, fig. 9 .) habituellement vigoureuse des Diodora. Pate//a Vi11ce11ti BRIART, A . et MANN, M., 19 l 5, p . I.R.Sc.N.B.). 2. - Diodora corneti (RUTOT in CossMANN, 1915). Parei/a regularis BRIART, . t R T, •• ., 1 70-1 7, (Pl. I, fig. 7 .) fa c. 4, 1 7, p. 7 , pl. ' L , fig. , n-d. - o.'­ Fissurella Comeri CosSMANN, M., 1915, p. 12, pl. I, fig. 36-38 MANN, M., 1915, p. 'pl. l fig. _Q- __ (c . fi . n• . 01 7 (holotype n ° 3023 I.R.Sc.N.B.). I.R. .B.). Parei/a 111011re11sis o MA , M., 1915, p. , pl. 1 fig. 1 -1 7 (holotype n ° 301 l.R. .B.). G i s e m e n t . - Calcaire de Mons. G i e m en t . - alcair d' M 11 • Lo c al i té . - Mons (Puits COPPÉE). L o c a l i tés . - M 11 (Puit F I T Nombre d ' ex e m p 1 aires. - Dix. COPPÉE). R e m a r q u e . - Diodoro corneti appartient Nombre d m p 1 air ingt-huit.
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