{"refrec":{"BRefID":220610,"RR":"<b>Voigt, E</b> (1987). Tome III: Die bryozoen des klassischen Dano Montiens von Mons. <i>Toelichtende Verhandelingen voor de Geologische Kaart en Mijnkaart van België = Mémoires pour servir à l'explication des cartes géologiques et minières de la Belgique</i>, 17(3). Geologische Dienst van België: Brussel.  161 p., 23 pl., 3 tbl. pp.","BEntID":212343,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Toelichtende Verhandelingen voor de Geologische Kaart en Mijnkaart van België = Mémoires pour servir à l'explication des cartes géologiques et minières de la Belgique</i>, 17(3). Geologische Dienst van België: Brussel.  161 p., 23 pl., 3 tbl. pp.","DocTypID":5,"DocType":"Book/Monograph","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Voigt, E","OrigTitleTranslFlag":0,"Authorstringtrunc":"Voigt, E","Englishabstract":null,"AbstractOtherLang":"In this paper the Bryozoa of  the Dano-Montian from the new scientific Borehole in Mons and the older classic Borehole of the \"puits artésien de  l'Ecole  des Mines\" (now Faculté des Mines)  in Mons are described. Among the 58 species of Bryozoa  are 18 Cyclostomata and 40 Cheilostamata. These comprise only a part of the very much richer Bryozoan Fauna of the Dano-Montian, in particular that of the Tuffeau  de Ciply and its  basal  bed  (Poudingue  de  la Malogne) m  Belgium and the  so -called  \"Postmaastrichtian \" of the Netherlands (South Limburg).The following  genera are new :    Retecavella, Monticellaria, Diplobeisselina, Schizemiellopsis and Taenioporella.The subgenus Puncturiellina is new.New species are :    Crisidia   lagaaiji.  Retepondea  pseudolichenoides,   Rectecavella   broodi,  Callopora  tegulata,     Pithodella impar.  Stamenocella marlierei, Planicellaria bugei, \"Membranipora\" rectangulata,     \"Membranipora\"  subclavatoides,  Onychocella  meijeri,  Pseudothyracella  ciplyensis,  Floridina     eisdenensis,   Floridina    membraniporoides,  Lunulites   ratheimensis,   Hemistylus  dissimilis,     Monticellaria obscure n.g n.sp., Porina hamulifera and Floridina scutata brevior n.subsp.The uppermost 1 2 m of the Möns Borehole, corresponding to the stratotype of the Montian sensu stricto, has yielded  a  very characteristic assemblage  of cheilostomatous Bryozoa consisting almost entirely of segments of articulated (\"cellariiform\") zoaria, among which Monsella eocene (MEUNIER & PERGENS), Poricellaria diplodidymyoides (MEUNIER & PERGENS), Pseudothyrecelle (?) mucronete. Nellia pergensii DARTEVELLE and Nellie tenelle LAMARCK and other flexible  genera predominate.This assemblage settling on seaweeds indicates a high energy environment  in Litoral and Sublitoral zones, and IS itself  of no biostratigraphical significance. This part of the  succession approximately equates with the upper Triginglymus horizon of the ostracod zonation established by MARLI ERE (1 958) for the Ecole des  Mines Borehole. The underlying succession  of the Möns Borehole comprises a transition zone with Cytheretta and a deeper horizon with Cytherelloidee, which corresponds to the Tuffeau de Ciply. In contrast to the Ostracoda, the Bryozoa exhibit no significant fauna! change between the upper and lower units. The considerable number of bryozoan species in the Tuffeau de Ciply, which are known also from the Baltic  Daman, supports the idea - already suggested by other palaeontological and  micropalaeontological studies  (e.g. BERGGREN (1 964) RASMUSSEN (1 962, 1 965) MEIJER (1 969), POZARYSKA (1 966), MOORKENS  (1982), that the Tuffeau de Ciply equates with the  Middle  and Upper Danian, even though many of the  characteristic  species of the  type Danian are lacking m the  Belgian and Dutch Dano-Montian. Due to the  fact, that no bryozoan faunal sequences are known from the  Paleocene, which  continue through to the  Eocene and which can be compared with the material considered here, it is not yet possible to erect a  zonation for the Dano-Montian and later Paleocene  based on Bryozoa alone. To avoid misunderstanding,  the term \"Dano-Montian\" is retained here to cover the bryozoan faunes of the southern faunal  province  comprising  Belgium, the Netherlands and western  Germany  in contradistinction to  those  of the boreal  province comprising the Baltic - Polish Danian  and Selandian. The possibility cannot be excluded, that the  bryozoan faunas in question, including those of the Tuffeau de Ciply and the Limburg \"Postmaastrichtian\",  are  partly later,  and  perhaps even of  Selandian age.  This problem  is  discussed in  the light of  micropalaeontological investigations.  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Belgische Geologische Dienst: Bruxelles.  ISSN 0408-9510","Ser2BRefID":null,"Ser2RR":null,"StandardTitleSer":"Toelichtende Verhandelingen voor de Geologische Kaart en Mijnkaart van België = Mémoires pour servir à l'explication des cartes géologiques et minières de la Belgique","ISSN":"0408-9510","AbbrevSer":"Toelicht. Verhand. Belg. Geol. Dienst = Mém. Expl. Serv. géol. 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