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ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 2002 Band/Volume: 27 Autor(en)/Author(s): Harzhauser Mathias Artikel/Article: Marine und brachyhaline Gastropoden aus dem Karpatium des Korneuburger Beckens und der Kreuzstettener Bucht (Österreich, Untermiozän) 61-159 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 27: 61-159, Wien 2002 Marine und brachyhaline Gastropoden aus dem Karpatium des Korneuburger Beckens und der • • Kreuzstettener Bucht (Österreich, Untermiozän) von Mathias H a r zh a u se r * Harzhauser , M. (2002): Marine und brachyhaline Gastropoden aus dem Karpatium des Korneuburger Beckens und der Kreuzstettener Bucht (Österreich, Untermiozän). — Beitr. Paläont., 27: 61-159, 12 Taf., Wien. Zusammenfassung chen Grabungen geborgene Material ermöglicht. Zum an­ Die marine und brachyhaline Gastropodenfauna des Kor­ deren lieferte die umfangreiche Sammlung des Naturhi­ storischen Museums Wien einen reichhaltigen Fundus. neuburger Beckens und der Kreuzstettener Bucht (Nie­ Neben der systematisch-taxonomischen Beschreibung derösterreich) wird beschrieben. Die Assoziationen ge­ der Fauna wurde auch eine paläoökologische und biostra­ ben mit 132 Arten einen guten Einblick in die Zusam­ tigraphische Analyse der bis jetzt unzureichend doku­ mensetzung der Gastropodenfauna des höheren Unter­ mentierten Faunengemeinschaften durchgeführt. Auffäl­ miozäns (Karpatium) in der Zentralen Paratethys. lig ist dabei der moderne, beinahe mittelmiozäne Charak­ Die paläoökolgische Charakterisierung der bearbeiteten ter der Assoziationen aufgrund des hohen Anteils an Ar­ Lokalitäten weist auf starken ästuarin-fluviatilen Einfluß ten, die in der Zentralen Paratethys im Eggenburgium und im südlichen Korneuburger Becken hin, der gegen Nor­ Ottnangium noch fehlen. den zu abnimmt, während die Kreuzstettner Bucht voll­ Die paläoökolgische Auswertung der Faunen weist auf marine Verhältnisse aufweist. beträchtlichen Brackwassereinfluß im Korneuburger Tornus kuemeli nov. sp. wird als neue Art eingeführt. Becken hin, der - mit marinen Unterbrechungen - am stärksten im südlichen Teil rund um Stetten nachzuweisen ist. Gegen Norden deuten die Faunen von Kamabrunn und Abstract Kleinebersdorf vermehrt auf marine Verhältnisse, die be­ The marine and brachyhaline gastropod fauna of the Kor- sonders auch in der Kreuzstettener Bucht vorherrschten. neuburg Basin and the Kreuzstetten Bay is described. Im ersten Teil der Monographie: „Das Karpat des Kor­ With 132 species the assemblages give a good impressi­ neuburger Beckens“ (Sovis & Schmid, 1998) gibt W es­ on of the gastropod fauna of the late Lower Miocene sely (1998) eine ausführliche Darstellung des geolo­ (Karpatian) in the Central Paratethys. gisch-tektonischen Rahmens des Korneuburger Beckens; The palecological characterisation of the investigated eine Beschreibung der bearbeiteten Profile und Auf­ sections documents strong fluvial influx in the southern schlüsse ist im selben Band bei Sovis (1998) nachzule­ Komeuburg Basin, which becomes weaker towards the sen. Im folgenden bezieht sich die Bezeichnung „Stetten“ north. In the Kreuzstetten Bay normal marine conditions als Fundortangabe auf die Grabungen im Bereich des Tei- prevailed. ritzberges. Tornus kuemeli nov. sp. is introduced as new species. 2. Historisches Schlüsselwörter Gastropodenführende Aufschlüsse aus dem Bearbei­ Gastropoda - Karpatium - Untermiozän - Korneuburger tungsraum waren schon Hörnes (1856) bekannt, der aus Becken - Niederösterreich - Paläoökologie - Biostrati­ Ebersdorf, Weinsteig und Niederkreuzstetten mnd 54 Ar­ graphie ten nennt und z.T. in seiner großen Monographie abbil­ det. Wenig später sind Gastropoden des Korneuburger Raumes erneut Ziel der Bearbeitung durch R. Hörnes & 1. Einleitung Auinger (1897-91), die die von M. Hörnes beschriebene Fauna revidieren und durch etliche Arten erweitern. Rund Die mit 132 Arten überraschend artenreiche marine und zwei Jahrzehnte später veröffentlicht Schaffer (1907, brachyhaline Gastropodenfauna des Korneuburger 1908) eine erste, lediglich 13 Gastropodentaxa umfassen­ Beckens und der Kreuzstettener Bucht wird hier zum er­ de Liste vom Teiritzberg und erwähnt auch Leobendorf sten Mal umfassend dargestellt. Diese Bearbeitung wurde als Fundpunkt. Wenig später beschreibt V etters (1910, zum einen durch das von Dr. Wofgang Sovis in zahlrei­ 1914) erneut die Fauna vom Teiritzberg, die er gemein­ * Anschrift d. Verf.: Dr. Mathias Harzhauser, Naturhistorisches sam mit Fundpunkten des tieferen Mittelmiozäns be­ Museum Wien, [email protected] arbeitet und die er - wie schon Schaffer (1908) - als ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien 62 Beitr. Paläont., 27, Wien 2002 Gründer Schichten zusammenfaßt. 1926 schließlich pu­ denster Assoziationen, die an die jeweiligen Umweltbe­ bliziert Glaessner erstmals eine ausführliche, 56 Gastro- dingungen angepaßt waren. Da viele der beschriebenen podentaxa umfassende Liste vom Teiritzberg bei Stetten. Taxa aus der Sammlung des NHMW stammen, war es Auch er betrachtet die beschriebene Fauna noch als Äqui­ nicht möglich, alle genannten Arten den entsprechenden valent der jüngeren Molluskenfauna aus den Gründer Probennummem in Sovis (1998) zuzuordnen. Es werden Schichten. Zwei Jahre darauf führenB obies & Kölbl daher nur die beiden signifikanten Proben 001/D/C und (1928) einige charakteristische Gastropoden des Korneu­ 001/Z/C im Detail behandelt. burger Beckens an und stufen die Sedimente ins „obere Helvet“ ein. Erst in den 30er Jahren beschäftigt sich Sie­ ber in mehreren systematischen Arbeiten eingehend mit 3. 1. 1. Proben 001/D/C und 001/Z/C den Gastropodenfaunen Niederösterreichs und behandelt 001/D/C dabei wiederholt Material aus dem Korneuburger Raum. 1936 erscheint seine Arbeit zu den Cancellariiden, Diodora (Diodora) itálica (Defrance , 1820) 1936/37 folgt die Darstellung der Potamididen, Cerithi- Nerita (Theliostyla) plutonis (Basterot , 1825) iden und Triphoriden und 1937 veröffentlicht er seine Ar­ Agapilia pachii (Hôrnes , 1848) (Boettger , 1906) beit über die Fasciolariden. In den 50er Jahren folgen Re­ Pareuchelus heres Granulolabium plicatum (Bruguière , 1792) visionen der Bullaceen (1953) und Ringiculiden (1954) Granulolabium bicinctum (Brocchi, 1814) erger durch B und der Bucciniden und Nassariiden durch Ptychopotamides papaveraceus (Basterot , 1825) B eer -B istricky (1958), in denen auch auf Arten des Terebraba bidentata (Defrance in Grateloup , 1840) Korneuburger Beckens und der Kreuzstettener Bucht ein- Sandbergeria spiralissima (Dubois, 1831) gegegangen wird. Zusätzlich publiziert Papp (1952) seine Turritella (Eichwaldiella) bicarinata (Eichwald , 1830) Gedanken zur Gruppe um „Clithon pictus “ und zur Caecum (Brochinia) banoni Benoist , 1874 Gattung „P irenella“ Im Gegensatz dazu erwähnen Melanopsis impressa Krauss , 1852 Schaffer (1942, 1943), Schaffer & Grill (1951) und Fossarus costatus (Brocchi, 1814) Hydrobia cf. frauenfeldi (Hôrnes , 1856) Grill (1953) in ihren geologischen Darstellungen des Hydrobia? sp. Korneuburger Beckens vorwiegend die von Glaessner Tornus kuemeli nov. sp. (1926) beschriebenen Faunen, ohne neue Gastropoden- Stossichia multicingulata (Boettger , 1887) taxa anzuführen. Calyptraea (Calyptraea) depressa Lamarck , 1822 Eine der letzten systematischen Bearbeitungen neogener Polinices pseudoredemptus (Friedberg , 1923) österreichischer Gastropoden, die auch Funde aus dem Natica tigrina Defrance , 1825 Korneuburger Becken berücksichtigt, stammt wieder von Murex (Bolinus) subtorularius Hôrnes & Auinger , 1885 Sieber (1960) und behandelt die Turritellen. Dieselbe Hexaplex (Phyllonotus) pomiformis Gruppe wird 1989 von Stürmer in einer unpublizierten Pyrene (Alia) polonica (Pusch, 1837) Dissertation revidiert. In einer weiteren unpublizierten Nassariidae indet. Dissertation behandelt Stoiaspal (1974) auch die Ocine- Clavatula dorotheae (Hôrnes & Auinger , 1891) brinen des österreichischen Karpatiums. Neben diesen Perrona jouanneti (Des Moulins , 1842) s. 1. systematischen Darstellungen gibt Sovis (1987) in einem Acteon pinguis d ’Orbigny , 1852 Ausstellungskatalog eine Zusammenstellung einiger be­ Acteon semistriatus burdigalensis d ’Orbigny , 1852 Turbonilla cf. pseudcostellata hoernesiana Sacco, 1892 sonders typischer Gastropoden vom Teiritzberg, die Odostomia (Megastomia) conoidea (Brocchi, 1814) durch die kurzen Faunenlisten in Stürmer & al. (1991) noch ergänzt werden. 2001 werden einige der charakteri­ stischen Brackwassergastropoden des Korneuburger 001/Z/C Beckens von H arzhauser & K owalke dargestellt und mit jenen des frühmiozänen Mittelmeerraumes ver­ Agapilia pachii (Hôrnes , 1848) glichen. Hydrobia cf. frauenfeldi (Hôrnes , 1856) Tornus kuemeli nov. sp. Turboella acuticosta Sacco, 1895 Alvania montagui trochiformis Csepreghy -Meznerics , 1956 3. Faunenbestand und Paläoökologie Alvania cf. oceani (d ‘Orbigny , 1852) 3.1. Teiritzberg bei Stetten Triphora perversa (Linné , 1758) Odostomia (Megastomia) conoidea (Brocchi, 1814) Die reichste Gastropodenfauna des Untersuchungsgebie­ Odostomia cf. peregrina Boettger , 1901 tes stammt vom Teiritzberg bei Stetten. Mit 87 Spezies Cingulina miocaenica Boettger , 1901 repräsentiert der Teiritzberg rund 2/3 des bekannten Ar­ Turbonilla cf. pseudcostellata hoernesiana Sacco, 1892 teninventars des Korneuburger Beckens.
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    PALEONTOLOGY AND STRATIGRAPHY OF EOCENE ROCKS AT PULALI POINT, JEFFERSON COUNTY, EASTERN OLYMPIC PENINSULA, WASHINGTON by RICHARD L. SQUIRES, JAMES L. GOEDERT, and KEITH L. KALER WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES REPORT OF INVESTIGATIONS 31 1992 ., WASHINGTON STATE DEPARTMENT OF Natural Resources Brian Boyle • Commhstoner of Public Lands An Steo_r0$ - Superv1sor Division ol Geology and Earth Resources Raymond Lcmnanls. State Geologlsl PALEONTOLOGY AND STRATIGRAPHY OF EOCENE ROCKS AT PULALI POINT, JEFFERSON COUNTY, EASTERN OLYMPIC PENINSULA, WASHINGTON by RICHARD L. SQUIRES, JAMES L. GOEDERT, AND KEITH L. KALER WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES REPORT OF INVESTIGATIONS 31 1992 W>.SHING'TON STAT1r OEPARTMDIT or Natural Resources 8ncll) Bov,. · COmmmioner ot Pu!xk: tancb M $i.atni; S\lp$1'WOJ' DtY!llcn 01 Gtology ahCS £artti ~ Raymond l.mlMn.:I ~Geologist Cover: From left, ?Falsifusus marysvillensis; Pachycrommium clarki; large bivalve, Veneri­ cardia hornii s.s.; Delectopecten cf. D. vancouverensis sanjuanensis; Turritella uvasana hendoni. These specimens are shown at 150 percent of the dimensions on Plates 1 and 3. Use of trade, product, or firm names in this report is for descriptive purposes only and does not consitute endorsement by the Washington Division of Geology and Earth Resources. This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 1.85 Tax (Stale residenl.t only) .15 Total $ 2.00 Mail orders must be prepaid; please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources.
  • THE LISTING of PHILIPPINE MARINE MOLLUSKS Guido T

    THE LISTING of PHILIPPINE MARINE MOLLUSKS Guido T

    August 2017 Guido T. Poppe A LISTING OF PHILIPPINE MARINE MOLLUSKS - V1.00 THE LISTING OF PHILIPPINE MARINE MOLLUSKS Guido T. Poppe INTRODUCTION The publication of Philippine Marine Mollusks, Volumes 1 to 4 has been a revelation to the conchological community. Apart from being the delight of collectors, the PMM started a new way of layout and publishing - followed today by many authors. Internet technology has allowed more than 50 experts worldwide to work on the collection that forms the base of the 4 PMM books. This expertise, together with modern means of identification has allowed a quality in determinations which is unique in books covering a geographical area. Our Volume 1 was published only 9 years ago: in 2008. Since that time “a lot” has changed. Finally, after almost two decades, the digital world has been embraced by the scientific community, and a new generation of young scientists appeared, well acquainted with text processors, internet communication and digital photographic skills. Museums all over the planet start putting the holotypes online – a still ongoing process – which saves taxonomists from huge confusion and “guessing” about how animals look like. Initiatives as Biodiversity Heritage Library made accessible huge libraries to many thousands of biologists who, without that, were not able to publish properly. The process of all these technological revolutions is ongoing and improves taxonomy and nomenclature in a way which is unprecedented. All this caused an acceleration in the nomenclatural field: both in quantity and in quality of expertise and fieldwork. The above changes are not without huge problematics. Many studies are carried out on the wide diversity of these problems and even books are written on the subject.
  • Gofas XP 95-104

    Gofas XP 95-104

    Bollettino Malacologico, Roma, 39 (5-8): 95-104, [2003] 2004 - Società Italiana di Malacologia Nomenclature of the smaller Mediterranean Cerithium species Serge Gofas, Vittorio Garilli & Marie-Catherine Boisselier-Dubayle KEY WORDS: Cerithiidae, Mediterranean, taxonomy, lectotype designations. ABSTRACT The Mediterranean morphotypes generally confused under the name Cerithium rupestre have been shown to belong to two different species. The cor- rect name for one of the species, living in very shallow rocky areas including splashpools, is Cerithium lividulum Risso,1826, and for the other, usual- ly living in the shallow infralittoral community of photophilous algae, C. renovatum Monterosato, 1884. Type material is figured for all nominal species in this species group introduced prior to 1900, and for some of the species proposed later. Orientations for future work in the taxonomy of this species group are suggested. RIASSUNTO E’ stato mostrato che le entità morfologiche generalmente confuse sotto il nome Cerithium rupestre appartengono a due specie distinte. I nomi corretti per questi taxa sono Cerithium lividulum Risso, 1826, per la specie vivente su fondali rocciosi in acque più superficiali dell’infralitorale superiore e nelle pozze di marea, e Cerithium renovatum Monterosato, 1884, per la specie solitamente vivente su fondali infralitorali ricoperti da alghe fotofile. Cerithium lividulum ha una conchiglia robusta con giri appena convessi, coste assiali talora tuberculate e cordoni spirali piani. La colorazione è data da screziature bruno-verdastre decorrenti spiralmente su uno sfondo bianco. La conchiglia di Cerithium renovatum è più piccola (inferiore ai 20 mm nel materiale esaminato), più delicata e snella, e presenta una serie regolare di tubercoli, costantemente di colore bianco, che iniziano nei primi giri e raggiungono il loro massimo sviluppo in corrispondenza del penultimo.
  • Constructional Morphology of Cerithiform Gastropods

    Constructional Morphology of Cerithiform Gastropods

    Paleontological Research, vol. 10, no. 3, pp. 233–259, September 30, 2006 6 by the Palaeontological Society of Japan Constructional morphology of cerithiform gastropods JENNY SA¨ LGEBACK1 AND ENRICO SAVAZZI2 1Department of Earth Sciences, Uppsala University, Norbyva¨gen 22, 75236 Uppsala, Sweden 2Department of Palaeozoology, Swedish Museum of Natural History, Box 50007, 10405 Stockholm, Sweden. Present address: The Kyoto University Museum, Yoshida Honmachi, Sakyo-ku, Kyoto 606-8501, Japan (email: [email protected]) Received December 19, 2005; Revised manuscript accepted May 26, 2006 Abstract. Cerithiform gastropods possess high-spired shells with small apertures, anterior canals or si- nuses, and usually one or more spiral rows of tubercles, spines or nodes. This shell morphology occurs mostly within the superfamily Cerithioidea. Several morphologic characters of cerithiform shells are adap- tive within five broad functional areas: (1) defence from shell-peeling predators (external sculpture, pre- adult internal barriers, preadult varices, adult aperture) (2) burrowing and infaunal life (burrowing sculp- tures, bent and elongated inhalant adult siphon, plough-like adult outer lip, flattened dorsal region of last whorl), (3) clamping of the aperture onto a solid substrate (broad tangential adult aperture), (4) stabilisa- tion of the shell when epifaunal (broad adult outer lip and at least three types of swellings located on the left ventrolateral side of the last whorl in the adult stage), and (5) righting after accidental overturning (pro- jecting dorsal tubercles or varix on the last or penultimate whorl, in one instance accompanied by hollow ventral tubercles that are removed by abrasion against the substrate in the adult stage). Most of these char- acters are made feasible by determinate growth and a countdown ontogenetic programme.