Reitner, Joachim

[["dc.bibliographiccitation.firstpage","335"],["dc.bibliographiccitation.journal","Geologisch-paläontologische Mitteilungen, Innsbruck"],["dc.bibliographiccitation.lastpage","347"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Mehl, Dorte"],["dc.date.accessioned","2019-07-10T08:12:34Z"],["dc.date.available","2019-07-10T08:12:34Z"],["dc.date.issued","1995"],["dc.description.abstract","Sponges are primitive metazoan organisms which occur since the late Proterozoic. The oldest sponge remains (hexactinellids) are from a shallow marine carbonate facies of the late Sinian Shibantan Member (China). From the Tommotian (Sansha, China) protospongiid and rossellimorph hexactinellids were discovered in shallow marine silicified rocks. The middle part of this section consists of silty shales with entirely preserved hexactinellid sponges: Sanshadictya, Hyalosinica, Solactinella, Triticispongia, Hunanospongia. The hexactinellids typically are soft bottom dwellers, which sometimes grow on and form in situ spiculites (spicule mats). The sponges from the Chengjiang deposits of Atdabanian age, which show a rossellimorph spicule organization typical of the conservative hexactinellid groups, which inhabited the deep sea during most of the Phanerozoic, were also typical soft bottom dwellers. All sponge taxa (Leptomitella, Leptomitus, Paraleptomitella etc.) described from this locality we consider to be hexactinellids and not demosponges, as originally classified. The sponge communities of carbonate-dominated archaeocyathid mounds are completely different from the above described sponge mounds. The sponges from the archaeocyath mounds of the Flinders Ranges (S.Australia) are characterized by Calcarea and demosponges ($; modern type of pharetronid Calcarea Gravestockia pharetroniensis, and many tetractinellid demosponges, Geodiida). Questionable is the origin of four-rayed demosponge spicules found in some archaeocyaths. The oldest ceractinomorph demosponges are documented from the middle Cambrian (Vauxia - an aspicular sponge with keratose affinities, and isolated sigmata microscleres). Sponge communities of the Early Cambrian were highly developed, and already then they were taxonomically strongly dependent on substrates and trophic conditions."],["dc.description.abstract","Schwammfragmente (Hexactinelliden) stammen aus einer flachmarinen Karbonatfazies im späten Sinium des Shibatan Members in China. Aus dem Tommotium (Sansha, China) wurden protospongiide und rossellimorphe Hexactinelliden innerhalb flachmariner, verkieselter Gesteinsformationen entdeckt. Der mittlere Abschnitt dieses Profils besteht aus siltigem Tongestein mit körperlich erhaltenen hexactinelliden Schwämmen: Sanshadictya, Hyalosinica, Solactinella, Triticispongia, Hunanospongia. Die Hexactinelliden sind typische Weichbodenbewohner, die manchmal in-situ-Spiculite (Spicula-Matten) bilden und auf diesen wachsen. Die Schwämme der Chengjiang Lagerstätte (Atdabatium), die eine • rossellimorphe Sklerenanordnung, typisch für konservative Hexactinellidengruppen des tieferen Wassers während des Phanerozoikums, zeigen, waren ebenfalls charakteristische Weichbodenbewohner. Alle Spoilgien-Taxa, die von dieser Lokalität beschrieben sind (Leptomitella, Leptomitus, Paraleptomitella, ect.), werden von uns als Hexactinellida angesehen und nicht als Demospongiae, wie sie sie ursprünglich klassifiziert wurden. Die Schwamm-Gemeinschaften der karbonatreichen Acrchaeocyathidenmounds unterscheiden sich von den oben beschriebenen Spongien mounds signifikant. Die Schwämme aus den Archaeocyathenmounds der Flinders Ranges (Südaustralien) sind charakteristischerweise Calcarea und Demospongiae (pharetronide Calcarea von \"moderner\" Organisation wie Gravestockia pharetroniensis und viele tetractinellide Demospongiae der Geodiida). Umstritten bleibt der Ursprung der vierstrahligen demospongiiden Spicula, die in einigen Archaeocyathen gefunden wurden. Die bisher ältesten ceractinomorphen Demospongien sind aus dem mittleren Kambrium nachgewiesen (Vauxia - ein aspikulärer Schwamm mit Affinität zu den Keratosen, und isolierte Sigmata\\ Mikroskleren). Spongien-Gemeinschaften des frühen Kambriums waren hochentwickelt und in ihrer taxonomischen Zusammensetzung schon damals sehr vom Substrat und Nahrungsangebot abhängig."],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","50499400x"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2195"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60963"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Early paleozoic diversification of sponges ; new data and evidences"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","837"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Eclogae geologicae Helvetiae"],["dc.bibliographiccitation.lastpage","849"],["dc.bibliographiccitation.volume","84"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Föllmi, Karl B."],["dc.date.accessioned","2019-07-10T08:12:36Z"],["dc.date.available","2019-07-10T08:12:36Z"],["dc.date.issued","1991"],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","502068930"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2208"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60973"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","A new \"deep-water\" Chaetetopsis Species (Chaetetopsis favositiformis n. sp., Demospongiae) from the Plattenwald Bed (Mid-Cretaceous Garschella Formation, Vorarlberg, Austria)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","425"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","Neues Jahrbuch für Geologie und Paläontologie"],["dc.bibliographiccitation.lastpage","430"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Engeser, Theo"],["dc.date.accessioned","2019-07-10T08:12:34Z"],["dc.date.available","2019-07-10T08:12:34Z"],["dc.date.issued","1981"],["dc.description.abstract","The squid Loligosepia dusslingensis n. sp. is the oldest known teuthid from the Swabian Jutassic."],["dc.description.abstract","Die Teuthidenart Loligosepia dusslingensis n. sp.ist der bislang älteste Teuthide aus dem schwäbischen Jura."],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","501735909"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2198"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60966"],["dc.language.iso","de"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Eine neue Teuthiden-Art aus dem unteren Sinemurium (Lias alpha 3, Ölschiefer) von Dusslingen bei Tübingen (Baden-Württemberg)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1695"],["dc.bibliographiccitation.issue","10"],["dc.bibliographiccitation.journal","Geochimica et cosmochimica acta"],["dc.bibliographiccitation.lastpage","1703"],["dc.bibliographiccitation.volume","64"],["dc.contributor.author","Böhm, Florian"],["dc.contributor.author","Joachimski, Michael M."],["dc.contributor.author","Dullo, Wolf-Christian"],["dc.contributor.author","Eisenhauer, Anton"],["dc.contributor.author","Lehnert, Helmut"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Wörheide, Gert"],["dc.date.accessioned","2008-10-29T20:05:18Z"],["dc.date.accessioned","2021-10-27T13:13:56Z"],["dc.date.available","2008-10-29T20:05:18Z"],["dc.date.available","2021-10-27T13:13:56Z"],["dc.date.issued","2000"],["dc.description.abstract","Oxygen isotope values of the extant Caribbean coralline sponge Ceratoporella nieholsoni are compared with published temperatures and alSo of water calculated from salinities. The measured values from aragonitic sponge skeletons have a mean offsel of 1.0 ± 0.1 %0 from calculated calcite equilibrium values (aaragOnilC.catCilC = 1.0010). This is in good agreement with published values from synthetic aragonite. They further agree with published near-equilibrium oxygen isotope values of temperate and cold water molluscs and foraminifera extrapolated to the temperature range of the coralline sponges. These results and the mode of skeleton formation of Ceratoporella nicholsoni suggest that these sponges precipitate aragonite elose to isotopic equilibrium. The temperature dependence of oxygen isotopic fractionation between the aragonite of Ceratoporella nieholsoni and water is only roughly constrained by the available data, due to the narrow temperature range of the Caribbean reef sites. However, as the data suggest oxygen isotopic equilibrium, we can calculate a weil constrained temperature equation combining temperate and cold water equilibrium values from molluscs and foraminifera with our sponge data: 103lnaaragonitc_watcT = (18.45 ± 0.4) 103rr (K) - (32.54 ± 1.5) and T (0C) = (20.0 ± 0.2) - (4.42 ± 0.10) (aa - aw); for 3° < T < 28°."],["dc.format.mimetype","application/pdf"],["dc.identifier.doi","10.1016/S0016-7037(99)00408-1"],["dc.identifier.ppn","506956784"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2187"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/91818"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Oxygen isotope fractionation in marine aragonite of coralline sponges"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","167"],["dc.bibliographiccitation.journal","Mitteilungen aus dem Geologisch-Paläontologischen Institut der Universität Hamburg"],["dc.bibliographiccitation.lastpage","177"],["dc.bibliographiccitation.volume","68"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Engeser, Theo"],["dc.date.accessioned","2019-07-10T08:12:36Z"],["dc.date.available","2019-07-10T08:12:36Z"],["dc.date.issued","1989"],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","502001925"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2214"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60977"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Coralline Demospongiae (Porifera) aus dem Campan von Pobla de Segur (Pyrenäen, Nordspanien)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","231"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Neues Jahrbuch für Geologie und Paläontologie"],["dc.bibliographiccitation.lastpage","241"],["dc.contributor.author","Engeser, Theo"],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2019-07-10T08:12:37Z"],["dc.date.available","2019-07-10T08:12:37Z"],["dc.date.issued","1992"],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","502129174"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2218"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60980"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Description of the first Rhaetian nautiloid (Grypoceras rhaeticum n. sp.) from the Kössen Beds of the Fonsjoch near Achensee (Austria)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","496"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Neues Jahrbuch für Geologie und Paläontologie"],["dc.bibliographiccitation.lastpage","501"],["dc.bibliographiccitation.volume","165"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Engeser, Theo"],["dc.date.accessioned","2019-07-10T08:12:35Z"],["dc.date.available","2019-07-10T08:12:35Z"],["dc.date.issued","1983"],["dc.description.abstract","The \"unusual belemnite\" Chitinobelus acifer FISCHER with an \"almost purely organic, pinlike epirostrum\" and a \"calcitic primary rostrum\" (FISCHER 1981: 142) is attributed to the order Belemnoteuthida STOLLEY 1919. Carbonate diagenesis suggests that ortho- and epirostrum, were originally aragonitic."],["dc.description.abstract","Der von FISCHER (1981) beschriebene \"ungewöhnliche Belemnit\" Chitinobelus acifer, mit einem \"nadelförmigen, fast rein organischen Epirostrum\" und einem \"kalzitischen Primärrostrum\" (FISCHER 1981: 142) wird zur Ordnung Belemnoteuthida STOLLEY 1919 gestellt. Aufgrund der Karbonatdiagenese läßt sich ein aragonitisches Ortho- und Epirostrum folgern."],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","501741321"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2207"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60972"],["dc.language.iso","de"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Chitinobelus acifer Fischer 1981, ein Belemnoteuthide (Coleoidea) mit Epirostrum"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","291"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Neues Jahrbuch für Geologie und Paläontologie,"],["dc.bibliographiccitation.lastpage","304"],["dc.contributor.author","Riegraf, Wolfgang"],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2019-07-10T08:12:36Z"],["dc.date.available","2019-07-10T08:12:36Z"],["dc.date.issued","1979"],["dc.description.abstract","The \"soft-part-belemnites\" In the Holzmaden Posidonia Shales are forged. · Soft-parts of Phragmoteuthis conocauda (QUENSTEDT) have been compounded with belemnite rostra of Passaloteuthis paxillosa (SCHLOTHEIM). The systematic position of Phragmoteuthis conocauda (QUENSTEDT) is di scussed. The systematics and the reconstruction of the belemnite animal are questionable again."],["dc.description.abstract","Die sogenannten \" Weichteilbelemniten\" aus dem Holzmadencr Posidonienschiefer sind Fälschungen von Sammlern. Die Verfasser untersuchten drei der gefälschten Stücke, je eines in Tübingen, Frankfurt/M. und Karlsruhe, und glauben, daß es keine echten Weichteilbelemniten aus dem Posidonienschiefer gibt. Die \"Weichteilbelemniten\" wurden aus Belemnitenrostren und den Weichteilen von Phragmoteuthis conocauda (QUENST.) gefertigt. Da auch die alten englischen \"Weichteilbelemniten\" des vorigen Jahrhunderts in ähnlicher Weise montiert wurden, existieren bis heute keine Funde von Belemniten mit Weichteilerhaltung. Daraus ergeben sich für die Systematik und die Rekonstruktion der Belemnitida ZITTEL gravierende Konsequenzen. Fraßreste mit Armhäkchen in Ichthyosauriermägen müssen auf Phragmoteuthisartige Cephalopoden zurückgeführt werden. Die Systematik von Phragmoteuthis conocauda (QUENST.) wird hier diskutiert."],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","50173144x"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2211"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60976"],["dc.language.iso","de"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Die \"Weichteilbelemniten\" des Posidonienschiefers (Untertoarcium) von Holzmaden (Baden-Württemberg) sind Fälschungen"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","273"],["dc.bibliographiccitation.journal","Berliner geowissenschaftliche Abhandlungen"],["dc.bibliographiccitation.lastpage","293"],["dc.bibliographiccitation.seriesnr","3"],["dc.bibliographiccitation.volume","3"],["dc.contributor.author","Reitner, Joachim"],["dc.contributor.author","Neuweiler, Fritz"],["dc.contributor.editor","Kohring, Rolf"],["dc.date.accessioned","2019-07-10T08:12:30Z"],["dc.date.available","2019-07-10T08:12:30Z"],["dc.date.issued","1992"],["dc.description.abstract","Aus dem Unter-/Mittelalb von Nordspanien wird ein Profil mit bis zu 8 m mächtigen Lithocodium/ Bacinella Boundstones vorgesteUt. Die mikrofaziell-sedimentologische Analyse des Profils crgibt für die Lithocodium/ Bacinella Bänke eine bathymetrische Position vom tieferen Subtidal bis flachsten Subtidal/lntertidal. Die maximale Tiefenposition ist an die photische Zone gebunden, die wiederum durch das Ausmaß toniger Suspensionen beeinflußt wird. Die bathymetrische Obergrenze ist mechanisch kontrolliert (z.B. WeUenenergie, Tidenströme). Lithocodium/Bacinella ist zusammen mit anderen Algen/Mikroben ein charakteristischer Bestandteil thrombolithischer Mud Mounds (z.B. Gandara Mound). Die funktionelle Rolle von Lithocodium/Bacinella bei der Mud Mound Genese umfaßt Baffling und Binding, AutomikritProduktion durch Kalzifizierung innerhalb organischer Schleimhüllen und eine Mikritproduktion über intensive Bohraktivitäten an eingelagerten karbonatischen Hartteilen. Das massenhafte Auftreten von Lithocodillm/ Bacinella und diversen Algen/Mikroben kann mit einer längerfristigen Eutrophierung des Lebensraumes oder mit Schwankungen der Karbonat-Alkalinät des Meerwassers erklärt werden."],["dc.description.abstract","A section including Lithocodium/ Bacinella boundstones with a thickness of up to 8 m is reported from the Lower /Middle Albian of northern Spain. According to microfacies and sedimentological analyses the bathymetric position of the Lithocodium/ Bacinella banks ranges from deeper subtidal to shaUowest subtidal/intertidal conditions. The maximum depth is related to the photic zone, which ,itself is controled by the amount of muddy suspension. The upper bathymetric limit is mechanically defin'ed and corresponds to increased depositional energy (i.e. waves and tidal currents). Together with other algae and microbes Lithocodium/ Bacinella is a major constituent of thrombolitic mud mounds (Gandara mound). In the context of mud mound genesis the functional role of Lithocodium/ Bacinella includes baffling and binding, the production of micrite via the calcification inside of mucilagenous sheaths, and via intensive boring activities upon and inside of skeletal hardparts. The mass occurrence of Lithocodium/ Bacinella with associated algae and microbes may be explained by a longer ranging eutrophism of the environment or by shifts in seawater carbonate alkalinity."],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","50213349x"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2172"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60942"],["dc.language.iso","de"],["dc.notes.intern","Migrated from goescholar"],["dc.publisher","Fachber. Geowissenschaften"],["dc.publisher.place","Berlin"],["dc.relation.crisseries","Berliner geowissenschaftliche Abhandlungen. Reihe E, Paläobiologie"],["dc.relation.ispartof","Miscellanea palaeontologica"],["dc.relation.ispartofseries","Berliner geowissenschaftliche Abhandlungen. Reihe E;3"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Karbonatbänke mit Lithocodium aggregatum Elliott, Bacinella irregularis Radoicic ; Paläobathymetrie, Paläoökologie und stratigraphisches Äquivalent zu thrombolithischen Mud Mounds"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","245"],["dc.bibliographiccitation.issue","¾"],["dc.bibliographiccitation.journal","Paläontologische Zeitschrift"],["dc.bibliographiccitation.lastpage","260"],["dc.bibliographiccitation.volume","59"],["dc.contributor.author","Engeser, Theo"],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2019-07-10T08:12:32Z"],["dc.date.available","2019-07-10T08:12:32Z"],["dc.date.issued","1985"],["dc.description.abstract",": From the Early Aptian (\"Töck\") of Heligoland (North Germany) three new species, one new genus and one new family of Teuthids are described: M astigophora stuehmeri n. sp., Boreopeltis helgolandiae n. gen. n. sp. and Maioteuthis damesi n. sp. The new genus Boreopeltis n. gen. ist placed in the family Plesioteuthididae NAEF 1921. The genus Mastigophora OWEN 1856 previously attributed to the family Loligosepiidae VAN REGTEREN ALTENA 1949 is proposed as type genus of the new family Mastigophoridae. Two poorly preserved specimens cannot\"be identified specifically (?Trachyteuthis sp. and Plesioteuthis sp.). Kurz fas sung: Aus dem Unterapt (»Töck«) von Helgoland werden drei neue Arten, eine neue Gattung und eine neue Familie von Teuthiden beschrieben: M astigophora stuehmeri n. sp., Boreopeltis helsolandiae n. gen. n. sp. und Maioteuthis damesi n. sp. Die Gattung Boreopeltis n. gen. wird zur Familie PleslOteuthididae NAEF 1921 gestellt. Die Gattung Mastigophora OWEN 1856, bisher zur Familie Loligosepiidae VAN REGTEREN ALTENA 1949 gestellt, wird zur Typusgattung der neuen Familie Mastigophoridae vorgeschlagen. Zwei weitere Exemplare können nicht näher bestimmt werden (?Trachyteuthis sp. und Plesioteuthis sp.)."],["dc.format.mimetype","application/pdf"],["dc.identifier.ppn","501760415"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/2184"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/60954"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.rights","Goescholar"],["dc.rights.access","openAccess"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject","Paläontologie: Allgemeines"],["dc.subject.ddc","560"],["dc.title","Teuthiden aus dem Unterapt (\"Töck\") von Helgoland (Schleswig-Holstein, Norddeutschland)"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]