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","1535"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Biogeosciences"],["dc.bibliographiccitation.lastpage","1548"],["dc.bibliographiccitation.volume","15"],["dc.contributor.author","Duda, Jan-Peter"],["dc.contributor.author","Thiel, Volker"],["dc.contributor.author","Bauersachs, Thorsten"],["dc.contributor.author","Mißbach, Helge"],["dc.contributor.author","Reinhardt, Manuel"],["dc.contributor.author","Schäfer, Nadine"],["dc.contributor.author","Van Kranendonk, Martin J."],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2019-07-09T11:45:21Z"],["dc.date.available","2019-07-09T11:45:21Z"],["dc.date.issued","2018"],["dc.description.abstract","Archaean hydrothermal chert veins commonly contain abundant organic carbon of uncertain origin (abiotic vs. biotic). In this study, we analysed kerogen contained in a hydrothermal chert vein from the ca. 3.5 Ga Dresser Formation (Pilbara Craton, Western Australia). Catalytic hydropyrolysis (HyPy) of this kerogen yielded n-alkanes up to n-C22, with a sharp decrease in abundance beyond n-C18. This distribution ( n-C18) is very similar to that observed in HyPy products of recent bacterial biomass, which was used as reference material, whereas it differs markedly from the unimodal distribution of abiotic compounds experimentally formed via Fischer–Tropsch-type synthesis. We therefore propose that the organic matter in the Archaean chert veins has a primarily microbial origin. The microbially derived organic matter accumulated in anoxic aquatic (surface and/or subsurface) environments and was then assimilated, redistributed and sequestered by the hydrothermal fluids (“hydrothermal pump hypothesis”)"],["dc.identifier.doi","10.5194/bg-15-1535-2018"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/15113"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/59212"],["dc.language.iso","en"],["dc.relation.issn","1726-4189"],["dc.relation.orgunit","Abteilung Geobiologie"],["dc.subject.ddc","550"],["dc.title","Ideas and perspectives: hydrothermally driven redistribution and sequestration of early Archaean biomass – the “hydrothermal pump hypothesis”"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["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","125"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Journal of Microbiological Methods"],["dc.bibliographiccitation.lastpage","134"],["dc.bibliographiccitation.volume","40"],["dc.contributor.author","Manz, W."],["dc.contributor.author","Arp, Gernot"],["dc.contributor.author","Schumann-Kindel, G."],["dc.contributor.author","Szewzyk, U."],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2018-11-07T11:16:13Z"],["dc.date.available","2018-11-07T11:16:13Z"],["dc.date.issued","2000"],["dc.description.abstract","Widefield deconvolution epifluorescence microscopy (WDEM) combined with fluorescence in situ hybridization (FISH) was performed to identify and characterize single bacterial cells within sections of the mediterranean sponge Chondrosia reniformis. Sponges were embedded in paraffin wax or plastic prior to the preparation of thin sections, in situ hybridization and microscopy. Serial digital images generated by widefield epifluorescence microscopy were visualized using an exhaustive photon reassignment deconvolution algorithm and three-dimensional rendering software. Computer processing of series of images taken at different focal planes with the deconvolution technique provided deblurred three-dimensional images with high optical resolution on a submicron scale. Results from the deconvolution enhanced widefield microscopy were compared with conventional epifluorescent microscopical images. By the application of the deconvolution algorithm on digital image data obtained with widefield epifluorescence microscopy after FISH, the occurrence and spatial arrangement of Desulfovibrionaceae closely associated with micropores of Chondrosia reniformis could be visualized. (C) 2000 Elsevier Science B.V. All rights reserved."],["dc.identifier.doi","10.1016/S0167-7012(99)00103-7"],["dc.identifier.isi","85934600002"],["dc.identifier.pmid","10699668"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11243"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/54538"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0167-7012"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","CC BY-NC-ND 3.0"],["dc.rights.uri","http://creativecommons.org/licenses/by-nc-nd/3.0/"],["dc.title","Widefield deconvolution epifluorescence microscopy combined with fluorescence in situ hybridization reveals the spatial arrangement of bacteria in sponge tissue"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","3"],["dc.bibliographiccitation.journal","Facies"],["dc.bibliographiccitation.lastpage","39"],["dc.bibliographiccitation.volume","29"],["dc.contributor.author","Reitner, Joachim"],["dc.date.accessioned","2010-08-21T10:38:36Z"],["dc.date.accessioned","2021-10-27T13:13:58Z"],["dc.date.available","2010-08-21T10:38:36Z"],["dc.date.available","2021-10-27T13:13:58Z"],["dc.date.issued","1993"],["dc.description.abstract","From shallow water caves of fringing reefs related to continental islands of the Lizard Island Section thrombolitic micritic microbialites were observed. The microbialites exhibit always a light decreasing facies succession. The succession starts with a coralgal community and ends with light independent microbial biofilms and benthos (coralline sponges). The sessile mineralized benthos community is constructed of crustose foraminifera, serpuli$, thecidean brachiopods, bryozoans, and coralline sponges. The observed benthic community is very similar 10 thoseone bbserved in cryptic habitates of Aptian and Albian reefs of northem Spain. For longtime studies of the m~crobialite formation and growth rates of coralline sponges the specimens were stained in vivo, within their natural habitat with histochemical fluorochromes and nonfluorescent agents. Main results are a very slow growth of the microbialite and associated sponges (50-100 Ilm/y). Only few calcifying microbes are participators during microbialite formation. Calcifying acidic organic macromolecules are mainly responsible for microbialite formation by cementing detritical material. FelMn-bacterial biofilms are responsible for strong corrosion of the microbialite. Beside the corrosive activity of the Fe/Mn-bacterial biofilms boring sponges (Aka, Cliona) are the main destructors. The investigations began in 1990 with a pilot study in fringing reefs of Lizard Island (Great Barrier Reef) and reefs of the outer barrier for comparison. Main goals are to study this environment under normal conditions and for comparison under controlled artificial conditions in seawater running aquaria. Two reef caves were selected for longtime research and all experiments were carried out within these caves. H.ZANKL(Marburg)hasrecentlyfoundnearly similar microbialites in cryptic habitates of reefs of St.Croix (US Virgin Islands, central Caribbean realm) (ZANKL 1993). Comparative fossil examples were studied by NEUWEILER (1993) on middle Albian reefs of northem Spain and KEupp et al. (this volume) for Jurassic ones. Both studies refer to the presented data. Purpose of this study is to demonstrate the growing procedure of a modem type of cryptic, light independent microbialite, the interaction with associated benthos, and its significance as a key facies to understandfossil metazoan-micriticl microbialitereefs. To understand these very complex processes it is neecessary to review and compile modem concepts of biomineralisation, biofilms, and e.g. the alkalinity question. Therefore mixing of own results and reviews is planned and intended! Main goal of this study is creation of a working hypothesis to understand the processes of formation of micritic/microbial build ups (\"mud mounds\"). Geochemically the observed microbiali tes are composed of mainly high-Mg calcites and exhibit high positive ö13C (+3 to +4) values."],["dc.format.mimetype","application/pdf"],["dc.identifier.doi","10.1007/BF02536915"],["dc.identifier.ppn","502141557"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/4488"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/91822"],["dc.language.iso","en"],["dc.notes.intern","Migrated from goescholar"],["dc.relation.issn","1612-4820"],["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.ddc","560"],["dc.title","Modern cryptic microbialite/metazoan facies from Lizard Island (Great Barrier Reef, Australia) formation and concepts"],["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"]]