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The Barremian Heteromorph Ammonite Dissimilites from Northern Italy: Taxonomy and Evolutionary Implications
The Barremian heteromorph ammonite Dissimilites from northern Italy: Taxonomy and evolutionary implications ALEXANDER LUKENEDER and SUSANNE LUKENEDER Lukeneder, A. and Lukeneder, S. 2014. The Barremian heteromorph ammonite Dissimilites from northern Italy: Taxon- omy and evolutionary implications. Acta Palaeontologica Polonica 59 (3): 663–680. A new acrioceratid ammonite, Dissimilites intermedius sp. nov., from the Barremian (Lower Cretaceous) of the Puez area (Dolomites, northern Italy) is described. Dissimilites intermedius sp. nov. is an intermediate form between D. dissimilis and D. trinodosum. The new species combines the ribbing style of D. dissimilis (bifurcating with intercalating single ribs) with the tuberculation style of D. trinodosum (trituberculation on entire shell). The shallow-helical spire, entirely comprising single ribs intercalated by trituberculated main ribs, is similar to the one of the assumed ancestor Acrioceras, whereas the increasing curvation of the younger forms resembles similar patterns observed in the descendant Toxoc- eratoides. These characters support the hypothesis of a direct evolutionary lineage from Acrioceras via Dissimilites to Toxoceratoides. D. intermedius sp. nov. ranges from the upper Lower Barremian (Moutoniceras moutonianum Zone) to the lower Upper Barremian (Toxancyloceras vandenheckii Zone). The new species allows to better understand the evolu- tion of the genus Dissimilites. The genus appears within the Nicklesia pulchella Zone represented by D. duboise, which most likely evolved into D. dissimilis. In the Kotetishvilia compressissima Zone, two morphological forms developed: smaller forms very similar to Acrioceras and forms with very long shaft and juvenile spire like in D. intermedius sp. nov. The latter most likely gave rise to D. subalternatus and D. trinodosum in the M. -
Origin of the Tethyan Hemihoplitidae Tested with Cladistics (Ancyloceratina, Ammonoidea, Early Cretaceous): an Immigration Event? Didier Bert, Stéphane Bersac
Origin of the Tethyan Hemihoplitidae tested with cladistics (Ancyloceratina, Ammonoidea, Early Cretaceous): an immigration event? Didier Bert, Stéphane Bersac To cite this version: Didier Bert, Stéphane Bersac. Origin of the Tethyan Hemihoplitidae tested with cladistics (Ancylo- ceratina, Ammonoidea, Early Cretaceous): an immigration event?. Carnets de Geologie, Carnets de Geologie, 2014, 14 (13), pp.255-272. insu-01071656 HAL Id: insu-01071656 https://hal-insu.archives-ouvertes.fr/insu-01071656 Submitted on 17 Oct 2014 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Carnets de Géologie [Notebooks on Geology] - vol. 14, n° 13 Origin of the Tethyan Hemihoplitidae tested with cladistics (Ancyloceratina, Ammonoidea, Early Cretaceous): an immigration event? Didier BERT 1, 2 Stéphane BERSAC 2 Abstract: The Late Barremian Hemihoplitidae (Ancyloceratina, Ammonoidea) are widely known in the northern Tethyan Margin and the Essaouira-Agadir Basin (Morocco). Their rapid evolution and diversifi- cation make them one of the key groups for that period, but their origin remains poorly known and several competing hypotheses have been published. These hypotheses are tested here with cladistic analysis in order to reject those receiving the least support and discuss those well supported. -
(Ammonoidea, Gassendiceratinae), and New Ammonite Biohorizon for the Upper Barremian of Southeastern France
Carnets de Géologie / Notebooks on Geology - Article 2009/02 (CG2009_A02) Pseudoshasticrioceras bersaci nov. sp. (Ammonoidea, Gassendiceratinae), and new ammonite biohorizon for the Upper Barremian of southeastern France Didier BERT* 1 Gérard DELANOY 2 Abstract: Research in the Feraudianus Subzone of the Sartousiana Zone of the Barremian stage led to the discovery of a new species of Pseudoshasticrioceras: P. bersaci nov. sp. Its study provides evidence concerning the developments of the latest Gassendiceratinae BERT et alii, 2006, and the relationship between the genus Pseudoshasticrioceras DELANOY, 1998, and Gassendiceras BERT et alii, 2006. In particular, this new species is derived from Pseudoshasticrioceras magnini (DELANOY, 1992) by a minor revision in the processes of ontogenesis (retardation of ornamentation - neoteny). However, the evolution towards Pseudoshasticrioceras autrani DELANOY, 1998, implies a "failure" in this process that may possibly be related to parallel changes in environmental conditions. On the other hand, the very closely defined stratigraphic position of Pseudoshasticrioceras bersaci nov. sp., and its position in the anagenetic lineage of Pseudoshasticrioceras, demonstrates its interest as a biostratigraphic marker: a new Bersaci Biohorizon is proposed; it is located between the Magnini and the Autrani biohorizons. Key Words: Ammonitinae; Pseudoshasticrioceras; Gassendiceratinae; Upper Barremian; Sartousiana Zone; Feraudianus Subzone; biozonation; southeastern France. Citation: BERT D. & DELANOY G. (2009).- -
A Comparison of the Ammonite Faunas of the Antarctic Peninsula and Magallanes Basin
J. geol. Soc. London, Vol. 139, 1982, pp. 763-770, 1 fig, 1 table. Printed in Northern Ireland A comparison of the ammonite faunas of the Antarctic Peninsula and Magallanes Basin M. R. A. Thomson SUMMARY: Ammonite-bearingJurassic and Cretaceous sedimentary successions are well developed in the Antarctic Peninsula and the Magallanes Basin of Patagonia. Faunas of middle Jurassic-late Cretaceous age are present in Antarctica but those of Patagonia range no earlier than late Jurassic. Although the late Jurassic perisphinctid-dominated faunas of the Antarctic Peninsulashow wide-ranging Gondwana affinities, it is not yet possible to effect a close comparison with faunas of similar age in Patagonia because of the latter's poor preservation and our scant knowledge of them. In both regions the Neocomian is not well represented in the ammonite record, although uninterrupted sedimentary successions appear to be present. Lack of correspondence between the Aptian and Albian faunas of Alexander I. and Patagonia may be due to major differences in palaeogeographical setting. Cenomanian-Coniacian ammonite faunas are known only from Patagonia, although bivalve faunas indicate that rocks of this age are present in Antarctica. Kossmaticeratid faunas mark the late Cretaceous in both regions. In Antarcticathese have been classified as Campanian, whereas in Patagonia it is generally accepted, perhaps incorrectly, that these also range into the Maestrichtian. Fossiliferous Jurassic and Cretaceous marine rocks are rize first those of the Antarctic Peninsula and then to well developedin theAntarctic Peninsula, Scotia compare them with those of Patagonia. Comparisons Ridge andPatagonia (Fig. 1A).In Antarcticathese between Antarctic ammonite faunas and other Gond- rocks are distributed along the western and eastern wana areas wereoutlined by Thomson (1981a), and margins of theAntarctic Peninsula, formerly the the faunas of the marginal basin were discussed in magmatic arc from which the sediments were derived. -
THE HETEROMORPHS and AMMONOID EXTINCTION by JOST WIEDMANN Geologisch-Palaontologischesinstitut, Universitat Tiibingen
Biol. Rev. (1969), 44, pp. 563-602 563 THE HETEROMORPHS AND AMMONOID EXTINCTION BY JOST WIEDMANN Geologisch-PalaontologischesInstitut, Universitat Tiibingen (Received 19 May 1969) CONTENTS I. Introduction . 563 B. Developmental plasticity in space and time in heterornorphs . 590 11. Discussion . 565 C. Phylogenetic ‘laws’ and hetero- A. Triassic heteromorphs . 567 morphs . 590 B. Jurassic heteromorphs . 569 D. Factors in heteromorph evolution 592 E. Ammonoid extinction 593 C. Cretaceous heteromorphs . 572 . D. The course of heteromorph evolu- IV. Summary . 598 tion ..... 599 111. General remarks . A. Homologies and sutures in hetero- morphs and ammonoids . 588 I. INTRODUCTION The image of heteromorph ammonoids is today linked in our minds with notions of aberrant shell form, degeneration, typolysis and phylogenetic extinction. In most palaeontological works dealing with evolutionary principles the so-called heteromorphs are seen as a welcome illustration of the more or less synchronous extinction of com- plete Bauplane, a phenomenon which cannot be observed in nature and is therefore explicable only with difficulty. ‘There are furthermore aberrant forms which rapidly, one after another, show an ever stronger tendency to degenerate and produce biologically absurd structures which, if not directly lethal, have always been impartially understood as ridiculous for the basic concept of the ammonite form.’ (Translated from DacquC, 1935, p. 32.) ‘Just as the great ceratitoid group of ammonoids produced retrogressive as well as stationary and progressive forms during the Trias, so from one, or several, of the families just mentioned there arose decadent lines of descent. .Thus in Baculites the whole organization was affected by decadent influences, and it is therefore the most perfect impression of all-round retro- gression among the ammonoids.’ (Swinnerton, 1930, pp. -
Heteromorphic Ammonites from Northern Germany
New data on Early Cretaceous (Hauterivian-Barremian) heteromorphic ammonites from northern Germany Micheil V. Kakabadze & Philip J. Hoedemaeker Kakabadze, M.V. & Hoedemaeker, Ph.J. New data on Early Cretaceous (Hauterivian-Barremian) hetero- morphic ammonites from northern Germany. Scripta Geologica, 140: 1-168, 86 pls., 12 figs., Leiden, Janu- ary 2010. M.V. Kakabadze, A. Djanelidze Institute of Geology, M. Alexidze St. 1/9, 0193 Tbilisi, Georgia ([email protected]); Ph.J. Hoedemaeker, Nationaal Natuurhistorisch Museum, P.O. Box 9517, NL-2300 RA Leiden, The Netherlands ([email protected]). Key words – heteromorphic ammonites, systematics, Hauterivian, Barremian, stratigraphy, northern Germany, new taxa. The stratigraphic ranges and systematics of heteromorphic ammonites from Lower Cretaceous (Haute- rivian-Barremian) deposits in Lower Saxony, northern Germany, are revised. Nine genera and forty- seven species of the family Ancyloceratidae Gill, 1871, are described. One genus (Fissicostaticeras) and 20 species are new; Emericiceras ressense, E. sornayiforme, E. serpentinum, E. subtilicostatum, E. gotti, E. hanno verense, E. kemperi, Crioceratites hastensis, C. subisocostatus, C. vermiformis, Fissicostaticeras claviferum, F. aequicostatoides, F. rarocinctoides, Paracrioceras kleini, Acrioceras (Acrioceras) sarstedtense, A. (A.) crassico statum, A. (A.) aegidii, A. (A.) longum, A. (A.) astrictum and Uhligia aegidii. Contents Introduction ................................................................................................................................................................ -
Nannoconid Assemblages in Upper Hauterivian-Lower Aptian Limestones of Cuba: Their Correlation with Ammonites and Some Planktonic Foraminifers2
STUDIA GEOLOGI CA POLONICA Vol. 114, Krak6w 1999, pp. 35-75. Mesozoic stratigraphy of Cuba Edited by A. Pszczolkowski Andrzej PSZCZOL• KOWSKI 1 & Ryszard MYCZYNSKI' I Nannoconid assemblages in Upper Hauterivian-Lower Aptian limestones of Cuba: their correlation with ammonites and some planktonic foraminifers2 (Figs 1- 13, Tabs 1- 3) Abstract. The nannoconids are abundant in the Lower Cretaceous pelagic limestones in western and central Cuba. In some lin1estone beds, these nannofossils occur together with ammonites or planktonic foraminifers. Our samples were collected from the Polier, Veloz and Paraiso formations. The Late Hauterivian to Early Aptian age of the studied samples is based mainly on ammonites. The nannoconids identified in these samples are grouped in 4 assemblages: Late Hauterivian, Early Barremian, Late Barremian and late Early Aptian. In the Early Barremian assemblage, the narrow canal nannoconids are by far more frequent than the wide-canal ones. Small specimens, classified herein provisionally as N truittii truittii, occur also in this assemblage. On the other hand, the representatives of the Nannoconus steinmannii group are absent in the late Early Aptian assemblage, which includes the wide canal forms only. Nannoconids found in one sample may represent an assemblage of the earliest Aptian age. Key words: Nannoconid assemblages, ammonites, planktonic foraminifers, Lower Cretaceous, western and central Cuba. INTRODUCTION Pelagic limestones are the most important lithologic components of the Creta ceous passive continental margin and basinal successions in Cuba. These fine grained limestones often lack identifiable macrofauna, while stratigraphically use ful microfossils are scarce or absent, especially in the Hauterivian to Aptian carbon ate rocks. -
Berichte Der Geologischen Bundesanstalt Nr. 46 V
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Berichte der Geologischen Bundesanstalt Nr. 46 V International Symposium Cephalopods - Present and Past Vienna 6 - 9th September 1999 Institute of Palaeontology, University of Vienna Geological Survey of Austria Museum of Natural History Vienna ABSTRACTS VOLUME Edited by Kathleen Histon Geologische Bundesanstalt Vienna, July 1999 1 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Reference to this Volume: HISTON, K. (Ed.) V International Symposium Cephalopods - Present and Past, Vienna. Abstracts Volume. - Ber. Geol. Bundesanst. 46, 1-134, 111., Wien 1999 ISSN 1017-8880 Editor's address: Kathleen Histon Geological Survey of Austria Rasumofskygasse 23 A-1031 Vienna Austria Impressum: Alle Rechte für das In- und Ausland vorbehalten. Copyright Geologische Bundesanstalt, Wien, Österreich. Medieninhaber, Herausgeber und Verleger: Verlag der Geologischen Bundesanstalt, A-1031 Wien, Postfach 127, Rasumofskygasse 23, Österreich. Für die Redaktion verantwortlich: Kathleen Histon, Geologische Bundesanstalt Layout: Kathleen Histon, Geologische Bundesanstalt Druck: Offsetschnelldruck Riegelnik, A-1080 Wien Verlagsort und Gerichtsstand ist Wien Herstellungsort Wien Die Autoren sind für ihre Beiträge verantwortlich. Ziel der "Berichte der Geologischen Bundesanstalt" ist die Verbreitung wissenschaftlicher Ergebnisse durch die Geologische Bundesanstalt. Die "Berichte der Geologischen Bundesanstalt" sind im Buchhandel nur eingeschränkt erhältlich. 2 ©Geol. Bundesanstalt, Wien; -
Ecological Replacement of Associations of Mollusc Plankton and Giant Filter Feeders After the Cretaceous?
The old and the new plankton: ecological replacement of associations of mollusc plankton and giant filter feeders after the Cretaceous? Amane Tajika1, Alexander Nützel2 and Christian Klug1 1 Paläontologisches Institut und Museum, Universität Zürich, Zürich, Switzerland 2 SNSB-Bayerische Staatssammlung für Paläontologie und Geologie, Department of Earth and Environmental Sciences, Palaeontology & Geobiology, GeoBio-Center LMU, München, Germany ABSTRACT Owing to their great diversity and abundance, ammonites and belemnites represented key elements in Mesozoic food webs. Because of their extreme ontogenetic size increase by up to three orders of magnitude, their position in the food webs likely changed during ontogeny. Here, we reconstruct the number of eggs laid by large adult females of these cephalopods and discuss developmental shifts in their ecologic roles. Based on similarities in conch morphology, size, habitat and abundance, we suggest that similar niches occupied in the Cretaceous by juvenile ammonites and belemnites were vacated during the extinction and later partially filled by holoplanktonic gastropods. As primary consumers, these extinct cephalopod groups were important constituents of the plank- ton and a principal food source for planktivorous organisms. As victims or, respectively, profiteers of this case of ecological replacement, filter feeding chondrichthyans and cetaceans likely filled the niches formerly occupied by large pachycormid fishes during the Jurassic and Cretaceous. Subjects Developmental Biology, Evolutionary Studies, Marine Biology, Paleontology, Zoology Keywords Belemnitida, Ammonoidea, Cretaceous, Fecundity, Palaeogene, Filter feeders, Holoplanktonic gastropoda, Pachycormiformes, Mass extinctions Submitted 25 September 2017 Accepted 12 December 2017 Published 9 January 2018 INTRODUCTION Corresponding author Christian Klug, [email protected] The fate of individual groups of marine organisms at mass extinctions is of considerable Academic editor interest (e.g., Jablonski & Raup, 1994; Jablonski, 2008). -
Size Reduction and Ornamental Oscillation Within a Barremian
Size reduction and ornamental oscillation within a Barremian lineage of giant heteromorphic ammonites (Early Cretaceous, northwestern Tethyan margin) Didier Bert, Stéphane Bersac, Josep Juárez-Ruiz, Zoë Hughes To cite this version: Didier Bert, Stéphane Bersac, Josep Juárez-Ruiz, Zoë Hughes. Size reduction and ornamental oscilla- tion within a Barremian lineage of giant heteromorphic ammonites (Early Cretaceous, northwestern Tethyan margin). Cretaceous Research, Elsevier, 2018, 88, pp.173-189. 10.1016/j.cretres.2017.02.001. insu-01461722 HAL Id: insu-01461722 https://hal-insu.archives-ouvertes.fr/insu-01461722 Submitted on 8 Feb 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Size reduction and ornamental oscillation within a Barremian lineage of giant heteromorphic ammonites (Early Cretaceous, northwestern Tethyan margin) Didier Bert, Stéphane Bersac, Josep Juárez-Ruiz, Zoë Hughes PII: S0195-6671(16)30212-9 DOI: 10.1016/j.cretres.2017.02.001 Reference: YCRES 3523 To appear in: Cretaceous Research Received Date: 14 September 2016 Revised Date: 1 February 2017 Accepted Date: 1 February 2017 Please cite this article as: Bert, D., Bersac, S., Juárez-Ruiz, J., Hughes, Z., Size reduction and ornamental oscillation within a Barremian lineage of giant heteromorphic ammonites (Early Cretaceous, northwestern Tethyan margin), Cretaceous Research (2017), doi: 10.1016/j.cretres.2017.02.001. -
05. Palaeontology
104 05. Palaeontology Torsten Scheyer, Christian Klug, Lionel Cavin, Allison Daley Schweizerische Paläontologische Gesellschaft, Kommission des Swiss Journal of Palaeontology (KSJP) Symposium 5: Palaeontology TALKS: 5.1 Balcarcel A., Sánchez-Villagra M.R., Orliac M.: The Pleistocene Camelid Brain 5.2 Bastiaans D., Herbst E.C., Scheyer T.M.: Re-fleshing fossils: cranial reconstructions of Thalattosauriformes. 5.3 Bath Enright O., Minter N., Sumner S., Mangano M.G., Buatois L.: A doomed expedition? Investigating the concept of doomed pioneers using an annular flume and the polychaete, Alitta virens 5.4 Benites-Palomino A., Aguirre-Fernández G., Carrillo-Briceño1 J.D., Sánchez R., Moreno-Bernal J.W., Jaramillo C., Vanegas A., Reyes A., Sánchez-Villagra M.R.: New Miocene aquatic mammal remains from Northern South America 5.5 Cemile Solak: Benthic foraminifera and facies of the Albian-Cenomanian platform limestones in the Geyik Dağı area, Central Taurides, Turkey 5.6 Daley A.C.: Diversity and Evolution of Radiodonta during the Early Paleozoic 5.7 Edward O., Bucher H., Leu M., Adatte T., Baud A., Vennemann T.: Do Tethyan mercury anomalies reflect a global volcanic trigger for the Smithian/Spathian boundary climatic and biotic crisis? 5.8 Galasso F., Feist Burkhardt S., Schmid-Röhl A., Benasconi S., Schneebeli-Hermann E.: The marine and terrestrial response during the Lower Jurassic: A multi-proxy approach to reconstruct the depositional environment 5.9 Hautmann M., Friesenbichler E., Bucher H.: Evolutionary ecology of benthic marine communities -
Paleontological Journal
ISSN 0031-0301 PALEONTOLOGICAL JOURNAL A TRANSLATION OF IIAJIEOHTOJIOfllqECl\liM JI\YPHAJI 2. Ruzhencev, V. E. and M. F. Bogoslovakaya, 1971, Namyurskii etap v evolyutsii ammonoidey. Rannenamyurskiye ammonoidei. (The Namurian stage in ammonoid evo lution. Early Namurian ammonoids. ) Tr. Paleontol. in-ta AN SSSR, Moscow, Vol. 133. 3. Ruzhencev, V. E. and M. F. Bogoslovskaya, 1978, Namyurskii etap v evolyutsii ammonoidey. Pozdnenamyurskiye ammonoidei. (The Namurian stage in ammonoid evolution. Late Namurian ammonoids). Tr. Paleontol. in-ta AN SSSR, Moscow, Vol. 168. 4. Bisat, W. s., 1950, The junction faunas of Visean and Namurian. Trans. Leeds Geol. Assoc. , Vol. 6, Pt. 3, pp. 10-26. 5. Currie, E. D. , 1954, Scottish Carboniferous goniatites, Trans. Roy. Soc. Edin burgh, Vol. 62, Pt. 2, pp. 527-602. 6. Gordon, M. , 1964, Carboniferous cephalopods of Arkansas. U. S. Geol. Surv. Profess. Paper 460, pp. 1-322. 7. Korn, D. , 1988, Die Goniatiten des Kulmplattenkalkes (Cephalopoda, Ammonoidea; Untercai'bon; Rheinisches Schiefergebirge). Geol. und Palaontol. West f. ' MUnster, No. 11. 8. Kullmann, J., 1981, Carboniferous goniatites. In: The Ammonoidea. Syst. Assoc. Spec. Volume 18, London, pp. 37-48. 9. Plummer, F. B. and G. Scott, 1937, Upper Paleozoic ammonites in Texas. In: The Geology of Texas, Vol. 3, Univ. Texas Bull. 3701. 10. Ramsbottom, W. H. C. , 1970, Some British Carboniferous goniatites of the family Anthracoceratidae. Bull. Geol. Surv. Gr. Brit,, No. 32, pp. 53-60. UDC 564. 53:551. 763 REVISION OF HETEROMORPH AMMONOIDS. GEOGRAPHIC DISTRIBUTION OF Emericiceras SARKAR, 1954 S. S. Sarkar Howrah, West Bengal, India The most recent review of uncoiled Lower Cretaceous ammonoids, based on materi al collected during the last 15 0 years and housed in various universities and mu seums in France, and on the Astier collection in the British Museum of Natural Hi story, London, was published 35 years ago [26].