The Hydrostatics and Hydrodynamics of Prominent Heteromorph Ammonoid Morphotypes and the Functional Morphology of Ammonitic Septa

Total Page:16

File Type:pdf, Size:1020Kb

The Hydrostatics and Hydrodynamics of Prominent Heteromorph Ammonoid Morphotypes and the Functional Morphology of Ammonitic Septa THE HYDROSTATICS AND HYDRODYNAMICS OF PROMINENT HETEROMORPH AMMONOID MORPHOTYPES AND THE FUNCTIONAL MORPHOLOGY OF AMMONITIC SEPTA A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy By DAVID JOSEPH PETERMAN M.S., Wright State University, 2016 B.S., Wright State University, 2014 2020 Wright State University WRIGHT STATE UNIVERSITY GRADUATE SCHOOL April 17th, 2020 I HEREBY RECOMMEND THAT THE DISSERTATION PREPARED UNDER MY SUPERVISION BY David Joseph Peterman ENTITLED The hydrostatics and hydrodynamics of prominent heteromorph ammonoid morphotypes and the functional morphology of ammonitic septa BE ACCEPTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Doctor of Philosophy Committee on Final Examination Christopher Barton, PhD Dissertation Director Charles Ciampaglio, PhD Don Cipollini, PhD Director, Environmental Sciences PhD program Margaret Yacobucci, PhD Barry Milligan, PhD Interim Dean of the Graduate School Sarah Tebbens, PhD Stephen Jacquemin, PhD ABSTRACT Peterman, David Joseph. PhD. Environmental Sciences PhD Program, Wright State University, 2020. The hydrostatics and hydrodynamics of prominent heteromorph ammonoid morphotypes and the functional morphology of ammonitic septa. Ammonoid cephalopods have chambered shells that regulated buoyancy. The morphology of their shells strongly influenced the physical properties acting on these animals during life. Heteromorph ammonoids, which undergo changes in coiling throughout ontogeny, are the focus of this dissertation. The biomechanics of these cephalopods are investigated in a framework involving functional morphology, paleoecology, and possible modes of life. Constructional constraints were investigated for the marginally-corrugated septal walls within the chambered ammonoid shell. These constraints governed the positive relationship between septal complexity and terminal size. Furthermore, increased septal complexity facilitated liquid retention via surface tension. More complex septa would have increased liquid retention at larger scales, which could have been used as liquid ballasts, reserves for buoyancy adjustment, or to prevent disruptive sloshing of cameral liquid. New methods for the virtual reconstruction of cephalopod shells are described. The shell constrains the volume and shape of each material of unique density that influenced organismal mass and its distribution. Therefore, these virtual models can be used to compute the conditions for neutral buoyancy, hydrostatic stability, syn vivo orientation, and the directional efficiency of movement. The rigid shell also constrains how the living ammonoid would have interacted with fluids in a dynamic setting. A new iii method for the construction of neutrally-buoyant, physical models is described, which can be used to compute hydrodynamic properties such as drag and swimming velocity. The biomechanics of three heteromorph ammonoid morphotypes from the North American Western Interior Seaway are discussed. These morphotypes represent the families Baculitidae, Nostoceratidae, and Scaphitidae. These investigations provide a better understanding of the hydrostatic and hydrodynamic properties that constrained the modes of life for the majority of prominent ammonoid taxa from the Late Cretaceous of the U.S. Western Interior. Novel modeling techniques provide data that suggests heteromorph ammonoids had selective pressures imposed on them for specific biological functions or life habits, rather than pointless morphological experimentation or liberation from such evolutionary pressures. These syn vivo physical properties also influenced the biogeographic dispersal and paleoecology for these enigmatic creatures that were once vital components of marine ecosystems. iv TABLE OF CONTENTS Page LIST OF FIGURES .............................................................................................. xi LIST OF TABLES .............................................................................................. xiv LIST OF INSTITUTIONAL ABBREVIATIONS .............................................. xvi PUBLICATION LIST OF THE DISSERTATION ........................................... xvii AUTHOR CONTRIBUTIONS ............................................................................ xix ACKNOWLEDGEMENTS ................................................................................. xxi 1.0 INTRODUCTION ...................................................................................................1 1.1 REFERENCES ............................................................................................8 2.0 Power scaling of ammonitic suture patterns from Cretaceous Ancyloceratina (Ammonoidea): constraints on septal/sutural complexity ......................................9 2.1 INTRODUCTION ....................................................................................10 2.1.1 Fractal geometry of ammonitic sutures .........................................12 2.1.2 Previous studies of the power scaling of ammonitic sutures ........14 2.2 METHODS ...............................................................................................16 2.2.1 Box-counting method of fractal analysis ......................................16 2.2.2 Box method as implemented by the fractal analysis software – Benoit 1.3 ......................................................................................16 2.2.3 Reconstruction of a baculite septum for capillary retention experiments ....................................................................................18 v 2.3 RESULTS ..................................................................................................19 2.3.1 Distribution in complexity and whorl height .................................19 2.3.2 Sutural ontogeny in Baculites compressus ....................................21 2.3.3 Sutural symmetry and asymmetry in heteromorphic ammonites ..22 2.3.4 Sutural complexity and whorl height .............................................23 2.3.5 Capillary retention simulated by 3D printed models .....................27 2.4 DISCUSSION ............................................................................................29 2.4.1 Septal asymmetry in 3D coiled heteromorphs and the scaling properties of their hemisutures .......................................................29 2.4.2 Sutural/septal scaling, shell size, and constructional constraints ...30 2.4.3 Functional constraints of septal frilling by capillary retention of cameral liquids ...............................................................................33 2.5 CONCLUSIONS........................................................................................36 2.6 ACKNOWLEDGEMENTS .......................................................................37 2.7 REFERENCES ..........................................................................................38 3.0 Mode of life and hydrostatic stability of orthoconic ectocochleate cephalopods: hydrodynamic analyses of restoring moments from 3D-printed, neutrally buoyant models ....................................................................................................................44 3.1 INTRODUCTION .....................................................................................45 3.1.1 Function of ectocochleate cephalopod shells and their hydrostatics ....................................................................................................................45 3.1.2 Previous studies of baculite hydrostatics and mode of life ............47 3.1.3 Three-dimensional modeling of ectocochleate cephalopods .........49 vi 3.2 METHODS ................................................................................................51 3.2.1 Modeled specimens ........................................................................51 3.2.2 Virtual model generation ...............................................................52 3.2.3 Hydrostatic calculations .................................................................56 3.2.4 Restoring moment experiments with 3D-printed models .............58 3.2.5 Experiments on active locomotion to overcome hydrostatic stability .........................................................................................62 3.3 RESULTS ..................................................................................................64 3.3.1 Virtual 3D models of Baculites compressus ..................................64 3.3.2 Restoring moments of Nautilus pompilius .....................................73 3.3.3 Restoring moment of Baculites compressus ..................................75 3.3.4 Thrust required to overcome the Baculites compressus restoring moment .........................................................................................79 3.4 DISCUSSION ............................................................................................81 3.4.1 Hydrostatic properties of Baculites compressus ............................81 3.4.2 Restoring moment of the stable, orthoconic morphotype ..............84 3.4.3 Were orthoconic cephalopods able to overcome their restoring moments? ......................................................................................84 3.4.4 Insights on the mode of life for highly-stable orthoconic cephalopods ..................................................................................86 3.5 CONCLUSIONS........................................................................................90
Recommended publications
  • Представители Семейства Bochianitidae (Ammonoidea) Из Нижнего Мела Горного Крыма © 2008 Г
    ПАЛЕОНТОЛОГИЧЕСКИЙ ЖУРНАЛ, 2008, № 5, с. 18-26 УДК 564.5:551.76(477.9) ПРЕДСТАВИТЕЛИ СЕМЕЙСТВА BOCHIANITIDAE (AMMONOIDEA) ИЗ НИЖНЕГО МЕЛА ГОРНОГО КРЫМА © 2008 г. В. В. Аркадьев Санкт-Петербургский государственный университет e-mail: [email protected] Поступила в редакцию 10.04.2007 г. Принята к печати 21.06.2007 г. Приведены результаты ревизии гетероморфньгх аммонитов семейства Bochianitidae из нижнего ме­ ла Горного Крыма. Автором подтверждена валидность рода Janenschites, выделенного из рода Bo- chianites. Из берриаса Горного Крыма описаны виды Bochianites neocomiensis (d'Orbigny), В. goubech- ensis Mandov, В. levis sp. nov. и В. crymensis sp. nov., из нижнего баррема - виды Janenschites oosteri (Sarasin et Schondelmayer) и J. incisus sp. nov. Бохианиты, появившись в начале берриаса в южных обла­ стях (Африка, Крым), в валанжине и готериве распространились в северные районы Западной Европы. Гетероморфные аммониты рода Bochianites тарктиды (Kelly, 1995; Lomas, 1999) и Новой Гви¬ редко встречаются в нижнемеловых отложениях неи (Benson, 1923). Горного Крыма. До настоящего времени из этого В последнее время вид В. cf. neocomiensis най­ региона было описано лишь два вида - Bochianites ден в пограничных отложениях валанжина - готе- oosteri и В. neocomiensis (Каракаш, 1907). Между рива Большого Кавказа (Захаров и др., 2006). тем, представители этого рода занимают значи¬ Крымские бохианиты после Н.И. Каракаша тельное место в нижнемеловых (в частности (1907) никем не изучались. Этот исследователь верхневаланжинских) аммонитовых комплексах виды B. neocomiensis и В. oosteri определил и опи¬ западной части Тетической области (Сесса, 1998; сал из красных известняков разреза на р. Кача в Lukeneder, 2005). Географическое распростране¬ Горном Крыму. Е.Ю. Барабошкин (1997) данный ние рода Bochianites чрезвычайно широкое.
    [Show full text]
  • Handbook of Texas Cretaceous Fossils
    University of Texas Bulletin No. 2838: October 8, 1928 HANDBOOK OF TEXAS CRETACEOUS FOSSILS B y W. S. ADKINS Bureau of Economic Geology J. A. Udden, Director E. H. Sellards, Associate Director PUBLISHED BY THE UNIVERSITY FOUR TIMES A MONTH, AND ENTERED AS SECOND-CLASS MATTER AT THE POSTOFFICE AT AUSTIN, TEXAS. UNDER THE ACT OF AUGUST 24. 1912 The benefits of education and of useful knowledge, generally diffused through a community, are essential to the preservation of a free govern­ m en t. Sam Houston Cultivated mind is the guardian genius of democracy. It is the only dictator that freemen acknowl­ edge and the only security that free­ men desire. Mirabeau В. Lamar CONTENTS P age Introduction __________________________________________________ 5 Summary of Formation Nomenclature_______________________ 6 Zone Markers and Correlation_______________________________ 8 Types of Texas Cretaceous Fossils___________________________ 36 Bibliography ________________________________________________ 39 L ist and Description of Species_________________________________ 46 P lants ______________________________________________________ 46 Thallophytes ______________________________________________ 46 Fungi __________________________________________________ 46 Algae __________________________________________________ 47 Pteridophytes ____________________________________________ 47 Filices __________________________________________________ 47 Spermatophytes __________________________________________ 47 Gymnospermae _________________________________________
    [Show full text]
  • On the Barremian - Lower Albian Stratigraphy of Colombia
    On the Barremian - lower Albian stratigraphy of Colombia Philip J. Hoedemaeker Hoedemaeker, Ph.J. 2004. On the Barremian-lower Albian stratigraphy of Colombia. Scripta Geologica, 128: 3-15, 3 figs., Leiden, December 2004. Ph.J. Hoedemaeker, Department of Palaeontology, Nationaal Natuurhistorisch Museum, P.O. Box 9517, 2300 RA Leiden, The Netherlands (e-mail: [email protected]). Key words – stratigraphy, Barremian, Aptian, depositional sequences, Colombia. The biostratigraphy and sequence stratigraphy of the Barremian deposits, and the biostratigraphy of the Aptian deposits in the Villa de Leyva area in Colombia are briefly described. Contents Introduction ....................................................................................................................................................... 3 Barremian ............................................................................................................................................................ 4 Barremian sequence stratigraphy ............................................................................................................ 6 Aptian ................................................................................................................................................................. 11 Lowermost Albian ........................................................................................................................................ 13 Conclusions ....................................................................................................................................................
    [Show full text]
  • New Late Campanian Ammonites from the Gschliefgraben
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 1999 Band/Volume: 24 Autor(en)/Author(s): Kennedy William James, Summesberger Herbert Artikel/Article: New Late Campanian Ammonites from the Gschliefgraben near Gmunden (Ultrahelvetic, Austria) 23-39 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont. 24:23-39, Wien 1999 New Late Campanian Ammonites from the Gschliefgraben near Gmunden (Ultrahelvetic, Austria) by William J. K ennedy 1 & Herbert Summesberger 1 2 Kennedy , WJ. & S ummesberger , H., 1999. New Late Campanian Ammonites from the Gschliefgraben near Gmunden (Ultrahelvetic, Austria). - Beitr. Palaont., 24:23-39, 1 Text-fig., 3 Plates, Wien. Contents [in:] Tr Oger et al., 1999, this volume). The first note on the ammonite fauna of the Gschliefgraben was pub­ Abstract, Zusammenfassung.................................... 23 lished by M ojsisovics & Schl Onbach (1868, p. 213: Introduction.............................................................. 23 „Baculites, Hamites, Scaphites, Ammonites“). B rink ­ Systematic Palaeontology 24 mann (1935) noted five ammonite taxa. Twenty-five Sedimentology 31 Stratigraphic conclusions..................................... 31 taxa were described by K ennedy & S ummesberger Palaeobiogeography................................................31 (1984). The geologic situation of the Gschliefgraben References .................................................................31
    [Show full text]
  • A New Decapod Crustacean Assemblage from the Lower Aptian of La Cova Del Vidre (Baix Ebre, Province of Tarragona, Catalonia)
    Accepted Manuscript A new decapod crustacean assemblage from the lower Aptian of La Cova del Vidre (Baix Ebre, province of Tarragona, Catalonia) Àlex Ossó, Barry van Bakel, Fernando Ari Ferratges-Kwekel, Josep Anton Moreno- Bedmar PII: S0195-6671(17)30554-2 DOI: 10.1016/j.cretres.2018.07.011 Reference: YCRES 3924 To appear in: Cretaceous Research Received Date: 27 December 2017 Revised Date: 11 June 2018 Accepted Date: 19 July 2018 Please cite this article as: Ossó, À., van Bakel, B., Ferratges-Kwekel, F.A., Moreno-Bedmar, J.A., A new decapod crustacean assemblage from the lower Aptian of La Cova del Vidre (Baix Ebre, province of Tarragona, Catalonia), Cretaceous Research (2018), doi: 10.1016/j.cretres.2018.07.011. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT 1 A new decapod crustacean assemblage from the lower Aptian of La Cova del Vidre 2 (Baix Ebre, province of Tarragona, Catalonia) 3 4 Àlex Ossó a, Barry van Bakel b, Fernando Ari Ferratges-Kwekel c, Josep Anton Moreno- 5 Bedmar d,* 6 7 a Llorenç de Vilallonga, 17B, 1er-1ª. 43007 Tarragona, Catalonia 8 b Oertijdmuseum, Bosscheweg 80, 5283 WB Boxtel, the Netherlands 9 c Área de Paleontología, Departamento de Ciencias de la Tierra, Universidad de Zaragoza, Zaragoza, Spain 10 d Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, Ciudad de 11 México, 04510 Mexico 12 13 14 * Corresponding author.
    [Show full text]
  • Vol. 3 No.3 September 1999
    ISSN 1342-8144 Formerly Transactions and Proceedings of the Palaeontological Society of Japan Vol. 3 No.3 September 1999 The Palaeontological Society of Japan Co-Editors Kazushige Tanabe and Tomoki Kase Language Editor Martin Janal (New York, USA) Associate Editors Jan Bergstrom (Swedish Museum of Natural History, Stockholm, Sweden), Alan G. Beu (Institute of Geological and Nuclear Sciences, Lower Hutt, New Zealand), Satoru Chiba (Tohoku University, Sendai, Japan), Yoichi Ezaki (Osaka City University, Osaka, Japan), James C. Ingle, Jr. (Stanford University, Stanford, USA), Kunio Kaiho (Tohoku University, Sendai, Japan), Susan M. Kidwell (University of Chicago, Chicago, USA), Hiroshi Kitazato (Shizuoka University, Shizuoka, Japan), Naoki Kohno (National Science Museum, Tokyo, Japan), Neil H. Landman (Amemican Museum of Natural History, New York, USA), Haruyoshi Maeda (Kyoto University, Kyoto, Japan), Atsushi Matsuoka (Niigata University, Niigata, Japan), Rihito Morita (Natural History Museum and Institute, Chiba, Japan), Harufumi Nishida (Chuo University, Tokyo, Japan), Kenshiro Ogasawara (University of Tsukuba, Tsukuba, Japan), Tatsuo Oji (University of Tokyo, Tokyo, Japan), Andrew B. Smith (Natural History Museum, London, Great Britain), Roger D.K. Thomas (Franklin and Marshall College, Lancaster, USA), Katsumi Ueno (Fukuoka University, Fukuoka, Japan), Wang Hongzhen (China University of Geosciences, Beijing, China), Yang Seong Young (Kyungpook National University, Taegu, Korea) Officers for 1999-2000 President: Kei Mori Councillors:
    [Show full text]
  • Download Curriculum Vitae
    NEIL H. LANDMAN CURATOR, CURATOR-IN-CHARGE AND PROFESSOR DIVISION OF PALEONTOLOGY HIGHEST DEGREE EARNED Ph.D. AREA OF SPECIALIZATION Evolution, life history, and systematics of externally shelled cephalopods EDUCATIONAL EXPERIENCE Ph.D. in Geology, Yale University, 1982 M. Phil. in Geology, Yale University, 1977 M.S. in Earth Sciences, Adelphi University, 1975 B.S. in Mathematics, summa cum laude, Polytechnic University of New York, 1972 PREVIOUS EXPERIENCE IN DOCTORAL EDUCATION FACULTY APPOINTMENTS Adjunct Professor, Department of Biology, City College Adjunct Professor, Department of Geology, Brooklyn College GRADUATE ADVISEES Susan Klofak, Biology, CUNY, 1999-present Krystal Kallenberg, Marine Sciences, Stony Brook, 2003-present GRADUATE COMMITTEES Christian Soucier, Biology, Brooklyn College, 2004-present Krystal Kallenberg, Marine Sciences, Stony Brook, 2003-present Yumiko Iwasaki, Geology, CUNY, 2000-2009 Emily Allen, Geology, University of Chicago, 2002-2005 Susan Klofak, Biology, CUNY, 1996-present Claude Monnet, University of Zurich, presently Sophie Low, Geology, Harvard University RESEARCH GRANT SUPPORT Kosciuszko Foundation. Comparative study of ammonite faunas from the United States Western Interior and Polish Lowland. Post-doc: Izabela Ploch, Geological Museum of Polish Geological Institute. 2011. NSF Grant MR1-R2 (Co-PI): Acquisition of a High Resolution CT-Scanner at the American Museum of Natural History: 2010-2013. NSF Grant No. DBI 0619559 (Co-PI): Acquisition of a Variable Pressure SEM at the AMNH: 2006-2009 NSF Grant No. EAR 0308926 (PI): Collaborative Research: Paleobiology, paleoceanography, and paleoclimatology of a time slice through the Western Interior Seaway: 2003-2006 National Science Foundation, Collaborative Research: Soft Tissues and Membrane Preservation in Permian Cephalopods, $40,000, February 1, 2002-January 31, 2006.
    [Show full text]
  • 71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
    ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas.
    [Show full text]
  • Stratigraphic Constraints on the Late Jurassic–Cretaceous Paleotectonic Interpretations of the Placetas Belt in Cuba, in C
    Pszczo´łkowski, A., and R. Myczyn´ ski, 2003, Stratigraphic constraints on the Late Jurassic–Cretaceous paleotectonic interpretations of the Placetas belt in Cuba, in C. Bartolini, R. T. Buffler, and J. Blickwede, eds., The Circum-Gulf of Mexico and the Caribbean: Hydrocarbon habitats, basin 25 formation, and plate tectonics: AAPG Memoir 79, p. 545–581. Stratigraphic Constraints on the Late Jurassic–Cretaceous Paleotectonic Interpretations of the Placetas Belt in Cuba Andrzej Pszczo´łkowski Institute of Geological Sciences, Polish Academy of Sciences, Warszawa, Poland Ryszard Myczyn´ski Institute of Geological Sciences, Polish Academy of Sciences, Warszawa, Poland ABSTRACT he Placetas belt in north-central Cuba consists of Late Jurassic–Cretaceous rocks that were highly deformed during the Paleocene to middle Eocene T arc-continent collision. The Late Proterozoic marble and Middle Jurassic granite are covered by the shallow-marine arkosic clastic rocks of late Middle Jurassic(?) or earliest Late Jurassic(?) ages. These arkosic rocks may be older than the transgressive arkosic deposits of the Late Jurassic–earliest Cretaceous Con- stancia Formation. The Berriasian age of the upper part of the Constancia For- mation in some outcrops at Sierra Morena and in the Jarahueca area does not confirm the Late Jurassic (pre-Tithonian) age of all deposits of this unit in the Placetas belt. The Tithonian and Berriasian ammonite assemblages are similar in the Placetas belt of north-central Cuba and the Guaniguanico successions in western Cuba. We conclude that in all paleotectonic interpretations, the Placetas, Camajuanı´, and Guaniguanico stratigraphic successions should be considered as biogeographically and paleogeographically coupled during the Tithonian and the entire Cretaceous.
    [Show full text]
  • The Cretaceous-Tertiary Boundary Interval in Badlands National Park, South Dakota
    The Cretaceous-Tertiary Boundary Interval in Badlands National Park, South Dakota Philip W. Stoffer1 Paula Messina John A. Chamberlain, Jr. Dennis O. Terry, Jr. U.S. Geological Survey Open-File Report 01-56 2001 U.S. DEPARTMENT OF THE INTERIOR Gale A. Norton, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The Cretaceous/Tertiary (K-T) boundary study interval at the Rainbow Colors Overlook along Badlands Loop Road, North Unit of Badlands National Park. This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey (USGS) editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1345 Middlefield Road, Menlo Park, CA 94025 http://geopubs.wr.usgs.gov/open-file/of01-056/ ABSTRACT A marine K-T boundary interval has been identified throughout the Badlands National Park region of South Dakota. Data from marine sediments suggest that deposits from two asteroid impacts (one close, one far away) may be preserved in the Badlands. These impact- generated deposits may represent late Maestrichtian events or possibly the terminal K-T event. Interpretation is supported by paleontological correlation, sequence stratigraphy, magnetostratigraphy, and strontium isotope geochronology. This research is founded on nearly a decade of NPS approved field work in Badlands National Park and a foundation of previously published data and interpretations. The K-T boundary occurs within
    [Show full text]
  • 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.
    [Show full text]
  • On the Supposed Aptian Occurrence of the Ammonite Genus Neodeshayesites in Colombia and Venezuela; with an Appendix on Neodeshayesites JL Karsteni (Marcou)
    On the supposed aptian occurrence of the ammonite genus Neodeshayesites in Colombia and Venezuela; with an appendix on Neodeshayesites JL Karsteni (Marcou). ™W FERNANDO ETAYO SERNA1 • I—RESUMEN El genero norandino de amonitas Neodeshayesites, ha sido encontrado asociado con otros generos de amonitas, que forma parte de una fauna del Albiano inferior o Albiano medio basal. El registro de este genero en capas supuestamente de edad aptiana se basa en datos sin apoyo estratigraf ico o en el listado conjunto de faunas procedentes de diferentes localidades. ABSTRACT— Where associated with other ammonites Neodeshayesites, a group of Northern South American species, forms part of a Lower Albian or basal Middle Albian fauna. The supposed record of the genus from Aptian strata is based on inconclusive stratigraphical data or falacious listing of faunas from diff­ erent localities. CONSIDERATIONS ON THE SO-CALLED APTIAN could also be explained as a condensed deposit. However, OCCURRENCE OF NEODESHAYESITES all the other criteria for a condensed deposit are missing.." In 1954, E. Rod and W. Maync published a "Revision of At time of publication of Rod and Maync's paper, no the Lower Cretaceous Stratigraphy of Venezuela"; in part I precise knowledge existed on the stratigraphic position of of this paper (p. 207-208) Rod stressed that he himself the group of species described by Riedel (1938, p 37-40), had". isolated a specimen looking like a Douvilleiceras under Deshayesites. When proposing the .genus Neodeshaye­ out of a Deshayesites pavement of a big concretion. the sites for the same group of species, Casey chose "Deshaye­ Douvilleiceras indicates Lower Albian age and the Deshaye­ sites stutzeri Riedel" as type species (1964, p.
    [Show full text]