2002 Uas Ceno.Pmd
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Geologie Und Paläontologie in Westfalen Heft 51
WESTFÄLISCHES MUSEUM FÜR NATURKUNDE Geologie und Paläontologie in Westfalen Heft 51 c '5 1 1 CU E Calycoceras 1 1 1 o guerangeri 1 1 c Zone Q) 0 3 0 1 .._ 1 1 1 Q) 1 1 1 ...Q -----------------------------· 1 1 lnoceramus pictus 0 1 1 Event 1 2 5 1 1 1 1 1 Acanthoceras 1 1 1 1 1 1 jukesbrownei ~'.:._'.:._'.:._~'-=-~-'o'.:.."""'=-'.:..~-=:-= 1 Zone 1 1 1 1 1 1 1 0 1 1 1 1 1 c 1 1 CU -·--------------------- --- --- 1 1 1 E 1 1 1 0 5- c ~ 1 1 1 Q) '- ~ 1 1 1 Cl) cb 1 1 0 ~Cl) 1 ~ & Turrilites acutus- 1 1 1 Q; _g cu Subzone 1 1 ...... E 1 1 1 ...... ~ .8 ...... (.) 0 0 1 1 · - <:(..t:: 1 1 1 ~ 1 1 1 1 1 Stratigraph ie und Ammonitenfaunen des westfälischen Cenoman Ulrich Kaplan, William James Kenn edy, Jens Lehmann und Ryszard Marcinowski [~r.:·11~j Landschaftsverband tttfüt) Westfalen-Lippe Hinweise für Autoren In der Schriftenreihe Geologie und Paläontologie in Westfalen werden geowissenschaftliche Beiträge veröffent• licht, die den Raum Westfalen betreffen. Druckfertige Manuskripte sind an die Schriftleitung zu schicken. Aufbau des Manuskriptes 1. Titel kurz und bezeichnend. 2. Klare Gliederung. 3. Zusammenfassung in Deutsch am Anfang der Arbeit. Äußere Form 4. Manuskriptblätter einseitig und weitzeilig beschreiben; Maschinenschrift, Verbesserungen in Druckschrift. 5. Unter der Überschrift: Name des Autors (ausgeschrieben), Anzahl der Abbildungen, Tabellen und Tafeln; An schrift des Autors auf der 1. Seite unten. 6. Literaturzitate im Text werden wie folgt ausgeführt: (AUTOR, Erscheinungsjahr: evtl. -
Sucesión De Amonitas Del Cretácico Superior (Cenomaniano – Coniaciano) De La Parte Más Alta De La Formación Hondita Y De L
Boletín de Geología Vol. 33, N° 1, enero-junio de 2011 SUCESIÓN DE AMONITAS DEL CRETÁCICO SUPERIOR (CENOMANIANO – CONIACIANO) DE LA PARTE MÁS ALTA DE LA FORMACIÓN HONDITA Y DE LA FORMACIÓN LOMA GORDA EN LA QUEBRADA BAMBUCÁ, AIPE - HUILA (COLOMBIA, S. A.) Pedro Patarroyo1 RESUMEN La sección de la quebrada Bambucá (Aipe - Huila) posee una buena exposición de los depósitos del Cretácico del Valle Superior del Magdalena. De la parte alta de la Formación Hondita se recolectaron Acanthoceras sp. y Rhynchostreon sp. del Cenomaniano superior. Dentro del segmento inferior de la Formación Loma Gorda se hallaron Choffaticeras (C.) cf. segne, Fagesia cf. catinus, Neoptychites cf. andinus, Mitonia gracilis, Morrowites sp., Nannovascoceras ? sp., Quitmaniceras ? sp., Benueites ? sp. junto con Mytiloides kossmati, M. goppelnensis y Anomia sp. del Turoniano inferior. Estratigráficamente arriba aparecen Paramammites ? sp., Hoplitoides sp. H. ingens, H. cf. lagiraldae, Codazziceras ospinae, Allocrioceras sp., que pueden estar representando entre el Turoniano inferior y medio. Para la parte alta de este segmento se encontraron Prionocycloceras sp. P. guayabanum, Reesidites subtuberculatum, Subprionotropis colombianus, Mytiloides scupini, Dydimotis sp., Gauthiericeras sp., Anagaudryceras ? sp., Eulophoceras jacobi, Paralenticeras sieversi, Hauericeras cf. madagascarensis, Peroniceras (P.) subtricarinatum, Forresteria (F.) sp., Barroisiceras cf. onilahyense, Ankinatsytes venezolanus que abarcan entre el Turoniano superior y el Coniaciano. Con base en la fauna colectada no es posible establecer los límites Cenomaniano/Turoniano y Turoniano/Coniaciano. Palabras clave: Amonitas, Cretácico superior, Valle Superior del Magdalena, Aipe-Huila-Colombia. UPPER CRETACEOUS AMMONITE SUCCESSION (CENOMANIAN – CONIACIAN) RELATED TO THE UPPER HONDITA AND LOMA GORDA FORMATIONS ALONG THE BAMBUCÁ CREEK, AIPE - HUILA (COLOMBIA, S.A.) ABSTRACT The Bambucá creek section (Aipe - Huila) shows a very good exposition of the Upper Magdalena Valley Cretaceous deposits. -
Redalyc.SUCESIÓN DE AMONITAS DEL CRETÁCICO SUPERIOR (CENOMANIANO – CONIACIANO) DE LA PARTE MÁS ALTA DE LA FORMACIÓN HONDIT
Boletín de Geología ISSN: 0120-0283 [email protected] Universidad Industrial de Santander Colombia Patarroyo, Pedro SUCESIÓN DE AMONITAS DEL CRETÁCICO SUPERIOR (CENOMANIANO – CONIACIANO) DE LA PARTE MÁS ALTA DE LA FORMACIÓN HONDITA Y DE LA FORMACIÓN LOMA GORDA EN LA QUEBRADA BAMBUCÁ, AIPE - HUILA (COLOMBIA, S. A.) Boletín de Geología, vol. 33, núm. 1, enero-junio, 2011, pp. 69-92 Universidad Industrial de Santander Bucaramanga, Colombia Disponible en: http://www.redalyc.org/articulo.oa?id=349632022005 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Boletín de Geología Vol. 33, N° 1, enero-junio de 2011 SUCESIÓN DE AMONITAS DEL CRETÁCICO SUPERIOR (CENOMANIANO – CONIACIANO) DE LA PARTE MÁS ALTA DE LA FORMACIÓN HONDITA Y DE LA FORMACIÓN LOMA GORDA EN LA QUEBRADA BAMBUCÁ, AIPE - HUILA (COLOMBIA, S. A.) Pedro Patarroyo1 RESUMEN La sección de la quebrada Bambucá (Aipe - Huila) posee una buena exposición de los depósitos del Cretácico del Valle Superior del Magdalena. De la parte alta de la Formación Hondita se recolectaron Acanthoceras sp. y Rhynchostreon sp. del Cenomaniano superior. Dentro del segmento inferior de la Formación Loma Gorda se hallaron Choffaticeras (C.) cf. segne, Fagesia cf. catinus, Neoptychites cf. andinus, Mitonia gracilis, Morrowites sp., Nannovascoceras ? sp., Quitmaniceras ? sp., Benueites ? sp. junto con Mytiloides kossmati, M. goppelnensis y Anomia sp. del Turoniano inferior. Estratigráficamente arriba aparecen Paramammites ? sp., Hoplitoides sp. -
Upper Cretaceous) Rocks in Texas and the Western Interior of the United States
Tarrantoceras Stephenson and Related Ammonoid Geneva from Cenomanian (Upper Cretaceous) Rocks in Texas and the Western Interior of the United States U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1473 AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTTS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, -
CENOMANIAN CEPHALOPODS from the GLAUCONITIC LIMESTONE SOUTHEAST of ESFAHAN, IRAN Boreal Middle Cretaceous Ammonite Faunas Have L
ACT A PAL A EON T 0 LOG ICA POLONICA Vol. 24 1919 No. J W. J. KENNEDY, M. R. CHAHIDA AND M. A. DJAFARIAN CENOMANIAN CEPHALOPODS FROM THE GLAUCONITIC LIMESTONE SOUTHEAST OF ESFAHAN, IRAN KENNEDY W. J., CHAHIDA M. R. and DJAFARIAN M. A.: Cenomanian cepha lopods from the Glauconitic Limestone southeast of Esfahan, Iran. Acta Palaeont Polonica, 24, I, 3-50, April 20, 1979. The Glauconitic Limestone of the area southeast of Esfahan yields a rich Ceno manian cephalopod fauna of Boreal aspect, including species of Anglonautllus, Stomohamites, Sciponoceras, Idiohamites, Ostllngoceras. Mariella, Hypoturrllites. Turrllites, Scaphites, Puzosia, Austiniceras, Hyphoplltes, Schloenbachia. Mantelll ceras, Sharpeiceras and Acompsoceras, most of which represent new records for the area. The age of this fauna Is unequivocally Lower Cenomanian, and can be correlated in detail at a distance of 5000 km with parts of the northwest European Hypoturrll!tes carcitanens!s and Mante!liceras saxbit Zones. The material studied includes none of the Upper Albian, Middle and Upper Cenomanian elements re corded from the unit by previous workers. The fauna Is numerically dominated by acanthoceratids, in marked contrast to the Schloenbachia-dominated faunas of northwestern Europe. This suggests the area lay In the southern parts of the Boreal Realm, where Schloenbachia Is known to become progressively scarcer, as Is supported by proximity to the Zagros line marking the juncture of Asian and Arabian plates. Key w 0 r d s: Boreal Ammonites, Esfahan, Lower Cenomanian, Glauconitic Li mestone. W. J. Kennedy, Geological Co!lections. University Museum. Parks Road. England; M. R. Chahida and M. A. -
Double Alignments of Ammonoid Aptychi from the Lower Cretaceous of Southeast France: Result of a Post−Mortem Transport Or Bromalites?
Double alignments of ammonoid aptychi from the Lower Cretaceous of Southeast France: Result of a post−mortem transport or bromalites? STÉPHANE REBOULET and ANTHONY RARD Reboulet, S. and Rard, A. 2008. Double alignments of ammonoid aptychi from the Lower Cretaceous of Southeast France: Result of a post−mortem transport or bromalites? Acta Palaeontologica Polonica 53 (2): 261–274. A new preservation of aptychi is described from the Valanginian limestone−marl alternations of the Vergol section (Drôme), located in the Vocontian Basin (SE France). Aptychi are arranged into two parallel rows which are generally 50 mm in length and separated by 4 mm. The alignments are very often made by entire aptychi (around 10 mm in length), oriented following their harmonic margin. Aptychi show the outside of valve to the viewer: they are convex−up. This fos− silization of aptychi is successively interpreted as the result of post−mortem transport by bottom currents (taphonomic− resedimentation process) or the residues (bromalites: fossilized regurgitation, gastric and intestinal contents, excrement) from the digestive tract of an ammonoid−eater (biological processes). Both the parallel rows of aptychi are more likely in− terpreted as a coprolite (fossil faeces) and they could be considered as both halves (hemi−cylindrical in shape) of the same cylindrical coprolite which would have been separated in two parts (following the long axis) just after the animal defe− cated. Considering this hypothesis, a discussion is proposed on the hypothetical ammonoid−eater responsible for them. Key words: Ammonoidea, taphonomy, aptychus, coprolite, predation, Valanginian, Cretaceous, France. Stéphane Reboulet [stephane.reboulet@univ−lyon1.fr], Université de Lyon, (UCBL1, La Doua), UFR des Sciences de la Terre, CNRS−UMR 5125 PEPS, Bâtiment Géode, 2 Rue Raphaël Dubois, 69622 Villeurbanne cedex, France; Anthony Rard [anthony.rard@cc−thouarsais.fr], Centre d'interprétation géologique du Thouarsais, Réserve Naturelle Géologique du Toarcien, Les Ecuries du Château, 79100 Thouars, France. -
(Early Late Cretaceous) Ammonoid Faunas of Western Europe. Part I, Biochronology (Unitary Associations) and Diachronism of Datums
Cenomanian (early Late Cretaceous) ammonoid faunas of Western Europe. Part I, Biochronology (Unitary Associations) and diachronism of datums Autor(en): Monnet, Claude / Bucher, Hugo Objekttyp: Article Zeitschrift: Eclogae Geologicae Helvetiae Band (Jahr): 95 (2002) Heft 1 PDF erstellt am: 10.10.2021 Persistenter Link: http://doi.org/10.5169/seals-168946 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch 0012-9402/02/010057-17 $1.50 + 0.20/0 Eclogae geol. Helv. 95 (2002) 57-73 Birkhäuser Verlag, Basel, 2002 Cenomanian (early Late Cretaceous) ammonoid faunas of Western Europe Part I: Biochronology (Unitary Associations) and diachronism of datums Claude Monnet1 & Hugo Bûcher1 Key words: Ammonoids. -
The Eagle Ford Group Returns to Big Bend National Park, Brewster County, Texas 163
A Publication of the Gulf Coast Association of Geological Societies www.gcags.org T E F G R B B N P, B C, T Matthew Wehner1, Rand D. Gardner2, Michael C. Pope1, and Arthur D. Donovan1 1Department of Geology and Geophysics, Texas A&M University, MS 3115, College Station, Texas 77843, U.S.A. 2Total E&P USA, 1201 Louisiana St., Ste. 1800, Houston, Texas 77002, U.S.A. ABSTRACT The Upper Cretaceous succession in the Big Bend Region of West Texas is plagued by the continued use of provincial lithostratigraphic terms not used elsewhere in the state of Texas. These provincial terms greatly limit: (1) correlating these strata to coeval units in outcrops, as well as the subsurface, elsewhere in Texas; and (2) utilizing these outcrops as windows to examine strata coeval to economically important unconventional reservoirs within the Eagle Ford Group in the subsurface of South Texas. However, with the use of petrophysical and geochemical techniques (handheld spectrometer, X–ray fluorescence [XRF], and stable isotopes), it is possible to identify and define the Eagle Ford and Austin groups, as well as potentially a rem- nant of the older Woodbine Group, within Big Bend National Park, Brewster County, Texas. Because the Hot Springs section is west of the classic Eagle Ford and Austin outcrops in the Lozier Canyon region of Terrell County (West Texas), the Big Bend outcrops also provide insights into lateral facies changes within these units. As historically defined, within the Big Bend region, the Boquillas Formation overlies the Buda Formation and is overlain by the Pen Formation. -
Preservation of Nautilid Soft Parts Inside and Outside the Conch
Klug et al. Swiss J Palaeontol (2021) 140:15 https://doi.org/10.1186/s13358-021-00229-9 Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access Preservation of nautilid soft parts inside and outside the conch interpreted as central nervous system, eyes, and renal concrements from the Lebanese Cenomanian Christian Klug1* , Alexander Pohle1, Rosemarie Roth1, René Hofmann2, Ryoji Wani3 and Amane Tajika4,5 Abstract Nautilid, coleoid and ammonite cephalopods preserving jaws and soft tissue remains are moderately common in the extremely fossiliferous Konservat-Lagerstätte of the Hadjoula, Haqel and Sahel Aalma region, Lebanon. We assume that hundreds of cephalopod fossils from this region with soft-tissues lie in collections worldwide. Here, we describe two specimens of Syrionautilus libanoticus (Cymatoceratidae, Nautilida, Cephalopoda) from the Cenomanian of Hadjoula. Both specimens preserve soft parts, but only one shows an imprint of the conch. The specimen without conch displays a lot of anatomical detail. We homologise the fossilised structures as remains of the digestive tract, the central nervous system, the eyes, and the mantle. Small phosphatic structures in the middle of the body chamber of the specimen with conch are tentatively interpreted as renal concrements (uroliths). The absence of any trace of arms and the hood of the specimen lacking its conch is tentatively interpreted as an indication that this is another leftover fall (pabulite), where a predator lost parts of its prey. Other interpretations such as incomplete scavenging are also conceivable. Keywords: Cephalopoda, Nautilida, Cretaceous, Anatomy, Konservat-Lagerstätte, Taphonomy Introduction and aragonite shells were dissolved. Tere are records As shown by Clements et al. -