APS Bulletin September 1993
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Palaeoecology and Depositional Environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania)
Mitt. Mus. Nat.kd. Berl., Geowiss. Reihe 5 (2002) 19-44 10.11.2002 Palaeoecology and depositional environments of the Tendaguru Beds (Late Jurassic to Early Cretaceous, Tanzania) Martin Aberhan ', Robert Bussert2, Wolf-Dieter Heinrich', Eckhart Schrank2, Stephan Schultkal, Benjamin Sames3, Jiirgen =wet4 & Saidi Kapilima5 With 6 figures, 2 tables, and 2 plates Abstract The Late Jurassic to Early Cretaceous Tendaguru Beds (Tanzania, East Africa) have been well known for nearly a century for their diverse dinosaur assemblages. Here, we present sedimentological and palaeontological data collected by the German- Tanzanian Tendaguru Expedition 2000 in an attempt to reconstruct the palaeo-ecosystems of the Tendaguru Beds at their type locality. Our reconstructions are based on sedimentological data and on a palaeoecological analysis of macroinverte- brates, microvertebrates, plant fossils and microfossils (ostracods, foraminifera, charophytes, palynomorphs). In addition, we included data from previous expeditions, particularly those on the dinosaur assemblages. The environmental model of the Tendaguru Beds presented herein comprises three broad palaeoenvironmental units in a marginal marine setting: (1) Lagoon-like, shallow marine environments above fair weather wave base and with evidence of tides and storms. These formed behind barriers such as ooid bar and siliciclastic sand bar complexes and were generally subject to minor salinity fluctuations. (2) Extended tidal flats and low-relief coastal plains. These include low-energy, brackish coastal lakes and ponds as well as pools and small fluvial channels of coastal plains in which the large dinosaurs were buried. Since these environments apparently were, at best, poorly vegetated, the main feeding grounds of giant sauropods must have been elsewhere. -
A Preliminary Assessment of Paleontological Resources at Bighorn Canyon National Recreation Area, Montana and Wyoming
A PRELIMINARY ASSESSMENT OF PALEONTOLOGICAL RESOURCES AT BIGHORN CANYON NATIONAL RECREATION AREA, MONTANA AND WYOMING Vincent L. Santucci1, David Hays2, James Staebler2 And Michael Milstein3 1National Park Service, P.O. Box 592, Kemmerer, WY 83101 2Bighorn Canyon National Recreation Area, P.O. Box 7458, Fort Smith, MT 59035 3P.O. Box 821, Cody, WY 82414 ____________________ ABSTRACT - Paleontological resources occur throughout the Paleozoic and Mesozoic formations exposed in Bighorn Canyon National Recreation Area. Isolated research on specific geologic units within Bighorn Canyon has yielded data on a wide diversity of fossil forms. A comprehensive paleonotological survey has not been previously undertaken at Bighorn Canyon. Preliminary paleontologic resource data is presented in this report as an effort to establish baseline data. ____________________ INTRODUCTION ighorn Canyon National Recreation Area (BICA) consists of approximately 120,000 acres within the Bighorn Mountains of north-central Wyoming and south-central Montana B (Figure 1). The northwestern trending Bighorn Mountains consist of over 9,000 feet of sedimentary rock. The predominantly marine and near shore sedimentary units range from the Cambrian through the Lower Cretaceous. Many of these formations are extremely fossiliferous. The Bighorn Mountains were uplifted during the Laramide Orogeny beginning approximately 70 million years ago. Large volumes of sediments, rich in early Tertiary paleontological resources, were deposited in the adjoining basins. This report provides a preliminary assessment of paleontological resources identified at Bighorn Canyon National Recreation Area. STRATIGRAPHY The stratigraphic record at Bighorn Canyon National Recreation Area extends from the Cambrian through the Cretaceous (Figure 2). The only time period during this interval that is not represented is the Silurian. -
Mollusca, Bivalvia): Protocardiinae, Laevicardiinae, Lahilliinae, Tulongocardiinae Subfam
Zoologica Scripta, Vol. 24, No. 4, pp. 321-346, 1995 Pergamon Elsevier Science Ltd The Norwegian Academy of Science and Letters Printed in Great Britain 0300-3256(95)00011-9 Phytogeny of the Cardiidae (Mollusca, Bivalvia): Protocardiinae, Laevicardiinae, Lahilliinae, Tulongocardiinae subfam. n. and Pleuriocardiinae subfam. n. JAY A. SCHNEIDER Accepted 7 June 1995 Schneider, J.A. 1995. Phytogeny of the Cardiidae (Mollusca, Bivalvia): Protocardiinae, Laevicar- diinae, Lahilliinae, Tulongocardiinae subfam.n. and Pleuriocardiinae subfam.n.—Zool. Scr. 24: 321-346. In a preliminary cladistic analysis of the bivalve family Cardiidae (Schneider 1992), members of the subfamilies Protocardiinae, Lahilliinae, and Laevicardiinae, plus the genus Nemocardium, were found to be the least derived taxa of cardiids. A cladistic analysis is undertaken of the genera and subgenera of these cardiid taxa, plus several Mesozoic taxa which have never been assigned to any subfamily. The Late Triassic Tulongocardium, which is placed in Tulongocardiinae subfam. n., is the sister taxon to all other cardiids. Protocardiinae is restricted to the genus Protocardia. Most other Mesozoic taxa which have been placed in the Protocardiinae are found to be members of the Lahilliinae. Nemocardium is placed in the Laevicardiinae. Incacardium, Pleuriocardia, and Dochmocardia form a monophyletic group, Pleuriocardiinae subfam. n. Pleuriocardiinae, Laevi- cardiinae, and the remaining members of the Cardiidae (herein informally termed "cucardiids") form a monophyletic group. Jay A. Schneider, Smithsonian Tropical Research Institute, Box2072, Balboa, Republic of Panama. Present address: Department of Geology, Youngstown State University, Youngstown, OH 44555- 3672, C/.S./l. re7..2;6-742-77JJ;Fa%.276-742-/7J4 Introduction Bivalves of the family Cardiidae (cockles and giant clams) Outgroup Palaeocardita originated in the Late Triassic and have a present-day Septocardia diversity of nearly 200 species (Rosewater 1965; Fischer- Protocardia | PROTOCARDIINAE Integricardium I Piette 1977). -
The Tendaguru Formation (Late Jurassic to Early Cretaceous, Southern Tanzania): Definition, Palaeoenvironments, and Sequence Stratigraphy
Fossil Record 12 (2) 2009, 141–174 / DOI 10.1002/mmng.200900004 The Tendaguru Formation (Late Jurassic to Early Cretaceous, southern Tanzania): definition, palaeoenvironments, and sequence stratigraphy Robert Bussert1, Wolf-Dieter Heinrich2 and Martin Aberhan*,2 1 Institut fr Angewandte Geowissenschaften, Technische Universitt Berlin, Skr. BH 2, Ernst-Reuter-Platz 1, 10587 Berlin, Germany. E-mail: [email protected] 2 Museum fr Naturkunde – Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, Invalidenstr. 43, 10115 Berlin, Germany. E-mail: [email protected]; [email protected] Abstract Received 8 December 2008 The well-known Late Jurassic to Early Cretaceous Tendaguru Beds of southern Tanza- Accepted 15 February 2009 nia have yielded fossil plant remains, invertebrates and vertebrates, notably dinosaurs, Published 3 August 2009 of exceptional scientific importance. Based on data of the German-Tanzanian Tenda- guru Expedition 2000 and previous studies, and in accordance with the international stratigraphic guide, we raise the Tendaguru Beds to formational rank and recognise six members (from bottom to top): Lower Dinosaur Member, Nerinella Member, Middle Dinosaur Member, Indotrigonia africana Member, Upper Dinosaur Member, and Ruti- trigonia bornhardti-schwarzi Member. We characterise and discuss each member in de- tail in terms of derivation of name, definition of a type section, distribution, thickness, lithofacies, boundaries, palaeontology, and age. The age of the whole formation appar- ently ranges at least from the middle Oxfordian to the Valanginian through Hauterivian or possibly Aptian. The Tendaguru Formation constitutes a cyclic sedimentary succes- sion, consisting of three marginal marine, sandstone-dominated depositional units and three predominantly coastal to tidal plain, fine-grained depositional units with dinosaur remains. -
Redalyc.Upper Jurassic Ammonites and Bivalves from the Cucurpe
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Villaseñor, Ana Bertha; González Léon, Carlos M.; Lawton, Timothy F.; Aberhan, Martin Upper Jurassic ammonites and bivalves from the Cucurpe Formation, Sonora (Mexico) Revista Mexicana de Ciencias Geológicas, vol. 22, núm. 1, 2005, pp. 65-87 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57222107 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas,Upper v. 22, Jurassic núm. 1, ammonites 2005, p. 65-87 and bivalves from Sonora 65 Upper Jurassic ammonites and bivalves from the Cucurpe Formation, Sonora (Mexico) Ana Bertha Villaseñor1,*, Carlos M. González-León2, Timothy F. Lawton3, and Martin Aberhan4 1 Departamento de Paleontología, Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, 04510 México, D. F., Mexico. 2 Estación Regional del Noroeste, Instituto de Geología, Universidad Nacional Autónoma de México, 83000 Hermosillo, Sonora, Mexico. 3 Department of Geological Sciences, New Mexico State University, Las Cruces, NM 88003, USA. 4 Museum für Naturkunde, Zentralinstitut der Humboldt-Universität zu Berlin, Institut für Paläontologie, Invalidenstr. 43, D-10115 Berlin, Germany. * [email protected] ABSTRACT Four new molluscan assemblages from north-central Sonora indicate that the Cucurpe Formation ranges in age from late Oxfordian to early Tithonian. These assemblages extend the known paleogeographic range of Late Jurassic Tethyan fossil groups several hundred km to the northwest and improve correlation of Upper Jurassic strata in northern Mexico. -
Mollusca of the Buda Limestone
Bulletin No. 205 Series C, Systematic Geology and Paleontology, 59 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHAKLES D. WALCOTT, DIRECTOR THE MOLLUSCA OF THE BUDA LIMESTONE BY GEORGE BURBANK SHATTUCK WITH AN APPENDIX ON THE CORALS OF THE BUDA LIMESTONE THOMAS WAYLAND VAUGHAN WASHINGTON GOVERNMENT PRINTING OFFICE 1903 CONTENTS. Page. Letter of transmittal, by T. W. Stanton .................................. 7 Preparatory note .----..-................,.........:..._................... 9 Historical review . ... .................................................... 9 Bibliography.............................._..........................'.. 11 Geology of the Bnda limestone..... .....--.....'-...---...-...--.-........ 12 List of species in Buda limestone.......---.-..-...--....-................ 14 Descriptions of species.................................................... 15 Mollusca ...... ._--.-._-.-.-------...-__..-.... ..-..'.-.......-....... 15 Pelecypoda.... .................-...................-.-..-------- 15 Pectinidse .................................................. .... 15 Limidse ................:...................................... 17 Pernidae....................................................... 19' Pinnidae..................................................... 19 Spondylidffi--_---.-.......................................... 20 Ostreidae ......................... ............................ 20 Mytilidae.......... ...................'.............. ....... 23 Arcidse...................................................... -
Redalyc.Upper Cretaceous (Cenomanian-Turonian) Bivalves from Northern Jordan, Middle East
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Perrilliat, María del Carmen; Ahmad, Fayez; Vega, Francisco J. Upper Cretaceous (Cenomanian-Turonian) bivalves from northern Jordan, Middle East Revista Mexicana de Ciencias Geológicas, vol. 23, núm. 1, 2006, pp. 96-106 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57230107 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative 96 PerrilliatRevista Mexicanaet al. de Ciencias Geológicas, v. 23, núm 1, 2006, p. 96-106 Upper Cretaceous (Cenomanian–Turonian) bivalves from northern Jordan, Middle East María del Carmen Perrilliat1,*, Fayez Ahmad2, and Francisco J. Vega1 1 Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, 04510 México, D. F., Mexico. 2 Faculty of Natural Resources and Environment, Department of Earth and Environmental Sciences, The Hashemite University, P. O. Box 150459, 13115 Zarqa, Jordan. *[email protected] ABSTRACT Twelve species of bivalves are described for the Upper Cretaceous Ajlun Group of northern Jordan. The specimens were collected in three localities of the Fuheis (?middle to late Cenomanian), Hummar (late Cenomanian), and Shuayb (early Turonian) formations. Some of the species here described are reported for the fi rst time in Jordan and confi rm Tethyan paleobiogeographic affi nities. Key words: Bivalvia, Upper Cretaceous, northern Jordan, Middle East. RESUMEN Se describen e ilustran doce especies de bivalvos procedentes del Cretácico Superior del Grupo Ajlun en el norte de Jordania. -
Mesozoic Litho- and Magneto-Stratigraphic Evidence from the Central Tibetan Plateau for Megamonsoon Evolution and Potential Evaporites
Gondwana Research 37 (2016) 110–129 Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Mesozoic litho- and magneto-stratigraphic evidence from the central Tibetan Plateau for megamonsoon evolution and potential evaporites Xiaomin Fang a,⁎, Chunhui Song b, Maodu Yan a, Jinbo Zan a, Chenglin Liu c, Jingeng Sha d,WeilinZhanga, Yongyao Zeng b, Song Wu b, Dawen Zhang a a CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, CAS, Beijing 100101, China b School of Earth Sciences & Key Laboratory of Western China's Mineral Resources of Gansu Province, Lanzhou University, Lanzhou 730000, China c MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China d Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, No.39 East Beijing Road, Nanjing 210008, China article info abstract Article history: The megamonsoon was a striking event that profoundly impacted the climatic environment and related mineral Received 3 September 2015 sources (salts, coals and oil-gases) in the Mesozoic. How this event impacted Asia is unknown. Here, we firstly Received in revised form 19 May 2016 reported a Mesozoic stratigraphic sequence in the northern Qiangtang Basin, in the central Tibetan Plateau, Accepted 21 May 2016 based on lithofacies and chronologies of paleontology and magnetostratigraphy. How the planetary and Available online 02 July 2016 megamonsoon circulations controlled the Asian climate with time has been recorded. Using the basic principles Handling Editor: Z.M. -
A Multidisciplinary Study of Late Jurassic Bivalves from a Semi
1 A multidisciplinary study of Late Jurassic bivalves from a semi-enclosed basin – Examples of adaptation and speciation and their stratigraphic and taphonomic background (Lusitanian Basin, central Portugal) Dissertation zur Erlangung des Doktorgrades (Dr. rer. nat.) an der Fakultät für Geowissenschaften der Ludwig-Maximilians-Universität München vorgelegt von Simon Schneider im September 2009 2 3 Dekan: Prof. Dr. Wolfram Mauser Erster Gutachter: Prof. Dr. Michael R. W. Amler Zweiter Gutachter: Prof. Dr. Franz T. Fürsich Tag der mündlichen Prüfung: 13.01.2010 4 5 Ehrenwörtliche Versicherung Ich versichere hiermit ehrenwörtlich, dass die Dissertation von mir selbstständig, ohne Beihilfe angefertigt worden ist. München, 15.09.2009 ___________________________ Erklärung Hiermit erkläre ich, dass die Dissertation noch nicht in einem anderen Prüfungsverfahren vorgelegt und bewertet wurde. Hiermit erkläre ich, dass ich mich anderweitig einer Doktorprüfung ohne Erfolg nicht unterzogen habe. München, 15.09.2009 ___________________________ 6 7 Contents 1. Introduction 8 2. Study area 10 3. Lithologic and stratigraphic overview 12 4. Fossil flora and fauna 17 Historical perspective: The work of LÉON PAUL CHOFFAT 21 5. Material 23 6. Methods 23 6.1. Isotope analyses 23 6.2. Palaeoecological analysis 24 6.3. Morphometry 25 6.4. Statistical analyses 25 7. Results and discussion 26 7.1. Isotope analyses 26 7.2. Shell concentrations 27 7.3. Benthic associations and assemblages 28 7.4. Phylogeny and ecophenotypy of the target taxa 28 7.5. Colour pattern preservation 33 8. Conclusions 33 9. Future perspectives 35 9.1. Upper Jurassic bivalves from Portugal 35 9.2. Transfer of concepts 37 Acknowledgements 37 Systematic list of Bivalvia 40 References 44 Papers included in this Thesis 53 8 1. -
Quay County, New Mexico Barry S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/52 Nearshore fauna of the Tucumcari Formation (Lower Cretaceous, Albian), Quay County, New Mexico Barry S. Kues and Spencer G. Lucas, 2001, pp. 229-249 in: Geology of Llano Estacado, Lucas, Spencer G.;Ulmer-Scholle, Dana; [eds.], New Mexico Geological Society 52nd Annual Fall Field Conference Guidebook, 340 p. This is one of many related papers that were included in the 2001 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Review of Fossil Collections in Scotland Scotland South Scotland South
Detail of Permian footprints Chelichnus duncani in sandstone from Dumfries and Galloway. Dumfries Museum and Camera Obscura. © Dumfries and Galloway Council Museums Service Review of Fossil Collections in Scotland Scotland South Scotland South Dumfries Museum and Camera Obscura (Dumfries and Galloway Council) Sanquhar Tolbooth Museum (Dumfries and Galloway Council) Stranraer Museum (Dumfries and Galloway Council) Gem Rock Museum Newton Stewart Museum Tweeddale Museum (Live Borders) Hawick Museum (Live Borders) 1 Dumfries Museum and Camera Obscura (Dumfries and Galloway Council) Collection type: Local authority Accreditation: 2018 The Observatory, Rotchell Road, Dumfries, DG2 7SW Contact: [email protected] Location of collections The original Museum was located in a windmill dating from the late 1700s, preserved in the 1830s by the newly-formed Dumfries and Maxwelltown Astronomical Society for use as an observatory. An extension built in the 1860s added a large gallery and mezzanine level with further gallery and storage space added in the 1980s. Collections are onsite in displays and a main storeroom. Size of collections 1,000-1,200 fossils. Onsite records Information is in an Adlib CMS database transcribed from several previous electronic systems and various paper documents, such as MDA and other index card systems, Gift Books, Accession Registers, free text catalogues, inventories and listings. Fossils are catalogued with other geological material as a series of numbered boxes with a list compiled in the 1980s by James Williams (1944- 2009). An online catalogue is available at: https://dgc-web.adlibhosting.com/home but does not yet contain fossil entries. Collection highlights 1. Permian vertebrate trackways from Locharbriggs and Corncockle quarries linked to Reverend Henry Duncan (1774-1846) and former curator Alfred Truckell (1919-2007). -
The Triassic Marine Biota of Eastern Indonesia and Its Interregional and Global Correlation: a Review
Jurnal Geologi Indonesia, Vol. 5 No. 1 Maret 2010: 31-47 The Triassic Marine Biota of Eastern Indonesia and its Interregional and Global Correlation: A Review F. HASIBUAN Geological Survey Institute Jln. Diponegoro 57, Bandung 40122, Indonesia ABSTRACT The interregional and global correlation of the Triassic biota of Indonesia was based on the review of previous workers and the author himself. Scythian Epoch (Early Triassic) in Timor is subdivided into Early Scythian with Ophiceras demisso, Meekoceras sp., Pseudomonotis subaurita, Gervillia subpannonica, and Myophoria sp., whilst Late Scythian is indicated by the presence of Owenites egrediens and Sibirites sp. The presence of Anisian Stage (Middle Triassic) in Misool is indicated by ammonite Beyrichites and bivalve Daonella lilintana. In Timor, this stage is pointed out by the presence of Joannites cymbiformis, Monophyl- lites wengensis, Protrachyceras archaelus, Daonella indica, Tracyceras cf. aon, Brochidium timorense, and Lima subpunctatoides. Terebellina mackayi found above Beyrichites-bearing bed in Misool has an age range from Anisian to Ladinian. It is concluded that the boundary between Anisian and Ladinian lies between beds with Beyrichites and Terebellina mackayi. Early Carnian Stage (Late Triassic) in Timor is indicated by the presence of Joanites cymbiformis, Waldhausenites sp., Miltites sp., and Halogyra cipitiensis; whereas Late Carnian is indicated by the presence of Cladicites crassestriatus and Tropites subbulatus. The presence of Halobia verbeeki, Pinacoceras parma, Neobetites sp., Parabetites sp., Malayites sp., Amarassites sp., and Halorites sp., indicates the Early Norian Stage, whilst the presence of Cladiscites tornatus, Cyrtopleurits malayicus, and Trachypleuraspidites sp. implies the Late Norian. The Rhaetian Stage in Timor contains Choristoceras indoaustralicum, whereas in Misool it contains Choristoceras sp.