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GC 57-2.Indb
Geologia Croatica 57/2 117–137 13 Figs. 3 Pls. ZAGREB 2004 Lower Aptian Rudist Faunas (Bivalvia, Hippuritoidea) from Croatia Jean-Pierre MASSE1, Mukerrem FENERCI-MASSE1, Tvrtko KORBAR2 and Ivo VELIĆ2 Key words: Rudist faunas, Lower Aptian, Lower Cre- – from Svilaja Mt., in the hinterland of Split, caprinid taceous, Adriatic Carbonate Platform, Croatia. facies including a few Offneria sp. and Glossomyo- phorus costatus MASSE, SKELTON & SLIŠKOVIĆ of Early Aptian age was reported by CVETKO- Abstract TEŠOVIĆ et al. (2003). Lower Aptian rudist faunas from Croatia consist of Requienia? zla- tarskii PAQUIER, Toucasia sp., Agriopleura sp., Glossomyophorus The foregoing shows that the Aptian is a key stage costatus MASSE, SKELTON & SLIŠKOVIĆ, Himeraelites sp. and Offneria sp. This assemblage has a clear Southern Tethyan (Arabo– for Lower Cretaceous rudist studies in Croatia, as African) significance and typifies the Early Aptian. Faunas from the well as in adjacent regions: in Slovenia, where Aptian interior of the Adriatic Carbonate Platform in Istria are dominated by caprinids have been described by PLENIČAR & BUS- Requieniidae while those from the northeastern area in the vicinity of ER (1967) and TURNŠEK et al. (1992), and in Bosnia, Tounj–Ogulin, close to the platform margin, exhibit a higher diversity and include, beside requieniids, Caprinidae, Caprotinidae and Mono- where caprinids and caprotinids have been studied by pleuridae, in conjunction with evidence of open marine conditions. MASSE et al. (1984). The objective of the present paper is to specify the taxonomic position of Lower Aptian rudists found in the Kanfanar area of Istria, and the Tounj area of central Croatia (Fig. -
Geology of Tunceli - Bingöl Region of Eastern Turkey
GEOLOGY OF TUNCELİ - BİNGÖL REGION OF EASTERN TURKEY F. A. AFSHAR Middle East Technical University, Ankara ABSTRACT. — This region is located in the Taurus orogenic belt of the highland district of Eastern Turkey. Lower Permian metasediments and Upper Permian suberystalline limestone are the oldest exposed formations of this region. Lower Cretaceous flysch overlies partly eroded Upper Permian limestone discordantly. The enormous thickness of flysch, tuffs, basaltic - andesitic flows, and limestones constitute deposits of Lower Cretaceous, Upper Cretaceous, and Lower Eocene; the deposits of each of these periods are separated from the others by an unconformity. Middle Eocene limestone is overlain discordantly by Lower Miocene marine limestone which grades upward into lignite-bearing marls of Middle Miocene and red beds of Upper Miocene. After Upper Miocene time, this region has been subjected to erosion and widespread extrusive igneous activities. During Permian this region was part of Tethys geosyncline; in Triassic-Jurassic times it was subjected to orogenesis, uplift and erosion, and from Lower Cretaceous until Middle Eocene it was part of an eugeosyncline. It was affected by Variscan, pre-Gosauan, Laramide, Pyrenean, and Attian orogenies. The entire sedimentary section above the basement complex is intensely folded, faulted, subjected to igneous intrusion, and during five orogenic episodes has been exposed and eroded. INTRODUCTION In the August of 1964 the Mineral Research and Exploration Institute of Turkey assigned the writer to undertake geologic study of the region which is the subject of discussion in this report. This region is located in the highland district of Eastern Turkey, extending from Karasu River in the north to Murat River in the south. -
Albian Rudist Biostratigraphy (Bivalvia), Comanche Shelf to Shelf Margin, Texas
Carnets Geol. 16 (21) Albian rudist biostratigraphy (Bivalvia), Comanche shelf to shelf margin, Texas Robert W. SCOTT 1, 2 2 Yulin WANG 2 Rachel HOJNACKI Yulin WANG 3 Xin LAI 4 Highlights • Barremian-Albian caprinids biostratigraphic zones are revised and integrated with ammonites and benthic foraminifers. • New caprinid rudist species are the key to revising long-held correlations of Albian strata on the Co- manche shelf, Texas. • On the San Marcos Arch, central Texas, the shallow shelf Person Formation is the upper unit of the Fredericksburg Group. • The Person underlies the basal Washita Group sequence boundary Al Sb Wa1 and the Georgetown Formation. Abstract: Rudists were widespread and locally abundant carbonate producers on the Early Cretaceous Comanche Shelf from Florida to Texas, and on Mexican atolls. As members of the Caribbean Biogeogra- phic Province, their early ancestors emigrated from the Mediterranean Province and subsequently evol- ved independently. Comanchean rudists formed biostromes and bioherms on the shelf interior and at the shelf margin. Carbonate stratigraphic units of the Comanche Shelf record rudist evolution during the Barremian through the Albian ages and an established zonal scheme is expanded. This study documents new Albian rudist occurrences from the Middle-Upper Albian Fredericksburg and Washita groups in Central and West Texas. Rudists in cores at and directly behind the shelf margin southeast of Austin and San Antonio, Texas, complement the rudist zonation that is integrated with ammonites and foraminifers. These new rudist data test long-held correlations of the Edwards Group with both the Fredericksburg and Washita groups based solely on lithologies. Rudist and foraminifer biostratigraphy indicate that the Edwards Group is coeval with the Fredericksburg not the Washita Group. -
The Mesozoic Mesozoic Things to Think About
The Mesozoic Mesozoic Things to think about • Breakup of Pangea and its relationship to sealevel and climate • Dominance of reptiles • Origin of birds • Origin of mammals • Origin of flowers (angiosperms) • Expansion of insects • Life in the seas assumes an (almost) modern form 1 2 3 4 5 Triassic Period 248 to 206 Million Years Ago 6 The Connecticut River Valley 7 Dinosaur Footprints of the Connecticut Valley Edward Hitchcock Fossil Fish of the Connecticut Valley 8 Jurassic Period 206 to 144 Million Years Ago 9 Cretaceous Period 144 to 65 Million Years Ago 10 11 Mesozoic Ammonites 12 Cretaceous Heteromorph Ammonites Nipponites mirabilis Kamchatka, Russia Macroscaphites sp. Baculites sp. Didymoceras stevensoni Rudistid Bivalves: Jurassic- Cretaceous 13 Durania cornupastoris at Abu Roash, Western Desert near Gizah, Egypt Fringing Upper Cretaceous rudist reef reservoirs flanking basement highs, Augila oil field, eastern Libya Reef-forming rudist (Radiolites) from Sarvak Formation, Cenomanian, south Iran. 14 Biostrome of hippuritid rudists at Montagne des Cornes; Santonian, Pyrenees, France Rudistid Buildups 15 Biostrome of Vaccinites vesiculosus (Woodward, 1855); Campanian of Saiwan, Oman Monopleura marcida Albian, Viotía, Greece 16 Chalk 17 Pterosaurs Mosasaurs 18 Plesiosaurs Ichthyosaurs 19 A Dinosaur Family Tree (aka Phylogeny) 20 Sauropods Theropods 21 Dilong paradoxus Early Cretaceous, China A feathered tyrannosaurid? 22 A Dinosaur Family Tree (aka Phylogeny) Ornithopods (aka Hadrosaurs) 23 Thyreophorans (aka Ankylosaurs, etc) Margincephalians (aka Ceratopsians) 24 A Dinosaur Family Tree (aka Phylogeny) The Liaoning Fauna: An early Cretaceous Lagerstatten Some highlights: -- feathered dinosaurs -- preserved internal organs -- oldest placental mammal 25 The Liaoning Fauna The Liaoning Fauna Caudipteryx. Microraptor gui MICRORAPTOR zhaoianus. -
Biotic Resources of Indio Mountains Research Station
BIOTIC RESOURCES OF INDIO MOUNTAINS RESEARCH STATION Southeastern Hudspeth County, Texas A HANDBOOK FOR STUDENTS AND RESEARCHERS Compiled by: Richard D. Worthington Carl Lieb Wynn Anderson Pp. 1 - 85 El Paso, Texas Fall, 2004 (Continually Reviewed and Updated) by Jerry D. Johnson (Last Update) 16 September 2010 1 TABLE OF CONTENTS INTRODUCTION - Pg. 3 COLLECTING IMRS RESOURCES – Pg. 4 POLICIES FOR THE PROTECTION OF RESOURCES – Pg. 4 PHYSICAL SETTING – Pg. 5 CHIHUAHUAN DESERT – Pg. 6 CLIMATE – Pg. 6 GEOLOGY – Pg. 8 SOILS – Pg. 12 CULTURAL RESOURCES – Pg. 13 PLANT COMMUNITIES – Pg. 14 LICHENS – Pg. 15 NONVASCULAR PLANTS – Pg. 18 VASCULAR PLANTS – Pg. 19 PROTOZOANS – Pg. 34 FLATWORMS – Pg. 34 ROUNDWORMS – Pg. 34 ROTIFERS – Pg. 35 ANNELIDS – Pg. 36 MOLLUSKS – Pg. 36 ARTHROPODS – Pg. 37 VERTEBRATES – Pg. 64 IMRS GAZETTEER – Pg. 80 2 INTRODUCTION It is our pleasure to welcome students and visitors to the Indio Mountains Research Station (IMRS). A key mission of this facility is to provide a research and learning experience in the Chihuahuan Desert. We hope that this manual will assist you in planning your research and learning activities. You will probably be given a short lecture by the station Director upon entering the station. Please pay attention as IMRS is not without potential hazards and some long-term research projects are underway that could be disturbed if one is careless. Indio Mountains Research Station came into being as a result of the generosity of a benefactor and the far-sighted vision of former UTEP President Haskell Monroe. Upon his death in 1907, the will of Boston industrialist Frank B. -
Convergent and Parallel Evolutionary Traits in Early Cretaceous Rudist Bivalves (Hippuritidina)
International Journal of Paleobiology & Paleontology ISSN: 2642-1283 MEDWIN PUBLISHERS Committed to Create Value for Researchers Convergent and Parallel Evolutionary Traits in Early Cretaceous Rudist Bivalves (Hippuritidina) Masse JP* and Fenerci Masse M Review Article Aix-Marseille University, France Volume 4 Issue 1 Received Date: December 07, 2020 *Corresponding author: Jean Pierre Masse, Aix-Marseille University, Place Victor Hugo. Published Date: January 12, 2021 13331 Marseille Cedex 03, France, Email: [email protected] Abstract Early Cretaceous Hippuritida clades, requieniide (family Requieniidae) and hippuritide (families Radiolitidae, Polyconitidae, Caprinidae, “Caprinulidae” and Caprinuloideidae), show distinctive myophoral arrangements and shell structures. Nevertheless they share some characters, such as the transverse shell thickening of the myophores of the attached valve which are convergent traits in Lovetchenia (Requieniidae) and Homopleura (Monopleuridae). The bent posterior myophore of the right valve of Pseudotoucasia (Requieniidae) closely resemble the posterior myophore of the left valve of Horiopleura and Polyconites (Polyconitidae). The shell cellular structure is one of the key attributes of the family Radiolitidae (e.g. Eoradiolites) but this structure is also present in some advanced Requieniidae (“Toucasia-Apricardia “group). Canaliculate shell structures are convergent evolutionary traits which are common in the Caprinidae and Caprinuloideidae and also exist in parallel evolution: expansion of canals into the entire shell and increasing complexity of canal architecture. Convergent taxa the Polyconitidae and “Caprinulidae”. In most of the foregoing canaliculated groups, two trends are well expressed, reflecting took some advantages by using former innovations. An Albian peak of convergence coincided with the emergence of new clades, which suggests a reset following the mid-Aptian extinction event. -
End of a Modern Geological Myth: There Are No Rudists in Brazil! Paleobiogeographic Implications
Carnets de Géologie [Notebooks on Geology] - vol. 15, n° 11 End of a modern geological myth: there are no rudists in Brazil! Paleobiogeographic implications Bruno GRANIER 1 Dimas DIAS-BRITO 2 Abstract: Out of the few records of rudists from the Cretaceous strata of the South Atlantic coastal basins only two refer to Brazilian localities. However, petrographic analyses demonstrate that these shells should be assigned to Ostreids or to Pycnodontids rather than to Rudistids. More specifically, the domain considered herein, north of the Río Grande Rise - Walvis Ridge barrier, was part of the warm- water "tropical" realm, but it was not part of the Mesogean domain because both Rudistids and Orbitolinas are missing. In addition, the scarcity of corals leads us to ascribe the taphonomic assemblage to the Chloralgal facies. Neither generalized hypersalinity or extreme sea-water tempe- ratures seem to account for these biotic peculiarities. Instead, our alternative hypothesis favors the driving role played by oceanic circulation in the dispersal of the benthic organisms. Key Words: Rudists; Ostreids; Pycnodontids; corals; Orbitolinids; calcareous algae; Cretaceous; Albian; Cenomanian; South Atlantic; Tethys; Mesogea; Chloralgal; paleobiogeography. Citation: GRANIER B. & DIAS-BRITO D. (2015).- End of a modern geological myth: there are no rudists in Brazil! Paleobiogeographic implications.- Carnets Géol., Madrid, vol. 15, nº 11, p. 123-136. Résumé : Fin d'un mythe géologique moderne : il n'y a pas de rudistes au Brésil ! et ses implications paléobiogéographiques.- Parmi les quelques signalements de rudistes dans les séries crétacées des bassins côtiers de l'Océan Atlantique Sud, deux seulement correspondent à des sites brésiliens. Toutefois, les analyses pétrographiques montrent que ces coquilles ne sauraient être attribuées à des rudistes mais plutôt à des Ostréidés ou à des Pycnodontidés. -
Cretaceous Rudists and Carbonate Platforms
CRETACEOUS RUDISTS AND CARBONATE PLATFORMS June 23-25, 2008 Dokuz Eylül University zmir-TUREY EIGHTH INTERNATIONAL CONGRESS ON RUDISTS June 23-25, 2008-�zmir, Turkey EIGHTH INTERNATIONAL CONGRESS ON RUDISTS CRETACEOUS RUDISTS AND CARBONATE PLATFORMS ABSTRACTS June 23-25, 2008 Dokuz Eylül University zmir-TURKEY 2 EIGHTH INTERNATIONAL CONGRESS ON RUDISTS June 23-25, 2008-�zmir, Turkey SPONSORS Organizing committee wishes to thank the following for their generosity in supporting the Eighth International Congress on Rudists Dokuz Eylül University TÜBTAK (The Scientific and Research Council of Turkey) Chamber of Geological Engineers of Turkey Turkish Petroleum Corporation General Directorate of Mineral Research and Exploration zmir Metropolitan Municipality Konak Municipality Buca Municipality Ministry of Culture and Tourism Efes Pilsen Beer A.;. Yazgan Wine A.;. Do=u> Çay A.;. Sevinç Pastanesi 3 EIGHTH INTERNATIONAL CONGRESS ON RUDISTS June 23-25, 2008-�zmir, Turkey HONORARY COMMITTEE Emin ALICI, Rector of the Dokuz Eylül University Cüneyt GÜZEL;, Dean of the Faculty of Engineering Özkan P;KN, Chairman of the Department of Geological Engineering ORGANIZING COMMITTEE Sacit ÖZER, Chairman, Department of Geological Engineering, Dokuz Eylül University, �zmir Bilal SARI, Secretary, Department of Geological Engineering, Dokuz Eylül University, �zmir Erdin BOZKURT, Editor of the “Turkish Journal of Earth Sciences”, and Middle East Technical University, Ankara Muhittin GÖRMÜ;, Department of Geological Engineering, Süleyman Demirel University, Isparta -
Geologic Quadrangle Map No. 19: Fall Prong Quadrangle, Kimble
BUREAU OF ECONOMIC GEOLOGY THE UNIVERSITY OF TEXAS AUSTIN 12, TEXAS John T.Lonsdale,Director GEOLOGeologic Quadrangle Map No. 19 FallProng Quadrangle Kimble,Gillespie, andMason Counties, Texas By Virgil E. Barnes May 1956 Geology of the Fall Prong Quadrangle, Kimble, Gillespie, and Mason Counties VIRGIL E. BARNES GeneralSetting Granuleintraformationalconglomerate Angular granules are common in the Fredericksburg Group proximatedby following the black band scribed in the text of the Wendel quad- and Barnes,1944; Barnes, Romberg,and common near the base of the Edwards composed of one-fourth-inch aphanitic lower part of the Hensell sand; upward Included within the Fredericksburg mentioned above. rangle. Anderson,1954a, 1954b, 1955).The area limestone, butnone weremapped within Fall Prong quadrangle is in the mar- granules in a fine-grained matrix is the Hensell is finer grained, containing group of the Fall Prong quadrangle is The Comanche Peak limestone is No fossil collectionswere madewithin of lowgravity valuesin thenortheastern the Fall Prong quadrangle. ginal portion Plateau of the Edwards common. Glauconite is mostly rather much silt and clay. In the western part about 300 feet of Edwards limestone, describedbelow in the sections measured the quadrangle, and no attempt was part of the quadrangle is associatedwith Sandstones in the Cambrian probably near thesoutheasterncorner of theLlano Peak scarce but ina few beds is rather abun- of the quadrangle the upper part of the about 32 feet of Comanche lime- along Little Devils River just west of made to find silicified fossils, although a minimum whichincludes the northern are present beneathmuch of the quad- region. Almost three-quarters of the stone, clay. -
Geology of the Eagle Mountains, Hudspeth County, Texas James R
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/31 Geology of the Eagle Mountains, Hudspeth County, Texas James R. Underwood Jr., 1980, pp. 183-193 in: Trans Pecos Region (West Texas), Dickerson, P. W.; Hoffer, J. M.; Callender, J. F.; [eds.], New Mexico Geological Society 31st Annual Fall Field Conference Guidebook, 308 p. This is one of many related papers that were included in the 1980 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. -
Rudists of Tibet and the Tarim Basin, China: Significance to Requieniidae Phylogeny
J. Paleont., 84(3), 2010, pp. 000–000 Copyright ’ 2010, The Paleontological Society 0022-3360/10/0000-0000$03.00 RUDISTS OF TIBET AND THE TARIM BASIN, CHINA: SIGNIFICANCE TO REQUIENIIDAE PHYLOGENY ROBERT W. SCOTT,1 XIAQIAO WAN,2 JINGENG SHA,3 AND SHI-XUAN WEN3 1Department of Geosciences, University of Tulsa, Tulsa, Oklahoma 74104, ,[email protected].; 2China University of Geosciences, Beijing, China; and 3LPS, Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing ABSTRACT—Rudists are a principal biotic component of Cretaceous carbonates in Tibet and in the Western Tarim Basin. Barremian to Maastrichtian carbonate units are widespread on the northern margin of the Indian Plate and in Tethyan tectonic slices that were welded onto Eurasia in successive stages during the Late Cretaceous and Paleogene. In far northwestern Tibet, Barremian-Cenomanian endemic rudists and cosmopolitan orbitolinid foraminifera occupied isolated carbonate platforms in the eastern Tethys. Rudists, corals, and stromatoporoids composed bioherms up to 10 m thick and several kilometers in lateral extent. A unique endemic requieniid rudist, Rutonia, is compared to morphologically similar but older, less derived genera. Associated specimens in this assemblage are indeterminate requieniid valves, monopleurids, and two genera with three radiolitid species that are re-described and taxonomic positions re-evaluated. In southern Tibet, mainly endemic Campanian-Maastrichtian radiolitid rudists and cosmopolitan larger benthic foraminifera contributed to carbonate shelves on the northern Indian Plate near the Cretaceous equator. In the Western Tarim Basin Cenomanian strata yield Tethyan rudist species. Coiling morphometric analysis using the three-dimensional morphology Raup diagram shows that Requieniidae valves in contact with the substrate are convergent with the basic gastropod shell. -
Ocean Drilling Program Initial Reports Volume
Winterer, E.L., Sager, W.W., Firth, J.V., and Sinton, J.M. (Eds.), 1995 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 143 1. EARLY CRETACEOUS RUDIST FAUNA OF ALLISON AND RESOLUTION GUYOTS, MID-PACIFIC MOUNTAINS1 Nicola H.M. Swinburne2 and Jean-Pierre Masse3 ABSTRACT Rudists from Resolution and Allison guyots (Mid-Pacific Mountains), recovered during Leg 143 of the Ocean Drilling Program (ODP), are recorded from Barremian to Albian strata. Taxa present belong to the families Requieniidae, Monopleuridae, and Caprinidae. Radiolitidae are noticeably absent. The Barremian interval yielded only one determinable monopleurid mdist, Petalodontia. This occurrence is compatible with its known range in Europe and establishes a circum-global Tethyan distribution for this form. Early Aptian strata produced a rich and diverse fauna of primitive caprinids, corresponding in their evolutionary development to species known from Europe and America from beds of this age. A new species of Caprina, a closely related form, also probably from that genus, and a form of unknown genus are described. All these taxa have right valves with simple, rectangular canals developed mainly on the dorsal and anterior margins. Although there is some relationship between our forms and European and American caprinids endemism exists at the generic and specific levels. The Albian interval also yielded several types of caprinids, but of larger size and having systems of pallial canals different from those of the Aptian. Of particular interest is the occurrence of "Caprina" cf. mulleri, which was previously described by Hamilton (1956) from Cape Johnson Guyot, also in the Mid-Pacific Mountains. This distinctive form may be an indicator of a Pacific Province, or endemic center.