Rudist Classification for the Revised Bivalvia Volumes of the 'Treatise On
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Die Rudisten (Bechermuscheln) Von St
Die Rudisten (Bechermuscheln) von St. Bartholomä in der Weststeiermark Teil 1 Version 4 – August 2017 Die St. Bartholomä-Formation („Zementmergel-Folge“) des Gosaubeckens von Kainach – St. Bartholomä, ihre Rudisten und ihr größerer Rahmen (i.w. Campanium, Oberkreide, ca. 70-85 Millionen Jahre vor heute) Eine Literaturzusammenfassung Einleitung Altertümliche, exotische Muscheln in St. Bartholomä in der Weststeiermark? Etwa 20 km südlicher, um St. Josef, ja, da gibt es 15 Millionen Jahre alte Austern und Venusmuscheln und viele mehr. Aber von diesen ist hier nicht die Rede, sondern von einer Gruppe von Muscheln, die in der Zeit der Saurier und Ammoniten lebte und heute völlig ausgestorben ist – und die noch dazu gar nicht wie Muscheln aussahen. Es ist die Rede von den Rudisten, den Bechermuscheln, die aus der Gegend um St. Bartholomä schon fast seit den ersten geologischen Erkundungen um die Mitte des 19. Jhdts. bekannt sind. Sie verstecken sich ein wenig, aber beim Spazieren in den wenigen Gräben, in alten Steinbrüchen und in manchen straßennahen Felsen der Gegend kann man ihre mehr oder weniger auffälligen, teilweise sehr gut erhaltenen Reste doch immer wieder entdecken. Zuerst jedoch ein Überblick über diese exotischen, lange vergangenen Zeiten und ihre Wesen. Die Zeit der oberen Kreide – die Erde als „Thermalbad im Treibhausklima“ Gegenüber dem heutigen Zwischeneiszeitklima war die Zeit der Oberkreide, etwa von 100-66 Millionen Jahre (Ma) vor heute, Großteils eine Zeit des Treibhausklimas. Die Lufttemperaturen waren durchschnittlich um 10°C höher als heute und die Meerestemperaturen erreichten in den Tropen möglicherweise Spitzenwerte von 42° C – zu heiß zum Baden; und selbst die Temperaturen in der Tiefsee lagen zeitweise über 20° C. -
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. -
Palaeontologia Electronica RUDIST TAXONOMY USING X-RAY
Palaeontologia Electronica http://palaeo-electronica.org RUDIST TAXONOMY USING X-RAY COMPUTED TOMOGRAPHY Ann Molineux, Robert W. Scott, Richard A. Ketcham, and Jessica A. Maisano Ann Molineux. Texas Natural Science Center, University of Texas, Austin, TX 78705, U.S.A. [email protected] Robert W. Scott. Precision Stratigraphy Associates and University of Tulsa, 600 South College Avenue, Tulsa, OK 74104, U.S.A. [email protected] Richard A. Ketcham. Jackson School of Geosciences, 1 University Station, C-1100, University of Texas at Austin, Austin, TX 78712-0254, U.S.A. [email protected] Jessica A. Maisano. Jackson School of Geosciences, 1 University Station, C-1100, University of Texas at Austin, Austin, TX 78712-0254, U.S.A. [email protected] ABSTRACT X-ray CT provides three-dimensional (3-D) representations of internal features of silicified caprinid bivalves from the Lower Cretaceous (Albian Stage) Edwards Forma- tion in Texas. This technique enables the specific identification of caprinid rudists that otherwise could only be identified by sectioning the specimen. The abundant Edwards species is Caprinuloidea perfecta because it has only two rows of polygonal canals on its ventral and anterior margins. Ontogeny of these unusual gregarious bivalves is also demonstrated by means of these images. KEY WORDS: Rudists; Caprinidae; Cretaceous, Lower; X-ray, CT INTRODUCTION tures, and by shooting stereoscopic pairs, a 3-D image can be obtained (Zangerl 1965). X-ray com- The examination of internal structures of puted tomography (CT) scans of limestone cores three-dimensional megafossils such as caprinid show the general outlines of rudists and succes- bivalves and brachiopods without destruction of sive slices can be stacked by computer to form 3-D specimens has been a challenge. -
The End-Cretaceous Mass Extinction Event at the Impact Area: a Rapid Macrobenthic Diversification and Stabilization
EPSC Abstracts Vol. 14, EPSC2020-65, 2020 https://doi.org/10.5194/epsc2020-65 Europlanet Science Congress 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. The end-Cretaceous mass extinction event at the impact area: A rapid macrobenthic diversification and stabilization Francisco Javier Rodriguez Tovar1, Christopher M. Lowery2, Timothy J. Bralower3, Sean P.S. Gulick2,4,5, and Heather L. Jones3 1University of Granada, Stratigraphy and Palaeontology, Granada, Spain ([email protected]) 2Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78758, USA 3Department of Geosciences, Pennsylvania State University, University Park, Pennsylvania 16802, USA 4Center for Planetary Systems Habitability, University of Texas at Austin, Austin, Texas 11 78712, USA 5Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78712, USA The Cretaceous-Paleogene (K-Pg) mass extinction, 66.0 Ma (Renne et al., 2013), was one of the most important events in the Phanerozoic, severely altering the evolutionary and ecological history of biotas (Schulte et al., 2010). This extinction was caused by paleoenvironmental changes associated with the impact of an asteroid (Alvarez et al., 1980) on the Yucatán carbonate-evaporite platform in the southern Gulf of Mexico, which formed the Chicxulub impact crater (Hildebrand et al., 1991). Prolonged impact winter resulting in global darkness and cessation of photosynthesis, and acid rain have been considered as major killing mechanisms on land and in the oceans. Major animal groups disappeared across the boundary (e.g., the nonavian dinosaurs, marine and flying reptiles, ammonites, and rudists), and other groups suffered severe species level (but not total) extinction, including planktic foraminifera, and calcareous nannofossils. -
Barremian-Lower Aptian Qishn Formation, Haushi-Huqf Area, Oman: a New Outcrop Analogue for the Kharaib/Shu’Aiba Reservoirs
GeoArabia, Vol. 9, No. 1, 2004 Gulf PetroLink, Bahrain Barremian-lower Aptian Qishn Formation, Haushi-Huqf area, Oman: a new outcrop analogue for the Kharaib/Shu’aiba reservoirs Adrian Immenhauser, Heiko Hillgärtner, Ute Sattler, Giovanni Bertotti, Pascal Schoepfer, Peter Homewood, Volker Vahrenkamp, Thomas Steuber, Jean-Pierre Masse, Henk Droste, José Taal-van Koppen, Bram van der Kooij, Elisabeth van Bentum, Klaas Verwer, Eilard Hoogerduijn Strating, Wim Swinkels, Jeroen Peters, Ina Immenhauser-Potthast and Salim Al Maskery ABSTRACT Limestones of the middle Cretaceous Qishn Formation are exposed in the Haushi-Huqf area of Oman. These carbonates preserved reservoir properties due to shallow burial and an arid post-exhumation climate. This characteristic makes the Qishn Formation an excellent outcrop analogue for the Upper Kharaib and Lower Shu’aiba oil reservoirs in the Interior Oman basins. The aim of this paper is to provide a broad overview of results from an industry-oriented field study recently performed in the Qishn Formation outcrops belts. The comparison of these results with studies undertaken in the Northern Oman Mountains and the Oman Interior subsurface is the topic of ongoing research. The age of the Qishn Formation is middle Barremian to mid-early Aptian, the Hawar Member (equivalent) is earliest Aptian in age. The paleo-environments recorded range from the tidal mudflat to the argillaceous platform setting (outer ramp) below the storm wave base. In terms of sequence stratigraphy, four large-scale transgressive-regressive cycles of Cretaceous age (Jurf and Qishn formations) were distinguished. Sequence I, a dolomitized succession termed Jurf Formation, is the equivalent of the Lekhwair, the Lower Kharaib and possibly older Cretaceous units. -
Mid-Cretaceous Step-Wise Demise of the Carbonate Platform Biota in The
Palaeogeography, Palaeoclimatology, Palaeoecology 245 (2007) 462–482 www.elsevier.com/locate/palaeo Mid-Cretaceous step-wise demise of the carbonate platform biota in the Northwest Pacific and establishment of the North Pacific biotic province ⁎ Yasuhiro Iba a, , Shin-ichi Sano b a Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-0033, Japan b Fukui Prefectural Dinosaur Museum, Katsuyama, Fukui 911-8601, Japan Received 9 March 2006; received in revised form 6 July 2006; accepted 14 September 2006 Abstract The global spatiotemporal distribution of the Cretaceous carbonate platform biota, which is characterized by “tropical” Mesogean (= Cretaceous Tethys) taxa, is an important aspect of Earth's paleobiogeography. All available records of this biota in the Northwest Pacific (Japan and Sakhalin Island) are summarized in order to elucidate its stratigraphic distribution patterns and faunal changes, with special attention given to the biota of the Late Aptian–Early Albian. This carbonate platform biota flourished from the Berriasian to Early Albian interval in the Northwest Pacific, indicating that the Northwest Pacific clearly belonged to the Tethyan biotic realm at that time. A step-wise demise of the carbonate platform biota transpired in the latest Aptian to middle Albian interval. Mesogean key taxa (rudists and dasycladacean algae), some Mesogean indicators (hermatypic corals and stromatoporoids) and nerineacean gastropods disappeared at the Late Aptian to Early Albian transition. Following this event, other Mesogean indicators (orbitolinid foraminifers and calcareous red algae) and coated grains disappeared at the Early to middle Albian transition. There is no record of carbonate platform biota in the Northwest Pacific during the long interval between the Middle Albian and Paleocene. -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
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. -
Earliest Aptian Caprinidae (Bivalvia, Hippuritida) from Lebanon Jean-Pierre Masse, Sibelle Maksoud, Mukerrem Fenerci-Masse, Bruno Granier, Dany Azar
Earliest Aptian Caprinidae (Bivalvia, Hippuritida) from Lebanon Jean-Pierre Masse, Sibelle Maksoud, Mukerrem Fenerci-Masse, Bruno Granier, Dany Azar To cite this version: Jean-Pierre Masse, Sibelle Maksoud, Mukerrem Fenerci-Masse, Bruno Granier, Dany Azar. Earliest Aptian Caprinidae (Bivalvia, Hippuritida) from Lebanon. Carnets de Geologie, Carnets de Geologie, 2015, 15 (3), pp.21-30. <10.4267/2042/56397>. <hal-01133596> HAL Id: hal-01133596 https://hal-confremo.archives-ouvertes.fr/hal-01133596 Submitted on 23 Mar 2015 HAL is a multi-disciplinary open access L'archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destin´eeau d´ep^otet `ala diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publi´esou non, lished or not. The documents may come from ´emanant des ´etablissements d'enseignement et de teaching and research institutions in France or recherche fran¸caisou ´etrangers,des laboratoires abroad, or from public or private research centers. publics ou priv´es. Carnets de Géologie [Notebooks on Geology] - vol. 15, n° 3 Earliest Aptian Caprinidae (Bivalvia, Hippuritida) from Lebanon Jean-Pierre MASSE 1, 2 Sibelle MAKSOUD 3 Mukerrem FENERCI-MASSE 1 Bruno GRANIER 4, 5 Dany AZAR 6 Abstract: The presence in Lebanon of Offneria murgensis and Offneria nicolinae, two characteristic components of the Early Aptian Arabo-African rudist faunas, fills a distributional gap of the cor- responding assemblage between the Arabic and African occurrences, on the one hand, and the Apulian occurrences, on the other hand. This fauna bears out the palaeogeographic placement of Lebanon on the southern Mediterranean Tethys margin established by palaeostructural reconstructions. -
First North American Occurrence of the Rudist Durania Sp
TRANSACTIONS OF THE KANSAS Vol. 115, no. 3-4 ACADEMY OF SCIENCE p. 117-124 (2012) Bombers and Bivalves: First North American occurrence of the rudist Durania sp. (Bivalvia: Radiolitidae) in the Upper Cretaceous (Cenomanian) Greenhorn Limestone of southeastern Colorado Bruce A. Schumacher USDA Forest Service, 1420 E. 3rd St., La Junta, CO 81050 [email protected] A colonial monospecific cluster of rudist bivalves from the lowermost Bridge Creek Limestone Member, Greenhorn Limestone (Upper Cenomanian) are attributable to Durania cf. D. cornupastoris. This discovery marks only the eighth recorded pre- Coniacian occurrence of rudist bivalves in the Cretaceous Western Interior and the only Cenomanian record of rudist Durania in North America. Discovered in 2011, the specimen was unearthed by aerial bombing at a training facility utilized during World War II. The appearance of rudist bivalves at mid-latitudes coincident with marked change in marine sediments likely represents the onset of mid-Cretaceous global warming. Keywords: Cenomanian, climate, Durania, Greenhorn, rudist Introduction The Greenhorn Limestone in southeastern Colorado (Fig. 3) is divided into the three Some seventy years ago southeastern Colorado subunits (Cobban and Scott 1972; Hattin 1975; was utilized during World War II (1943 – 1945) Kauffman 1986). Roughly the lower two-thirds as a training area for precision bombing practice of the unit is comprised of the basal Lincoln and air-to-ground gunnery. The La Junta Limestone Member (5 m) and the Hartland Municipal Airport was created in April 1940 as Shale Member (19 m). The dominant lithology La Junta Army Air Field (Thole 1999) and was of the lower members is calcareous shale with used by the United States Army Air Forces for minor amounts of thin calcarenite beds. -
TREATISE ONLINE Number 48
TREATISE ONLINE Number 48 Part N, Revised, Volume 1, Chapter 31: Illustrated Glossary of the Bivalvia Joseph G. Carter, Peter J. Harries, Nikolaus Malchus, André F. Sartori, Laurie C. Anderson, Rüdiger Bieler, Arthur E. Bogan, Eugene V. Coan, John C. W. Cope, Simon M. Cragg, José R. García-March, Jørgen Hylleberg, Patricia Kelley, Karl Kleemann, Jiří Kříž, Christopher McRoberts, Paula M. Mikkelsen, John Pojeta, Jr., Peter W. Skelton, Ilya Tëmkin, Thomas Yancey, and Alexandra Zieritz 2012 Lawrence, Kansas, USA ISSN 2153-4012 (online) paleo.ku.edu/treatiseonline PART N, REVISED, VOLUME 1, CHAPTER 31: ILLUSTRATED GLOSSARY OF THE BIVALVIA JOSEPH G. CARTER,1 PETER J. HARRIES,2 NIKOLAUS MALCHUS,3 ANDRÉ F. SARTORI,4 LAURIE C. ANDERSON,5 RÜDIGER BIELER,6 ARTHUR E. BOGAN,7 EUGENE V. COAN,8 JOHN C. W. COPE,9 SIMON M. CRAgg,10 JOSÉ R. GARCÍA-MARCH,11 JØRGEN HYLLEBERG,12 PATRICIA KELLEY,13 KARL KLEEMAnn,14 JIřÍ KřÍž,15 CHRISTOPHER MCROBERTS,16 PAULA M. MIKKELSEN,17 JOHN POJETA, JR.,18 PETER W. SKELTON,19 ILYA TËMKIN,20 THOMAS YAncEY,21 and ALEXANDRA ZIERITZ22 [1University of North Carolina, Chapel Hill, USA, [email protected]; 2University of South Florida, Tampa, USA, [email protected], [email protected]; 3Institut Català de Paleontologia (ICP), Catalunya, Spain, [email protected], [email protected]; 4Field Museum of Natural History, Chicago, USA, [email protected]; 5South Dakota School of Mines and Technology, Rapid City, [email protected]; 6Field Museum of Natural History, Chicago, USA, [email protected]; 7North