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Precise Age and Biostratigraphic Significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA
Precise age and biostratigraphic significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA Spencer G. Lucas1, Bruce D. Allen2, Karl Krainer3, James Barrick4, Daniel Vachard5, Joerg W. Schneider6, William A. DiMichele7 and Arden R. Bashforth8 1New Mexico Museum of Natural History, 1801 Mountain Road N.W., Albuquerque, New Mexico, 87104, USA email: [email protected] 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, New Mexico, 87801, USA email: [email protected] 3Institute of Geology and Paleontology, University of Innsbruck, Innsbruck, A-6020, Austria email: [email protected] 4Department of Geosciences, Texas Tech University, Box 41053, Lubbock, Texas, 79409, USA email: [email protected] 5Université des Sciences et Technologies de Lille, UFR des Sciences de la Terre, UPRESA 8014 du CNRS, Laboratoire LP3, Bâtiment SN 5, F-59655 Villeneuve d’Ascq, Cédex, France email: [email protected] 6TU Bergakademie Freiberg, Cottastasse 2, D-09596 Freiberg, Germany email:[email protected] 7Department of Paleobiology, NMNH Smithsonian Institution, Washington, DC 20560 email: [email protected] 8Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark email: [email protected] ABSTRACT: The Kinney Brick Quarry is a world famous Late Pennsylvanian fossil Lagerstätte in central New Mexico, USA. The age assigned to the Kinney Brick Quarry (early-middle Virgilian) has long been based more on its inferred lithostratigraphic position than on biostratigraphic indicators at the quarry. We have developed three datasets —-stratigraphic position, fusulinids and conodonts— that in- dicate the Kinney Brick Quarry is older, of middle Missourian (Kasimovian) age. -
New Permian Fauna from Tropical Gondwana
ARTICLE Received 18 Jun 2015 | Accepted 18 Sep 2015 | Published 5 Nov 2015 DOI: 10.1038/ncomms9676 OPEN New Permian fauna from tropical Gondwana Juan C. Cisneros1,2, Claudia Marsicano3, Kenneth D. Angielczyk4, Roger M. H. Smith5,6, Martha Richter7, Jo¨rg Fro¨bisch8,9, Christian F. Kammerer8 & Rudyard W. Sadleir4,10 Terrestrial vertebrates are first known to colonize high-latitude regions during the middle Permian (Guadalupian) about 270 million years ago, following the Pennsylvanian Gondwanan continental glaciation. However, despite over 150 years of study in these areas, the bio- geographic origins of these rich communities of land-dwelling vertebrates remain obscure. Here we report on a new early Permian continental tetrapod fauna from South America in tropical Western Gondwana that sheds new light on patterns of tetrapod distribution. Northeastern Brazil hosted an extensive lacustrine system inhabited by a unique community of temnospondyl amphibians and reptiles that considerably expand the known temporal and geographic ranges of key subgroups. Our findings demonstrate that tetrapod groups common in later Permian and Triassic temperate communities were already present in tropical Gondwana by the early Permian (Cisuralian). This new fauna constitutes a new biogeographic province with North American affinities and clearly demonstrates that tetrapod dispersal into Gondwana was already underway at the beginning of the Permian. 1 Centro de Cieˆncias da Natureza, Universidade Federal do Piauı´, 64049-550 Teresina, Brazil. 2 Programa de Po´s-Graduac¸a˜o em Geocieˆncias, Departamento de Geologia, Universidade Federal de Pernambuco, 50740-533 Recife, Brazil. 3 Departamento de Cs. Geologicas, FCEN, Universidad de Buenos Aires, IDEAN- CONICET, C1428EHA Ciudad Auto´noma de Buenos Aires, Argentina. -
The Los Medaños Member of the Permian (Ochoan) Rustler Formation
The Los Medaños Member of the Permian (Ochoan) Rustler Formation by Dennis W. Powers, HC 12 Box 87, Anthony, TX 79821; and Robert M. Holt, Dept. of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM 87801 Abstract We propose Los Medaños Member as the formal name for the lower part of the Upper Permian (Ochoan) Rustler Formation, below R31E the Culebra Dolomite Member, in the north- ern Delaware Basin. The stratotype is at the exhaust shaft of the Waste Isolation Pilot Exhaust Plant (WIPP) site in sec 20 T22S R31E, Eddy shaft T22S County, New Mexico. The name is derived from the nearby sand dune field (Los Meda- ños) and the quadrangle map of the same WIPP site name. Cores of the Los Medaños from WIPP studies correspond to the exhaust-shaft Los Medanos~ geology, though larger features revealed in T23S the shaft must be inferred. Geophysical log signatures permit regional correlations and interpretation of lithology. Outcrops of this Midland unit are poorly exposed and have been little Basin studied. Recent radiometric ages from cor- Hobbs relative units in the Texas panhandle sug- San Simon Study gest that the top of the Rustler is near the area Permian–Triassic boundary. Carlsbad The stratotype consists of 34.4 m of silici- WIPP Central Basin clastics, halitic mudstones, muddy halite, Nash Draw and sulfates (mainly anhydrite). Bedding, Platform invertebrate fossil remains, and bioturba- New Mexico Midland tion indicate a saline lagoon with connec- Texas tions to open marine water, in contrast to the Odessa shallow-water, desiccating evaporite cycles of the underlying Salado Formation. -
Integrated Multi-Stratigraphic Study of the Coll
Integrated multi-stratigraphic study of the Coll de Terrers late Permian–Early Triassic continental succession from the Catalan Pyrenees (NE Iberian Peninsula): A geologic reference record for equatorial Pangaea Eudald Mujal, Josep Fortuny, Jordi Pérez-Cano, Jaume Dinarès-Turell, Jordi Ibáñez-Insa, Oriol Oms, Isabel Vila, Arnau Bolet, Pere Anadón To cite this version: Eudald Mujal, Josep Fortuny, Jordi Pérez-Cano, Jaume Dinarès-Turell, Jordi Ibáñez-Insa, et al.. Inte- grated multi-stratigraphic study of the Coll de Terrers late Permian–Early Triassic continental succes- sion from the Catalan Pyrenees (NE Iberian Peninsula): A geologic reference record for equatorial Pan- gaea. Global and Planetary Change, Elsevier, 2017, 159, pp.46-60. 10.1016/j.gloplacha.2017.10.004. hal-01724348 HAL Id: hal-01724348 https://hal.sorbonne-universite.fr/hal-01724348 Submitted on 6 Mar 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Integrated multi-stratigraphic study of the Coll de Terrers late MARK Permian–Early Triassic continental succession from the Catalan -
The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/63 The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G. Lucas, Karl Krainer, Dan S. Chaney, William A. DiMichele, Sebastian Voigt, David S. Berman, and Amy C. Henrici, 2012, pp. 345-376 in: Geology of the Warm Springs Region, Lucas, Spencer G.; McLemore, Virginia T.; Lueth, Virgil W.; Spielmann, Justin A.; Krainer, Karl, New Mexico Geological Society 63rd Annual Fall Field Conference Guidebook, 580 p. This is one of many related papers that were included in the 2012 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. -
Tobey-Dawn-Msc-ERTH-September
Water and Wind: The Fluvial and Eolian Forces Behind the Pennsylvanian-Permian Halgaito Formation, Utah By Dawn E. Tobey Submitted in partial fulfillment of the requirements for the degree of Masters of Science at Dalhousie University Halifax, Nova Scotia September 2020 © Copyright by Dawn E. Tobey, 2020 Table Of Contents List of Tables ............................................................................................................................... v List of Figures ........................................................................................................................... vi Abstract ..................................................................................................................................... vii List of Abbreviations Used ................................................................................................. viii Acknowledgements .................................................................................................................ix Chapter 1: Introduction .......................................................................................................... 1 1.1 Statement of Problem................................................................................................................ 1 1.2 Objectives ....................................................................................................................................... 6 1.3 Contributions of the Author .................................................................................................. -
Permian Tetrapods from the Sahara Show Climate-Controlled Endemism in Pangaea
letters to nature 6. Wysession, M. et al. The Core-Mantle Boundary Region 273–298 (American Geophysical Union, faunas that dominated tropical-to-temperate zones to the north Washington, DC, 1998). 13–15 7. Sidorin, I., Gurnis, M., Helmberger, D. V.& Ding, X. Interpreting D 00 seismic structure using synthetic and south . Our results show that long-standing theories of waveforms computed from dynamic models. Earth Planet. Sci. Lett. 163, 31–41 (1998). Late Permian faunal homogeneity are probably oversimplified as 8. Boehler, R. High-pressure experiments and the phase diagram of lower mantle and core constituents. the result of uneven latitudinal sampling. Rev. Geophys. 38, 221–245 (2000). For over 150 yr, palaeontologists have understood end-Palaeozoic 9. Alfe`, D., Gillan, M. J. & Price, G. D. Composition and temperature of the Earth’s core constrained by combining ab initio calculations and seismic data. Earth Planet. Sci. Lett. 195, 91–98 (2002). terrestrial ecosystems largely on the basis of Middle and Late 10. Thomas, C., Kendall, J. & Lowman, J. Lower-mantle seismic discontinuities and the thermal Permian tetrapod faunas from southern Africa. The fauna of these morphology of subducted slabs. Earth Planet. Sci. Lett. 225, 105–113 (2004). rich beds, particularly South Africa’s Karoo Basin, has provided 11. Thomas, C., Garnero, E. J. & Lay, T. High-resolution imaging of lowermost mantle structure under the fundamental insights into the origin of modern terrestrial trophic Cocos plate. J. Geophys. Res. 109, B08307 (2004). 16 12. Mu¨ller, G. The reflectivity method: A tutorial. Z. Geophys. 58, 153–174 (1985). structure and the successive adaptations that set the stage for the 13 13. -
High-Resolution U-Pb Geochronology of Terrestrial Cretaceous-Paleogene and Permo-Triassic Boundary Sequences in North America
High-resolution U-Pb Geochronology of Terrestrial Cretaceous-Paleogene and Permo-Triassic Boundary Sequences in North America by William Stuart Mitchell, III A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Chemistry in the Graduate Division of the University of California, Berkeley Committee in charge: Professor Paul Renne, Co-chair Professor Evan Williams, Co-chair Professor Heino Nitsche Professor Donald DePaolo Spring 2014 High-resolution U-Pb Geochronology of Terrestrial Cretaceous-Paleogene and Permo-Triassic Boundary Sequences in North America Copyright 2014 by William Stuart Mitchell, III 1 Abstract High-resolution U-Pb Geochronology of Terrestrial Cretaceous-Paleogene and Permo-Triassic Boundary Sequences in North America by William Stuart Mitchell, III Doctor of Philosophy in Chemistry University of California, Berkeley Professor Paul Renne, Co-chair Professor Evan Williams, Co-chair High-resolution geochronology provides a means to evaluate the timescales of responses to major shifts in Earth history, such as ecosystem recovery following a major impact event or a mass extinction. Additionally, geochronology can be used to correlate sections across the marine and terrestrial realm and around the world. Changes in ecosystems or isotopic composition of deposited rocks will be influenced by local effects, but can also have a global signal. With geochronlogy, the same time interval can be found in distant regions, and if a phenomenon (e.g. a carbon isotope excursion) was global in scope, many different localities each from the same time interval would show the same signal. Here I present high-resolution uranium-lead geochronology pertaining to two mass ex- tinctions: the Cretaceous-Paleogene mass extinction (around 66 million years ago, Ma) and the Permo-Triassic mass extinction (around 252 Ma). -
Preliminary Geologic Map of the Albuquerque 30' X 60' Quadrangle
Preliminary Geologic Map of the Albuquerque 30’ x 60’ Quadrangle, north-central New Mexico By Paul L. Williams and James C. Cole Open-File Report 2005–1418 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Williams, Paul L., and Cole, James C., 2006, Preliminary Geologic Map of the Albuquerque 30’ x 60’ quadrangle, north-central New Mexico: U.S. Geological Survey Open-File Report 2005-1418, 64 p., 1 sheet scale 1:100,000. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Abstract.................................................................................................................1 Introduction ...........................................................................................................2 Geography and geomorphology.........................................................................3 -
Registre Sedimentari I Icnològic Del Fini-Carbonífer, Permià I Triàsic Continentals Dels Pirineus Catalans Evolució I Crisis Paleoambientals a L’Equador De Pangea
Departament de Geologia, Facultat de Ciències, Universitat Autònoma de Barcelona Registre sedimentari i icnològic del fini-Carbonífer, Permià i Triàsic continentals dels Pirineus Catalans Evolució i crisis paleoambientals a l’equador de Pangea Memòria presentada per Eudald Mujal Grané per optar al títol de Doctor en Geologia Juny de 2017 Tesi doctoral dirigida per: Dr. Oriol Oms Llobet, Departament de Geologia, Universitat Autònoma de Barcelona Dr. Josep Fortuny Terricabras, Institut Català de Paleontologia Miquel Crusafont Dr. Oriol Oms Llobet Dr. Josep Fortuny Terricabras Eudald Mujal Grané Capítol 5. Constraining the Permian/Triassic transition in continental environments: Stratigraphic and paleontological record from the Catalan Pyrenees (NE Iberian Peninsula) Capítol 5. Constraining the Permian/Triassic transition in continental environments: Stratigraphic and paleontological record from the Catalan Pyrenees (NE Iberian Peninsula) El capítol 5 correspon a l’article publicat a la revista Palaeogeography, Palaeoclimatology, Palaeoecology l’1 de març de 2016 (online el 21 de desembre de 2015): Mujal, E., Gretter, N., Ronchi, A., López-Gómez, J., Falconnet, J., Diez, J.B., De la Horra, R., Bolet, A., Oms, O., Arche, A., Barrenechea, J.F., Steyer, J.-S., Fortuny, J., 2016. Constraining the Per- mian/Triassic transition in continental environaments: Stratigraphic and paleontological record from the Catalan Pyrenees (NE Iberian Peninsula). Palaeogeography, Palaeoclimatology, Palaeoecology, 445: 18–37. https://doi.org/10.1016/j.palaeo.2015.12.008 En aquest article l’autor E. M. ha contribuït en: plantejament del treball; tasques de camp, incloent prospecció i documentació de les traces fòssils; elaboració dels models fotogramètrics 3D de les icni- tes; anàlisis de sedimentologia i icnologia; interpretació i discussió de tots els resultats; redacció del manuscrit; preparació de les figures 6–14; maquetació de les figures 2, 6–14; preparació del material suplementari. -
Integrated Multi-Stratigraphic Study of the Coll De Terrers Late Permian
Integrated multi-stratigraphic study of the Coll de Terrers late MARK Permian–Early Triassic continental succession from the Catalan Pyrenees (NE Iberian Peninsula): A geologic reference record for equatorial Pangaea ⁎ Eudald Mujala,c, , Josep Fortunyb,c, Jordi Pérez-Canoa,f, Jaume Dinarès-Turelld, Jordi Ibáñez-Insae, Oriol Omsa, Isabel Vilaf, Arnau Boletc, Pere Anadóne a Departament de Geologia, Universitat Autònoma de Barcelona, E-08193 Bellaterra, Spain b Centre de Recherches en Paléobiodiversité et Paléoenvironnements, UMR 7202 CNRS-MNHN-UPMC, Muséum national d'Histoire naturelle, Bâtiment de Paléontologie, 8 rue Buffon, CP38, F-75005 Paris, France c Institut Català de Paleontologia Miquel Crusafont, ICTA-ICP building, c/de les columnes, s/n, E-08193 Cerdanyola del Vallès, Spain d Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, I-00143 Roma, Italy e Institut de Ciències de la Terra Jaume Almera, ICTJA-CSIC, c/Lluís Solé i Sabarís s/n, E-08028 Barcelona, Spain f Departament de Dinàmica de la Terra i de l'Oceà (Facultat de Geologia), Universitat de Barcelona, c/Martí i Franquès s/n, E-08028 Barcelona, Spain ARTICLE INFO ABSTRACT Keywords: The most severe biotic crisis on Earth history occurred during the Permian–Triassic (PT) transition around Permian-Triassic transition 252 Ma. Whereas in the marine realm such extinction event is well-constrained, in terrestrial settings it is still Stratigraphy poorly known, mainly due to the lack of suitable complete sections. This is utterly the case along the Western Orbital forcing Tethys region, located at Pangaea's equator, where terrestrial successions are typically build-up of red beds often X-ray diffraction characterised by a significant erosive gap at the base of the Triassic strata. -
Western Portion of the Panhandle of Texas
f B, Descriptive Geology, 114 "Water-Supply and Irrigation Paper No. 191 \ 0, Underground Waters, 68 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR THE GEOLOGY AND WATER RESOURCES WESTERN PORTION OF THE PANHANDLE OF TEXAS CHARLES 1ST. WASHINGTON GOVERNMENT PRINTING OFFICE 1907 CONTENTS. Page. Introduction................................................................ 7 Area covered........................................................... 7 Sources of data. ......................................................... 7 Topography.................................................................. 7 General features....................................................... 7 High Plains.......................................................... 8 Valleys and canyons................................................... 9 Canadian River valley............................................. 9 Palo Duro Canyon.'................................................ 10 Minor stream valleys.............................................. 11 Beaver Creek valley............................................ 11 Coldwater Creek valley......................................... 11 Palo Duro Creek valley.......................................... 12 Carriso and Perico Creek valleys................................. 12 Big Blue Creek valley.......................................... 12 Tierra Blanca Creek valley...................................... 12 Geology.................................................................. 12 General