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Contents of Volume 58 Acta Palaeontologica Polonica 58 (4): 889– 892, 2013
Contents of Volume 58 Acta Palaeontologica Polonica 58 (4): 889– 892, 2013 Issue 1 (published March 2013) Christian Foth and Oliver W.M. Rauhut Macroevolutionary and morphofunctional patterns in theropod skulls: A morphometric approach . 1–16 Alexander O. Averianov and J. David Archibald New material and reinterpretation of the Late Cretaceous eutherian mammal Paranyctoides from Uzbekistan . 17–23 Xing Xu, Paul Upchurch, Qingyu Ma, Michael Pittman, Jonah Choiniere, Corwin Sullivan, David W. E. Hone, Qingwei Tan, Lin Tan, Dong Xiao, and Fenglu Han Osteology of the Late Cretaceous alvarezsauroid Linhenykus monodactylus from China and comments on alvarezsauroid biogeography . 25–46 Stephen L. Brusatte and Roger B.J. Benson The systematics of Late Jurassic tyrannosauroid theropods from Europe and North America . 47–54 Victoria M. Arbour, Nicolai L. Lech−Hernes, Tom E. Guldberg, Jørn H. Hurum, and Philip J. Currie An ankylosaurid dinosaur from Mongolia with in situ armour and keratinous scale impressions . 55–64 Tomasz Sulej and Grzegorz Niedźwiedzki A new large capitosaur temnospondyl amphibian from the Early Triassic of Poland . 65–75 Steffen Kiel, Jörn Peckmann, and Klaus Simon Catshark egg capsules from a Late Eocene deep−water methane−seep deposit in western Washington State, USA . 77–84 Anna Kozłowska, Kinga Dobrowolska, and Denis E.B. Bates A new type of colony in Silurian (upper Wenlock) retiolitid graptolite Spinograptus from Poland. 85–92 Timothy P. Topper, Lars E. Holmer, Christian B. Skovsted, Glenn A. Brock, Uwe Balthasar, Cecilia M. Larsson, Sandra Pettersson Stolk, and David A.T. Harper The oldest brachiopods from the lower Cambrian of South Australia. 93–109 Brief reports Heyo Van Iten, Juliana de M. -
A New Microvertebrate Assemblage from the Mussentuchit
A new microvertebrate assemblage from the Mussentuchit Member, Cedar Mountain Formation: insights into the paleobiodiversity and paleobiogeography of early Late Cretaceous ecosystems in western North America Haviv M. Avrahami1,2,3, Terry A. Gates1, Andrew B. Heckert3, Peter J. Makovicky4 and Lindsay E. Zanno1,2 1 Department of Biological Sciences, North Carolina State University, Raleigh, NC, USA 2 North Carolina Museum of Natural Sciences, Raleigh, NC, USA 3 Department of Geological and Environmental Sciences, Appalachian State University, Boone, NC, USA 4 Field Museum of Natural History, Chicago, IL, USA ABSTRACT The vertebrate fauna of the Late Cretaceous Mussentuchit Member of the Cedar Mountain Formation has been studied for nearly three decades, yet the fossil-rich unit continues to produce new information about life in western North America approximately 97 million years ago. Here we report on the composition of the Cliffs of Insanity (COI) microvertebrate locality, a newly sampled site containing perhaps one of the densest concentrations of microvertebrate fossils yet discovered in the Mussentuchit Member. The COI locality preserves osteichthyan, lissamphibian, testudinatan, mesoeucrocodylian, dinosaurian, metatherian, and trace fossil remains and is among the most taxonomically rich microvertebrate localities in the Mussentuchit Submitted 30 May 2018 fi fi Accepted 8 October 2018 Member. To better re ne taxonomic identi cations of isolated theropod dinosaur Published 16 November 2018 teeth, we used quantitative analyses of taxonomically comprehensive databases of Corresponding authors theropod tooth measurements, adding new data on theropod tooth morphodiversity in Haviv M. Avrahami, this poorly understood interval. We further provide the first descriptions of [email protected] tyrannosauroid premaxillary teeth and document the earliest North American record of Lindsay E. -
A Revision of the Classification of the Plesiosauria with a Synopsis of the Stratigraphical and Geographical Distribution Of
LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 59. Nr l. KUNGL. FYSIOGRAFISKA SÅLLSKAPETS HANDLINGAR, N. F. Bd 74. Nr 1. A REVISION OF THE CLASSIFICATION OF THE PLESIOSAURIA WITH A SYNOPSIS OF THE STRATIGRAPHICAL AND GEOGRAPHICAL DISTRIBUTION OF THE GROUP BY PER OVE PERSSON LUND C. W. K. GLEER UP Read before the Royal Physiographic Society, February 13, 1963. LUND HÅKAN OHLSSONS BOKTRYCKERI l 9 6 3 l. Introduction The sub-order Plesiosauria is one of the best known of the Mesozoic Reptile groups, but, as emphasized by KuHN (1961, p. 75) and other authors, its classification is still not satisfactory, and needs a thorough revision. The present paper is an attempt at such a revision, and includes also a tabular synopsis of the stratigraphical and geo graphical distribution of the group. Some of the species are discussed in the text (pp. 17-22). The synopsis is completed with seven maps (figs. 2-8, pp. 10-16), a selective synonym list (pp. 41-42), and a list of rejected species (pp. 42-43). Some forms which have been erroneously referred to the Plesiosauria are also briefly mentioned ("Non-Plesiosaurians", p. 43). - The numerals in braekets after the generic and specific names in the text refer to the tabular synopsis, in which the different forms are numbered in successional order. The author has exaroined all material available from Sweden, Australia and Spitzbergen (PERSSON 1954, 1959, 1960, 1962, 1962a); the major part of the material from the British Isles, France, Belgium and Luxembourg; some of the German spec imens; certain specimens from New Zealand, now in the British Museum (see LYDEK KER 1889, pp. -
Source-Rock Geochemistry of the San Joaquin Basin Province, California
Petroleum Systems and Geologic Assessment of Oil and Gas in the San Joaquin Basin Province, California Chapter 11 Source-Rock Geochemistry of the San Joaquin Basin Province, California By Kenneth E. Peters, Leslie B. Magoon, Zenon C. Valin, and Paul G. Lillis HIO for all source-rock units except the Tumey formation of Contents Atwill (1935). Abstract-----------------------------------------------------------------------------------1 Thick, organic-rich, oil-prone shales of the upper Mio- Introduction------------------------------------------------------------------------------ 1 cene Monterey Formation occur in the Tejon depocenter in Methods----------------------------------------------------------------------------------2 the southern part of the basin with somewhat less favorable Discussion--------------------------------------------------------------------------------3 occurrence in the Southern Buttonwillow depocenter to the Upper Miocene Antelope shale---------------------------------------------------3 north. Shales of the upper Miocene Monterey Formation Eocene Tumey formation-----------------------------------------------------------4 Eocene Kreyenhagen Formation--------------------------------------------------4 generated most of the petroleum in the San Joaquin Basin. Cretaceous-Paleocene Moreno Formation--------------------------------------5 Thick, organic-rich, oil-prone Kreyenhagen Formation source Conclusions----------------------------------------------------------------------------- -5 rock occurs in the Buttonwillow -
A Revised Taxonomy of the Iguanodont Dinosaur Genera and Species
ARTICLE IN PRESS + MODEL Cretaceous Research xx (2007) 1e25 www.elsevier.com/locate/CretRes A revised taxonomy of the iguanodont dinosaur genera and species Gregory S. Paul 3109 North Calvert Station, Side Apartment, Baltimore, MD 21218-3807, USA Received 20 April 2006; accepted in revised form 27 April 2007 Abstract Criteria for designating dinosaur genera are inconsistent; some very similar species are highly split at the generic level, other anatomically disparate species are united at the same rank. Since the mid-1800s the classic genus Iguanodon has become a taxonomic grab-bag containing species spanning most of the Early Cretaceous of the northern hemisphere. Recently the genus was radically redesignated when the type was shifted from nondiagnostic English Valanginian teeth to a complete skull and skeleton of the heavily built, semi-quadrupedal I. bernissartensis from much younger Belgian sediments, even though the latter is very different in form from the gracile skeletal remains described by Mantell. Currently, iguanodont remains from Europe are usually assigned to either robust I. bernissartensis or gracile I. atherfieldensis, regardless of lo- cation or stage. A stratigraphic analysis is combined with a character census that shows the European iguanodonts are markedly more morpho- logically divergent than other dinosaur genera, and some appear phylogenetically more derived than others. Two new genera and a new species have been or are named for the gracile iguanodonts of the Wealden Supergroup; strongly bipedal Mantellisaurus atherfieldensis Paul (2006. Turning the old into the new: a separate genus for the gracile iguanodont from the Wealden of England. In: Carpenter, K. (Ed.), Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. -
Appendices D Through I
Appendix D Operation & Maintenance Appendix D. Operation and Maintenance Plan Operation and Maintenance Plan This document presents the operation and maintenance (O&M) plan for Western Area Power Administration’s (Western) Sierra Nevada Region (SNR) transmission line systems. 1.0 Inspection/System Management In compliance with Western’s Reliability Centered Maintenance Program, Western would conduct aerial, ground, and climbing inspections of its existing transmission infrastructure since initial construction. The following paragraphs describe Western’s inspection requirements. Aerial Inspections Aerial inspections would be conducted a minimum of every 6 months by helicopter or small plane over the entire transmission system to check for hazard trees1 or encroaching vegetation, as well as to locate damaged or malfunctioning transmission equipment. Typically, aerial patrols would be flown between 50 and 300 feet above Western’s transmission infrastructure depending on the land use, topography, and infrastructure requirements. In general, the aerial inspections would pass over each segment of the transmission line within a one-minute period. Ground Inspections Annual ground inspections would check access to the towers/poles, tree clearances, fences, gates, locks, and tower hardware, and ensure that each structure would be readily accessible in the event of an emergency. They would allow for the inspection of hardware that would not be possible by air, and identify redundant or overgrown access roads that should be permanently closed and returned to their natural state. Ground inspections would typically be conducted by driving a pickup truck along the ROW and access roads. Detailed ground inspections would be performed on 20 percent of all lines and structures annually, for 100 percent inspection every 5 years. -
Lower Cretaceous Avian-Dominated, Theropod
Lower cretaceous avian-dominated, theropod, thyreophoran, pterosaur and turtle track assemblages from the Tugulu Group, Xinjiang, China: ichnotaxonomy and palaeoecology Lida Xing1,2, Martin G. Lockley3, Chengkai Jia4, Hendrik Klein5, Kecheng Niu6, Lijun Zhang7, Liqi Qi8, Chunyong Chou2, Anthony Romilio9, Donghao Wang2, Yu Zhang2, W Scott Persons10 and Miaoyan Wang2 1 State Key Laboratory of Biogeology and Environmental Geology, China University of Geoscience (Beijing), Beijing, China 2 School of the Earth Sciences and Resources, China University of Geoscience (Beijing), Beijing, China 3 Dinosaur Trackers Research Group, University of Colorado at Denver, Denver, United States 4 Research Institute of Experiment and Detection of Xinjiang Oil Company, PetroChina, Karamay, China 5 Saurierwelt Paläontologisches Museum, Neumarkt, Germany 6 Yingliang Stone Natural History Museum, Nan’an, China 7 Institute of Resources and Environment, Key Laboratory of Biogenic Traces & Sedimentary Minerals of Henan Province, Collaborative Innovation Center of Coalbed Methane and Shale Gas for Central Plains Economic Region, Henan Polytechnic University, Jiaozuo, China 8 Faculty of Petroleum, China University of Petroleum (Beijing) at Karamay, Karamay, China 9 School of Biological Sciences, The University of Queensland, Brisbane, Australia 10 Mace Brown Museum of Natural History, Department of Geology and Environmental Geosciences, College of Charleston, Charleston, United States ABSTRACT Rich tetrapod ichnofaunas, known for more than a decade, from the Huangyangquan Reservoir (Wuerhe District, Karamay City, Xinjiang) have been an abundant source Submitted 10 January 2021 of some of the largest Lower Cretaceous track collections from China. They originate Accepted 26 April 2021 from inland lacustrine clastic exposures of the 581–877 m thick Tugulu Group, 28 May 2021 Published variously divided into four formations and subgroups in the northwestern margin of Corresponding author the Junggar Basin. -
Speleogenesis and Delineation of Megaporosity and Karst
Stephen F. Austin State University SFA ScholarWorks Electronic Theses and Dissertations 12-2016 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas Jon T. Ehrhart Stephen F. Austin State University, [email protected] Follow this and additional works at: https://scholarworks.sfasu.edu/etds Part of the Geology Commons, Hydrology Commons, and the Speleology Commons Tell us how this article helped you. Repository Citation Ehrhart, Jon T., "Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas" (2016). Electronic Theses and Dissertations. 66. https://scholarworks.sfasu.edu/etds/66 This Thesis is brought to you for free and open access by SFA ScholarWorks. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of SFA ScholarWorks. For more information, please contact [email protected]. Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas Creative Commons License This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This thesis is available at SFA ScholarWorks: https://scholarworks.sfasu.edu/etds/66 Speleogenesis and Delineation of Megaporosity and Karst Geohazards Through Geologic Cave Mapping and LiDAR Analyses Associated with Infrastructure in Culberson County, Texas By Jon Ehrhart, B.S. Presented to the Faculty of the Graduate School of Stephen F. Austin State University In Partial Fulfillment Of the requirements For the Degree of Master of Science STEPHEN F. -
Precambrian Basement and Late Paleoproterozoic to Mesoproterozoic Tectonic Evolution of the SW Yangtze Block, South China
minerals Article Precambrian Basement and Late Paleoproterozoic to Mesoproterozoic Tectonic Evolution of the SW Yangtze Block, South China: Constraints from Zircon U–Pb Dating and Hf Isotopes Wei Liu 1,2,*, Xiaoyong Yang 1,*, Shengyuan Shu 1, Lei Liu 1 and Sihua Yuan 3 1 CAS Key Laboratory of Crust-Mantle Materials and Environments, University of Science and Technology of China, Hefei 230026, China; [email protected] (S.S.); [email protected] (L.L.) 2 Chengdu Center, China Geological Survey, Chengdu 610081, China 3 Department of Earthquake Science, Institute of Disaster Prevention, Langfang 065201, China; [email protected] * Correspondence: [email protected] (W.L.); [email protected] (X.Y.) Received: 27 May 2018; Accepted: 30 July 2018; Published: 3 August 2018 Abstract: Zircon U–Pb dating and Hf isotopic analyses are performed on clastic rocks, sedimentary tuff of the Dongchuan Group (DCG), and a diabase, which is an intrusive body from the base of DCG in the SW Yangtze Block. The results provide new constraints on the Precambrian basement and the Late Paleoproterozoic to Mesoproterozoic tectonic evolution of the SW Yangtze Block, South China. DCG has been divided into four formations from the bottom to the top: Yinmin, Luoxue, Heishan, and Qinglongshan. The Yinmin Formation, which represents the oldest rock unit of DCG, was intruded by a diabase dyke. The oldest zircon age of the clastic rocks from the Yinmin Formation is 3654 Ma, with "Hf(t) of −3.1 and a two-stage modeled age of 4081 Ma. Another zircon exhibits an age of 2406 Ma, with "Hf(t) of −20.1 and a two-stage modeled age of 4152 Ma. -
Oil and Gas Plays Ute Moutnain Ute Reservation, Colorado and New Mexico
Ute Mountain Ute Indian Reservation Cortez R18W Karle Key Xu R17W T General Setting Mine Xu Xcu 36 Can y on N Xcu McElmo WIND RIVER 32 INDIAN MABEL The Ute Mountain Ute Reservation is located in the northwest RESERVATION MOUNTAIN FT HALL IND RES Little Moude Mine Xcu T N ern portion of New Mexico and the southwestern corner of Colorado UTE PEAK 35 N R16W (Fig. UM-1). The reservation consists of 553,008 acres in Montezu BLACK 666 T W Y O M I N G MOUNTAIN 35 R20W SLEEPING UTE MOUNTAIN N ma and La Plata Counties, Colorado, and San Juan County, New R19W Coche T Mexico. All of these lands belong to the tribe but are held in trust by NORTHWESTERN 34 SHOSHONI HERMANO the U.S. Government. Individually owned lands, or allotments, are IND RES Desert Canyon PEAK N MESA VERDE R14W NATIONAL GREAT SALT LAKE W Marble SENTINEL located at Allen Canyon and White Mesa, San Juan County, Utah, Wash Towaoc PARK PEAK T and cover 8,499 acres. Tribal lands held in trust within this area cov Towaoc River M E S A 33 1/2 N er 3,597 acres. An additional forty acres are defined as U.S. Govern THE MOUND R15W SKULL VALLEY ment lands in San Juan County, Utah, and are utilized for school pur TEXAS PACIFIC 6-INCH OIL PIPELINE IND RES UNITAH AND OURAY INDIAN RESERVATION Navajo poses. W Ramona GOSHUTE 789 The Allen Canyon allotments are located twelve miles west of IND RES T UTAH 33 Blanding, Utah, and adjacent to the Manti-La Sal National Forest. -
Early Cretaceous Pterosaur Tracks from a “Buried” Dinosaur Tracksite In
Available online at www.sciencedirect.com Palaeoworld 21 (2012) 50–58 Research paper Early Cretaceous pterosaur tracks from a “buried” dinosaur tracksite in Shandong Province, China a,b,∗ c d,e f Li-Da Xing , Jerald D. Harris , Gerard D. Gierlinski´ , Murray K. Gingras , a g a Julien D. Divay , Yong-Gang Tang , Philip J. Currie a Department of Biological Sciences, University of Alberta, 11455 Saskatchewan Drive, Edmonton, Alberta T6G 2E9, Canada b Key Laboratory of Evolutionary Systematics of Vertebrates, Chinese Academy of Sciences, PO Box 643, Beijing 100044, China c Physical Sciences Department, Dixie State College, 225 South 700 East, St. George, UT 84770, USA d ´ JuraPark, ul. Sandomierska 4, 27-400 Ostrowiec Swi˛etokrzyski, Poland e Polish Geological Institute, Rakowiecka 4, 00-975 Warszawa, Poland f Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada g Institute of Geology and Palaeontology, Linyi University, Linyi 276000, China Received 27 September 2011; received in revised form 13 January 2012; accepted 9 February 2012 Available online 16 February 2012 Abstract Here we describe the pterosaur and tridactyl dinosaur footprint assemblage from a new tracksite in the Early Cretaceous Qugezhuang For- mation near the Wenxiyuan Community in Jimo County-level City, Qingdao City, Shandong Province, East China. The construction of a community building has, since the discovery, covered the majority of tracks, but a few specimens on abandoned building stones constitute the first pterosaur track record in eastern China. The pterosaur tracks are assigned to Pteraichnus isp. and were probably made by a small to medium-sized pterodactyloid. The new pterosaur trackway contributes to the growing database of pterosaurian ichnites in Asia. -
A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, Usa
A FOSSIL LOCALITY PREDICTIVE MODEL FOR THE EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION, UTAH, USA A THESIS PRESENTED TO THE DEPARTMENT OF HUMANITIES AND SOCIAL SCIENCE IN CANDIDACY FOR THE DEGREE OF MASTER OF SCIENCE By DANIEL BURK NORTHWEST MISSOURI STATE UNIVERSITY MARYVILLE, MISSOURI OCTOBER, 2014 FOSSIL LOCALITY PREDICTIVE MODEL A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, USA Daniel Burk Northwest Missouri State University THESIS APPROVED Thesis Advisor, Dr. Yi-Hwa Wu Date Dr. Ming-Chih Hung Date Dr. John P. Pope Date Dean of Graduate School Date A Fossil Locality Predictive Model for the Early Cretaceous Cedar Mountain Formation, Utah, USA Abstract Hard work and chance are nearly always among the deciding factors in finding new, important, and productive paleontological localities. Fossil locality predictive models have the potential to reduce unproductive field time and maximize hard work thus increasing the chances researchers have to find important localities. This study uses remotely sensed data to design and test a fossil locality predictive model for the Early Cretaceous Cedar Mountain Formation. Landsat 8 OLI/TIRS data from known localities were summarized, reclassified and used in a weighted suitability analysis to categorize fossil locality potential of the study area. Field work was conducted to test model functionality. Field observations were used to refine the weighted suitability analysis. Landsat 8 OLI/TIRS data alone offers a less accurate prescription of fossil locality potential. Additional physical and environmental factors play a role in determining the chance of finding fossils. Slope degree and aspect data from known localities were summarized and analyzed to further refine the model.