Permophiles Issue #36 2000 EXECUTIVE NOTES Notes from the SPS Secretary Henderson Will Accept Them Until December 15
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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. -
1 Revision 2 1 K-Bentonites
1 Revision 2 2 K-Bentonites: A Review 3 Warren D. Huff 4 Department of Geology, University of Cincinnati, Cincinnati, OH 45221 USA 5 Email: [email protected] 6 Keywords: K-bentonite, bentonite, tephra, explosive volcanism, volcanic ash 7 Abstract 8 Pyroclastic material in the form of altered volcanic ash or tephra has been reported and described 9 from one or more stratigraphic units from the Proterozoic to the Tertiary. This altered tephra, 10 variously called bentonite or K-bentonite or tonstein depending on the degree of alteration and 11 chemical composition, is often linked to large explosive volcanic eruptions that have occurred 12 repeatedly in the past. K-bentonite and bentonite layers are the key components of a larger group of 13 altered tephras that are useful for stratigraphic correlation and for interpreting the geodynamic 14 evolution of our planet. Bentonites generally form by diagenetic or hydrothermal alteration under 15 the influence of fluids with high Mg content and that leach alkali elements. Smectite composition is 16 partly controlled by parent rock chemistry. Studies have shown that K-bentonites often display 17 variations in layer charge and mixed-layer clay ratios and that these correlate with physical 18 properties and diagenetic history. The following is a review of known K-bentonite and related 19 occurrences of altered tephra throughout the time scale from Precambrian to Cenozoic. 20 Introduction 21 Volcanic eruptions are often, although by no means always, associated with a profuse output 22 of fine pyroclastic material, tephra. Tephra is a term used to describe all of the solid material 23 produced from a volcano during an eruption (Thorarinsson, 1944). -
The Biopolitical Elements in Yan Lianke's Fiction Worlds
Eastern Illinois University The Keep Masters Theses Student Theses & Publications 2018 The iopB olitical Elements in Yan Lianke's Fiction Worlds Xiaoyu Gao Eastern Illinois University This research is a product of the graduate program in English at Eastern Illinois University. Find out more about the program. Recommended Citation Gao, Xiaoyu, "The iopoB litical Elements in Yan Lianke's Fiction Worlds" (2018). Masters Theses. 3619. https://thekeep.eiu.edu/theses/3619 This is brought to you for free and open access by the Student Theses & Publications at The Keep. It has been accepted for inclusion in Masters Theses by an authorized administrator of The Keep. For more information, please contact [email protected]. The GraduateSchool � EA'ill 11.'1I·��-- h l:'ll\'tll\11'\' Thesis Maintenance and Reproduction Certificate FOR: Graduate candidates Completing Theses in PartialFulfillment of the Degree Graduate Faculty Advisors Directing the Theses RE: Preservation, Reproduction, and Distribution of Thesis Research Preserving, reproducing, and distributing thesis research is an important part of Booth Library's responsibility to provide access to scholarship. In order to further this goal, Booth Library makes all graduate theses completed as part of a degree program at Eastern Illinois University available for personal study, research, and other not-for profit educational purposes. Under 17 U.S.C. § 108, the library may reproduce and distribute a copy without infringing on copyright; however, professional courtesy dictates that permission be requested from the author before doing so. Your signatures affirm the following: •The graduate candidate is the author of this thesis. •The graduate candidate retains the copyright and intellectual property rights associated with the original research, creative activity, and intellectual or artistic content of the thesis. -
Permophiles Issue
Contents Notes from the SPS Secretary ...........................................................................................................................1 Shen Shuzhong Notes from the SPS Chair ..................................................................................................................................2 Charles M. Henderson Meeting Report: Report on the Continental Siena Meeting, Italy, September 2006.....................................3 G. Cassinis, A. Lazzarotto, P. Pittau Working Group Report: Short report on 2005-2006 activities of the non-marine – marine correlation work- ing group of SPS ..................................................................................................................................................5 J.W. Schneider Report of SPS Working Group on “Using Permian transitional biotas as gateways for global correlation”7 Guang R. Shi International Permian Time Scale ...................................................................................................................10 Voting Members of the SPS ............................................................................................................................. 11 Submission guideline for Issue 49 ....................................................................................................................12 Reports: Ostracods (Crustacea) from the Permian-Triassic boundary interval of South China (Huaying Mountains, eastern Sichuan Province): paleo-oxygenation significance .......................................................12 -
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1973
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1973 GEOLOGICAL SURVEY BULLETIN 1395-A NOV1419/5 5 81 Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1973 By GEORGE V. COHEE and WILNA R. WRIGHT CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1395-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1975 66 01-141-00 oM UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Cohee, George Vincent, 1907 Changes in stratigraphic nomenclatures by the U. S. Geological Survey, 1973. (Contributions to stratigraphy) (Geological Survey bulletin; 1395-A) Supt. of Docs, no.: I 19.3:1395-A 1. Geology, Stratigraphic Nomenclature United States. I. Wright, Wilna B., joint author. II. Title. III. Series. IV. Series: United States. Geological Survey. Bulletin; 1395-A. QE75.B9 no. 1395-A [QE645] 557.3'08s 74-31466 [551.7'001'4] For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, B.C. 20402 Price 95 cents (paper cover) Stock Number 2401-02593 CONTENTS Page Listing of nomenclatural changes ______ _ Al Beulah Limestone and Hardscrabble Limestone (Mississippian) of Colorado abandoned, by Glenn R. Scott _________________ 48 New and revised stratigraphic names in the western Sacramento Valley, Calif., by John D. Sims and Andre M. Sarna-Wojcicki __ 50 Proposal of the name Orangeburg Group for outcropping beds of Eocene age in Orangeburg County and vicinity, South Carolina, by George E. Siple and William K. Pooser _________________ 55 Abandonment of the term Beattyville Shale Member (of the Lee Formation), by Gordon W. -
Meike International Holdings Limited 美克
Hong Kong Exchanges and Clearing Limited, The Stock Exchange of Hong Kong Limited (the “HKEx”) and the Securities and Futures Commission (the “SFC”) take no responsibility for the contents of this Web Proof Information Pack, make no representation as to its accuracy or completeness and expressly disclaim any liability whatsoever for any loss howsoever arising from or in reliance upon the whole or any part of the contents of this Web Proof Information Pack. Web Proof Information Pack of MEIKE INTERNATIONAL HOLDINGS LIMITED A1A1 LR8.02 美克國際控股有限公司 (Incorporated in the Cayman Islands with limited liability) WARNING This Web Proof Information Pack is being published as required by the HKEx/the SFC solely for the purpose of providing information to the public in Hong Kong. This Web Proof Information Pack is in draft form. The information contained in it is incomplete and is subject to change which could be material. By viewing this document, you acknowledge, accept and agree with Meike International Holdings Limited (the “Company”), any of its affiliates, sponsors, advisers and members of the underwriting syndicate that: (a) this Web Proof Information Pack is solely for the purpose of facilitating equal dissemination of information to investors in Hong Kong and not for any other purposes. No investment decision should be based on the information contained in this Web Proof Information Pack; (b) the posting of the Web Proof Information Pack or any supplemental, revised or replacement pages thereof on the HKEx’s website does not give rise to any obligation of the Company, any of its affiliates, sponsors, advisers or members of the underwriting syndicate to proceed with an offering in Hong Kong or any other jurisdiction. -
Cephalopod Aptychi from Los Loyos Limestone, Madera Group (Middle
wise not a probable candidate. Glyptosaurus sensustricto (Sullivan, 1.979)seems the most aptychifrom reasonabletaxonomic assignment based on Gephalopod tubercular arrangement and osteoderm size. LosMoyos Limestoro, Madera Group Biostratigraphic and biogeographic significance The discovery of cI. Glyptosaurusin the (MiddlePennsyluanian), BacaFormation of south-central New Mexico is significant in three ways: 1.)Glyptosaurus is a late Wasatchian-Uintan genus known from nearAlbuquerque, New Mexico Colorado, Utah, and Wyoming (Sullivan, 1979);its occurrence in the Baca Formation by Barry S. Kues,Department of Geology, University of New Mexico, Albuquerque, NM near Carthageis consistent with, though not conclusive proof of, the Bridgerian-age assignmentmade by Lucasand others (1982). Introduction sils, to discuss their relationships with the 2) Other glyptosaurs known from New Mex- cephalopod conchs in the fauna, and to pro- ico are from the San Basin and are of Aptychi are bivalved structures that prob- fuan vide a brief summary of the fauna itself, Paleoceneand early Eocene age (Sullivan, ably functioned asopercula on somecephalo- which includes some taxa not previously re- 1981);therefore, UNM BE-012 is the pods (see Yochelson,1983), although they ported from the Pennsylvanian of New Mex- youngest glyptosaur known from New Mex- have also been interpreted as cephalopod ico. Specimensmentioned and illustrated ico. 3) To our knowledge, UNM BE-012also lower jaws (Morton, 1981).Aptychi are here are in the University of New Mexico representsthe most southerly occurrenceof a known from many genera of Mesozoic Department of Geology paleontology collec- specimenthat apparently pertains to Glypto- ammonoids (Arkell, 1,957,p. L82) but are ex- tions and have been assigned UNM num- saurus. -
Final Program of CCC2020
第三十九届中国控制会议 The 39th Chinese Control Conference 程序册 Final Program 主办单位 中国自动化学会控制理论专业委员会 中国自动化学会 中国系统工程学会 承办单位 东北大学 CCC2020 Sponsoring Organizations Technical Committee on Control Theory, Chinese Association of Automation Chinese Association of Automation Systems Engineering Society of China Northeastern University, China 2020 年 7 月 27-29 日,中国·沈阳 July 27-29, 2020, Shenyang, China Proceedings of CCC2020 IEEE Catalog Number: CFP2040A -USB ISBN: 978-988-15639-9-6 CCC2020 Copyright and Reprint Permission: This material is permitted for personal use. For any other copying, reprint, republication or redistribution permission, please contact TCCT Secretariat, No. 55 Zhongguancun East Road, Beijing 100190, P. R. China. All rights reserved. Copyright@2020 by TCCT. 目录 (Contents) 目录 (Contents) ................................................................................................................................................... i 欢迎辞 (Welcome Address) ................................................................................................................................1 组织机构 (Conference Committees) ...................................................................................................................4 重要信息 (Important Information) ....................................................................................................................11 口头报告与张贴报告要求 (Instruction for Oral and Poster Presentations) .....................................................12 大会报告 (Plenary Lectures).............................................................................................................................14 -
Salinas Pueblo Missions National Monument U.S
National Park Service Geologic Map of Salinas Pueblo Missions National Monument U.S. Department of the Interior Geologic Resources Inventory New Mexico Natural Resource Stewardship and Science Pa NPS Boundary Qpy Peidmont alluvium, younger deposits (upper Pleistocene to Holocene) Pu Arroyo de Alamillo and Abo Formations, undifferentiated (Lower Permian (Leonardian and Wolfcampian)) Qgm Qayo Stream alluvium, younger subunit (uppermost Pleistocene to Holocene) Pa Abo Formation (Lower Permian (Leonardian and Wolfcampian)) Infrastructure Qae Stream alluvium and eolian sand (late Pleistocene to late Holocene) Pal Abo Formation, lower units (Lower Permian (Leonardian and Wolfcampian)) 55 point of interest roads Qaam Abo Arroyo stream terrace, intermediate deposit (upper Pleistocene) Yeso Formation Qa Pa Point Geologic Units Pym Mesa Blanca Member (Lower Permian (Leonardian)) Qgm Qgm Gravel derived from Manzano Mountains sources (Pleistocene) # Tim - Mafic dike rocks (Tertiary) Pa Pyt Torres Member (Lower Permian (Leonardian)) Folds Qgc Gravel derived from Chupadera Mesa sources (Pleistocene) Madera Group Quarai anticline, approximate M Qls Landslide deposits (Pleistocene) Pb Bursum Formation (Lower Permian) Qa syncline, approximate Qca Colluvium and alluvium, undivided (middle to upper Pleistocene) Sites of SalinasSites Pueblo of Missions Salinas National Monument Pueblo Missions National Monument Qgm O PNm5 Wild Cow Formation, middle and upper part of La Casa Member (Upper Pennsylvanian (Virgilian)) Pu Faults: Dashed where approximate, dotted -
Permian (Artinskian to Wuchapingian) Conodont Biostratigraphy in the Tieqiao Section, Laibin Area, South China
Permian (Artinskian to Wuchapingian) conodont biostratigraphy in the Tieqiao section, Laibin area, South China Y.D. Suna, b*, X.T. Liuc, J.X. Yana, B. Lid, B. Chene, D.P.G. Bondf, M.M. Joachimskib, P.B. Wignallg, X.L. Laia a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China b GeoZentrum Nordbayern, Universität Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany c Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China d Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Ministry of Land and Resources, Guangzhou, 510075, China e State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, 39 East Beijing Road, Nanjing, 210008, R.P. China f School of Environmental Sciences, University of Hull, Hull HU6 7RX, UK g School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK *Corresponding authors Email: [email protected] (Y.D. Sun) © 2017, Elsevier. Licensed under the Creative Commons Attribution- NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/ licenses/by-nc-nd/4.0/ 1 Abstract Permian strata from the Tieqiao section (Jiangnan Basin, South China) contain several distinctive conodont assemblages. Early Permian (Cisuralian) assemblages are dominated by the genera Sweetognathus, Pseudosweetognathus and Hindeodus with rare Neostreptognathodus and Gullodus. Gondolellids are absent until the end of the Kungurian stage—in contrast to many parts of the world where gondolellids and Neostreptognathodus are the dominant Kungurian conodonts. A conodont changeover is seen at Tieqiao and coincided with a rise of sea level in the late Kungurian to the early Roadian: the previously dominant sweetognathids were replaced by mesogondolellids. -
1 Contemporary Ethnic Identity of Muslim Descendants Along The
1 Contemporary Ethnic Identity Of Muslim Descendants Along the Chinese Maritime Silk Route Dru C Gladney Anthropology Department University of South Carolina U.S.A At the end of five day's journey, you arrive at the noble-and handsome city of Zaitun [Quanzhoui] which has a port on the sea-coast celebrated for the resort of shipping, loaded with merchandise, that is afterwards distributed through every part of the province .... It is indeed impossible to convey an idea of the concourse of merchants and the accumulation of goods, in this which is held to be one of the largest and most commodious ports in the world. Marco Polo In February 1940, representatives from the China Muslim National Salvation society in Beijing came to the fabled maritime Silk Road city of Quanzhou, Fujian, known to Marco Polo as Zaitun, in order to interview the members of a lineage surnamed "Ding" who resided then and now in Chendai Township, Jinjiang County. In response to a question on his ethnic background, Mr. Ding Deqian answered: "We are Muslims [Huijiao reo], our ancestors were Muslims" (Zhang 1940:1). It was not until 1979, however, that these Muslims became minzu, an ethnic nationality. After attempting to convince the State for years that they belonged to the Hui nationality, they were eventually accepted. The story of the late recognition of the members of the Ding lineage in Chendai Town and the resurgence of their ethnoreligious identity as Hui and as Muslims is a fascinating reminder that there still exist remnants of the ancient connections between Quanzhou and the Western Regions, the origin points of the Silk Road. -
Paper Number: 4008
Paper Number: 4008 Characterization of conodont biostratigraphy in the basal Moscovian boundary interval at the Naqing section, Loudian, Guizhou, South China Lambert, L. L.1, Qi, Y. P.2, Nemyrovska, T. I.3, Wang, X. D.2, Hu, K. Y.2, and Wang, Q. L.2 1Geological Sciences, University of Texas at San Antonio, One UTSA Circle, San Antonio, TX 78249, USA [email protected] 2State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, PR China 3Institute of Geological Sciences, National Academy of Sciences of Ukraine, O. Gonchar Str. 55-b, 01601 Kiev, Ukraine ___________________________________________________________________________ A major criterion for selecting a Global Stratotype Section and Point (GSSP) is to demonstrate depositional continuity. Depositional continuity is most often accepted where there is a transitional morphocline from an ancestral species to its descendent. The GSSP is then selected to correspond with the phylogenetic first occurrence of the descendent species. Ideally, strata elsewhere are subsequently correlated with the GSSP using the local first appearance of the descendent species, or by other taxa associated with the GSSP providing supplementary biostratigraphic data. Any other stratigraphic methods can be used for correlation once the GSSP has been ratified by the International Union of Geological Sciences Commission on Stratigraphy. Multiple conodont lineages with complete transitional morphologies characterize the Bashkirian- Moscovian boundary interval in the Naqing section. The presence of all these chronoclines through the section demonstrates depositional continuity at Naqing, and provides numerous possible conodont- based levels available for selecting a basal Moscovian GSSP.