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Coal and Francis Creek Shale
University of Pennsylvania ScholarlyCommons Department of Earth and Environmental Departmental Papers (EES) Science January 1970 A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale R. A. Peppers Illinois State Geological Survey Hermann W. Pfefferkorn University of Pennsylvania, [email protected] Follow this and additional works at: https://repository.upenn.edu/ees_papers Recommended Citation Peppers, R. A., & Pfefferkorn, H. W. (1970). A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale. Retrieved from https://repository.upenn.edu/ees_papers/18 This material has been published in Smith, W.H., Nance, R.B., Hopkins, Johnson, R.G., and Shabica, C.W. Depositional environments in parts of the Carbondale formation, western and northern Illinois: Francis Creek Shale and associated strata and Mazon Creek biota, Illinois State Geological Survey Field Guidebook Series, No. 8, p. 61-74, 1970 NOTE: At the time of publication, author Hermann W. Pfefferkorn was affiliated with the Illinois State Geological Survey. Currently (September 2005) he is a faculty member in the Department of Earth and Environmental Science at the University of Pennsylvania. This paper is posted at ScholarlyCommons. https://repository.upenn.edu/ees_papers/18 For more information, please contact [email protected]. A comparison of the floras of the Colchester (No. 2) Coal and Francis Creek Shale Abstract Abundant data from spore studies of the Colchester (no. 2) Coal Member and from investigations of plant compressions in the Francis Creek Shale provide an opportunity to compare the flora of the coal with that of the overlying shale in the northeastern part of the Illinois Basin. -
Orta Toroslar'da Konodont Biy Ostratigrafisi(1 )
Türkiye Jeoloji Kurumu Bülteni, e. 20, 35-48, Şubat 1977 Bulîetin of the Geölogical Boclety of Turkey, v. 20, 35-48, February 1977 Orta Toroslar'da konodont biy ostratigrafisi(1 ) Conodontbiostratigra/phy in the Middle Taurus ÎSMET GEDİK Jeoloji Bölümü, Karadeniz Teknik Üniversitesi, Trabzon ÖZ: Çalışılan bölgede, Kambriyen-Triyas arasına ait konodont faunası saptanmış ve kısaca tanıtılmıştır. Metamorfik Alan- ya Masifinin bir nap şeklinde Sedre Triyas'mm üzerine geldiği ve bunun da bir tektonik pencere olarak görüldüğü görü- şüne varılmıştır. Hadimopanella oezgueli n. gen. n. sp. (incertae sedis) ve üç yeni konodont türü bulunmuştur. ABSTRACT: in the area studied Cambrian to Triassie systems are distinguished by the use of conodonts and their fauna is deseribed briefly. it is believed that the metamorphic Alanya massif overlays the Sedre Triassie as a nappe, forming a teetonic window. Hadimopanella oezgueli n. gen. n. sp. (İncertae sedis) and three new conodont speeies are established. (1) Bu yazı Türkiye Jeoloji Kurumu 30. Bilimsel Kurultayında bildiri olarak sunulmuştur. 36 GEDÎK GİRİŞ ve Monod, 1970). İçlerinde bazı trilobit lanmasmdon oluşan ve kalınlığı 1000 m parçalarına rastlanmıştır. Üste doğru kil yi aşan Seydişehir Formasyonuna geçti- Bu çalışma, özellikle son 20 yılda oranı gittikçe artarak, yaklaşık 50 m ği görülür. Bu formasyonun ilk 50 m lik büyük stratigrafik önem kazanan ve ge- kalınlığındaki kırmızımsı - morumsu, alt düzeylerinde bulunan kireçtaşı mer- niş çapta jeolojik formasyonların korre- yumrulu kireçtaşlarına geçilir. Bu dü- ceklerinden elde eddlen lasyonunda kullanılan konodontlardan zey içinde bol olarak Conocoryphe, Oneotodus tenu4s yararlanarak, ülkemizin bir bölgesinin Öoryneocochus, vb. gibi Orta Kambriyen stratigrafisini biraz daha aydınlığa ka- Fumishina furnishi yaşındaki tribolitlere ve akrotretid bra- Hertzima bisulcata vuşturmak ve dolayısiyle jeolojik yapısı- kiyopodlara rastlanılmıştır. -
Bedrock Geology of Carbondale Quadrangle
BEDROCK GEOLOGY OF CARBONDALE QUADRANGLE Prairie Research Institute JACKSON AND WILLIAMSON COUNTIES, ILLINOIS Illinois Geologic Quadrangle Map ILLINOIS STATE GEOLOGICAL SURVEY IGQ Carbondale-BG W. John Nelson 2013 89°15' 12'30" 10' 89°07'30" 720 000FEET (IL E) 3 000mE 3 3 3 3 3 3 R. 1 W. 2 590 000 FEET (IL W) R. 1 E. 3 37°45' 03 04 05 06 07 08 10 12 37°45' 51 4180 7 8 9 10 11 12 7 8 000m &c 4180 N 13 &c Creek d r a & h t c m r C CG 508 O &c k" m r a U.S. 366 41 b e" 79 Fish and 18 17 16 15 &t 18 17 &c 13 Wildlife Ho g an 14 Po i n t 4179 m O b r a c r h Pine C a Lo n g Vi ew Island 390000 r 13 d Park FEET (IL E) Sk" 98 390 000 Ck" 322 k" 97 FEET (IL W) m 152 E 4178 k e" K r o A F L 41 ¿ S 273 78 k" PO D ¿ m R e 13 A l C t H t r i CARBONDALE C L R EXPLANATION O 19 22 19 20 20 23 24 B m A 21 R ¿ C Holocene sm Surface mine 4177 k" 105 &t ¿ m c s ¿ 41 e &t 77 Univ ersity l i &c Carbondale Formation School P m » m Desmoinesian Tradewater Formation s s, Stonefort Limestone Member m m, Murphysboro Coal Member Pennsylvanian c c, Curlew Member Southern Illinois ¿ University S 62 &t k" &t-mb Murray Bluff Sandstone Member » &t s 4176 Atokan ¿ &t &t-o olive shale member 27 4176 29 &t-g Grindstaff Sandstone Member 29 C s am e 28 30 pus Lak À 26 25 30 42'30" À 42'30" ¿ 270 m À k" S 1201 &t 290 270 Ü k" k" ªNorth uthern Hill s m So 4175 s k"317 k" 137 s 4175 &t-mb ¿ Symbols Marberry Arboretum 40 Strike and dip of bedding; number indicates degree of dip Carbondale &t r ¿ Reservoi m Horizontal bedding &t r sm ¿ 31 Evergreen Terrace C 32 Vertical joints 4174 31 34 35 36 32 k r 33 ¿ c o ¿ » Shaft mine Sk" 250 F 51 4174 ¿ S ¿ y ¿ Slope mine &t-mb c a m o ¿ À » r m Drift mine c e s m le ¿ ¿ i & ¿ t-mb m ¿ P sm ( À T. -
The Unique Devonian of Immouzer-Du-Kandar (Middle Atlas Basement) – Biostratigraphy, Faunas, and Facies Development
Aboussalam & al. Devonian of Immouzer-du-Kandar The unique Devonian of Immouzer-du-Kandar (Middle Atlas basement) – biostratigraphy, faunas, and facies development ZHOR SARAH ABOUSSALAM, RALPH THOMAS BECKER, JULIA RICHTER, SVEN HARTENFELS, AHMED EL HASSANI & STEPHAN EICHHOLT Fig. 1: View (from the hill at Douar Ahmed-ben-Mellouk) on Devonian exposures of Immouzer-du-Kandar (hill rising from Chabat el Jenanet, Sections C2 and C3 of CYGAN et al. 1990), our Section C4, with outcrop of the lower Emsian conglomerate (Chabat Jenanet Formation) along and above the track, faulted upper Emsian to lower Givetian limestones in the lower slope (new Ahmed-ben-Mellouk Formation), the reef breccia forming a small terrace ca. 2/3 upwards, and the Famennian upper slope (new Chabat el Hallouf Formation, Section C5) towards the top. The slope to the left (NNE) is occupied by Triassic red beds. Section numbers are marked in circles. 1. Introduction Mesozoic Middle Atlas, with the best and most important outcrops in the tectonic window The Middle Atlas divides the Moroccan (“boutonnière”) at Immouzer-du-Kandar, ca. Meseta into the Western and Eastern Meseta, 40 km S of Fès. The wooded Jebel Kandar to which differ strongly in the Devonian in terms the SW is a more than 1600 m high mountain of facies and synsedimentary structural built of Jurassic strata (Fig. 2). Fossiliferous geology (e.g., overviews of EL HASSANI & Ordovician to Lower Carboniferous BENFRIKA 1995, 2000). There is restricted formations crop out to the NW, from Dour knowledge of the Palaeozoic basement of the Rouda towards the SE, the Chabat el Jenanet, Hassan II Academy of Science and Technology Frontiers in Science and Engineering - Vol. -
Conodonts and Foraminifers
Journal of Asian Earth Sciences 108 (2015) 117–135 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes An integrated biostratigraphy (conodonts and foraminifers) and chronostratigraphy (paleomagnetic reversals, magnetic susceptibility, elemental chemistry, carbon isotopes and geochronology) for the Permian–Upper Triassic strata of Guandao section, Nanpanjiang Basin, south China ⇑ Daniel J. Lehrmann a, , Leanne Stepchinski a, Demir Altiner b, Michael J. Orchard c, Paul Montgomery d, Paul Enos e, Brooks B. Ellwood f, Samuel A. Bowring g, Jahandar Ramezani g, Hongmei Wang h, Jiayong Wei h, Meiyi Yu i, James D. Griffiths j, Marcello Minzoni k, Ellen K. Schaal l,1, Xiaowei Li l, Katja M. Meyer l,2, Jonathan L. Payne l a Geoscience Department, Trinity University, San Antonio, TX 78212, USA b Department of Geological Engineering, Middle East Technical University, Ankara 06531, Turkey c Natural Resources Canada-Geological Survey of Canada, Vancouver, British Columbia V6B 5J3, Canada d Chevron Upstream Europe, Aberdeen, Scotland, UK e Department of Geology, University of Kansas, Lawrence, KS 66045, USA f Louisiana State University, Baton Rouge, LA 70803, USA g Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA h Guizhou Geological Survey, Bagongli, Guiyang 550011, Guizhou Province, China i College of Resource and Environment Engineering, Guizhou University, Caijiaguan, Guiyang 550003, Guizhou Province, China j Chemostrat Ltd., 2 Ravenscroft Court, Buttington Cross Enterprise Park, Welshpool, Powys SY21 8SL, UK k Shell International Exploration and Production, 200 N. Dairy Ashford, Houston, TX 77079, USA l Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA article info abstract Article history: The chronostratigraphy of Guandao section has served as the foundation for numerous studies of the Received 13 October 2014 end-Permian extinction and biotic recovery in south China. -
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Acta Geologica Polonica, Vol. 50 (2000), No. 1, pp. 67-97 Revision of ammonoid biostratigraphy in the Frasnian (Upper Devonian) of the Southern Timan (Northeast Russian Platform) R. THOMAS BECKER1, MICHAEL R. HOUSE2, VLADIMIR V. MENNER3 & N. S. OVNATANOVA4 1 Museum für Naturkunde der Humboldt-Universität zu Berlin, Invalidenstr. 43, D-10115 Berlin, Germany. E-mail: [email protected] 2 School of Ocean and Earth Science, Southampton Oceanography Centre, European Way, Southampton, SO 14 3ZH, U.K. 3 Institute of Geology and Exploitation of Combustible Fuel, Fersman 50, Moscow 117312, Russian Federation 4 All-Russia Research Geological Oil Prospecting Institute, Shosse Entuziastov 36, Moscow 105819, Russian Federation ABSTRACT: BECKER, R.T., HOUSE, M.R., MENNER, V.V. & OVNATANOVA, N.S. (2000). Revision of ammonoid biostratig- raphy in the Frasnian (Upper Devonian) of the Southern Timan (Northeast Russian Platform). Acta Geologica Polonica, 50 (1), 67-97, Warszawa. New field work in outcrops of the Ukhta Region (Southern Timan) together with the re-exanimation of former collections allows a detailed revision of the ammonoid zonation in one of the classical Frasnian regions of Russia. There is a total of 47 species, 18 of which are new or recorded for the first time from the region. The latter applies to representatives of Linguatornoceras, Phoenixites, Aulatornoceras s.str. and Acantho- clymenia. New taxa are Chutoceras manticoides n.gen. n.sp. and Linguatornoceras yudinae n.sp. In the Ust’yarega Formation regional Hoeninghausia nalivkini, Timanites keyserlingi and Komioceras stuckenber- gi Zones can be recognized which correlate with the international Frasnian divisions UD I-B/C. -
Conodonts in Ordovician Biostratigraphy
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Archivio istituzionale della ricerca - Università di Modena e Reggio Emilia 1 Conodonts in Ordovician biostratigraphy STIG M. BERGSTRÖM AND ANNALISA FERRETTI Conodonts in Ordovician biostratigraphy The long time interval after Pander’s (1856) original conodont study can in terms of Ordovician conodont biostratigraphic research be subdivided into three periods, namely the Pioneer Period (1856-1955), the Transition Period (1955-1971), and the Modern Period (1971-Recent). During the pre-1920s, the few published conodont investigations were restricted to Europe and North America and were not concerned about the potential use of conodonts as guide fossils. Although primarily of taxonomic nature, the pioneer studies by Branson & Mehl, Stauffer, and Furnish during the 1930s represent the beginning of the use of conodonts in Ordovician biostratigraphy. However, no formal zones were introduced until Lindström (1955) proposed four conodont zones in the Lower Ordovician of Sweden, which marks the end of the Pioneer Period. Because Lindström’s zone classification was not followed by similar work outside Baltoscandia, the time interval up to the late 1960s can be regarded as a Transition Period. A milestone symposium volume, entitled ‘Conodont Biostratigraphy’ and published in 1971, 2 summarized much new information on Ordovician conodont biostratigraphy and is taken as the beginning of the Modern Period of Ordovician conodont biostratigraphy. In this volume, the Baltoscandic Ordovician was subdivided into named conodont zones whereas the North American Ordovician succession was classified into a series of lettered or numbered Faunas. Although most of the latter did not receive zone names until 1984, this classification has been used widely in North America. -
From the Upper Triassic (Norian) of Northern Carnic Pre-Alps (Udine, Northeastern Italy)
GORTANIA. Geologia,GORTANIA Paleontologia, Paletnologia 35 (2013) Geologia, Paleontologia, Paletnologia 35 (2013) 11-18 Udine, 10.IX.2014 ISSN: 2038-0410 Alessandro Garassino ACANTHOCHIRANA TRIASSICA N. SP. Günter Schweigert Giuseppe Muscio AND ANTRIMPOS COLETTOI N. SP. (DECAPODA: AEGERIDAE, PENAEIDAE) FROM THE UPPER TRIASSIC (NORIAN) OF NORTHERN CARNIC PRE-ALPS (UDINE, NORTHEASTERN ITALY) Acanthochirana TRIASSICA N. SP. E AntrimPOS COLETTOI N. SP. (DECAPODA: AEGERIDAE, PENAEIDAE) DAL TRIASSICO SUPERIORE (NORICO) DELLA PREALPI CARNICHE SETTENTRIONALI (UDINE, ITALIA NORDORIENTALE) Riassunto breve - I crostacei decapodi del Triassico superiore (Norico) della Dolomia di Forni sono stati descritti da Ga- rassino et al. (1996). La recente scoperta di un piccolo campione, rivenuto nella Valle del Rio Seazza e in quella del Rio Rovadia, ha permesso un aggiornamento relativo ai crostacei decapodi delle Prealpi Carniche. Gli esemplari studiati sono stati assegnati a Acanthochirana triassica n. sp. (Aegeridae Burkenroad, 1963) e Antrimpos colettoi n. sp. (Penaeidae Rafinesque, 1815). Acanthochirana triassica n. sp. estende il range stratigrafico di questo genere nel Triassico superiore, mentre Antrimpos colettoi n. sp. rappresenta la seconda specie di questo genere segnalata nel Triassico superiore d’Italia. La scoperta di queste due nuove specie incrementa il numero delle specie di peneidi conosciuti nel Norico dell’alta Val Ta- gliamento (Prealpi Carniche settentrionali). Parole chiave: Crustacea, Decapoda, Aegeridae, Penaeidae, Triassico superiore, Prealpi Carniche. Abstract - The decapod crustaceans from the Upper Triassic (Norian) of the Dolomia di Forni Formation were reported by Garassino et al. (1996). The recent discovery of a small sample from this Formation between Seazza and Rovadia brooks allowed updating the decapod assemblages from the Norian of Carnic Pre-Alps. -
Calcium Stable Isotopes Place Devonian Conodonts As First Level Consumers V
Calcium stable isotopes place Devonian conodonts as first level consumers V. Balter, J.E. Martin, T. Tacail, G. Suan, Sabrina Renaud, Catherine Girard To cite this version: V. Balter, J.E. Martin, T. Tacail, G. Suan, Sabrina Renaud, et al.. Calcium stable isotopes place Devonian conodonts as first level consumers. Geochemical Perspectives Letters, European Assoication of Geochemistry, 2019, 10, pp.36-39. 10.7185/geochemlet.1912. hal-02112869 HAL Id: hal-02112869 https://hal.archives-ouvertes.fr/hal-02112869 Submitted on 27 Apr 2019 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. © 2019 The Authors Published by the European Association of Geochemistry Calcium stable isotopes place Devonian conodonts as first level consumers V. Balter1*, J.E. Martin1, T. Tacail2, G. Suan1, S. Renaud3, C. Girard4 Abstract doi: 10.7185/geochemlet.1912 Conodont animals are an extinct group of jawless vertebrates whose hard parts, also known as conodont elements, represent the earliest evidence of a mineralised skeleton in the vertebrate lineage. Conodont elements are interpreted as parts of a feeding apparatus, which together with the presence of eyes and microwear patterns, support the controversial hypothesis that conodont animals were macrophagous predators and/or scavengers. -
CONODONTS of the MOJCZA LIMESTONE -.: Palaeontologia Polonica
CONODONTS OF THE MOJCZA LIMESTONE JERZY DZIK Dzik, J. 1994. Conodonts of the M6jcza Limestone. -In: J. Dzik, E. Olemp ska, and A. Pisera 1994. Ordovician carbonate platform ecosystem of the Holy Cross Moun tains. Palaeontologia Polonica 53, 43-128. The Ordovician organodetrital limestones and marls studied in outcrops at M6jcza and Miedzygorz, Holy Cross Mts, Poland, contains a record of the evolution of local conodont faunas from the latest Arenig (Early Kundan, Lenodus variabilis Zone) to the Ashgill (Amorphognathus ordovicicus Zone), with a single larger hiatus corre sponding to the subzones from Eop/acognathus pseudop/anu s to E. reclinatu s. The conodont fauna is Baltic in general appearance but cold water genera , like Sagitto dontina, Scabbardella, and Hamarodus, as well as those of Welsh or Chinese af finities, like Comp/exodus, Phragmodus, and Rhodesognathu s are dominant in par ticular parts of the section while others common in the Baltic region, like Periodon , Eop/acognathus, and Sca/pellodus are extremely rare. Most of the lineages continue to occur throughout most of the section enabling quantitative studies on their phyletic evolut ion. Apparatuses of sixty seven species of thirty six genera are described and illustrated. Phyletic evolution of Ba/toniodus, Amorphognathu s, Comp/exodus, and Pygodus is biometrically documented. Element s of apparatu ses are homolog ized and the standard notation system is applied to all of them. Acodontidae fam. n., Drepa nodus kie/censis sp. n., and D. santacrucensis sp. n. are proposed . Ke y w o r d s: conodonts, Ordovici an, evolut ion, taxonomy. Jerzy Dzik, Instytut Paleobiologii PAN, A/eja Zwirk i i Wigury 93, 02-089 Warszawa , Poland. -
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 -
Conodont Stratigraphy of a Highly Tectonised Silurian-Devonian Section in the San Basilio Area (SE Sardinia, Italy)
Bollettino della Societa Paleontologica Italiana 40 (3), 2001 ISSN 0375-7633 Modena, Dicembre 2001 Conodont stratigraphy of a highly tectonised Silurian-Devonian section in the San Basilio area (SE Sardinia, Italy) Carlo CORRADINI F rancesco LEONE Alfredo Loi Enrico SERPAGLI Dipartimento del Museo di Paleobiologia Dipartimento di Scienze della Terra Dipartimento del Museo di Paleobiologia e dell'Orto Botanico Universita di Cagliari e dell'Orto Botanico Universidt di Modena e Reggio Emilia Universita di Modena e Reggio Emilia KEYWORDS- Conodonts, Biostratigraphy, Tectonics, Silurian, Devonian, SE Sardinia. ABSTRACT- Several conodont species belonging to five "late Silurian biozones (Ancoradella ploeckensis, Polygnathoides siluricus, Ozarkodina crispa, Ozarkodina remscheidensis, Oulodus elegans detortus) and four Early and Late Devonian biozones (delta, pesavis, kitabicus-excavatus and Late rhenana) allow a better interpretation of stratigraphy and tectonics of the San Basilio area in western Gerrei. Frasnian sediments are documented for the first time in SE Sardinia. RIASSUNTO- [Stratigrafia a conodonti di una sezione forremente tettonizzata di eta Siluriano-Devoniano nell'area di San Basilio (Sardegna SE)] - Grazie alla biostratigrafia a conodonti viene interpretata la complessa tettonica di una sezione nell'area di San Basilio (Sardegna sud-orientale) e viene ricostruita la successione originaria. Sono documentate cinque biozone a conodonti del Siluriano superiore (Ancoradella eioeckensis, Polygnathoides siluricus, Ozarkodina crispa,