New Perspectives and Advances in the Understanding of Lower and Middle Paleozoic Epeiric Carbonate Depositional Systems of the Iowa and Illinois Basins
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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. -
Stratographic Coloumn of Iowa
Iowa Stratographic Column November 4, 2013 QUATERNARY Holocene Series DeForest Formation Camp Creek Member Roberts Creek Member Turton Submember Mullenix Submember Gunder Formation Hatcher Submember Watkins Submember Corrington Formation Flack Formation Woden Formation West Okoboji Formation Pleistocene Series Wisconsinan Episode Peoria Formation Silt Facies Sand Facies Dows Formation Pilot Knob Member Lake Mills Member Morgan Member Alden Member Noah Creek Formation Sheldon Creek Formation Roxana/Pisgah Formation Illinoian Episode Loveland Formation Glasford Formation Kellerville Memeber Pre-Illinoian Wolf Creek Formation Hickory Hills Member Aurora Memeber Winthrop Memeber Alburnett Formation A glacial tills Lava Creek B Volcanic Ash B glacial tills Mesa Falls Volcanic Ash Huckleberry Ridge Volcanic Ash C glacial tills TERTIARY Salt & Pepper sands CRETACEOUS "Manson" Group "upper Colorado" Group Niobrara Formation Fort Benton ("lower Colorado ") Group Carlile Shale Greenhorn Limestone Graneros Shale Dakota Formation Woodbury Member Nishnabotna Member Windrow Formation Ostrander Member Iron Hill Member JURASSIC Fort Dodge Formation PENNSYLVANIAN (subsystem of Carboniferous System) Wabaunsee Group Wood Siding Formation Root Formation French Creek Shale Jim Creek Limestone Friedrich Shale Stotler Formation Grandhaven Limestone Dry Shale Dover Limestone Pillsbury Formation Nyman Coal Zeandale Formation Maple Hill Limestone Wamego Shale Tarkio Limestone Willard Shale Emporia Formation Elmont Limestone Harveyville Shale Reading Limestone Auburn -
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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. -
A New Species of Tiaracrinus from the Latest Emsian of Morocco and Its Phylogeny
A new species of Tiaracrinus from the latest Emsian of Morocco and its phylogeny CHRISTIAN KLUG, KENNETH DE BAETS, CAROLE JUNE NAGLIK, and JOHNNY WATERS Klug, C., De Baets, K., Naglik, C.J., and Waters, J. 2014. A new species of Tiaracrinus from the latest Emsian of Morocco and its phylogeny. Acta Palaeontologica Polonica 59 (1): 135–145. We describe a new species of the unusual crinoid Tiaracrinus, T. jeanlemenni sp. nov. from the latest Emsian of the fa- mous mudmound locality Hamar Laghdad, Morocco. It differs from the previously known species in the higher number of ribs and the vaulted rib-fields, which is corroborated by the comparison of simple quantitative characters and ratios as well as by the results of a cluster analysis and a Principal Component Analysis. Based on the new material and the published specimens, we discuss the phylogeny of the genus and suggest that T. oehlerti and T. moravicus represent the ancestral forms of this small clade. Key words: Crinoidea, mudmounds, phylogeny, morphometry, symmetry, Devonian, Morocco. Christian Klug [[email protected]] and Carole J. Naglik [[email protected]], Paläontologisches Institut und Museum, Universität Zürich, Karl Schmid-Strasse 4, CH-8006 Zürich, Switzerland; Kenneth De Baets [[email protected]], GeoZentrum Nordbayern, Fachgruppe PaläoUmwelt, Universität Erlan- gen, Loewenichstr. 28, D-91054 Erlangen, Germany; Johnny Waters [[email protected]], Department of Geology, Appalachian State University, ASU Box 32067, Boone, NC 28608-2067, USA. Received 30 November 2011, accepted 4 June 2012, available online 6 June 2012. Copyright © 2014 C. Klug et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. -
Download Printable Version of the Geology and Why It Matters Story
Geology and Why it Matters This story was made with Esri's Story Map Journal. Read the interactive version on the web at http://arcg.is/qrG8W. The geology, landforms and land features are extremely important components of watersheds. They influence water quality, hydrology and watershed resiliency. Every watershed has critical areas where water interacts with and mobilizes contaminants, including non-point and point source contributions to surface water bodies. Where and how nutrients, bacteria and/or pesticides are mobilized to reach surface water can be better understood through a careful study of subsurface hydrology, or hydrogeology, which, according to the Iowa Geological and Water Survey Bureau, “allows better identification for sources, pathways and delivery points for groundwater and contaminants transported through the watershed’s subsurface geological plumbing system.” Diagram courtesy of Iowa DNR Iowa Geological Survey The highly developed karst topography and highly permeable bedrock layers of the Upper Iowa River increase the depth from which actively circulating groundwater contributes to stream flows, making an understanding of the hydrogeology even more important. Fortunately, the Iowa Geological and Water Survey Bureau completed a detailed mapping project of bedrock geologic units, key subsurface horizons, and surficial karst features in the Iowa portion of the Upper Iowa River watershed in 2011. The project “provides information on the subsurface part of the watersheds, which is necessary for evaluating the vulnerability of groundwater to nonpoint-source contamination, the groundwater contributions to surface water contamination, and for targeting best management practices for water quality improvements.” The map on the right shows the surface elevation of bedrock in the state of Iowa and the Upper Iowa River Watershed. -
Columnals (PDF)
2248 22482 2 4 V. INDEX OF COLUMNALS 8 Remarks: In this section the stratigraphic range given under the genus is the compiled range of all named species based solely on columnals assigned to the genus. It should be noted that this range may and often differs considerably from the range given under the same genus in Section I, because that range is based on species identified on cups or crowns. All other abbreviations and format follow that of Section I. Generic names followed by the type species are based on columnals. Genera, not followed by the type species, are based on cups and crowns as given in Section I. There are a number of unlisted columnal taxa from the literature that are indexed as genera recognized on cups and crowns. Bassler and Moodey (1943) did not index columnal taxa that were not new names or identified genera with the species unnamed. I have included some of the omissions of Bassler and Moodey, but have not made a search of the extensive literature specifically for the omitted citations because of time constraints. Many of these unlisted taxa are illustrated in the early state surveys of the eastern and central United States. Many of the columnal species assigned to genera based on cups or crowns are incorrect assignments. An uncertain, but significant, number of the columnal genera are synonyms of other columnal genera as they are based on different parts of the stem of a single taxon. Also a number of the columnal genera are synonyms of genera based on cups and crowns as they come from more distal parts of the stem not currently known to be associated with the cup or crown. -
Water Flow in the Silurian-Devonian Aquifer System, Johnson County, Iowa
Hydrogeology and Simulation of Ground- Water Flow in the Silurian-Devonian Aquifer System, Johnson County, Iowa By Patrick Tucci (U.S. Geological Survey) and Robert M. McKay (Iowa Department of Natural Resources, Iowa Geological Survey) Prepared in cooperation with The Iowa Department of Natural Resources – Water Supply Bureau City of Iowa City Johnson County Board of Supervisors City of Coralville The University of Iowa City of North Liberty City of Solon Scientific Investigations Report 2005–5266 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 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 materials contained within this report. Suggested citation: Tucci, Patrick and McKay, Robert, 2006, Hydrogeology and simulation of ground-water flow in the Silurian-Devonian aquifer system, Johnson County, Iowa: U.S. Geological Survey, Scientific Investigations -
An Examination of the Devonian Bedrock and Overlying Pleistocene Sediments at Messerly & Morgan Quarries, Blackhawk County, Iowa
FromFFrroomm OceanOOcceeaann tottoo Ice:IIccee:: AnAAnn examinationeexxaammiinnaattiioonn ofooff thetthhee DevonianDDeevvoonniiaann bedrockbbeeddrroocckk andaanndd overlyingoovveerrllyyiinngg PleistocenePPlleeiissttoocceennee sedimentssseeddiimmeennttss ataatt MesserlyMMeesssseerrllyy &&& MorganMMoorrggaann Quarries,QQuuaarrrriieess,, BlackBBllaacckk HawkHHaawwkk County,CCoouunnttyy,, IowaIIoowwaa Geological Society of Iowa ______________________________________ April 24, 2004 Guidebook 75 Cover photograph : University of Northern Iowa Professor and field trip leader Dr. Jim Walters points to a stromatoporoid-rich bed in the Osage Springs Member of the Lithograph City Formation at the Messerly Quarry, the first stop of this field trip From Ocean to Ice: An examination of the Devonian bedrock and overlying Pleistocene sediments at Messerly & Morgan Quarries, Blackhawk County, Iowa prepared and led by: James C. Walters Department of Earth Science University of Northern Iowa Cedar Falls, IA 50614 John R. Groves Department of Earth Science University of Northern Iowa Cedar Falls, IA 50614 Sherman Lundy 4668 Summer St. Burlington IA 52601 with contributions by: Bill J. Bunker Iowa Geological Survey Iowa Department Natural Resources Iowa City, Iowa 52242-1319 Brian J. Witzke Iowa Geological Survey Iowa Department Natural Resources Iowa City, Iowa 52242-1319 April 24, 2004 Geological Society of Iowa Guidebook 75 i ii Geological Society of Iowa TABLE OF CONTENTS From Ocean to Ice: An examination of the Devonian bedrock and overlying Pleistocene -
Appendix 3.Pdf
A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin Item Type Thesis or dissertation Authors Nicholls, Keith H. Citation Nicholls, K. (2019). A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin. (Doctoral dissertation). University of Chester, United Kingdom. Publisher University of Chester Rights Attribution-NonCommercial-NoDerivatives 4.0 International Download date 26/09/2021 02:37:15 Item License http://creativecommons.org/licenses/by-nc-nd/4.0/ Link to Item http://hdl.handle.net/10034/622234 International Chronostratigraphic Chart v2013/01 Erathem / Era System / Period Quaternary Neogene C e n o z o i c Paleogene Cretaceous M e s o z o i c Jurassic M e s o z o i c Jurassic Triassic Permian Carboniferous P a l Devonian e o z o i c P a l Devonian e o z o i c Silurian Ordovician s a n u a F y r Cambrian a n o i t u l o v E s ' i k s w o Ichnogeneric Diversity k p e 0 10 20 30 40 50 60 70 S 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 Number of Ichnogenera (Treatise Part W) Ichnogeneric Diversity 0 10 20 30 40 50 60 70 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 c i o 63 z 65 o e 67 a l 69 a 71 P 73 75 77 79 81 83 n 85 a i r 87 b 89 m 91 a 93 C Number of Ichnogenera (Treatise Part W) -
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. -
UPPER DEVONIAN CONODONTS ASSOCIATED with a LARGE PLACODERM FISH SKULL from the CANNING BASIN, WESTERN... Download
Rec. West. Aust. Mus. 1987,13 (4): 501-513 Upper Devonian conodonts associated with a large placoderm fish skull from the Canning Basin, Western Australia John A. Long* Abstract Conodonts retrieved from limestone encasing the skull of a large placoderm fish, from an unknown lo'cation in the south-eastern Canning Basin, indicate an age of mid-Famennian (toIIB) because of the concurrent presence of the following taxa: Nothognathella palmatiformis, Nothognathella sp. nov, A. Druce 1976,Palmatolepis glabra pectinata, P. quadrantinodosa inflexa, P. quadrantinodosa inflexoidea, P. marginifera s.s., Polygnathus triphyllatus, P. glaber s.s. and P. germanus s.s. The assemblage represents a palmatolepid-polygnathid biofacies dominated by palmatolepids, and is typical of muddy outer shelf to sandy inner shelf environ ments. The occurrence of certain taxa which have only been previously recorded in the Canning Basin from the Virgin Hills Formation, together with the lithology of the specimen, and palaeoecological information afforded by the conodonts, suggests that the specimen was derived from the uppermost section of the Virgin Hills Formation. Introduction A large dinichthyid placoderm fish skull has recently been described as a new genus, Westralichthys Long (1987) even though the exact location and lithological source of the specimen is unknown. A limited conodont fauna of 76 elements was recovered from dilute acetic acid preparation of the dinichthyid skull. The fauna contains a number of age diagnostic species which have been used to narrow the possible age and stratigraphic source of the specimen. It is significant that the conodonts indicate a much younger age for the skull than the well known lower Frasnian Gogo fish fauna (Gardiner and Miles 1975), also from the same region. -
Taxonomic Note Palmatolepis Spallettae, New Name for a Frasnian
Journal of Paleontology, 91(3), 2017, p. 578 Copyright © 2017, The Paleontological Society 0022-3360/15/0088-0906 doi: 10.1017/jpa.2017.21 Taxonomic Note Palmatolepis spallettae, new name for a Frasnian conodont species Gilbert Klapper,1 Thomas T. Uyeno,2 Derek K. Armstrong,3 and Peter G. Telford4 1Department of Earth and Planetary Sciences, Northwestern University, Evanston, Illinois 60208, USA 〈[email protected]〉 2Emeritus, Geological Survey of Canada, 3303-33rd St NW, Calgary, Alberta, T2L 2A7, Canada 〈[email protected]〉 3Ontario Geological Survey, 933 Ramsey Road, Sudbury, Ontario, P3E 6B5, Canada 4Departmental Associate, Department of Palaeobiology, Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario, M5S 2C6, Canada R. Thomas Becker and Sven Hartenfels of the Westfälische (Klapper et al., 2004, p. 375); this is the preferred zonal Wilhelms-Universität, Münster, Germany, have kindly terminology used in that paper, as well as was formalized by informed us that the name Palmatolepis nodosa (Klapper et al., Klapper and Kirchgasser (2016). 2004, p. 381) based on a Frasnian conodont species from northern Ontario is preoccupied. An earlier name, Palmatolepis References marginifera nodosus, was established by Xiong (1983, p. 313) based on a Famennian conodont subspecies from southwest Klapper, G., and Kirchgasser, W.T., 2016, Frasnian Late Devonian conodont China. Species and subspecies within the same genus are biostratigraphy in New York: graphic correlation and taxonomy: Journal of coordinate for the purposes of homonymy. Nor does it prevent Paleontology, v. 90, p. 525–554. Klapper, G., Uyeno, T.T., Armstrong, D.K., and Telford, P.G., 2004, Conodonts homonymy that Xiong used a masculine ending for his of the Williams Island and Long Rapids formations (Upper Devonian, subspecies, as it is automatically corrected to a feminine ending Frasnian–Famennian) of the Onakawana B Drillhole, Moose River Basin, to agree with the gender of the genus name.