Annual Report to the Board of Natural Resources and Conservation
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Carboniferous Formations and Faunas of Central Montana
Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________ -
1 Correlation of the Base of the Serpukhovian Stage
Correlation of the base of the Serpukhovian Stage (Carboniferous; Mississippian) in northwest Europe GEORGE D. SEVASTOPULO* & MILO BARHAM✝ *Department of Geology, Trinity College Dublin, Dublin 2, Ireland ✝Milo Barham, Department of Applied Geology, Curtin University of Technology, GPO Box U1987, Perth, WA 6845, Australia Author for correspondence: [email protected] Running head: Correlation base Serpukhovian northwest Europe Abstract - The Task Group charged with proposing the GSSP for the base of the Serpukhovian Stage (Mississippian: Lower Carboniferous) is likely to use the global First Appearance Datum (FAD: evolutionary first appearance) of the conodont Lochriea ziegleri in the lineage Lochriea nodosa-L. ziegleri for the definition and correlation of the base of the stage. It is important to establish that the FOD (First Occurrence Datum) of L. ziegleri in different basins is essentially penecontemporaneous. Ammonoids provide high-resolution biostratigraphy in the late Mississippian but their use for international correlation is limited by provincialism. However, it is possible to assess the levels of diachronism of the FOD of L. ziegleri in sections in northwest Europe using ammonoid zones. Published compilations of conodont distribution in the Rhenish Slate Mountains of Germany show the FOD of L. ziegleri in the Emstites novalis Biozone (upper part of the P2c zone of the British/Irish ammonoid biozonation) but L. ziegleri has also been reported as occurring in the Neoglyphioceras spirale Biozone (P1d zone). In the Yoredale Group of northern England, the FOD of L. ziegleri is in either the P1c or P1d zone. In NW Ireland, the oldest records of both L. nodosa and L. ziegleri are from the Lusitanoceras granosum Biozone (P2a). -
Lithostratigraphy, Microlithofacies, And
Lithostratigraphy, Microlithofacies, and Conodont Biostratigraphy and Biofacies of the Wahoo Limestone (Carboniferous), Eastern Sadlerochit Mountains, Northeast Brooks Range, Alaska U. S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1568 j^^^fe^i^^t%t^^S%^A^tK-^^ ^.3lF Cover: Angular unconformity separating steeply dipping pre-Mississippian rocks from gently dipping carbonate rocks of the Lisburne Group near Sunset Pass, eastern Sadlerochit Mountains, northeast Brooks Range, Alaska. The image is a digital enhancement of the photograph (fig. 5) on page 9. Lithostratigraphy, Microlithofacies, and Conodont Biostratigraphy and Biofacies of the Wahoo Limestone (Carboniferous), Eastern Sadlerochit Mountains, Northeast Brooks Range, Alaska By Andrea P. Krumhardt, Anita G. Harris, and Keith F. Watts U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1568 Description of the lithostratigraphy, microlithofacies, and conodont bio stratigraphy and biofacies in a key section of a relatively widespread stratigraphic unit that straddles the Mississippian-Pennsylvanian boundary UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1996 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY GORDON P. EATON, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center, Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Published in the Eastern Region, Reston, Va. Manuscript approved for publication June 26, 1995. Library of Congress Cataloging in Publication Data Krumhardt, Andrea P. Lithostratigraphy, microlithofacies, and conodont biostratigraphy and biofacies of the Wahoo Limestone (Carboniferous), eastern Sadlerochit Mountains, northeast Brooks Range, Alaska / by Andrea P. Krumhardt, Anita G. Harris, and Keith F. -
Late Viséan Conodont Biostratigraphy and Biofacies in the Kingscourt Area, Ireland
Bollettino della Società Paleontologica Italiana Modena, Novembre 1999 Late Viséan conodont biostratigraphy and biofacies in the Kingscourt area, Ireland H.E. Anne SOMERVILLE Ian D. SOMERVILLE Department of Geology University College Duolin KEYWORDS- Conodonts Biostratigraphy, Biofacies, Carboniferous, Late Viséan, Kingscourt, Ireland. ABSTRACT - The Gnathodus bilineatus and Lochriea nodosa zones are recognised in the Kingscourt area, Ireland in both platform and basinal facies. The base ofthe nodosa Zone ù defined by the synchronous first occurrence ofL. nodosa and L. mononodosa in the same bed. Severa! conodont species (e.g. Mestognathus bipluti, Idioprioniodus healdi and Kladognathus macrodentata) are mostly restricted to the Brigantian (upper part ofthe bilineatus and nodosa zones). The richest and most diverse conodont faunas dominated by species ofGnathodus and Lochriea are Jrom late platform and basinallimestones within the L. nodosa Zone (Gnathodus-Lochriea Biofacies) . Lower yields and diversity are recorded Jrom early Brigantian platform limestones (upper p art ofthe G. bilineatus Zone); with the poorest conodont yields in late Asbian platform limestones and mudmounds ofthe lower G. bilineatus Zone. T here is a significant rise in the abundance and diversity of conodonts above the Asbian/Brigantian bounda'} a change which coincides with changes in foraminiferal assemblages and lithofacies; this indicates probable transgressive environmental injluences. A second major increase in conodont abundance and diversity is recognised at the base ofthe nodosa Zone, in platform and basinal {acies. Shallow-water, coarse-grainedAsbian platform limestones are dominated by Synclydognathus geminus and Kladognathus tenuis compfectens (Synclydognathus-Kladognathus Biofacies), the elements of which are ojten abraded and fragmented. The best preserved faunas are mostly from the wackestones in the nodosa Zone at Poulmore, which have the best representation ofall apparatus components. -
ANNUAL REPORT to the BOARD of NATURAL RESOURCES and CONSERVATION
Illinois State Geological Survey Annual Report May 1987-June 1988 Illinois Department of Energy and Natural Resources STATE GEOLOGICAL SURVEY DIVISION ANNUAL REPORT to the BOARD OF NATURAL RESOURCES AND CONSERVATION May 1987 to June 1988 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/annualreportto8788illi CONTENTS HIGHLIGHTS 1 MINERAL RESOURCES 8 Illinois Mineral Industry In 1986 and 1987 8 Other Noteworthy Mineral Resource Developments 9 Coal 10 Coal Database Management 11 Coal Resources 13 Coal Characterization 13 Coal Cleaning: Physical and Microbial 15 Coal Cleaning: Chemical and Thermal 16 Coal Combustion 18 Liquids and Gases from Coal 20 Technical Support Services 21 Coal Technology Transfer and Information Services 22 Oil and Gas 22 Oil and Gas Program for Illinois 23 Oil and Gas Statistics 23 Oil and Gas Resources 25 Improved Oil Recovery Methods and Concepts 25 New Exploration Methods and Concepts 27 Hydrocarbon Generation and Migration Studies 28 Oil and Gas Database Management 30 Oil and Gas Technology Transfer and Information Services 30 Other Energy Sources 31 Coal Gas 31 Geothermal Energy 31 Industrial Minerals 31 Mineral Resource Assessments 31 Limestone and Dolomite Resources 33 Sand and Gravel Resources 34 Silica and Industrial Sand 34 Clay Mineralogy and Clay Resources 35 Fluorspar and Metal Resources 35 Beneficiation/Processing 36 Technology Transfer and Information Services 36 Special Projects 38 Mineral Economics 39 Market Research 39 -
Visean – Moscovian Conodont Biostratigraphy of the Ko-Yama Limestone Group, Akiyoshi Belt, SW Japan
Natural Science Research, Univ. Tokushima (Peer-Reviewed Paper) Vol. 27, No. 3 (2013), p. 29 – 52. Visean – Moscovian conodont biostratigraphy of the Ko-yama Limestone Group, Akiyoshi Belt, SW Japan Keisuke ISHIDA 1*, Sigeyuki SUZUKI 2 and Noriyuki INADA 2,3 1 Laboratory of Geology, Institute of SAS, University of Tokushima, 770-8502, Tokushima, Japan * Corresponding author, e-mail: [email protected] 2 Graduate School of Natural Science and Technology, Okayama University, 700-8530, Okayama, Japan e-mail: [email protected] 3 Geoengineering Division of the Dia Consultants Co. Ltd., 331-0811, Saitama, Japan e-mail: [email protected] __________________________________________________________________________________________ Abstract Carboniferous clastic carbonates associated with basaltic pyroclasts and spicular chert beds in the lower part of the Ko-yama Limestone Group contain the Visean – Moscovian conodont succession of Gnathodus semiglaber (late Visean), Gnathodus praebilineatus – Lochriea multinodosa (late Visean), Lochriea ziegleri – Gnathodus girtyi girtyi s.l. (early Serpukhovian), Neoganthodus symmetricus – Idiognathodus primulus (middle – late Bashkirian), and Idiognathoides convexus – Gondolella clarki (early Moscovian). The FAD of Lochriea ziegleri marks the Visean/Serpukhovian boundary in the section. The middle – late Bashkirian Neoganthodus symmetricus – Idiognathodus primulus Fauna is a mixed fauna containing reworked Serpukhovian and older elements possibly related to an erosional event after the Early Bashkirian global eustatic low-stand. The revision of conodont zonal correlation in the Akiyoshi Belt was examined with the Mississippian/Pennsylvanian boundary considering the FAD of Declinognathodus noduliferus in the previously proposed zones in the similar Hina, Atetsu, Akiyoshi and Omi limestone groups. Idiognathodus craticulinodosus n. sp. was described as the middle – late Bashkirian to early Moscovian index. -
2014 Task Group Progress Report for the Viséan-Serpukhovian Boundary
2014 PROGRESS REPORT OF THE TASK GROUP TO ESTABLISH A GSSP CLOSE TO THE EXISTING VISÉAN-SERPUKHOVIAN BOUNDARY Chairman Barry C. Richards Barry C. Richards1 and Task Group 1Geological Survey of Canada-Calgary, 3303-33 St. N.W., Calgary, Alberta. Canada T2L 2A7 E-mail: [email protected] Introduction and general activities An index for boundary definition has been selected, but not voted on by the task group and SCCS for final approval, and work is well advanced at the two prime GSSP candidate sections: the Verkhnyaya Kardailovka in the southern Ural Mountains of Russia and the Naqing (Nashui) section in southern Guizhou Province, China. In the Cantabrian Mountains of northwest Spain, work continued on the Millaró and Vegas de Sotres sections, two other potential candidate sections for the GSSP. For boundary definition, the group is using the first evolutionary occurrence of the conodont Lochriea ziegleri Nemirovskaya, Perret & Meischner, 1994 in the lineage Lochriea nodosa (Bischoff, 1957)−Lochriea ziegleri. L. ziegleri appears in the Brigantian Substage of NW Europe somewhat below the current base of the Serpukhovian as defined by its lectostratotype section in the Zaborie quarry near the city of Serpukhov in the Moscow Basin, Russia (Kabanov et al., 2009, 2012, 2013). The most important accomplishments in 2014 were: 1) the completion of a manuscript by Nemirovska et al. (in progress) titled “Conodonts of the genus Lochriea near the Viséan/Serpukhovian boundary (Mississippian) at the Naqing section, Guizhou Province, South China”. That study enables confirmation and refinement of known lineages within the genus, and two lineages are proposed: a) the noded Lochriea species L. -
Pander Society Newsletter
Pander Society Newsletter Compiled and edited by P.H. von Bitter and J. Burke DEPARTMENT OF NATURAL HISTORY (PALAEOBIOLOGY SECTION), ROYAL ONTARIO MUSEUM, TORONTO, ONTARIO, CANADA M5S 2C6 Number 38 June 2006 www.conodont.net CHIEF PANDERER’S REMARKS Dear Conodont Colleagues: A year has gone by since I last communicated like this, and I’m pleased (and relieved) that another Pander Society Newsletter is ready to ‘go’. Thank you for having sent in your reports and questionnaires; without your willingness to going through a bit of pain there would be no Pander Society Newsletter, and our communications would be the poorer. I am very grateful to compiler and editor Joan Burke (Toronto) and webmaster Mark Purnell (Leicester) for their dedication and ongoing interest; they have helped me greatly and continue to make me look better than I really am, particularly in a time of personal and professional transition. You, the Pander Society membership, continue to ‘re-invent’ and apply conodonts in startling new ways. Some of this re-invention was seen at the Pander Society Symposium in Harrisburg, Pennsylvania, where on March 20-22, 2006 our (mostly) North American members focused on Conodonts & Sequence Stratigraphy. Looking ahead, the programme of ICOS 2006 on July 12-30/ 2006 in Leicester, England, promises not only to surprise and delight, but looks remarkably diverse and imaginative. Christian Pander, would, on the 150th anniversary of the publication of his major conodont study, no doubt be enormously impressed and pleased with the innovativeness and progress of his intellectual grandchildren. My best wishes to all of you. -
Water Resource Availability in the Kankakee River Basin, Indiana: Division of Water, Water Resources, Assessment 90-3
WATER RESOURCE AVAILABILITY IN THE KANKAKEE RIVER BASIN, DIVISION OF WATER published 1990 INDIANA - EXECUTIVE SUMMARY Figure 1. Location of the Kankakee River Basin In response to legislative directives contained in the 1983 Water Resource Management Act, the Indiana Department of Natural Resources, Division of Water published a report describing the availability, distribution, quality, and use of surface water and ground water in the Kankakee River Basin, Indiana.* The third in a series of 12 regional watershed assess- ments, the report provides hydrologic data and related information for persons interested in the basin’s water resource. The following is a summary of that report. The full report can be obtained from the Indiana Department of Natural Resources, Division of Water. For ordering information, please see the instructions printed at the end of this summary. The Kankakee River Basin drains 2989 sq. mi. (square miles) in northwest Indiana, 2169 sq. mi. in northeast Illinois, and about 7 sq. mi. in southwest Lower Michigan (figure 1). The Kankakee River heads near South Bend, Indiana, then flows westward into Illinois, where it joins with the Des Plaines River to form the Illinois River. The area of Lake County which originally drained to Lake Michigan but now drains by means of artificial diversion to the Illinois River is not considered to be part of the Kankakee River Basin study region. Although the Kankakee River basin includes portions of Indiana, Illinois, and Michigan, the discussion below will focus on the Indiana portion of the basin. SOCIOECONOMIC SETTING Thirteen Indiana counties lie completely or partially within the Kankakee River Basin, but nine counties consti- tute more than 90 percent of the basin’s land area in Indiana. -
Conodont Apparatus Reconstruction from the Lower Carboniferous Hart River Formation, Norther Yukon Territory
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2016 Conodont Apparatus Reconstruction from the Lower Carboniferous Hart River Formation, Norther Yukon Territory Lanik, Amanda Lanik, A. (2016). Conodont Apparatus Reconstruction from the Lower Carboniferous Hart River Formation, Norther Yukon Territory (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/25420 http://hdl.handle.net/11023/3324 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Conodont Apparatus Reconstruction from the Lower Carboniferous Hart River Formation, Northern Yukon Territory by Amanda Lanik A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE GRADUATE PROGRAM IN GEOLOGY AND GEOPHYSICS CALGARY, ALBERTA SEPTEMBER, 2016 © Amanda Lanik 2016 Abstract Conodonts sampled from the Lower Carboniferous Hart River Formation have yielded abundant, well-preserved elements with a relatively low diversity of species. In addition, they do not display much platform-overrepresentation, a phenomenon affecting the majority of Late Paleozoic conodont samples. These qualities make the Hart River conodont samples ideal for statistical apparatus reconstruction. The elements were divided into groups based on morphology and counted. Cluster analysis, in addition to empirical observations made during the counting process, was then used to reconstruct the original apparatus composition for the species present. -
2017 State of Illinois Department of Natural Resources Illinois Fishing Information Effective: April 1, 2017 Through March 31, 2018
2017 State of Illinois Department of Natural Resources Illinois Fishing Information Effective: April 1, 2017 through March 31, 2018 Wayne Herndon, veteran IDNR Fisheries Biologist, 45 years of service to the anglers of Illinois IDNR Division of Fisheries Division of Fisheries www.dnr.illinois.gov www.ifishillinois.org Building the Future of Fishing in Illinois FC1 Message from the Director Thank you for picking up a copy of the 2017 Illinois Fishing Information guide. The booklet is packed with useful information on places to fish and rules to follow when fishing in Illinois. In the pages that follow, those who enjoy fishing will find an updated summary of statewide fishing regulations in Illinois, as well as details on site-specific regulations that are organized by the body of water or water area at which those regulations apply. Once again for 2017, Illinois Free Fishing Days will be during the Father’s Day weekend in June – with the dates of Friday, June 16 through Monday, June 19. Free Fishing Days provide an opportunity for novice anglers and families to go fishing even if they have not yet purchased a fishing license. While we update the Illinois Fishing Information guide each year, some site-specific regulations may be changed in emergency situations through the administrative rule process. In those cases, the emergency changes to regulations will be posted at the location where the rules apply. We also post changes in rules online at www.ifishillinois.org. Illinois anglers are guardians of our state’s aquatic resources. The money you spend on fishing licenses and equipment helps fund our fishery programs, and helps ensure the future of fishing in Illinois. -
2021 Fishing Regulation Information
Illinois 2021 REGULATION INFORMATION Effective: April 1, 2021 through March 31, 2022 Inside: • Current fishing regulations • Aquatic nuisance species • Places to fish • Illinois fish and your health • Current state records • Catchable trout program • Angler Alerts! • Free Fishing Days Division of Fisheries www.dnr.illinois.govFC1 www.ifishillinois.org Message from the Director Thank you for your interest in fishing in Illinois and for reviewing this 2021 edition of the Illinois Fishing Information guide. This booklet is an excellent resource for details on the best places to fish in Illinois, along with the rules and regulations in place for the 2021 season. During the last year, as we all dealt with the many challenges of the coronavirus pandemic, we saw an increase in interest in spending time outdoors in Illinois, including new and renewed interest in fishing. Our Division of Fisheries staff prepared this 2021 Illinois Fishing Information guide to provide an updated summary of statewide fishing regulations, as well as details on important site-specific regulations organized by the body of water or water area at which those regulations apply. On occasion, some site-specific regulations may be changed in emergency situations through the administrative rule process. In those cases, the changes are posted at the location where the rules apply, and online at www.ifishillinois.org. A reminder that the 2021 Illinois Free Fishing Days will be Friday, June 18 through Monday, June 21 – Father’s Day weekend – providing families and individuals a chance to go fishing even if they have not yet purchased an Illinois fishing license. The purchases of fishing licenses and equipment help fund our fisheries programs and ensure the future of fishing in Illinois.