Depositional and Structural History of the Pennsylvanian System of the Illinois
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CONODONT BIOSTRATIGRAPHY and ... -.: Palaeontologia Polonica
CONODONT BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE PERTH LIMESTONE MEMBER, STAUNTON FORMATION (PENNSYLVANIAN) OF THE ILLINOIS BASIN, U.S.A. CARl B. REXROAD. lEWIS M. BROWN. JOE DEVERA. and REBECCA J. SUMAN Rexroad , c.. Brown . L.. Devera, 1.. and Suman, R. 1998. Conodont biostrati graph y and paleoec ology of the Perth Limestone Member. Staunt on Form ation (Pennsy lvanian) of the Illinois Basin. U.S.A. Ill: H. Szaniawski (ed .), Proceedings of the Sixth European Conodont Symposium (ECOS VI). - Palaeont ologia Polonica, 58 . 247-259. Th e Perth Limestone Member of the Staunton Formation in the southeastern part of the Illinois Basin co nsists ofargill aceous limestone s that are in a facies relati on ship with shales and sandstones that commonly are ca lcareous and fossiliferous. Th e Perth conodo nts are do minated by Idiognathodus incurvus. Hindeodus minutus and Neognathodu s bothrops eac h comprises slightly less than 10% of the fauna. Th e other spec ies are minor consti tuents. The Perth is ass igned to the Neog nathodus bothrops- N. bassleri Sub zon e of the N. bothrops Zo ne. but we were unable to co nfirm its assignment to earliest Desmoin esian as oppose d to latest Atokan. Co nodo nt biofacies associations of the Perth refle ct a shallow near- shore marine environment of generally low to moderate energy. but locali zed areas are more variable. particul ar ly in regard to salinity. K e y w o r d s : Co nodo nta. biozonation. paleoecology. Desmoinesian , Penn sylvanian. Illinois Basin. U.S.A. -
Bedrock Geology of Altenburg Quadrangle, Jackson County
BEDROCK GEOLOGY OF ALTENBURG QUADRANGLE Institute of Natural Resource Sustainability William W. Shilts, Executive Director JACKSON COUNTY, ILLINOIS AND PERRY COUNTY, MISSOURI STATEMAP Altenburg-BG ILLINOIS STATE GEOLOGICAL SURVEY E. Donald McKay III, Interim Director Mary J. Seid, Joseph A. Devera, Allen L. Weedman, and Dewey H. Amos 2009 360 GEOLOGIC UNITS ) ) ) 14 Qal Alluvial deposits ) 13 18 Quaternary Pleistocene and Holocene 17 360 ) 15 360 16 14 0 36 ) 13 Qf Fan deposits ) Unconformity Qal ) & 350 tl Lower Tradewater Formation Atokan ) ) Pennsylvanian 360 ) &cv Caseyville Formation Morrowan 24 360 ) Unconformity ) 17 Upper Elviran undivided, Meu ) Waltersburg to top of Degonia 19 20 Qal 21 22 23 ) 24 ) Mv Vienna Limestone 360 o ) 3 Mts ) 350 Mts Tar Springs Sandstone ) 20 360 ) Mgd 360 30 ) Mgd Glen Dean Limestone ) 21 350 360 Mts 29 ) Qal Hardinsburg Sandstone and J N Mhg Chesterian ) Golconda Formations h Æ Qal Mav anc 28 27 Br ) N oJ 26 25 JN 85 N ) Cypress Sandstone through J Mcpc Dsl 500 Paint Creek Formation JN N ) J o Mts N 5 J s ) Dgt 600 J N 70 J N Mgd Yankeetown Formation s ) Myr Db 80 28 Æ and Renault Sandstone N J 29 N J N ) Sb J Mgd Mississippian o Dgt Ssc 25 Clines o N 25 Msg 27 ) Qal J 80 s 3 Mav Aux Vases Sandstone N J N Mts o MILL J MISSISSIPPI 34 ) Qal J N ) N J Dsl 35 N 26 J o N 25 J Mgd Mgd ) Msg Ste. Genevieve Limestone 500 o Db DITCH J 20 Mgd N N N ) J J o RIVER o N 600 J 80 N ) 10 o J Mav Æ Msl St. -
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. -
Upper Carboniferous–Lower Permian Buildups of the Carnic Alps, Austria–Italy 201 Upper Carboniferous–Lower Permian Buildups of the Carnic Alps, Austria–Italy
Published in "SEPM Special Publication No. 78: 201-217, 2003" which should be cited to reference this work. UPPER CARBONIFEROUS–LOWER PERMIAN BUILDUPS OF THE CARNIC ALPS, AUSTRIA–ITALY 201 UPPER CARBONIFEROUS–LOWER PERMIAN BUILDUPS OF THE CARNIC ALPS, AUSTRIA–ITALY ELIAS SAMANKASSOU Université de Fribourg, Département de Géosciences, Géologie et Paléontologie, Pérolles, CH-1700 Fribourg, Switzerland e-mail: [email protected] ABSTRACT: A variety of buildup types occur in the upper Paleozoic Auernig and Rattendorf Groups, Carnic Alps, at the present-day Austrian–Italian border, including coral, diverse algal (Anthracoporella, Archaeolithophyllum, Rectangulina, and phylloid green), bryozoan, brachiopod, and sponge buildups. Thin mounds and banks have a diverse fossil association (e.g., Archaeolithophyllum–bryozoan– brachiopod mounds) and occur in siliciclastic-dominated intervals, as do coral buildups. Some of the biodiverse thin mounds occur in strata that were deposited in cooler water. However, the thickest mounds are nearly monospecific (e.g., Anthracoporella mounds) and grew in carbonate-dominated, warm-water environments. Most of the mounds considered in this paper, particularly algal mounds, grew in quiet-water environments below wave base but within the photic zone. Mound growth was variously stopped by siliciclastic input, e.g., auloporid coral mounds, sea-level rise, e.g., the drowning of Anthracoporella mounds of the Rattendorf Group, influence of cool water, e.g., algal mounds of the Auernig Group overlain by limestone of cool-water biotic association, or sea-level fall, e.g., phylloid algal mounds that were subsequently exposed subaerially. There is no indication of ecological succession during mound growth. Growth, dimensions, biotic association, and termination of mounds seem to have been controlled by extrinsic factors, mainly sea level and water temperature. -
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--.-------.- ___________________ -
Lodge History Book Centennial Crate
LODGE HISTORY BOOK CENTENNIAL CRATE National Order of the Arrow Committee July 2012 Members of the Lodge Key-3: You hold in your hand our Centennial Lodge History Book Binder. We ask that you use it as a guide to RAY CAPP write a history of the Order of the Arrow in your council as part of a nationwide project to collect local Chairman th histories of the Order as we lead up to our celebration of the 100 Anniversary of the Order (2015). JOHN P. REHM National Chief-2012 There are several well researched histories of the Order of the Arrow written from a national PRESTON H. MARQUIS perspective. This project, however, asks you to tell your perspective. Through it, we will endeavor to National Vice Chief-2012 gather almost three hundred histories from across the nation. Each lodge present at the 2012 CLYDE M. MAYER National Conference will be receiving this binder. One of the commonalities which bind all Arrowmen OA Director together is that we each have raised our hand and promised to “observe and preserve the traditions BRADLEY E. HADDOCK of the Order of the Arrow”. This is a terrific chance to do so locally in concert with your brothers from Immediate Past Chairman all over the country who will also be telling their stories. L. RONALD BELL Arrowhead of Service Contained in your binder is a template for helping your lodge research and compose the story of the Award Recipient Order of the Arrow in the council you serve. Notice that we are not necessarily asking for a lodge CRAIG B. -
Khsaa Boys' 3A Track & Field State Champions
KHSAA BOYS’ 3A TRACK & FIELD STATE CHAMPIONS Updated through 2021 state meet 110 METER HURDLES 1990 Reggie Wilkins Eastern 10.71 2004 Zachary Wilder Woodford County 4:17.88 Year Name(s) School Time 1991 Chris Jackson Woodford County 10.79 2005 Michael Eaton Greenwood 4:20.13 1977 Simmons Valley 14.20 1992 Brian Raspberry Male 10.81 2006 Thomas Davies St. Xavier 4:18.74 1978 LaPaille Pleasure Ridge Park 14.40 1993 Brian Raspberry Male 10.84 2007 Brian Long St. Xavier 4:26.09 1979 Anthony Jackson Bryan Station 14.90 1994 Brian Raspberry Male 10.70 2008 Ryan Eaton Greenwood 4:18.83 1980 Anthony Jackson Bryan Station 14.70 1995 Mark Miller Louisville Male 10.97 2009 Ryan Eaton Greenwood 4:18.39 1981 Bruce Ewing Valley 14.62 1996 Tony Driver Louisville Male 11.00 2010 Ryan Eaton Greenwood 4:17.91 1982 Preston Gray DuPont Manual 14.22 1997 Casey Combest Owensboro 10.75 2011 Andrew Stewart North Hardin 4:16.10 1983 Chris Lancaster Shelby County 14.61 1998 Casey Combest Owensboro 10.71 2012 Luke Weishaar Oldham County 4:19.52 1984 Chris Lancaster Shelby County 14.51 1999 Tyson Gay Lafayette 10.81 2013 Patrick Gregory Butler 4:18.15 1985 Chris Verhoven Lafayette 14.81 2000 Tyson Gay Lafayette 10.78 2014 William Mulloy St. Xavier 4:18.38 1986 Leon Bussell Christian County 14.70 2001 Tyson Gay Lafayette 10.46 2015 Ben Young Tates Creek 4:10.15 1987 Larry August Lafayette 15.08 2002 Todd Chisley Scott County 10.96 2016 Yared Nuguse DuPont Manual 4:12.10 1988 Doug Calhoun Henderson County 14.59 2003 William Carter Apollo 10.84 2017 Yared Nuguse DuPont Manual 4:17.94 1989 Doug Calhoun Henderson County 14.33 2004 Joe Petty Jeffersontown 10.93 2018 Trevor Warren Trinity (Lou.) 4:16.95 1990 Carlnell Whelen Pleasure Ridge Park 14.74 2005 Alfonso Smith Waggener 10.89 2019 Jacob Brizendine Oldham County 4:16.68 1991 Jeremy Petter St. -
BULLETINS of AMERICAN PALEONTOLOGY and PALAEONTOGRAPHICA AMERICANA
8'oL HARVARD UNIVERSITY |v 1 ^J^y^ MUS. COMP. BULLETINSZOoL ^ LIBRARY OF MAR 4 *97^ HAi UNJVERi^-AMERICAN PALEONTOLOGY VOL. LXIV 1973-74 Paleontological Research Institution Ithaca, New York 14850 U. S. A. In Memoriam Orville L. Bandy 1916-1973 CONTENTS OF VOLUME LXIV Bulletin No. Pages Plates 278. Palynology of the ASmond Formation (Upper Cretaceous) Rock Springs Uplift, Wyoming. By J. Fred Stone 1-136 1-20 279. Tabulate Corals and Echinoderms from the Pennsylvanian Winterset Limestone, Hog- shooter Formation, Northeastern Oklahoma. By H. L. Strimple and J. M. Cooke 137-168 21 280. Stratigraphy and Genera of Calcareous Foraminifera cf the Fraileys Fades (Missis- sippian) of Central Kentucky. By R. G. Browne and E. R. Pohl 169-244 22-31 281. Crinoid Studies. Part I. Some Pennsylvanian Crinoids from Nebraska. Part. II. Some Permian Crinoids from Nebraska, Kansas, and Oklahoma. By R. K. Pabian and H. L. Strimple 245-338 32-41 INDEX volume. Each number is No separate index is included in the listed in the begin- indexed separately. Contents of the volume are ning of the volume. BULLETINS MUS. COMP. 200U LIBRARY OF OCT 16 19^ AMERICAN t^S«?fALEONTOLOGY (Founded 1895) Vol. 64 No. 278 PALYNOLOGY OF THE ALMOND FORMATION (UPPER CRETACEOUS), ROCK SPRINGS UPLIFT, WYOMING By J. Fred Stone 1973 Paleontological Research Institution Ithaca, New York 14850, U.S.A. PALEONTOLOGIGAL RESEARCH INSTITUTION 1972 - 73 President Daniel B. Sass Vice-President Merrill W. Haas Secretary Philip C. Wakeley Assistant Secretary Rebecca S. Harris Director, Treasurer Katherine V. W. Palmer Counsel Armand L. Adams Representative AAAS Council John Pojeta, Jr. -
109Th Annual Report of the State Geologist
109TH ANNUAL REPORT OF THE STATE GEOLOGIST of INDIANA GEOLOGICAL SURVEY DEPARTMENT OF NATURAL RESOURCES for July 1, 1984 - June 30, 1985 GEOLOGICAL SURVEY ONE HUNDRED AND NINTH ANNUAL REPORT OF THE STATE GEOLOGIST PERMANENT PERSONNEL Administration John B. Patton •• • • • • • State Geologist Maurice E. Biggs • • Assistant State Geologist Mary E. Fox. • • • • • ••••Mineral Statistician E. Coleen George •• • • • • • Principal Secretary Coal and Industrial Minerals Section Donald D. Carr • • • •••••Geologist and Head Curtis H. Ault • • • .Geologist and Associate Head Donald L. Eggert ••••• Geologist Denver Harper ••• Geologist Nancy R. Hasenmueller. Geologist Walter A. Hasenmueller Geologist Paul N. Irwin (OSM) •• Geologist Christopher Schubert (USGS) •• Geologist Nelson R. Shaffer.' •••••• Geologist Christopher R. Smith • Geologist Belita J. Minett •• Secretary Kathryn R. Shaffer • • • • • Secretary Drafting and Photography Section William H. Moran ••. •••Chief Draftsman and Head Barbara T. Hill •••• • •••••••••••Photographer Richard T. Hill. ••• • Senior Geological Draftsman Roger L. Purcell •• •••• Senior Geological Draftsman *Kimberly H. Sowder•• • Draftsperson/Photographer Wilbur E. Stalions • • • • • • • .Artist/Draftsman **James R. Tolen • Senior Geological Draftsman *Salary 'paid in part from Department of Geology account **Salary paid from Department of Geology account Educational Services J 0 h n R. Hi 1 1 • • • • • • • Geologist and Head 1 r Geochemistry Section Richard K. Leininger • • • Geochemist and Head Margaret V. Ennis. -
Proceedings of the Indiana Academy of Science 1 05
Proceedings of the Indiana Academy of Science 1 05 (1997) Volume 106 p. 105-111 DISTRIBUTION OF LIMESTONE IN THE BRAZIL FORMATION (PENNSYLVANIAN) IN THE SUBSURFACE OF SOUTHWESTERN INDIANA AND WESTERN KENTUCKY John B. Droste and Alan S. Horowitz Department of Geological Sciences Indiana University 1005 East 10th Street Bloomington, Indiana 47405 ABSTRACT. Electric logs and samples of well cuttings indicate the existence of limestone bodies in the lower and middle Brazil Formation of southwest- ern Indiana and western Kentucky. The limestone bodies are elongated north- east-southwest, are as much as 60 feet thick, are as much as 3 miles in length, are interpreted to have formed on slight elevations on the sea floor, and were accumulated contemporaneously with adjacent terrigenous muds and sands until they were finally smothered by these terrigenous sediments. KEYWORDS: Brazil Formation, limestone, Pennsylvanian, subsurface south- western Indiana, subsurface western Kentucky. INTRODUCTION The Brazil Formation in Indiana lies below the Staunton Formation and above the Mansfield Formation in the Raccoon Creek Group (Figure 1). In the type area (Brazil, Clay County, Indiana), the Brazil includes rocks from the base of the Lower Block Coal Member to the top of the Minshall Coal Member (Hutchi- son, 1976). The Upper Block Coal Member is the only other named member of the Brazil Formation. The Brazil coals have irregular distributions along the out- crop and very limited distributions in the subsurface. Because the Minshall coal is of limited extent, the stratigraphic position of the base of the more widespread Perth Limestone Member, or of the sandstone that replaces it, was used in an earlier subsurface study (Droste and Horowitz, 1995) to mark the top of the Brazil. -
B2150-B FRONT Final
Bedrock Geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Kentucky, and Missouri By W. John Nelson THE PADUCAH CUSMAP QUADRANGLE: RESOURCE AND TOPICAL INVESTIGATIONS Martin B. Goldhaber, Project Coordinator T OF EN TH TM E U.S. GEOLOGICAL SURVEY BULLETIN 2150–B R I A N P T E E R D . I O S . R A joint study conducted in collaboration with the Illinois State Geological U Survey, the Indiana Geological Survey, the Kentucky Geological Survey, and the Missouri M 9 Division of Geology and Land Survey A 8 4 R C H 3, 1 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Schaefer, Acting 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 Library of Congress Cataloging-in-Publication Data Nelson, W. John Bedrock geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Ken- tucky, and Missouri / by W. John Nelson. p. cm.—(U.S. Geological Survey bulletin ; 2150–B) (The Paducah CUSMAP Quadrangle, resource and topical investigations ; B) Includes bibliographical references. Supt. of Docs. no. : I 19.3:2150–B 1. Geology—Middle West. I. Title. II. Series. III. Series: The Paducah CUSMAP Quadrangle, resource and topical investigations ; B QE75.B9 no. 2150–B [QE78.7] [557.3 s—dc21 97–7724 [557.7] CIP CONTENTS Abstract .......................................................................................................................... -
Description of the Physical Environment and Coal-Mining History of West-Central Indiana, with Emphasis on Six Small Watersheds
Description of the Physical Environment and Coal-Mining History of West-Central Indiana, with Emphasis on Six Small Watersheds United States Geological Survey Water-Supply Paper 2368-A AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current-year issues of the monthly catalog "New Publicati6ns of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. ' Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated monthly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Tech Books of the U.S. Geological Survey are available over the niques of Water-Resources Investigations, Circulars, publications of counter at the following U.S.