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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. -
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. -
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. -
Long-Range Petroleum Migration in the Illinois Basin CRAIG M
ILLINOIS STATE GEOLOGICAL SURVEY Interior Cratonic Basins, 1991, edited by Reprint Series 1991 - T26 M. W. Leighton, D. R. Kalata, D. F. Oltz, and J. J. Eidel: American Association of Petroleum Geologists Memoir 51,819 p. CHAPTER 26 Long-Range Petroleum Migration in the Illinois Basin CRAIG M. BETHKE DONALD F. OLTZ University of Illinois Illinois State Geological Survey Urbana, Illinois Champaign, Illinois JACKIE D. REED ARCO Oil and Gas Company Plano, Texas Editor's note: No treatment of oil and gas in the Illinois In this section, we define the migration that has basin would be complete without an overview of occurred in the Illinois basin on the basis of shale hydrocarbon migration. The following is a condensed petrographic observations and geochemical correla version, made especially for this volume, of an article tions. We emphasize the origin of oils found in shallow that will appear in the American Association of reservoirs, mostly in Silurian strata to the north and Petroleum Geologists Bulletin in 1991. northwest of the central basin (Figure 26-2), because these oils seem to have migrated farthest from source beds. We show that these oils, which are produced from reservoirs more than 125 mi (200 km) from the basin's depocenter, were derived from Devonian source rocks in the deep basin. We then use quantitative models of the basin's paleohydrology to INTRODUCTION investigate the past subsurface conditions that drove the migration. We conclude that long-range migration The distribution of petroleum production from the was not related to processes occurring as the basin Illinois basin extends considerably beyond the area subsided and infilled. -
Geology of the Devonian Marcellus Shale—Valley and Ridge Province
Geology of the Devonian Marcellus Shale—Valley and Ridge Province, Virginia and West Virginia— A Field Trip Guidebook for the American Association of Petroleum Geologists Eastern Section Meeting, September 28–29, 2011 Open-File Report 2012–1194 U.S. Department of the Interior U.S. Geological Survey Geology of the Devonian Marcellus Shale—Valley and Ridge Province, Virginia and West Virginia— A Field Trip Guidebook for the American Association of Petroleum Geologists Eastern Section Meeting, September 28–29, 2011 By Catherine B. Enomoto1, James L. Coleman, Jr.1, John T. Haynes2, Steven J. Whitmeyer2, Ronald R. McDowell3, J. Eric Lewis3, Tyler P. Spear3, and Christopher S. Swezey1 1U.S. Geological Survey, Reston, VA 20192 2 James Madison University, Harrisonburg, VA 22807 3 West Virginia Geological and Economic Survey, Morgantown, WV 26508 Open-File Report 2012–1194 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Ken Salazar, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 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 material contained within this report. -
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. -
Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio
SUBSURFACE FACIES ANALYSIS OF THE DEVONIAN BEREA SANDSTONE IN SOUTHEASTERN OHIO William T. Garnes A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2014 Committee: James Evans, Advisor Jeffrey Snyder Charles Onasch ii ABSTRACT James Evans, Advisor The Devonian Berea Sandstone is an internally complex, heterogeneous unit that appears prominently both in outcrop and subsurface in Ohio. While the unit is clearly deltaic in outcrops in northeastern Ohio, its depositional setting is more problematic in southeastern Ohio where it is only found in the subsurface. The goal of this project was to search for evidence of a barrier island/inlet channel depositional environment for the Berea Sandstone to assess whether the Berea Sandstone was deposited under conditions in southeastern Ohio unique from northeastern Ohio. This project involved looking at cores from 5 wells: 3426 (Athens Co.), 3425 (Meigs Co.), 3253 (Athens Co.), 3252 (Athens Co.), and 3251 (Athens Co.) In cores, the Berea Sandstone ranges from 2 to 10 m (8-32 ft) thick, with an average thickness of 6.3 m (20.7 ft). Core descriptions involved hand specimens, thin section descriptions, and core photography. In addition to these 5 wells, the gamma ray logs from 13 wells were used to interpret the architecture and lithologies of the Berea Sandstone in Athens Co. and Meigs Co. as well as surrounding Vinton, Washington, and Morgan counties. Analysis from this study shows evidence of deltaic lobe progradation, abandonment, and re-working. Evidence of interdistributary bays with shallow sub-tidal environments, as well as large sand bodies, is also present. -
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. -
Preliminary Geological Feasibility Report
R. L. LANGENHEfM, JR. EGN 111 DEPT. GEOL. UNIV. ILLINOIS 234 N.H. B., 1301 W. GREEN ST. URBANA, ILLINOIS 61801 Geological-Geotechnical Studies for Siting the Superconducting Super Collider in Illinois Preliminary Geological Feasibility Report J. P. Kempton, R.C. Vaiden, D.R. Kolata P.B. DuMontelle, M.M. Killey and R.A. Bauer Maquoketa Group Galena-Platteville Groups Illinois Department of Energy and Natural Resources ENVIRONMENTAL GEOLOGY NOTES 111 STATE GEOLOGICAL SURVEY DIVISION 1985 Geological-Geotechnical Studies for Siting the Superconducting Super Collider in Illinois Preliminary Geological Feasibility Report J.P. Kempton, R.C. Vaiden, D.R. Kolata P.B. DuMontelle, M.M. Killey and R.A. Bauer ILLINOIS STATE GEOLOGICAL SURVEY Morris W. Leighton, Chief Natural Resources Building 615 East Peabody Drive Champaign, Illinois 61820 ENVIRONMENTAL GEOLOGY NOTES 111 1985 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/geologicalgeotec1 1 1 kemp 1 INTRODUCTION 1 Superconducting Super Collider 1 Proposed Site in Illinois 2 Geologic and Hydrogeologic Factors 3 REGIONAL GEOLOGIC SETTING 5 Sources of Data 5 Geologic Framework 6 GEOLOGIC FRAMEWORK OF THE ILLINOIS SITE 11 General 1 Bedrock 12 Cambrian System o Ordovician System o Silurian System o Pennsylvanian System Bedrock Cross Sections 18 Bedrock Topography 19 Glacial Drift and Surficial Deposits 21 Drift Thickness o Classification, Distribution, and Description of the Drift o Banner Formation o Glasford Formation -
Bedrock Geology of Dixon West Quadrangle
STATEMAP Dixon West-BG Bedrock Geology of Dixon West Quadrangle Lee County, Illinois Dennis R. Kolata 2013 Prairie Research Institute ILLINOIS STATE GEOLOGICAL SURVEY 615 East Peabody Drive Champaign, Illinois 61820-6964 (217) 244-2414 http://www.isgs.illinois.edu © 2013 University of Illinois Board of Trustees. All rights reserved. For permission information, contact the Illinois State Geological Survey. INTRODUCTION STRATIGRAPHY The Dixon West Quadrangle is situated in northwestern Lee Bedrock in the Dixon West Quadrangle consists largely of County, Illinois. It encompasses the western parts of the city Ordovician dolomite and shale and a small area of Silurian of Dixon, which is the largest town in the county. Most of the dolomite in the southwestern part of the quadrangle. It has land is used for agricultural purposes but a moderate amount been standard practice of the ISGS during the past few of residential and commercial developments are present. decades to follow the Ordovician classification and nomen- clature proposed by Templeton and Willman (1963). Their The quadrangle lies in the Rock River Hill Country of the stratigraphy was followed in large part by Willman and Ko- Central Lowlands Province. The topography formed primar- lata (1978) who made minor revisions to some members and ily by deposition of glacial sediments (clay, silt, sand, and documented the presence of nine widespread K-bentonite gravel) in a till plain which was subsequently dissected by beds. These stratigraphic investigations have shown that the erosional processes of the Rock River and its tributaries. Upper Ordovician carbonate succession consists of distinc- Bedrock in the Dixon West Quadrangle is largely concealed tive rock units that can be traced over wide areas of the beneath the till plain except for local exposures along the riv- Midcontinent U.S. -
Open Kosei.Pdf
The Pennsylvania State University The Graduate School Department of Geosciences GEOCHEMISTRY OF ARCHEAN–PALEOPROTEROZOIC BLACK SHALES: THE EARLY EVOLUTION OF THE ATMOSPHERE, OCEANS, AND BIOSPHERE A Thesis in Geosciences by Kosei Yamaguchi Copyright 2002 Kosei Yamaguchi Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy May 2002 We approve the thesis of Kosei Yamaguchi Date of Signature ____________________________________ _______________________ Hiroshi Ohmoto Professor of Geochemistry Thesis Advisor Chair of Committee ____________________________________ _______________________ Michael A. Arthur Professor of Geosciences ____________________________________ _______________________ Lee R. Kump Professor of Geosciences ____________________________________ _______________________ Raymond G. Najjar Associate Professor of Meteorology ____________________________________ _______________________ Peter Deines Professor of Geochemistry Associate Head for Graduate Program and Research in Geosciences iii ABSTRACT When did the Earth's surface environment become oxic? The timing and mechanism of the rise of atmospheric pO2 level in the early Precambrian have been long debated but no consensus has been reached. The oxygenation of the atmosphere and oceans has significant impacts on the evolution of the biosphere and the geochemical cycles of redox-sensitive elements. In order to constrain the evolution of the atmosphere, oceans, biosphere, and geochemical cycles of elements, a systematic and multidisciplinary