Mississippi Geologic Research Papers-1963
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Middle Eocene Claiborne Group, United States Part of the Gulf of Mexico Basin
Geologic Assessment of Undiscovered Conventional Oil and Gas Resources —Middle Eocene Claiborne Group, United States Part of the Gulf of Mexico Basin By Paul C. Hackley U.S. Geological Survey Open-File Report 2012–1144 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 Suggested citation: Hackley, P.C., 2012, Geologic assessment of undiscovered conventional oil and gas resources—Middle Eocene Claiborne Group, United States part of the Gulf of Mexico Basin: U.S. Geological Survey Open–File Report 2012–1144, 87 p., available only at http://pubs.usgs.gov/of/2012/1144/. 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. ii Contents Abstract ......................................................................................................................................................................... 1 Acknowledgments -
Mesozoic Marine Reptile Palaeobiogeography in Response to Drifting Plates
ÔØ ÅÒÙ×Ö ÔØ Mesozoic marine reptile palaeobiogeography in response to drifting plates N. Bardet, J. Falconnet, V. Fischer, A. Houssaye, S. Jouve, X. Pereda Suberbiola, A. P´erez-Garc´ıa, J.-C. Rage, P. Vincent PII: S1342-937X(14)00183-X DOI: doi: 10.1016/j.gr.2014.05.005 Reference: GR 1267 To appear in: Gondwana Research Received date: 19 November 2013 Revised date: 6 May 2014 Accepted date: 14 May 2014 Please cite this article as: Bardet, N., Falconnet, J., Fischer, V., Houssaye, A., Jouve, S., Pereda Suberbiola, X., P´erez-Garc´ıa, A., Rage, J.-C., Vincent, P., Mesozoic marine reptile palaeobiogeography in response to drifting plates, Gondwana Research (2014), doi: 10.1016/j.gr.2014.05.005 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Mesozoic marine reptile palaeobiogeography in response to drifting plates To Alfred Wegener (1880-1930) Bardet N.a*, Falconnet J. a, Fischer V.b, Houssaye A.c, Jouve S.d, Pereda Suberbiola X.e, Pérez-García A.f, Rage J.-C.a and Vincent P.a,g a Sorbonne Universités CR2P, CNRS-MNHN-UPMC, Département Histoire de la Terre, Muséum National d’Histoire Naturelle, CP 38, 57 rue Cuvier, -
Application of Organic Petrography in North American Shale Petroleum Systems: a Review
International Journal of Coal Geology 163 (2016) 8–51 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo Application of organic petrography in North American shale petroleum systems: A review Paul C. Hackley a, Brian J. Cardott b a U.S. Geological Survey, MS 956 National Center, 12201 Sunrise Valley Dr, Reston, VA 20192, USA b Oklahoma Geological Survey, 100 E. Boyd St., Rm. N-131, Norman, OK 73019-0628, USA article info abstract Article history: Organic petrography via incident light microscopy has broad application to shale petroleum systems, including Received 13 April 2016 delineation of thermal maturity windows and determination of organo-facies. Incident light microscopy allows Received in revised form 10 June 2016 practitioners the ability to identify various types of organic components and demonstrates that solid bitumen Accepted 13 June 2016 is the dominant organic matter occurring in shale plays of peak oil and gas window thermal maturity, whereas Available online 16 June 2016 oil-prone Type I/II kerogens have converted to hydrocarbons and are not present. High magnification SEM obser- Keywords: vation of an interconnected organic porosity occurring in the solid bitumen of thermally mature shale reservoirs Organic petrology has enabled major advances in our understanding of hydrocarbon migration and storage in shale, but suffers Thermal maturity from inability to confirm the type of organic matter present. Herein we review organic petrography applications Shale petroleum systems in the North American shale plays through discussion of incident light photographic examples. In the first part of Unconventional resources the manuscript we provide basic practical information on the measurement of organic reflectance and outline Vitrinite reflectance fluorescence microscopy and other petrographic approaches to the determination of thermal maturity. -
Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2018PR004 The Late Cretaceous chimaeroid fish, Ischyodus bifurcatus Case, 1978 (Chondrichthyes: Holocephali), from California, USA, and its paleobiogeographical significance EVANAccepted D. JOHNSON-RANSOM1, EVGENY V. POPOV2,3, THOMAS A. DEMÉRÉ4, AND KENSHU SHIMADA1,5,6 1Department of Biological Sciences, DePaul University, 2325 North Clifton Avenue, Chicago, Illinois 60614, USA (e-mail: [email protected]) 2Department of Paleontology, Geological Faculty, Saratov State University, 83, Astrakhanskaya Street, Saratov 410012, Russia 3Institute of Geology and Petroleum Technology,manuscript Kazan Federal University, Kremlevskaya Str. 4/5, 420008 Kazan, Russia 4Department of Paleontology, San Diego Natural History Museum, 1788 El Prado, San Diego, California 92101, USA 5Department of Environmental Science and Studies, DePaul University, 1110 West Belden Avenue, Chicago, Illinois 60614, USA 6Sternberg Museum of Natural History, Fort Hays State University, 3000 Sternberg Drive, Hays, Kansas 67601, USA Abstract. A nearly complete right mandibular tooth plate of Ischyodus bifurcatus Case (Holocephali: Chimaeroidei) is reported from the Point Loma Formation (upper Campanian) of the Upper Cretaceous Rosario Group in southern California, USA. -
Geology of the Troy, Miss., 7.5 Minute Topographic Quadrangle Chickasaw and Pontotoc Counties Mississippi by Charles T
~ Geology of the Troy, Miss., 7.5 Minute Topographic Quadrangle Chickasaw and Pontotoc Counties Mississippi by Charles T. Swann, R.P.G. and Jeremy J. Dew Mississippi Mineral Resources Institute 310 Lester Hall University, Mississippi 38677 Mississippi Mineral Resources Institute Open - File Report 09-2S August, 2009 On The Cover The Mississippi Office of Geology drilled the MMRI-Reeves, No. 1 well in support of the MMRI’s surface mapping efforts. The cover picture is the drill rig set up in sand pits in sec.22, T.12S, R.3E. A set of core samples as well as a set of geophysical logs were obtained during the drilling operations. The well was begun in the lower Clayton section (Tertiary) and reached a total depth of 403 feet in the Demopolis Formation (Cretaceous). -i- TABLE OF CONTENTS On The Cover ............................................................................................................................. i Table of Contents . ..................................................................................................................... ii List of Tables ............................................................................................................................ iii List of Figures . ......................................................................................................................... iii Abstract...................................................................................................................................... 1 Introduction. ............................................................................................................................. -
Campanian and Austinian-Tayloran Stage Boundaries in Mississippi and Alabama Using Calcareous Microfossils
Documentation of the Santonian Campanian and Austinian-Tayloran Stage Boundaries in Mississippi and Alabama Using Calcareous Microfossils U.S. GEOLOGICAL SURVEY BULLETIN 1884 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 cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey 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 month ly, 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, Techniques of Water-Resources Investigations, Circulars, publications of -
B-50 Geology of the Coastal Plain of East Central Georgia
GEORGIA STATE DIVISION OF CONSERVATION DEPARTMENT OF MINES, MINING AND GEOLOGY GARLAND PEYTON, Director THE GEOLOGICAL SURVEY BULLETIN NUMBER 50- PART 1 GEOLOGY OF THE COASTAL PLAIN OF EAST-CENTRAL GEORGIA By PHILIP E. LA MOREAUX Geologist United States Geological Survey Published in cooperation with United States Department of Interior, Geological Survey, Washing.ton, D. C. ATLANTA 1946 I LETTER OF TRANSMITTAL DEPARTMENT OF MINES, MINING AND GEOLOGY ATLANTA, February 15, 1946. His Excellency, Ellis Arnall, Governor Commissioner Ex-Officio, State Division of Conservation Through The Honorable Nelson M. Shipp, Assistant Commissioner SIR: I have the honor to submit herewith Georgia Geological Survey Bulletin No. 50, Part I, "Geology of the Coastal Plain of East-Central Georgia." This is the first in a series of bulletins under this title. Others will be published from time to time until all of the Cretaceous area in the State has been mapped. The geology of east central Georgia, the area covered in this report, influences in three essential ways the economy of the State: The Tuscaloosa formation consists of thick beds of sand and gravel that are excellent aquifers. These water-bearing beds will furnish large additional quantities of water of good quality for industrial and municipal uses throughout a belt of 10 to 30 miles in width along the northern mar gin of the Coastal Plain of Georgia. Georgia produces approximately 80 per cent of the national output of kaolin. The major portion of this production is from deposits described in this report in Washington, Wilkinson a:nd Twiggs counties. Other com mercial minerals mined in this area include bauxite, fuller's earth, lime stone, and sand and gravel. -
Jason P. Schein
Curriculum Vitae JASON P. SCHEIN EXECUTIVE DIRECTOR BIGHORN BASIN PALEONTOLOGICAL INSTITUTE 3959 Welsh Road, Ste. 208 Willow Grove, Pennsylvania 19090 Office: (406) 998-1390 Cell: (610) 996-1055 [email protected] EDUCATION Ph.D. Student Drexel University, Department of Biology, Earth and Environmental Science, 2005-2013 M.Sc., Auburn University, Department of Geology and Geography, 2004 B.Sc., Auburn University, Department of Geology and Geography, 2000 RESEARCH AND PROFESSIONAL INTERESTS Mesozoic vertebrate marine and terrestrial faunas, paleoecology, paleobiogeography, faunistics, taphonomy, biostratigraphy, functional morphology, sedimentology, general natural history, education and outreach, paleontological resource assessment, and entrepreneurial academic paleontology. ACADEMIC, PROFESSIONAL, & BOARD POSITIONS 2019-Present Member of the Board, Yellowstone-Bighorn Research Association 2017-Present Founding Executive Director, Bighorn Basin Paleontological Institute 2017-Present Member of the Board, Delaware Valley Paleontological Society 2016-Present Scientific and Educational Consultant, Field Station: Dinosaurs 2015-Present Graduate Research Associate, Academy of Natural Sciences of Drexel University 2007-2017 Assistant Curator of Natural History Collections and Exhibits, New Jersey State Museum 2015-2017 Co-founder, Co-leader, Bighorn Basin Dinosaur Project 2010-2015 International Research Associate, Palaeontology Research Team, University of Manchester 2010-2014 Co-leader, New Jersey State Museum’s Paleontology Field Camp 2007-2009 Interim Assistant Curator of Natural History, New Jersey State Museum 2006-2007 Manager, Dinosaur Hall Fossil Preparation Laboratory 2004-2005 Staff Environmental Geologist, Cobb Environmental and Technical Services, Inc. 1 FIELD EXPERIENCE 2010-2019 Beartooth Butte, Morrison, Lance, and Fort Union formations, Bighorn Basin, Wyoming and Montana, U.S.A. (Devonian, Jurassic, Late Cretaceous, and earliest Paleocene, respectively) 2010 Hell Creek Formation, South Dakota, U.S.A. -
B-127 Lithostratigraphic Framework Of
&A 'NlOO,G-3 &i flo, 12 7 g l F£i&f THE LITHOSTRATIGRAPHIC FRAMEWORK OF \;\ .-t "- THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour Work Performed in Cooperation with United States Geological Survey (Cooperative Agreement Number 1434-92-A-0959) and U. S. Department of Energy (Cooperative Agreement Number DE-FG-09-92SR12868) GEORGIA DEPARTMENT OF NATURAL RESOURCES ENVIRONMENTAL PROTECTION DIVISION GEORGIA GEOLOGIC SURVEY Atlanta 1996 Bulletin 127 THE LITHOSTRATIGRAPHIC FRAMEWORK OF THE UPPERMOST CRETACEOUS AND LOWER TERTIARY OF EASTERN BURKE COUNTY, GEORGIA Paul F. Huddlestun and Joseph H. Summerour GEORGIA DEPARTMENT OF NATURAL RESOURCES Lonice C. Barrett, Commissioner ENVIRONMENTAL PROTECTION DIVISION Harold F. Reheis, Director GEORGIA GEOLOGIC SURVEY William H. McLemore, State Geologist Atlanta 1996 Bulletin 127 ABSTRACT One new formation, two new members, and a redefinition of an established lithostratigraphic unit are formally introduced here. The Oconee Group is formally recognized in the Savannah River area and four South Carolina Formations not previously used in Georgia by the Georgia Geologic Survey are recognized in eastern Burke County. The Still Branch Sand is a new formation and the two new members are the Bennock Millpond Sand Member of the Still Branch Sand and the Blue Bluff Member of the Lisbon Formation. The four South Carolina formations recognized in eastern Burke CountY include the Steel Creek Formation and Snapp Formation of the Oconee Group, the Black Mingo Formation (undifferentiated), and the Congaree Formation. The Congaree Formation and Still Branch Sand are considered to be lithostratigraphic components of the Claiborne Group. -
American Museum Novitates
AMERICAN MUSEUM NOVITATES Number 3954, 29 pp. June 16, 2020 A new genus of Late Cretaceous angel shark (Elasmobranchii; Squatinidae), with comments on squatinid phylogeny JOHN G. MAISEY,1 DANA J. EHRET,2 AND JOHN S.S. DENTON3 ABSTRACT Three-dimensional Late Cretaceous elasmobranch endoskeletal elements (including palato- quadrates, ceratohyals, braincase fragments, and a series of anterior vertebrae) are described from the Late Cretaceous University of Alabama Harrell Station Paleontological Site (HSPS), Dallas County, Alabama. The material is referred to the extant elasmobranch Family Squatinidae on the basis of several distinctive morphological features. It also exhibits features not shared by any modern or fossil Squatina species or the extinct Late Jurassic squatinid Pseudorhina. A new genus and species is erected, despite there being some uncertainty regarding potential synonymy with existing nominal species previously founded on isolated fossil teeth (curiously, no squatinid teeth have been docu- mented from the HSPS). A preliminary phylogenetic analysis suggests that the new genus falls on the squatinid stem, phylogenetically closer to Squatina than Pseudorhina. The craniovertebral articu- lation in the new genus exhibits features considered convergent with modern batomorphs (skates and rays), including absence of contact between the posterior basicranium and first vertebral cen- trum, and a notochordal canal which fails to reach the parachordal basicranium. Supporting evi- dence that similarities in the craniovertebral articulation of squatinoids and batomorphs are convergent rather than synapomorphic (as “hypnosqualeans”) is presented by an undescribed Early Jurassic batomorph, in which an occipital hemicentrum articulates with the first vertebral centrum as in all modern sharklike (selachimorph) elasmobranchs. The fossil suggests instead that the bato- 1 Department of Vertebrate Paleontology, American Museum of Natural History, NY. -
Paleoecological Analysis of the Clayton Formation (Paleocene) Near Malvern, Arkansas
The University of Southern Mississippi The Aquila Digital Community Honors Theses Honors College Spring 5-2017 Paleoecological Analysis of the Clayton Formation (Paleocene) near Malvern, Arkansas Brenna J. Hart University of Southern Mississippi Follow this and additional works at: https://aquila.usm.edu/honors_theses Part of the Paleontology Commons Recommended Citation Hart, Brenna J., "Paleoecological Analysis of the Clayton Formation (Paleocene) near Malvern, Arkansas" (2017). Honors Theses. 513. https://aquila.usm.edu/honors_theses/513 This Honors College Thesis is brought to you for free and open access by the Honors College at The Aquila Digital Community. It has been accepted for inclusion in Honors Theses by an authorized administrator of The Aquila Digital Community. For more information, please contact [email protected]. The University of Southern Mississippi Paleoecological Analysis of the Clayton Formation (Paleocene) near Malvern, Arkansas by Brenna Hart A Thesis Submitted to the Honors College of The University of Southern Mississippi in Partial Fulfillment of the Requirements for the Degree of Bachelor of Science in the Department of Geography and Geology May 2017 II Approved by ________________________________ Franklin Heitmuller, Ph.D., Associate Professor Department of Geography and Geology ________________________________ Mark Puckett, Ph.D., Chair Department of Geography and Geology ________________________________ Ellen Weinauer, Ph.D., Dean Honors College III Abstract The Clayton Formation is a section of the Midway Group immediately above the Cretaceous-Paleogene boundary that contains marine fossils from the Paleocene Epoch. The formation is composed of glauconitic sand, clay, marl, and limestone. Fossils within the formation commonly occur in clay or are concentrated in conglomeratic lag lenses. -
Alabama and Georgia: Its Lithostratigraphy, Biostratigraphy, and Bearing on the Ag,E @F T the Claibornian Stage
The Eocene TaJJahatta Formation of Alabama and Georgia: Its Lithostratigraphy, Biostratigraphy, and Bearing on the Ag,e @f t The Claibornian Stage U.S. GEOLOGICAL SURVEY BULLETIN 1615 The Eocene Tallahatta Formation of Alabama and Georgia: Its Lithostratigraphy, Biostratigraphy, and Bearing on the Age of The Claibornian Stage By laurel M. Bybell and Thomas G. Gibson U.S. GEOlOGICAl SURVEY BUllETIN 1615 DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE 1985 For sale by the Distribution Branch, Text Products Section U.S. Geological Survey 604 South Pickett St. Alexandria, VA 22304 Library of Congress Cataloging in Publication Data Bybell, Laurel M. The Eocene Tallahatta Formation of Alabama and Georgia. <U.S. Geological Survey bulletin; 1615) Bibliography: p. Supt. of Docs. no.: I 19.3:1615 1. Geology, Stratigraphic--Eocene. 2. Geology--Alabama. 3. Geology- Georgia. I. Gibson, Thomas G. II. Title. III. Series. QE75.B9 no. 1615 557.3 s [551.7'84] 84-600098 [QE692.2] CONTENTS Abstract 1 Introduction 1 Purpose and scope 1 Acknowledgments 2 Lithostratigraphy 2 Biostratigraphy 7 Paleoenvironmental analysis 15 The Tallahatta and the age of the Claibornian Stage 17 Conclusions 18 References cited 18 PLATES [Plates follow references cited] 1. Discoaster, Tribrachiatus, Helicosphaera, Rhabdosphaera, Transversopontis, Cyclococcolithus, and Reticulofenestra 2. Reticulofenestra, Blackites, Chiasmolithus, Lophodolithus, Transversopontis, Ellipsolithus, Discoaster, Campylosphaera, and Zygrhablithus FIGURES 1. Map showing localities in Alabama and western Georgia discussed in text 2 2. Correlation chart showing age placements for the Tallahatta and other formations of late Paleocene to middle Eocene age in Alabama and Georgia 3 3.