Taxonomy and Biostratigraphy of Sabinian Palynomorphs from the Wilcox Group (Paleocene-Eocene Epochs) of Southwestern Louisiana
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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 -
A High Resolution Palynozonation for the Pennsylvanian to Lower Permian
A high resolution palynozonation for the Pennsylvanian to Lower Permian Al Khlata Formation, south Oman Randall A. Penney, Consultant Palynologist, XGL/31, Petroleum Development Oman LLC, P.O. Box 100, Muscat Post Code 113, Sultanate of Oman. Email: [email protected] Michael H. Stephenson, British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. Email: [email protected]. Issam Al Barram, XGL/3X, Petroleum Development Oman LLC, P.O. Box 100, Muscat Post Code 113, Sultanate of Oman. Email: [email protected] Key words: Al Khlata Formation, Pennsylvanian, Lower Permian, Palynology, High Resolution Biozonation, Gondwana Correlation. ABSTRACT Palynology is the main method of correlating the subsurface glaciogenic Al Khlata Formation of Oman, due to extreme lateral variability of facies, and poor seismic resolution. The chief 1 operating company in Oman, Petroleum Development Oman, has developed a robust in-house palynozonation through almost 40 years of exploration and production based on thousands of samples and hundreds of well sections. In this paper the formal definitions of the biozones are published, and the biozones are correlated in detail with faunally-calibrated palynological biozones in Western Australia, thereby allowing correlation with the standard Russian stages. Seven biozones are distinguished. The oldest, biozones 2159A and B, of probable late Pennsylvanian age, are characterised by low diversity assemblages of Punctatisporites and monosaccate pollen, with Biozone 2159A having a lower proportion of monosaccate pollen than Biozone 2159B. Biozone 2165A, of probable Asselian age, is characterised by common cingulicamerate spores and Microbaculispora Group; while Biozone 2165B contains in addition to the above, common Horriditriletes Group, and is likely to be Asselian-Sakmarian in age. -
Ludvigson Et Al-Current Research.Indd
New Insights on the Sequence Stratigraphic Architecture of the Dakota Formation, Ludvigson et al. i New Insights on the Sequence Stratigraphic Architecture of the Dakota Formation in Kansas–Nebraska–Iowa from a Decade of Sponsored Research Activity Greg A. Ludvigson, Kansas Geological Survey, The University of Kansas, Lawrence, KS Brian J. Witzke, Iowa Geological Survey, Iowa Department of Natural Resources, Iowa City, IA R. M. Joeckel, Nebraska Conservation and Survey Division, School of Natural Resources, The University of Nebraska-Lincoln, Lincoln, NE Robert L. Ravn, The IRF Group, Anchorage, AK Preston Lee Phillips, Department of Geology and Geography, University of North Carolina at Pembroke, Pembroke, NC Luis A. González, Department of Geology, The University of Kansas, Lawrence, KS Robert L. Brenner, Department of Geoscience, The University of Iowa, Iowa City, IA Abstract The Cretaceous Dakota Formation in the areas of Kansas, Nebraska, and Iowa contains a rich and well-preserved microfl ora of fossil palynomorphs. A comprehensive listing of these taxa is presented in this publication as part of a continuing effort to develop a refi ned biostratigraphic scheme for mid-Cretaceous terrestrial deposits in North America. The Dakota Formation in this region contains four distinctive Albian–Cenomanian palynostratigraphic zones that are used to partition the unit into successive depositional cycles, and each zone records deposition in fl uvial-estuarine environments. The late Albian Kiowa–Skull Creek depositional cycle at the base of the Dakota Formation is recognized throughout the study area, and is also recognized in other parts of the Cretaceous North American Western Interior basin. The overlying newly recognized latest Albian “Muddy–Mowry Cycle” is formally defi ned for the fi rst time in this paper and correlates with depositional cycles recognized by other workers in other parts of the Western Interior basin. -
Carboniferous Outcrops at La Herradura Creek, San Juan Province (Western Argentina), Revisited: Age of the Transgressions
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by CONICET Digital Andean Geology 41 (1): 83-105. January, 2014 Andean Geology doi: 10.5027/andgeoV41n1-a0410.5027/andgeoV40n2-a?? formerly Revista Geológica de Chile www.andeangeology.cl Carboniferous outcrops at La Herradura Creek, San Juan Province (Western Argentina), revisited: age of the transgressions Valeria S. Pérez Loinaze1, Carlos O. Limarino2, Silvia N. Césari1 1 Museo Argentino de Ciencias Naturales ‘Bernardino Rivadavia’, Avda. Ángel Gallardo 470, C1405DJR Buenos Aires, Argentina. [email protected]; [email protected] 2 Departamento de Geología-Instituto de Geociencias Básicas, Ambientales y Aplicadas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellón 2, C1428EHA Buenos Aires, Argentina. [email protected] ABSTRACT. At the outcrops of the Tupe Formation in the La Herradura Creek, San Juan Province, two transgressive events are recorded, which range from few meters to tens of meters in thickness. These strata correspond to the stratotype of the faunal Tivertonia jachalensis-Streptorhynchus inaequiornatus Biozone. An evaluation of the timing of the two marine transgressions is made on the basis of palynological assemblages and available radiometric ages. A short-lived transgression is recorded in the latest Bashkirian-early Moscovian, and then a substantial sea level fall took place forming an irregular incision surface. Later, a major high eustatic sea-level occurred during the middle Moscovian resulting in a more important marine ingression. The palynological assemblages associated to the older transgressive event indicate the presence of the Raistrickia densa-Convolutispora muriornata (DM) Biozone (Subzone B). -
Permian–Triassic Non-Marine Algae of Gondwana—Distributions
Earth-Science Reviews 212 (2021) 103382 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Review Article Permian–Triassic non-marine algae of Gondwana—Distributions, natural T affinities and ecological implications ⁎ Chris Maysa,b, , Vivi Vajdaa, Stephen McLoughlina a Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden b Monash University, School of Earth, Atmosphere and Environment, 9 Rainforest Walk, Clayton, VIC 3800, Australia ARTICLE INFO ABSTRACT Keywords: The abundance, diversity and extinction of non-marine algae are controlled by changes in the physical and Permian–Triassic chemical environment and community structure of continental ecosystems. We review a range of non-marine algae algae commonly found within the Permian and Triassic strata of Gondwana and highlight and discuss the non- mass extinctions marine algal abundance anomalies recorded in the immediate aftermath of the end-Permian extinction interval Gondwana (EPE; 252 Ma). We further review and contrast the marine and continental algal records of the global biotic freshwater ecology crises within the Permian–Triassic interval. Specifically, we provide a case study of 17 species (in 13 genera) palaeobiogeography from the succession spanning the EPE in the Sydney Basin, eastern Australia. The affinities and ecological im- plications of these fossil-genera are summarised, and their global Permian–Triassic palaeogeographic and stra- tigraphic distributions are collated. Most of these fossil taxa have close extant algal relatives that are most common in freshwater, brackish or terrestrial conditions, and all have recognizable affinities to groups known to produce chemically stable biopolymers that favour their preservation over long geological intervals. -
Peat-Forming Environment of Permian Coal Seams from the Faxinal Coalfield (Paraná Basin) in Southern Brazil, Based on Palynology and Palaeobotany
Rev. bras. paleontol. 10(2):117-127, Maio/Agosto 2007 © 2007 by the Sociedade Brasileira de Paleontologia PEAT-FORMING ENVIRONMENT OF PERMIAN COAL SEAMS FROM THE FAXINAL COALFIELD (PARANÁ BASIN) IN SOUTHERN BRAZIL, BASED ON PALYNOLOGY AND PALAEOBOTANY MIRIAM CAZZULO-KLEPZIG, MARGOT GUERRA-SOMMER, RUALDO MENEGAT Instituto de Geociências, UFRGS, Av. Bento Gonçalves, 9500, 91501-970, Porto Alegre, RS, Brazil. [email protected], [email protected], [email protected] MARGARETE WAGNER SIMAS Programa de Pós Graduação em Geociências, UFRGS, Av.Bento Gonçalves, 9500, 91501-970, Porto Alegre, RS, Brazil. [email protected] JOÃO GRACIANO MENDONÇA FILHO Instituto de Geociências, UFRJ, Prédio de Ciências e Matemática, Bloco F, Ilha do Fundão, 21941-590, RJ, Brazil. [email protected] ABSTRACT – Coal seams from the Faxinal coalfield (Rio Bonito Formation, Lower Permian of Paraná Basin) are compositionally distinct from other South Brazilian coal palynofloras. The dominance of bisaccate and striate pollen grains such as Alisporites, Scheuringipollenites, Limitisporites, Vesicaspora and Protohaploxypinus in the palynofloras reflect a peat-forming plant community composed namely of glossopterids, cordaites and conifers. Subordinate trilete spores derived from lycopsids, sphenopsids and filicopsids (e.g. Lundbladispora, Punctatisporites, Granulatisporites, Leiotriletes, Deltoidospora, Calamospora) are less abundant, occurring in variable proportions. Algae-like elements, commonly found in south Brazilian coal palynofloras (Portalites, Tetraporina, -
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. -
Cretaceous Strata of Western Alabama
Studies of Pre-Selma Cretaceous Core Samples From the Outcrop Area in Western Alabama GEOLOGICAL SURVEY BULLETIN 1160 A group of papers by W: H. Monroe, R. E. Bergenback, N. F. Soh/, E. R. Applin, E. B. Leopold, H. M. Pakiser, and L. C. Conant UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 PREFACE In 1954 four core holes were drilled in the pre-Selma Cretaceous strata of the Alabama Coastal Plain in order to get unweathered samples within a few miles of the outcrops. During the next few years several specialists studied the cores, and their reports are published as consecutive parts of this bulletin. Watson H. Monroe, who spent many years studying the Coastal Plain strata in Alabama and Mississippi, conceived and supervised the drilling and planned the later studies. His earlier published re port (W. H. Monroe, 1955, Cores of pre-Selma Cretaceous rocks in the outcrop area in western Alabama: Gulf Coast Geol. Societies Trans., v. 5, p. 11-37) contains a brief description of the stratigraphy, together with logs and other information regarding the core holes, and he has provided the introductory chapter to this bulletin. Rich ard E. Bergenback studied the petrology of the cores, which included finding the distribution of grain sizes, determining the mineralogy of the grains and the matrix of the sediments, and having X-Ray iden tifications made of the clay minerals. -
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. -
Early Cenomanian Palynofloras and Inferred Resiniferous
Early Cenomanian palynofloras and inferred resiniferous forests and vegetation types in Charentes (southwestern France) Daniel Peyrot, Eduardo Barron, France Polette, David Batten, Didier Néraudeau To cite this version: Daniel Peyrot, Eduardo Barron, France Polette, David Batten, Didier Néraudeau. Early Cenomanian palynofloras and inferred resiniferous forests and vegetation types in Charentes (southwestern France). Cretaceous Research, Elsevier, 2019, 94, pp.168-189. 10.1016/j.cretres.2018.10.011. insu-01897273 HAL Id: insu-01897273 https://hal-insu.archives-ouvertes.fr/insu-01897273 Submitted on 17 Oct 2018 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. Accepted Manuscript Early Cenomanian palynofloras and inferred resiniferous forests and vegetation types in Charentes (southwestern France) Daniel Peyrot, Eduardo Barrón, France Polette, David J. Batten, Didier Néraudeau PII: S0195-6671(18)30252-0 DOI: 10.1016/j.cretres.2018.10.011 Reference: YCRES 3988 To appear in: Cretaceous Research Received Date: 21 June 2018 Revised Date: 19 September 2018 Accepted Date: 12 October 2018 Please cite this article as: Peyrot, D., Barrón, E., Polette, F., Batten, D.J., Néraudeau, D., Early Cenomanian palynofloras and inferred resiniferous forests and vegetation types in Charentes (southwestern France), Cretaceous Research (2018), doi: https://doi.org/10.1016/j.cretres.2018.10.011. -
Bureau of Economic Geology W
Bureau of Economic Geology W. L. Fisher, Director ad interim The University of Texas at Austin • Austin, Texas 78713-8924 • 1999 Report of Investigations No. 256 Groundwater Availability in the Carrizo-Wilcox Aquifer in Central Texas Numerical Simulations of 2000 through 2050 Withdrawal Projections by Alan R. Dutton Sponsored by Texas Water Development Board Contract No. 99-483-279 Cosponsored by San Antonio Water System Alcoa Inc. Aqua Water Supply Corporation Bureau of Economic Geology ~ 9 W. L. Fisher, Director ad interim ~ .. The University of Texas at Austin • Austin, Texas 78713-8924 • 1999 CONTENTS Abstract ............................................................................................................................................ 1 Introduction ................................................................................................................................... 1 Purpose and Objectives .................................................................................................................. 1 Conceptual Hydrogeologic Model ........................................................................................... 4 Data Availability .............................................................................................................................. 4 Hydrostratigraphy .......................................................................................................................... 4 Flow Paths and Flow Rates ............................................................................................................ -
Correlation of the Eocene Formations in Mississippi and Alabama
CORRELATION OF THE EOCENE FORMATIONS IN MISSISSIPPI AND ALABAMA By WYTHE CooKE INTRODUCTION clay and carbonaceous mate,rial were laid down in During Eocene time the site of the boundary be Mississippi, while shell marl, laminated sand, and tween the States of Mississippi and Alabama fell limestone were being formed in Alabama. The pur within the transition zone between the ¥ississippi pose of this paper is to point out the equivalences of embayment and the open Gulf of Mexico. That dif formations of different facies in the two States. The ferent types of deposition proceeded simultaneously correlation adopted is shown in the following table, within these two regions may be inferred from the all the formation names in which have been previ different facies which deposits of the same age exhibit ously used, except Kosciusko sandstone, a new name on opposite sides of the State line. In general, much proposed for a member of the Lisbon formation. Correlation of Eocene formations in Mississippi and Alabama Mississippi Alabama I Yazoo clay member Jackson Jackson ····························-······················---------·---·--·-········------------·····------- ---- --- Ocala limestone formation forma- east of Tombigbee River Moodys marl member tion I· Yegua formation Gosport sand i P. ;::! I 0 ························-····················------ ----- ------- -- --· ·······- -- -------------················ bh Lisbon ~ ~ forma- Kosciusko sandstone member Lisbon formation 1-o 0 tion :9 --··········-·····--------- -- -- --- ----- ---- ----- ------ -----·--------- -- -- -- ---· - --· ···········-- --- -- -- -- - • ~ 0 Winona sand member I Tallahatta formation Over- Grenada formation lapped Hatchetigbee formation area 0.. ;::! 0 Absent Bashi formation 6h M 0 0 Holly Springs sand Tuscahoma formation ~ I Over- lapped near Over- Tennessee Ackerman formation lapped Nanafalia formation boundary area Unex- I 0.. Tippah sandstone member plored Naheola formation ;::! Porters area 0 Creek to clay ...................