Taphonomy of Three Monospecific Dinosaur Bone Beds in the Late

Total Page:16

File Type:pdf, Size:1020Kb

Taphonomy of Three Monospecific Dinosaur Bone Beds in the Late University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1989 Taphonomy of three monospecific dinosaur bone beds in the Late Cretaceous Two Medicine Formation northwestern Montana: Evidence for dinosaur mass mortality related to episodic drought Raymond R. Rogers The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Rogers, Raymond R., "Taphonomy of three monospecific dinosaur bone beds in the Late Cretaceous Two Medicine Formation northwestern Montana: Evidence for dinosaur mass mortality related to episodic drought" (1989). Graduate Student Theses, Dissertations, & Professional Papers. 5871. https://scholarworks.umt.edu/etd/5871 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. COPYRIGHT ACT OF 1975 Th is is an unpublished m anuscript in which copyright SUBSISTS. A ny further r e p r in t in g of it s contents must be APPROVED BY THE AUTHOR. Mansfield Library University of Montana Date ; 1 9 B3 TAPHONOMY OF THREE MONOSPECIFIC DINOSAUR BONE BEDS IN THE LATE CRETACEOUS TWO MEDICINE FORMATION, NORTHWESTERN MONTANA; EVIDENCE FOR DINOSAUR MASS MORTALITY RELATED TO EPISODIC DROUGHT by Raymond R. Rogers B.S. Northern Arizona University, 1985 Presented in partial fulfillment of the requirements for the degree Master of Science University of Montana 1989 Approved by: Ccy^j^airman, Board of Examiners ----------------- Co-Chairman, Board of Examiners Derfh, Graduate School ^ i kL '/ Date UMI Number: EP36672 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT DituMTtaéon RjMuUiiing UMI EP36672 Published by ProQuest LLC (2013). Copyright in the Dissertation held by the Author. Microform Edition © ProQuest LLC. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code ProOuesf ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 Rogers, Raymond R., M.S., June 1989 Geology Taphonomy of Three Monospecific Dinosaur Bone Beds in the Late Cretaceous Two Medicine Formation, Northwestern Montana: Evidence for Dinosaur Mass M ortality Related to Episodic Drought (102 pp.) D irectors: John R. Horner Donald Winston ^ Monospecific and "single-species dominated" dinosaur bone beds are relatively common within the alluvial sedi­ ments of the Late Cretaceous (Campanian) Two Medicine Formation of northwestern Montana. Taphonomic analysis of three monospecific dinosaur bone beds in the upper litho- facies of the formation suggests dinosaur mass mortality related to episodic drought. Two of the bone beds. Canyon Bone Bed and Dino Ridge Quarry, preserve the remains of an as yet undescribed species of S tyrac osaurus. The third bone bed, Westside Quarry, preserves skeletal remains of undescribed prosauralophan hadrosaurs. Taphonomic and geo­ logic data indicate that all three dinosaur quarries are autochthonous, non-catastrophic mass mortality fossil assemblages. The styracosaurs in Canyon Bone Bed and Dino Ridge Quarry are buried in shallow, vegetated oxbow lake paleoenvironments. The prosauralophan hadrosaurs of West- side Quarry are interred within and around what may have been an ephemeral floodplain water hole. Pa le oc11 matic data suggest that the Two Medicine coastal plain was affected by a seasonal, semiarid, and warm climate during the la te s t Campanian. Each of the three bone beds is S t ratigraphically associated with sediments reflecting ab­ normally dry conditions, and I propose that episodic regional drought, and resultant malnutrition and disease, lead to the mass mortality events responsible for all three bone beds. Assuming a genetic re latio n sh ip between drought and the three bone beds, certain autécologie inferences can be drawn. The styracosaurs preserved within Canyon Bone Bed and Dino Ridge Quarry and the prosauralophan hadrosaurs of Westside Quarry may have been water-dependent species. During periods of drought, these particular dinosaurs may have had to remain close to perennial water sources. The monospecific nature of the quarries suggests that the dino­ saur species under investigation were probably social, herding animals during periods of water-stress, possibly year-round. Partitioning of dry season resources by dino­ saurs on the Two Medicine coastal plain, trophic dynamics, and interspecific aggression and territorial behavior are all possible motives behind the monospecific character of the three bone beds. 11 ACKNOWLEDGMENTS I would like to express my sincere gratitude to the mem­ bers of my thesis committee: Dr. John R. Horner, Dr. Donald Winston, Dr. Robert W. Fields, and Dr. Kerry Foresman. Their insight, encouragement, and editorial assistance are greatly appreciated. I would especially lik e to thank Jack Horner for the opportunity to work on his three bone beds. I also extend thanks to Pat Leiggi, Ken Carpenter, and the late Robert Makela for invaluable conversations and ideas. Robert Makela also graciously shared his time and knowledge familiarizing me with collecting dinosaurs. Dr. Greg Retallack provided assistance in understanding and in te rp re tin g paleosols, and Ed Brook, John Kruger, Pat Reynolds, and Kirsty Erickson all furnished help in the fie ld . I am very g ratefu l to Ricky Reagan and Gloria Sundquist for allowing access to their ranches. I would also like to thank Dr. James Sears, Dr. David Alt, and Scott Sampson for helpful discussions, and John Cuplin for assistance with my graphics. Lastly, I would like to thank the M.O.R. field crews; without their help none of this would have been possible. This research was partly funded by a Sigma-Xi Society grant awarded to the author and by National Science Foundation Grant No. EAR 8705986 and a John and Catherine MacArthur Foundation Fellowship, both of which were awarded to J. R. Horner. I ll TABLE OF CONTENTS PAGE ABSTRACT .......................................................................................................................... ii ACKNOWLEDGEMENTS ................................................................................................... i l l TABLE OF CONTENTS ............................................................................................... iv-v LIST OF ILLUSTRATIONS .............................................................................. v i-v ii PART ONE— INTRODUCTION ................................................................................. 1 Landslide Butte Field Area ............................................................ 6 Procedure .............................................................................................................. 8 PART TWO—TWO MEDICINE FORMATION ................................................... 11 General Geology ............................................................................................ 11 Structural Setting ................................................................................... 14 Stratigraphy and Sedimentology ................................................ 16 Paleogeography ............................................................................................... 25 Paleoclimate ..................................................................................................... 28 PART THREE--TAPHONOMIC DATA .................................................................. 33 CANYON BONE BED ............................................................................................. 38 GEOLOGIC DATA-- Stratigraphy, Sedimentology, and Depositional Environment ................................. 38 Physical and Chemical Modifications ........................ 40 BIOLOGIC DATA-- Biologic Constraints ..................................................................... 44 Biologic Modifications ............................................................... 44 1 V LIST OF ILLUSTRATIONS FIGURE.............................................................................................................................................PAGE 1. Location Map, Landslide Butte Field Area ........................ 7 2. Generalized Outcrop Map, Two Medicine Formation ........................................................................................................... 12 3. Montana Group Stratigraphy, Northwestern and North-Central Montana ........................................................................ 14 4. Fence Diagram Illu s tra tin g S tratigraphie Relationships of the Two Medicine Formation ... 17 5. Photograph of Two Red Horizons in the Landslide Butte Field Area ...................................................................................... 21 6. Photograph of a Typical Sandstone Channel Deposit in the Landslide Butte Field Area ............ 23 7. Photograph of Root Casts and Burrows on the Uppermost Surface of a Landslide Butte Paleo-channel ..............................................................................................
Recommended publications
  • Feeding Height Stratification Among the Herbivorous
    Mallon et al. BMC Ecology 2013, 13:14 http://www.biomedcentral.com/1472-6785/13/14 RESEARCH ARTICLE Open Access Feeding height stratification among the herbivorous dinosaurs from the Dinosaur Park Formation (upper Campanian) of Alberta, Canada Jordan C Mallon1,5*, David C Evans2, Michael J Ryan3 and Jason S Anderson4 Abstract Background: Herbivore coexistence on the Late Cretaceous island continent of Laramidia has been a topic of great interest, stemming from the paradoxically high diversity and biomass of these animals in relation to the relatively small landmass available to them. Various hypotheses have been advanced to account for these facts, of which niche partitioning is among the most frequently invoked. However, despite its wide acceptance, this hypothesis has not been rigorously tested. This study uses the fossil assemblage from the Dinosaur Park Formation of Alberta as a model to investigate whether niche partitioning facilitated herbivorous dinosaur coexistence on Laramidia. Specifically, the question of feeding height stratification is examined in light of the role it plays in facilitating modern ungulate coexistence. Results: Most herbivorous dinosaur species from the Dinosaur Park Formation were restricted to feeding no higher than approximately 1 m above the ground. There is minimal evidence for feeding height partitioning at this level, with ceratopsids capable of feeding slightly higher than ankylosaurs, but the ecological significance of this is ambiguous. Hadrosaurids were uniquely capable of feeding up to 2 m quadrupedally, or up to 5 m bipedally. There is no evidence for either feeding height stratification within any of these clades, or for change in these ecological relationships through the approximately 1.5 Ma record of the Dinosaur Park Formation.
    [Show full text]
  • A Phylogenetic Analysis of the Basal Ornithischia (Reptilia, Dinosauria)
    A PHYLOGENETIC ANALYSIS OF THE BASAL ORNITHISCHIA (REPTILIA, DINOSAURIA) Marc Richard Spencer A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements of the degree of MASTER OF SCIENCE December 2007 Committee: Margaret M. Yacobucci, Advisor Don C. Steinker Daniel M. Pavuk © 2007 Marc Richard Spencer All Rights Reserved iii ABSTRACT Margaret M. Yacobucci, Advisor The placement of Lesothosaurus diagnosticus and the Heterodontosauridae within the Ornithischia has been problematic. Historically, Lesothosaurus has been regarded as a basal ornithischian dinosaur, the sister taxon to the Genasauria. Recent phylogenetic analyses, however, have placed Lesothosaurus as a more derived ornithischian within the Genasauria. The Fabrosauridae, of which Lesothosaurus was considered a member, has never been phylogenetically corroborated and has been considered a paraphyletic assemblage. Prior to recent phylogenetic analyses, the problematic Heterodontosauridae was placed within the Ornithopoda as the sister taxon to the Euornithopoda. The heterodontosaurids have also been considered as the basal member of the Cerapoda (Ornithopoda + Marginocephalia), the sister taxon to the Marginocephalia, and as the sister taxon to the Genasauria. To reevaluate the placement of these taxa, along with other basal ornithischians and more derived subclades, a phylogenetic analysis of 19 taxonomic units, including two outgroup taxa, was performed. Analysis of 97 characters and their associated character states culled, modified, and/or rescored from published literature based on published descriptions, produced four most parsimonious trees. Consistency and retention indices were calculated and a bootstrap analysis was performed to determine the relative support for the resultant phylogeny. The Ornithischia was recovered with Pisanosaurus as its basalmost member.
    [Show full text]
  • Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex
    Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex By Karen E. Poole B.A. in Geology, May 2004, University of Pennsylvania M.A. in Earth and Planetary Sciences, August 2008, Washington University in St. Louis A Dissertation submitted to The Faculty of The Columbian College of Arts and Sciences of The George Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy August 31, 2015 Dissertation Directed by Catherine Forster Professor of Biology The Columbian College of Arts and Sciences of The George Washington University certifies that Karen Poole has passed the Final Examination for the degree of Doctor of Philosophy as of August 10th, 2015. This is the final and approved form of the dissertation. Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex Karen E. Poole Dissertation Research Committee: Catherine A. Forster, Professor of Biology, Dissertation Director James M. Clark, Ronald Weintraub Professor of Biology, Committee Member R. Alexander Pyron, Robert F. Griggs Assistant Professor of Biology, Committee Member ii © Copyright 2015 by Karen Poole All rights reserved iii Dedication To Joseph Theis, for his unending support, and for always reminding me what matters most in life. To my parents, who have always encouraged me to pursue my dreams, even those they didn’t understand. iv Acknowledgements First, a heartfelt thank you is due to my advisor, Cathy Forster, for giving me free reign in this dissertation, but always providing valuable commentary on any piece of writing I sent her, no matter how messy.
    [Show full text]
  • Dinosaur Eggshells from the Lower Maastrichtian St. Mary River Formation of Southern Alberta, Canada
    Canadian Journal of Earth Sciences Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0195.R1 Manuscript Type: Article Date Submitted by the Author: 13-Nov-2017 Complete List of Authors: Voris, Jared; University of Calgary, Geoscience; Zelenitsky, Darla; Department of Geoscience, Tanaka, Kohei; Nagoya Daigaku Hakubutsukan; University of Calgary, DepartmentDraft of Geoscience Therrien, François; Royal Tyrrell Museum of Palaeontology, Is the invited manuscript for consideration in a Special N/A Issue? : Keyword: eggshell, dinosaur, Cretaceous, Maastrichtian, Alberta https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 47 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern 10 Alberta, Canada 11 12 Jared T. Voris, Darla K. Zelenitsky,Draft François Therrien, Kohei Tanaka 13 J. T. Voris, D. K. Zelenitsky, and K. Tanaka. Department of Geoscience, University of 14 Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada; [email protected], 15 [email protected], [email protected] 16 K. Tanaka. Nagoya University Museum, Nagoya University Furocho, Chikusa-Ku, Nagoya, 17 464-8601, Japan; [email protected] 18 F. Therrien. Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, 19 Canada.; [email protected] 20 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 47 1 2 Abstract–North America is known for its rich uppermost Cretaceous record of dinosaur egg 3 remains, although a notable fossil gap exists during the lower Maastrichtian.
    [Show full text]
  • Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
    www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5.
    [Show full text]
  • A New Ankylosaurid Skeleton from the Upper Cretaceous
    www.nature.com/scientificreports OPEN A new ankylosaurid skeleton from the Upper Cretaceous Baruungoyot Formation of Mongolia: its implications for ankylosaurid postcranial evolution Jin‑Young Park1, Yuong‑Nam Lee1*, Philip J. Currie2, Michael J. Ryan3,4, Phil Bell5, Robin Sissons2, Eva B. Koppelhus2, Rinchen Barsbold6, Sungjin Lee1 & Su‑Hwan Kim1 A new articulated postcranial specimen of an indeterminate ankylosaurid dinosaur from the Upper Cretaceous (middle‑upper Campanian) Baruungoyot Formation from Hermiin Tsav, southern Gobi Desert, Mongolia includes twelve dorsal vertebrae, ribs, pectoral girdles, forelimbs, pelvic girdles, hind limbs, and free osteoderms. The new specimen shows that Asian ankylosaurids evolved rigid bodies with a decreased number of pedal phalanges. It also implies that there were at least two forms of fank armor within Ankylosauridae, one with spine‑like osteoderms and the other with keeled rhomboidal osteoderms. Unique anatomical features related to digging are present in Ankylosauridae, such as dorsoventrally fattened and fusiform body shapes, extensively fused series of vertebrae, anteroposteriorly broadened dorsal ribs, a robust humerus with a well‑developed deltopectoral crest, a short robust ulna with a well‑developed olecranon process, a trowel‑like manus, and decreased numbers of pedal phalanges. Although not fossorial, ankylosaurids were likely able to dig the substrate, taking advantage of it for self‑defence and survival. Ankylosaurs were herbivorous quadrupedal dinosaurs characterized by heavily ornamented skulls and transverse rows of osteoderms that covered the dorsolateral surfaces of their bodies1. Abundant remains of ankylosaurs have been found in Mongolia, and a total of nine taxa are currently known (Table 1). However, most of the taxa are based on skulls, whereas articulated postcranial specimens are scarce, with only three specimens currently described in the scientifc literature 2–4.
    [Show full text]
  • Collaborative Multimedia Judy Diamond University of Nebraska–Lincoln, [email protected]
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Alan Bond Publications Papers in the Biological Sciences 1995 Collaborative Multimedia Judy Diamond University of Nebraska–Lincoln, [email protected] Alan B. Bond University of Nebraska-Lincoln, [email protected] Beth Schenker University of Nebraska–Lincoln Debra Meier University of Nebraska-Lincoln, [email protected] Dana Twersky University of Nebraska State Museum Follow this and additional works at: http://digitalcommons.unl.edu/bioscibond Part of the Animal Sciences Commons, Biodiversity Commons, Ecology and Evolutionary Biology Commons, Environmental Studies Commons, Museum Studies Commons, and the Science and Technology Studies Commons Diamond, Judy; Bond, Alan B.; Schenker, Beth; Meier, Debra; and Twersky, Dana, "Collaborative Multimedia" (1995). Alan Bond Publications. 12. http://digitalcommons.unl.edu/bioscibond/12 This Article is brought to you for free and open access by the Papers in the Biological Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Alan Bond Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Collaborative Multimedia Judy Dia17101Ul, Alan Bond, Beth Schenker, Debra Meier, Dana Twersky ABSTRACT Six ~atur~ hist~~ institutions contributed video and other images to produce a single multimedia exhibit about famous paleontology sites throughout the United States. In Mesozoic Monsters. Mammals and Magnolias. users can view videos of the original excavation of each of the sites and also play computer games relating to each location. This project provides a model for how collaboration among museums can reduce the cost of multimedia exhibits while improving quality and making them available to wider audiences. MULTIMEDIA PARTNERSHIP The small girl examines the bones of a mosasaur, a giant fossil reptile 20 times her size.
    [Show full text]
  • A New Basal Ornithopod Dinosaur from the Lower Cretaceous of China
    A new basal ornithopod dinosaur from the Lower Cretaceous of China Yuqing Yang1,2,3, Wenhao Wu4,5, Paul-Emile Dieudonné6 and Pascal Godefroit7 1 College of Resources and Civil Engineering, Northeastern University, Shenyang, Liaoning, China 2 College of Paleontology, Shenyang Normal University, Shenyang, Liaoning, China 3 Key Laboratory for Evolution of Past Life and Change of Environment, Province of Liaoning, Shenyang Normal University, Shenyang, Liaoning, China 4 Key Laboratory for Evolution of Past Life and Environment in Northeast Asia, Ministry of Education, Jilin University, Changchun, Jilin, China 5 Research Center of Paleontology and Stratigraphy, Jilin University, Changchun, Jilin, China 6 Instituto de Investigación en Paleobiología y Geología, CONICET, Universidad Nacional de Río Negro, Rio Negro, Argentina 7 Directorate ‘Earth and History of Life’, Royal Belgian Institute of Natural Sciences, Brussels, Belgium ABSTRACT A new basal ornithopod dinosaur, based on two nearly complete articulated skeletons, is reported from the Lujiatun Beds (Yixian Fm, Lower Cretaceous) of western Liaoning Province (China). Some of the diagnostic features of Changmiania liaoningensis nov. gen., nov. sp. are tentatively interpreted as adaptations to a fossorial behavior, including: fused premaxillae; nasal laterally expanded, overhanging the maxilla; shortened neck formed by only six cervical vertebrae; neural spines of the sacral vertebrae completely fused together, forming a craniocaudally-elongated continuous bar; fused scapulocoracoid with prominent
    [Show full text]
  • Thesis, Dissertation
    SCRATCH-DIGGING IN THE CRETACEOUS BASAL ORNITHOPOD DINOSAUR ORYCTODROMEUS CUBICULARIS: EVIDENCE FROM MORPHOMETRIC ANALYSES AND RECONSTRUCTION OF THE FORELIMB MUSCULATURE by Jamie Lynn Fearon A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Science MONTANA STATE UNIVERSITY Bozeman, Montana May 2013 ©COPYRIGHT by Jamie Lynn Fearon 2013 All Rights Reserved ii APPROVAL of a thesis submitted by Jamie Lynn Fearon This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citation, bibliographic style, and consistency and is ready for submission to The Graduate School. David J. Varricchio Approved for the Department of Earth Sciences David Mogk Approved for The Graduate School Ronald W. Larsen iii STATEMENT OF PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Montana State University, I agree that the Library shall make it available to borrowers under rules of the Library. If I have indicated my intention to copyright this thesis by including a copyright notice page, copying is allowable only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Requests for permission for extended quotation from or reproduction of this thesis in whole or in parts may be granted only by the copyright holder. Jamie Lynn Fearon May 2013 iv TABLE OF CONTENTS 1. INTRODUCTION ...........................................................................................................1
    [Show full text]
  • Oil and Gas Geology of the Birch Creek-Sun River Area, Northwestern Montana
    OIL AND GAS GEOLOGY OF THE BIRCH CREEK-SUN RIVER AREA, NORTHWESTERN MONTANA. By EUGENE STEBINGER. INTRODUCTION. The area described in this paper lies adjacent to the front range of the Rocky Mountains in northwestern Montana and is part of a large region in the northern Great Plains of the United States and Canada which seems to deserve consideration as prospective territory for oil and gas development. The thick bodies of Upper Cretaceous shale, the sands of which have yielded the greater part of the oil produced in Wyoming and Colorado and large quantities of gas in Alberta, underlie much of this region, in many places at depths that can be reached by the drill. The outcrops of .these Cretaceous forma­ tions afford unquestionable evidence of being petroliferous, so that drilling in places of favorable structure, .such as on well-developed domes or anticlines, seems to offer a reasonable chance of success. It is certain that the plains of northwestern Montana can not be classed as barren of oil until a considerable number of the favorable lo­ calities have been carefully drilled. Random drilling regardless of the lay of the rocks, such as has been undertaken up to the present time, has been uniformly unsuccessful. Moreover, even though the region as a whole should eventually prove to contain fair amounts of oil, the area actually underlain by commercial pools might comprise much less than 1 per cent of the total area underlain by the Cretaceous formations, so that the chances of success by random locations are very slight. Predictions of oil pools from a formation some hundreds of miles beyond localities where it has already proved productive, on the basis of identical geologic age and kind of rock and un­ doubted indications that it is petroliferous, have often proved unwarranted in the Rocky Mountain region, especially in parts of southern Wyoming and western Colorado, and also in other parts of the United States.
    [Show full text]
  • Two Examples from the Late Cretaceous of Western North America
    Paleobotanical Estimates of Climate in Deep Time: Two Examples From the Late Cretaceous of Western North America Garland Upchurch1, Ann Marie Prue1, Joan Parrott1, Emilio Estrada-Ruiz2, and Dori Contreras3 1 Texas State University, San Marcos, TX 2 National Polytechnic Institute of Mexico, Mexico City, Mexico 3 University of California, Berkeley, CA Introduction • Paleobotany provides important information on paleoclimate. – Shallow geologic time • Closest living relatives of fossil plant species • Paleoclimate inferred from modern species distributions – Deep geologic time • Relationships with extant species and genera more distant. • Adaptive characteristics of plants – Physiognomy • Paleoclimate inferred from relation between plant adaptive characteristics and modern climate Physiognomy • Physiognomy: Adaptive features of plant structure – Environment: Evolved multiple times – Life form (PFT) – Organs – Tissue structure Tropical leaf (left) vs. • Leaves of dicot flowering plants temperate zone leaf – Margin, shape, size • Woods – Presence/absence of annual rings – Dicot woods: Amount of soft tissue, water conduit diameter, other features Tropical (balsa) wood Physiognomic Methods • Leaves – Simple Linear Regression • Leaf Margin Analysis (LMA) – Mean Annual Temperature (MAT) • Leaf Area Analysis (LAA) Left to right: – Mean Annual Precipitation (MAP) Tropical, desert, and – Multivariate ordination temperate leaves • Climate Leaf Analysis Multivariate Program (CLAMP) • Mean annual and seasonal temperatures, precipitation – Multiple regression
    [Show full text]
  • Tectonic and Sedimentary Controls, Age and Correlation of the Upper Cretaceous Wahweap Formation, Southern Utah, U.S.A
    i Tectonic and sedimentary controls, age and correlation of the Upper Cretaceous Wahweap Formation, southern Utah, U.S.A. Zubair Ali Jinnah A thesis submitted to the Faculty of Science, University of the Witwatersrand, in fulfilment of the requirements for the degree of Doctor of Philosophy Johannesburg 2011 ii Declaration I declare that this dissertation is my own, unaided work. It is being submitted for the Degree of Doctor of Philosophy in the University of the Witwatersrand, Johannesburg. It has not been submitted before for any degree or examination in any other University (Zubair Ali Jinnah) On the 10th day of October 2011 iii Abstract The Wahweap Formation is an ~400 m thick clastic sedimentary succession of fluvial and estuarine channel sandstones and floodbasin mudrocks that was deposited in western North America during the Late Cretaceous. It preserves important mammal, dinosaur, crocodile, turtle and invertebrate fossils that have been the subject of recent palaeontological investigations. The Wahweap Formation can be divided into lower, middle, upper, and capping sandstone members based on sand:mud ratios and degree of sandstone amalgamation. Facies analysis reveals the presence of ten facies associations grouped into channel and floodbasin deposits. Facies associations (FAs) from channels include: (1) single-story and (2) multistory lenticular sandstone bodies, (3) major tabular sandstone bodies, (4) gravel bedforms, (5) low-angle heterolithic cross-strata, and (10) lenticular mudrock, whereas floodbasin facies associations include: (6) minor tabular sandstone bodies, (7) lenticular interlaminated sandstone and mudrock, (8) inclined interbedded sandstone and mudrock, and (9) laterally extensive mudrock. The lower and middle members are dominated by floodbasin facies associations.
    [Show full text]