A High-Resolution 3-D Architecture of a Cretaceous Point Bar Using Terrestrial Laser Scanning of Multiple Exposures

Total Page:16

File Type:pdf, Size:1020Kb

A High-Resolution 3-D Architecture of a Cretaceous Point Bar Using Terrestrial Laser Scanning of Multiple Exposures A HIGH-RESOLUTION 3-D ARCHITECTURE OF A CRETACEOUS POINT BAR USING TERRESTRIAL LASER SCANNING OF MULTIPLE EXPOSURES: A FAR MORE COMPLEX MODEL OF BAR GROWTH AT THE SCALE OF A STEAM CHAMBER THAN PREVIOUSLY THOUGHT by MATTHEW PALMER Presented to the Faculty of the Graduate School of Texas Christian University in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE IN GEOLOGY TEXAS CHRISTIAN UNIVERSITY AUGUST 2015 ACKNOWLEDGEMENTS There are many people who have been vital to the success of this project. First, I would like to thank my advisor, Dr. John Holbrook for his instructions, insights, and means to accomplish this work. I am also indebted to Tamie Morgan and Xiangiang Xie (PhD) as committee members for this project. I am grateful for the assistance of Alex Torres who made this study enjoyable and also contributed valuable ideas. I am thankful to Lionel and Sally White, Carlos Aiken PhD., Tara Urbanski, and Becky Aguilar from the University of Texas at Dallas for their help in shooting and processing the photo-realistic LiDAR model. Also, collaboration with Stephen Hubbard and Paul Durkin from the University of Calgary was extremely valuable as they are familiar with the field area and provided important insights and guidance. Chris Seibel and colleagues at Nexen provided significant feedback and support. And finally, to Bruce Vanderlou who allowed us full access to the field area through his private property. Most importantly, I would like to thank my family, in particular my wife Chelsea and Daughter Lydia who will always be the reason and inspiration I need to accomplish hard things. ii TABLE OF CONTENTS ACKNOWLEDGEMENTS ....................................................................................................................................ii TABLE OF CONTENTS ...................................................................................................................................... iii LIST OF FIGURES ..............................................................................................................................................v LIST OF TABLES .............................................................................................................................................. vii CHAPTER 1 INTRODUCTION ............................................................................................................................ 1 1.1 AN OVERVIEW OF POINT BAR FORMATION ....................................................................................................... 2 1.2 TYPES OF POINT-BARS.................................................................................................................................. 6 1.2.1 The “Normal” Point Bar ................................................................................................................. 6 1.2.2 The “Normal Muddy” Point Bar ..................................................................................................... 8 1.2.3 The Counter Point Bar .................................................................................................................... 8 1.2.4 The Pseudo Point Bar ..................................................................................................................... 9 1.3 HETEROGENEITY OF POINT BARS .................................................................................................................. 10 1.4 THE “SADLER EFFECT” IN POINT BARS............................................................................................................ 11 1.5 THE BELLY RIVER GROUP ............................................................................................................................ 14 1.5.1 The Foremost Formation.............................................................................................................. 16 1.5.2 The Oldman Formation ................................................................................................................ 16 1.5.3 The Dinosaur Park Formation ...................................................................................................... 17 1.6 HYPOTHESES AND PREDICTIONS ................................................................................................................... 17 CHAPTER 2 METHODS ................................................................................................................................... 19 2.1 LOCATION ............................................................................................................................................... 19 2.2 STRATIGRAPHIC SECTIONS .......................................................................................................................... 21 2.3 LIDAR ACQUISITION ................................................................................................................................... 21 2.4 ARCHITECTURAL-ELEMENT ANALYSIS............................................................................................................. 23 2.5 DRAPE DISTRIBUTION CALCULATIONS ............................................................................................................ 24 CHAPTER 3 RESULTS ..................................................................................................................................... 26 3.1 STRATIGRAPHIC SECTIONS .......................................................................................................................... 26 3.1.1 Point Bar Lithofacies .................................................................................................................... 26 iii 3.1.2 Drape Types ................................................................................................................................. 27 3.1.3 Paleocurrent Measurements ....................................................................................................... 36 3.2 LIDAR MODEL AND ARCHITECTURAL-ELEMENT ANALYSIS ................................................................................... 39 3.3 DRAPE MEASUREMENTS ............................................................................................................................. 50 3.3.1 Area 1 ........................................................................................................................................... 53 3.3.2 Area 2 ........................................................................................................................................... 56 3.3.3 Area 3 ........................................................................................................................................... 61 CHAPTER 4 DISCUSSION ............................................................................................................................... 65 4.1 STRATIGRAPHIC SECTIONS .......................................................................................................................... 65 4.2 ARCHITECTURAL-ELEMENT ANALYSIS............................................................................................................. 65 4.2.1 0 and 1st Order Surfaces ............................................................................................................... 65 4.2.2 2nd Order Surfaces ........................................................................................................................ 66 4.2.3 3rd Order Surfaces ........................................................................................................................ 67 4.2.4 4th Order Surfaces ........................................................................................................................ 67 4.2.5 5th Order Surfaces ........................................................................................................................ 68 4.3 BAR ACCRETION TYPES AND PHASES .............................................................................................................. 68 4.3.1 Fragmentary Bar Phase ............................................................................................................... 68 4.3.2 Heterolithic Bar Abandonment Phase .......................................................................................... 70 4.4 THE “SADLER EFFECT” ............................................................................................................................... 72 4.5 THE EFFECTS OF DRAPING ON STEAM CHAMBER DEVELOPMENT .......................................................................... 72 CHAPTER 5 CONCLUSIONS ............................................................................................................................ 74 REFERENCES .................................................................................................................................................. 75 APPENDIX ...................................................................................................................................................... 79 VITA ABSTRACT iv LIST OF FIGURES FIGURE PAGE 1. Migration due to expansion, translation, and/or rotation ....................................................................... 4 2. Change in velocity vectors and helical flow in meander bends ................................................................ 5 3. Architecture of “Normal” and “Muddy Normal” point bars ..................................................................... 7 4.
Recommended publications
  • Final Report Analysis of Sediment Cores from the West Bay Diversion Receiving Area
    Final Report Analysis of Sediment Cores from the West Bay Diversion Receiving Area Alexander S. Kolker Louisiana Universities Marine Consortium 1. Introduction A. The setting. The Mississippi River Delta has one of the highest rate of land loss of any system on Earth. Present day rates of land loss average about 62 km2 yr‐1, and exceeded 100 km2 yr‐1 during the 1970s (Barras et al., 2003; Day et al., 2007). The causes of this land loss are numerous and a partial list includes high rates of subsidence, reduced sediment deposition, changes in the tidal prism of the delta's coastal bays, global sea level rise, hurricane impacts, salt water intrusion, canal construction, invasive species, and biogeochemical changes that are unfavorable for plant growth (Barras, 2006; Darby and Turner, 2008; Day et al., 2007; Fitzgerald et al., 2004; Gagliano et al., 1981; Kolker et al., 2010; Reed, 2002; Tornqvist et al., 2008). These drivers of wetland loss exist on a landscape that naturally experiences cycles of land gain and loss that result from changes in the course of the Mississippi River and occur on time scales decades to millennia (Coleman, 1988; Roberts, 1997; Tornqvist et al., 1996; Wells and Coleman, 1987). One potentially powerful way to restore the Mississippi River Delta is to partially divert the flow of the Mississippi River, thereby allow sediments and freshwater to enter the coastal landscape in a manner that mimics natural land‐building processes (Day et al., 2007; LACPRA, 2007; LADNR, 1998). Several natural and semi‐natural diversions provide strong evidence of the potential for river diversions to build land.
    [Show full text]
  • Stratigraphy, Age and Correlation of the Upper Cretaceous Tohatchi Formation, Western New Mexico Spencer G
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/54 Stratigraphy, age and correlation of the Upper Cretaceous Tohatchi Formation, western New Mexico Spencer G. Lucas, Dennis R. Braman, and Justin A. Spielmann, 2003, pp. 359-368 in: Geology of the Zuni Plateau, Lucas, Spencer G.; Semken, Steven C.; Berglof, William; Ulmer-Scholle, Dana; [eds.], New Mexico Geological Society 54th Annual Fall Field Conference Guidebook, 425 p. This is one of many related papers that were included in the 2003 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks.
    [Show full text]
  • Uplift Rate Transients at Subduction Margins Due to Earthquake Clustering
    Originally published as: Mouslopoulou, V., Oncken, O., Hainzl, S., Nicol, A. (2016): Uplift rate transients at subduction margins due to earthquake clustering. - Tectonics, 35, 10, pp. 2370—2384. DOI: http://doi.org/10.1002/2016TC004248 PUBLICATIONS Tectonics RESEARCH ARTICLE Uplift rate transients at subduction margins due 10.1002/2016TC004248 to earthquake clustering Key Points: Vasiliki Mouslopoulou1, Onno Oncken1, Sebastian Hainzl1, and Andrew Nicol2 • Transient uplift rates along fore-arc settings due to earthquake clustering 1German Research Centre for Geosciences, GFZ Helmholtz Centre Potsdam, Potsdam, Germany, 2Department of Geological • Earthquakes nucleate mostly on upper plate splay faults and less on the plate Sciences, University of Canterbury, Christchurch, New Zealand interface • Late Quaternary paleoshorelines may provide seismic hazard information Abstract Coastal uplift is common in continental fore-arc systems, with elevated paleoshorelines along seismically quiet subduction indicating that uplift rates can vary dramatically over time on individual margins. The origins of these margins changes in uplift rates are examined using a global data set of paleoshorelines together with 2-D numerical models of subduction systems. Empirical paleoshoreline data (N = 282) from eight subduction margins Supporting Information: indicate that uplift rates are generally not steady state and varied by up to a factor of 20 during the late • Supporting Information S1 ≤ fi • Table S1 Quaternary ( 125 ka). On many subduction margins uplift rates increase to the present day, a nding which • Supporting Information S2 we attribute to sampling bias toward those locations where Holocene uplift rates have been highest (with respect to other global margins which have undergone fast subsidence or no vertical motion—e.g., a Correspondence to: property akin to the so-called Sadler effect).
    [Show full text]
  • The Stratigraphy Machine Andrew D
    The Stratigraphy Machine Andrew D. Miall, University of Toronto John H. Holbrook, Texas Christian University Summary The stratigraphic record is constructed by multiple geological processes acting over time scales as short as a few seconds to as long as hundreds of millions of years. The probability of preservation of the products of high-frequency processes is very low. The full range of depositional and removal processes constitutes what may be termed a “Stratigraphy Machine.” Sedimentation rates and time scales Peter Sadler (1981) generated a graph that has long puzzled geologists – he Figure 1. Sadler’s (1981) relationship explained demonstrated that sedimentation rates in terms of the range of geological processes vary inversely with the duration of the that generate the sedimentary record. The elapsed time over which these rates are numbers in the boxes refer to a proposed measured, from the temporary flood-plain “Sedimentation Rate Scale” (Miall, 2015). deposits beside a river to the complete fill of a major sedimentary basin. This relationship has been referred to as the “Sadler effect.” Lengthy sections representing long time periods include a large number of sedimentary breaks. In fact, Ager (1973) remarked that the sedimentary record is “more gap than record.” However, it has taken the maturation of sedimentology and stratigraphy to provide a complete explanation of the Sadler effect. The science of stratigraphy has been revolutionized over the last fifty years. The emergence of sequence stratigraphy as the standard method for documentation and analysis, the increased sophistication of facies analysis and other sedimentological methods of documentation and interpretation, and the increasing accuracy and precision of the Geological Time Scale, have enabled ever more refined interpretations of geological processes.
    [Show full text]
  • The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M
    The Dinosaur Park - Bearpaw Formation Transition in the Cypress Hills Region of Southwestern Saskatchewan, Canada Meagan M. Gilbert Department of Geological Sciences, University of Saskatchewan; [email protected] Summary The Upper Cretaceous Dinosaur Park Formation (DPF) is a south- and eastward-thinning fluvial to marginal marine clastic-wedge in the Western Canadian Sedimentary Basin. The DPF is overlain by the Bearpaw Formation (BF), a fully marine clastic succession representing the final major transgression of the epicontinental Western Interior Seaway (WIS) across western North America. In southwestern Saskatchewan, the DPF is comprised of marginal marine coal, carbonaceous shale, and heterolithic siltstone and sandstone grading vertically into marine sandstone and shale of the Bearpaw Formation. Due to Saskatchewan’s proximity to the paleocoastline, 5th order transgressive cycles resulted in the deposition of multiple coal seams (Lethbridge Coal Zone; LCZ) in the upper two-thirds of the DPF in the study area. The estimated total volume of coal is 48109 m3, with a gas potential of 46109 m3 (Frank, 2005). The focus of this study is to characterize the facies and facies associations of the DPF, the newly erected Manâtakâw Member, and the lower BF in the Cypress Hills region of southwestern Saskatchewan utilizing core, outcrop, and geophysical well log data. This study provides a comprehensive sequence stratigraphic overview of the DPF-BF transition in Saskatchewan and the potential for coalbed methane exploration. Introduction The Dinosaur Park and Bearpaw Formations in Alberta, and its equivalents in Montana, have been the focus of several sedimentologic and stratigraphic studies due to exceptional outcrop exposure and extensive subsurface data (e.g., McLean, 1971; Wood, 1985, 1989; Eberth and Hamblin, 1993; Tsujita, 1995; Catuneanu et al., 1997; Hamblin, 1997; Rogers et al., 2016).
    [Show full text]
  • The Fauna from the Tyrannosaurus Rex Excavation, Frenchman Formation (Late Maastrichtian), Saskatchewan
    The Fauna from the Tyrannosaurus rex Excavation, Frenchman Formation (Late Maastrichtian), Saskatchewan Tim T. Tokaryk 1 and Harold N. Bryant 2 Tokaryk, T.T. and Bryant, H.N. (2004): The fauna from the Tyrannosaurus rex excavation, Frenchman Formation (Late Maastrichtian), Saskatchewan; in Summary of Investigations 2004, Volume 1, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2004-4.1, CD-ROM, Paper A-18, 12p. Abstract The quarry that contained the partial skeleton of the Tyrannosaurus rex, familiarly known as “Scotty,” has yielded a diverse faunal and floral assemblage. The site is located in the Frenchman River valley in southwestern Saskatchewan and dates from approximately 65 million years, at the end of the Cretaceous Period. The faunal assemblage from the quarry is reviewed and the floral assemblage is summarized. Together, these assemblages provide some insight into the biological community that lived in southwestern Saskatchewan during the latest Cretaceous. Keywords: Frenchman Formation, Maastrichtian, Late Cretaceous, southwestern Saskatchewan, Tyrannosaurus rex. 1. Introduction a) Geological Setting The Frenchman Formation, of latest Maastrichtian age, is extensively exposed in southwestern Saskatchewan (Figure 1; Fraser et al., 1935; Furnival, 1950). The lithostratigraphic units in the formation consist largely of fluvial sandstones and greenish grey to green claystones. Outcrops of the Frenchman Formation are widely distributed in the Frenchman River valley, southeast of Eastend. Chambery Coulee, on the north side of the valley, includes Royal Saskatchewan Museum (RSM) locality 72F07-0022 (precise locality data on file with the RSM), the site that contained the disarticulated skeleton of a Tyrannosaurus rex. McIver (2002) subdivided the stratigraphic sequence at this locality into “lower” and “upper” beds.
    [Show full text]
  • Shelf Sedimentation on a Tectonically Active Margin: a Modern Sediment Budget for Poverty Continental Shelf, New Zealand
    ARTICLE IN PRESS MARGO-04425; No of Pages 13 Marine Geology xxx (2009) xxx–xxx Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Shelf sedimentation on a tectonically active margin: A modern sediment budget for Poverty continental shelf, New Zealand Andrea J. Miller, Steven A. Kuehl ⁎ Virginia Institute of Marine Science, 1208 Greate Road, P.O. Box 1346, Gloucester Point, VA 23062, USA article info abstract Available online xxxx The combination of high sediment yields and the prevalence of tectonically controlled accommodation on collision margins such as that adjacent to the Waipaoa River, NZ, create the potential for these areas to Keywords: contain high-resolution records of natural and anthropogenic signals. This study describes modern (100-yr) Waipaoa River sedimentation patterns off the Waipaoa and quantifies a sediment budget for the continental shelf, which is continental margin compared to long-term Holocene trends. 210Pb and 239,240Pu geochronologies reveal three main shelf shelf sedimentation depocenters. Two of these depocenters are located in subsiding synclinal basins on the mid-shelf, landward 210Pb geochronology 239,240Pu geochronology of the actively deforming Ariel and Lachlan anticlines. The depocenters exhibit accumulation rates ranging −1 210 fi sediment budget from 0.75 to 1.5cmyr and display both steady-state and non-steady-state Pb activity pro les. Textural characteristics of the non-steady-state cores indicate the possible preservation of flood event layers. The third depocenter is located near the shelf break and has accumulation rates as high as 1.0cmyr−1. The inner shelf and central mid-shelf are characterized by low, uniform 210Pb activity profiles and low accumulation rates, indicating that sediment is bypassing the inner shelf region and being deposited on the mid- to outer shelf.
    [Show full text]
  • Morphometry of the Teeth of Western North American Tyrannosaurids and Its Applicability to Quantitative Classification
    Morphometry of the teeth of western North American tyrannosaurids and its applicability to quantitative classification TANYA SAMMAN, G. LAWRENCE POWELL, PHILIP J. CURRIE, and LEONARD V. HILLS Samman, T., Powell, G.L., Currie, P.J., and Hills, L.V. 2005. Morphometry of the teeth of western North American tyrannosaurids and its applicability to quantitative classification. Acta Palaeontologica Polonica 50 (4): 757–776. Gross tooth morphology and serration morphology were examined to determine a quantifiable method for classifying tyrannosaurid tooth crowns from western North America. From the examination of teeth in jaws, tyrannosaurid teeth could be qualitatively assigned to one of five types based on the cross−sectional shape of the base of the tooth and charac− teristics of the mesial carina. A principal component analysis (PCA) revealed that much of the variance in tooth shape was a result of isometry, but some gross morphological variables exhibited strong positive allometry. Non−size associated fac− tors were also important in determining tooth shape, particularly when data on denticle dimensions were considered in the analysis. While PCA identified important factors in variation, PCA ordination plots did not cluster the teeth into distinct, separate groupings based on taxon or bone of origin. The group classification functions determined by discriminant anal− ysis, though not universally successful for classifying unidentified isolated teeth of all tyrannosaurids, do identify bone of origin of adult Albertosaurus, Daspletosaurus, and Gorgosaurus teeth at a statistically acceptable level. Key words: Theropoda, Tyrannosauridae, dentition, classification, quantitative analysis, Cretaceous, North America. Tanya Samman [[email protected]] and Leonard.V. Hills [[email protected]], Department of Geology & Geo− physics, University of Calgary, AB, T2N 1N4 Canada; G.
    [Show full text]
  • Modeling Burial and Thermal History of the Central European Basins and Comparison with Organic Maturity Data
    Modeling burial and thermal history of the central European basins and comparison with organic maturity data Master’s thesis submitted in fulfilment of the requirements for the degree Master of Science (M.Sc.) in Geoscience January 2017 Georg-August-University Göttingen Faculty of Geosciences and Geography Department of Structural Geology and Geodynamics Geoscience Center by Tom Kaltofen Born in Berlin Supervisor: Dr. Elco Luijendijk Co-supervisor: Prof. Dr. Jonas Kley Contents Contents Abstract ......................................................................................................................................... III 1 Introduction .................................................................................................................................. 4 1.1 Paleozoic geological history of the study area .......................................................................... 5 1.2 Mesozoic geological history ..................................................................................................... 8 2 Methods........................................................................................................................................ 9 2.1 Burial and thermal history model ............................................................................................. 9 2.2 Input of thermal history model ................................................................................................. 9 2.3 Lithology ................................................................................................................................
    [Show full text]
  • Lack of a Weathering Signal with Increased Cenozoic Erosion?
    Received: 10 September 2016 | Revised: 27 May 2017 | Accepted: 2 June 2017 DOI: 10.1111/ter.12278 DEBATE ARTICLE Forum: The Editors of Terra Nova invite readers to contribute to a discussion of this topic on our forum at https://terranovadebates. wordpress.com/ Lack of a weathering signal with increased Cenozoic erosion? Kevin P. Norton1 | Fritz Schlunegger2 1School of Geography, Environment and Earth Sciences, Victoria University of Abstract Wellington, Wellington, New Zealand The Late Cenozoic has been marked by large and rapid fluctuations in temperature. 2Institute of Geological Sciences, University This cooling has been attributed to accelerated erosion, with concomitant increased of Bern, Bern, Switzerland chemical-weathering rates and CO2 drawdown from the atmosphere. At the same Correspondence time, much of the supporting evidence appears to be affected by a sampling bias, Dr. Kevin Norton, School of Geography, Environment and Earth Sciences, Victoria implying that global erosion and weathering have remained largely constant over University of Wellington, Wellington, the past millions of years. We suggest that sedimentary archives of geomorphic New Zealand. Email: [email protected] activity, such as grain size and the ratio of terrestrial to oceanic sedimentation, which show accelerated erosion are not subject to these biases. Furthermore, the active tectonic settings where these erosion increases were likely to have taken place are exactly those locations where chemical-weathering signals are least likely to faithfully follow physical erosion rates. A lack of evidence for an increase in chemical weathering does not necessarily preclude an increase in physical erosion. In this contribution, we suggest an alternative interpretation in which erosion rates have increased in the Late Cenozoic but without significantly increased silicate weathering, which can explain the meagre response of chemical-weathering proxies.
    [Show full text]
  • 2021 Northeast Geobiology Symposium April 9Th and 10Th Dartmouth College, Hanover, NH Talks Session 1: Proterozoic Earth 9:05 A.M
    2021 Northeast Geobiology Symposium April 9th and 10th Dartmouth College, Hanover, NH Talks Session 1: Proterozoic Earth 9:05 a.m. The rise of phosphorus recycling facilitated Earth's Great Oxidation Event Lewis J. Alcott, Benjamin J. W. Mills, Andrey Bekker, and Simon W. Poulton The rise of atmospheric oxygen during the Great Oxidation Event (GOE) ∼2.4 billion years ago (Ga) was a defining transition in the evolution of global biogeochemical cycles and life on Earth. There is, however, abundant evidence for mild oxidative continental weathering and the development of ocean oxygen oases several hundred million years prior to the GOE. The GOE thus represents a threshold, whereby primary productivity and O2 production overwhelmed the input of reduced species that consume O2, and its timing is assumed to be related to a balance between the riverine input of the major limiting nutrient, phosphate, and the dynamics of the solid Earth. However, the sequence of events that ultimately facilitated persistent atmospheric oxygenation remains elusive. Here, we report novel geochemical analyses of ∼2.65 to 2.43 Ga drill core samples from the Transvaal Supergroup, South Africa, which document an early rise of sedimentary phosphorus recycling as dissolved sulfide became more abundant in the ocean system, which itself was a progressive response to the onset of oxidative continental weathering. Biogeochemical modelling of the global implications for primary productivity shows that the evolution of phosphorus recycling was the critical step that enabled Earth's transition to a persistently oxygenated atmosphere. 9:25 a.m. Depositional rates in the Ediacaran Nafun Group, Oman, and the wider late Proterozoic world Marjorie D.
    [Show full text]
  • (Late Maastrichtian) Small Theropods and Birds: Teeth from The
    Sankey, J.T. and S. Baszio, eds. 2008. Vertebrate Microfossil Assemblages: Their Role in Paleoecology and Paleobiogeography. Indiana University Press. Diversity of Latest Cretaceous (Late Maastrichtian) Small Theropods and Birds: Teeth from the Lance and Hell Creek Formations Julia T. Sankey Department of Physics and Geology, California State University, Stanislaus, Turlock, California 95382. [email protected] 1. Abstract Late Maastrichtian (latest Cretaceous) small theropod dinosaur and bird diversity has been difficult to determine because of scarcity or skeletal remains. Numerous teeth of small theropods and birds from the Hell Creek (Montana) and Lance (Wyoming) Formations were analyzed. Relative abundances are: dromaeosaurids (23%), troodontids (14%), cf. Richardoestesia isosceles (35%), cf. Paronychodon (20%), and bird (8%). This Maastrichtian theropod assemblage is different from the late Campanian one from Alberta in three ways: 1) the abundance (55%) of two unusual small theropods, cf. Richardoestesia isosceles and Paronychodon; 2) the abundance of teeth, from all taxa, with a flat side and longitudinal ridges; 3) the lower abundance and diversity of dromaeosaurids. The late Maastrichtian had a lower diversity of small theropods compared to the late Campanian possibly due to competition for 1 prey between dromaeosaurids and juvenile tyrannosaurids and climatic and/or climatic and environmental changes during the latest Cretaceous. Key Words Theropod, dinosaur, Maastrichtian, Late Cretaceous, Teeth, Diversity 2. Introduction 2.1. Previous work The first detailed descriptions of small theropod teeth was done by CURRIE et al. (1990) based on collections from the late Campanian Judith River Group of Alberta. Identification and reference of isolated teeth to known taxa was possible due to the existence of jaws with teeth from some of the small theropods.
    [Show full text]