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Precise Age and Biostratigraphic Significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA
Precise age and biostratigraphic significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA Spencer G. Lucas1, Bruce D. Allen2, Karl Krainer3, James Barrick4, Daniel Vachard5, Joerg W. Schneider6, William A. DiMichele7 and Arden R. Bashforth8 1New Mexico Museum of Natural History, 1801 Mountain Road N.W., Albuquerque, New Mexico, 87104, USA email: [email protected] 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, New Mexico, 87801, USA email: [email protected] 3Institute of Geology and Paleontology, University of Innsbruck, Innsbruck, A-6020, Austria email: [email protected] 4Department of Geosciences, Texas Tech University, Box 41053, Lubbock, Texas, 79409, USA email: [email protected] 5Université des Sciences et Technologies de Lille, UFR des Sciences de la Terre, UPRESA 8014 du CNRS, Laboratoire LP3, Bâtiment SN 5, F-59655 Villeneuve d’Ascq, Cédex, France email: [email protected] 6TU Bergakademie Freiberg, Cottastasse 2, D-09596 Freiberg, Germany email:[email protected] 7Department of Paleobiology, NMNH Smithsonian Institution, Washington, DC 20560 email: [email protected] 8Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark email: [email protected] ABSTRACT: The Kinney Brick Quarry is a world famous Late Pennsylvanian fossil Lagerstätte in central New Mexico, USA. The age assigned to the Kinney Brick Quarry (early-middle Virgilian) has long been based more on its inferred lithostratigraphic position than on biostratigraphic indicators at the quarry. We have developed three datasets —-stratigraphic position, fusulinids and conodonts— that in- dicate the Kinney Brick Quarry is older, of middle Missourian (Kasimovian) age. -
Annual Repor T 2014
Annual Report 2014 2014 Highlights Forrest Steller sea lion, Eden, gave birth to a healthy male pup on July 20, 2014. Forrest is the first male Steller sea lion born in North American collections since the 1980s. This is the second pup for parents Woody and Eden. Eleanor, “Ellie,” was born on June 20, 2013. Eider Research 2014 brought the most successful breeding season for the Eider Research Program. For the first time since the program’s start, two female Steller’s eiders naturally incubated eggs and reared ducklings. The Alaska SeaLife Center is the only facility in North America to have Steller’s eiders naturally incubate and rear their young. Sea Otter BTS Another first for the Center: Sea Otter Behind-the-Scenes (BTS) Tours were offered to guests! The Sea Otter BTS provided a unique opportunity for guests to get paw-to-paw with three playful critters. New Ticketing Counter The ticketing counter got a makeover! Guests are now greeted with a harbor-themed front desk as they enter through the doors. Chiswell Island A record number of Steller sea lion births were recorded at Chiswell Island. Alaska SeaLife Center researchers confirmed 114 births as the highest number they’ve observed since research began in 1998. Family Science Night The Education Department implemented a new program for younger children and families in Seward. “Family Science Night” offers kids and adults of all ages fun and educational activities throughout the winter. 3 and its substantial research on the hearing capabilities of arctic seals. These vital connections with partner organizations enable the entire marine community to reach their goals, thereby creating sustainable marine From the President and CEO ecosystems the world over. -
Chondrichthyan Fishes (Sharks, Skates, Rays) Announcements
Chondrichthyan Fishes (sharks, skates, rays) Announcements 1. Please review the syllabus for reading and lab information! 2. Please do the readings: for this week posted now. 3. Lab sections: 4. i) Dylan Wainwright, Thursday 2 - 4/5 pm ii) Kelsey Lucas, Friday 2 - 4/5 pm iii) Labs are in the Northwest Building basement (room B141) 4. Lab sections done: first lab this week on Thursday! 5. First lab reading: Agassiz fish story; lab will be a bit shorter 6. Office hours: we’ll set these later this week Please use the course web site: note the various modules Outline Lecture outline: -- Intro. to chondrichthyan phylogeny -- 6 key chondrichthyan defining traits (synapomorphies) -- 3 chondrichthyan behaviors -- Focus on several major groups and selected especially interesting ones 1) Holocephalans (chimaeras or ratfishes) 2) Elasmobranchii (sharks, skates, rays) 3) Batoids (skates, rays, and sawfish) 4) Sharks – several interesting groups Not remotely possible to discuss today all the interesting groups! Vertebrate tree – key ―fish‖ groups Today Chondrichthyan Fishes sharks Overview: 1. Mostly marine 2. ~ 1,200 species 518 species of sharks 650 species of rays 38 species of chimaeras Skates and rays 3. ~ 3 % of all ―fishes‖ 4. Internal skeleton made of cartilage 5. Three major groups 6. Tremendous diversity of behavior and structure and function Chimaeras Chondrichthyan Fishes: 6 key traits Synapomorphy 1: dentition; tooth replacement pattern • Teeth are not fused to jaws • New rows move up to replace old/lost teeth • Chondrichthyan teeth are -
Subcommission on Permian Stratigraphy International
Number 30 June 1997 A NEWSLETTER OF THE SUBCOMMISSION ON PERMIAN STRATIGRAPHY SUBCOMMISSION ON PERMIAN STRATIGRAPHY INTERNATIONAL COMMISSION ON STRATIGRAPHY INTERNATIONAL UNION OF GEOLOGICAL SCIENCES (IUGS) Table of Contents Notes from the SPS Secretary...................................................................................................................-1- Claude Spinosa Note from the SPS Chairman....................................................................................................................-2- Bruce R. Wardlaw Proposed new chronostratigraphic units for the Upper Permian ..............................................................-3- Amos Salvador Comments on Subdivisions of the Permian and a Standard World Scale ................................................-4- Neil W. Archbold and J. Mac Dickins Permian chronostratigraphic subdivisions ................................................................................................-5- Jin Yugan, Bruce R. Wardlaw, Brian F. Glenister and Galina V. Kotlyar The Permian Time-scale ...........................................................................................................................-6- J. B. Waterhouse Sequence Stratigraphy along Aidaralash Creek and the Carboniferous/Permian GSSP ..........................-8- Walter S. Snyder and Dora M. Gallegos Upper Paleozoic Fusulinacean Biostratigraphy of the Southern Urals ...................................................-11- Vladimir I. Davydov, Walter S. Snyder and Claude Spinosa Cordaitalean -
Pennsylvanian Boundary Unconformity in Marine Carbonate Successions
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences Summer 6-2014 ORIGIN AND DISTRIBUTION OF THE MISSISSIPPIAN – PENNSYLVANIAN BOUNDARY UNCONFORMITY IN MARINE CARBONATE SUCCESSIONS WITH A CASE STUDY OF THE KARST DEVELOPMENT ATOP THE MADISON FORMATION IN THE BIGHORN BASIN, WYOMING. Lucien Nana Yobo University of Nebraska-Lincoln, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geochemistry Commons, Geology Commons, Sedimentology Commons, and the Stratigraphy Commons Nana Yobo, Lucien, "ORIGIN AND DISTRIBUTION OF THE MISSISSIPPIAN – PENNSYLVANIAN BOUNDARY UNCONFORMITY IN MARINE CARBONATE SUCCESSIONS WITH A CASE STUDY OF THE KARST DEVELOPMENT ATOP THE MADISON FORMATION IN THE BIGHORN BASIN, WYOMING." (2014). Dissertations & Theses in Earth and Atmospheric Sciences. 59. http://digitalcommons.unl.edu/geoscidiss/59 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. ORIGIN AND DISTRIBUTION OF THE MISSISSIPPIAN – PENNSYLVANIAN BOUNDARY UNCONFORMITY IN MARINE CARBONATE SUCCESSIONS WITH A CASE STUDY OF THE KARST DEVELOPMENT ATOP THE MADISON FORMATION IN THE BIGHORN BASIN, WYOMING. By Luscalors Lucien Nana Yobo A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Tracy D. -
UTEP) Geological Sciences
S. Pon1, D. De los Santos1, G. Alvarez-Rodriguez1, F. Enriquez1 S. Terrazas1, S. Terrazas1, J. Ricketts1, J.G. Olgin1,2, 1University of Texas at El Paso – Geological Sciences (500 University, El Paso, TX 79968), 2El Paso Community College – Physics Department (9570 Gateway N. Blvd, El Paso, TX 79924) Sarah Michelle Pon Deandra De Los Santos I am a senior at The University of Texas at El Paso, studying I am a senior at the University of Texas at El Paso (UTEP) Geological Sciences. I am excited to bring ideas and concepts of majoring in Geological Sciences and will graduate May, 2018. Abstract geology and planetary sciences to students. Whether it be During my time at UTEP, I have presented on salt diapirs and students who are pressuring a career in the sciences or students their possible entrainment methods at the Geological Society of just fulfilling their requirements. My goal with EIPS is to engage America conference in San Antonio. I also assisted Kuwanna Future Progress all students and get them asking questions and have them search Dyer-Pietras, a SUNY Binghampton University PhD candidate, The number of underrepresented minorities pursuing for the answers. with her research on boundaries between Eocene rock types For this internship, I have written a lab as an introduction to deposited in the shallow and deeper lake locations of the STEM fields, specifically in the sciences, has declined in remote sensing. I give a quick overview of what remote sensing is, Piceance basin in Rifle, Colorado, this past summer. I am now Furthermore, the Spring and Fall 2018 will include recent times [1]. -
A New Euselachian Shark from the Early Permian of the Middle Urals, Russia
A new euselachian shark from the early Permian of the Middle Urals, Russia ALEXANDER O. IVANOV, CHRISTOPHER J. DUFFIN, and SERGE V. NAUGOLNYKH Ivanov , A.O., Duffin, C.J., and Naugolnykh, S.V. 2017. A new euselachian shark from the early Permian of the Middle Urals, Russia. Acta Palaeontologica Polonica 62 (2): 289–298. The isolated teeth of a new euselachian shark Artiodus prominens Ivanov and Duffin gen. et sp. nov. have been found in the Artinskian Stage (Early Permian) of Krasnoufimskie Klyuchiki quarry (Sverdlovsk Region, Middle Urals, Russia). The teeth of Artiodus possess a multicuspid orthodont crown with from four to nine triangular cusps; prominent labial projection terminating in a large round tubercle; distinct ornamentation from straight or recurved cristae; oval or semilu- nar, elongate, considerably vascularized base; dense vascular network formed of transverse horizontal, ascending, short secondary and semicircular canals. The teeth of the new taxon otherwise most closely resemble the teeth of some prot- acrodontid and sphenacanthid euselachians possessing a protacrodont-type crown, but differ from the teeth of all other known euselachians in the unique structure of the labial projection. The studied teeth vary in crown and base morphol- ogy, and three tooth morphotypes can be distinguished in the collection reflecting a moderate degree of linear gradient monognathic heterodonty. The range of morphologies otherwise displayed by the collection of teeth shows the greatest similarity to that described for the dentitions of relatively high-crowned hybodontids from the Mesozoic. The internal structure of the teeth, including their vascularization system is reconstructed using microtomography. The highest chon- drichthyan taxonomic diversity is found in the Artinskian, especially from the localities of the Middle and South Urals. -
Geological Survey of Ohio
GEOLOGICAL SURVEY OF OHIO. VOL. I.—PART II. PALÆONTOLOGY. SECTION II. DESCRIPTIONS OF FOSSIL FISHES. BY J. S. NEWBERRY. Digital version copyrighted ©2012 by Don Chesnut. THE CLASSIFICATION AND GEOLOGICAL DISTRIBUTION OF OUR FOSSIL FISHES. So little is generally known in regard to American fossil fishes, that I have thought the notes which I now give upon some of them would be more interesting and intelligible if those into whose hands they will fall could have a more comprehensive view of this branch of palæontology than they afford. I shall therefore preface the descriptions which follow with a few words on the geological distribution of our Palæozoic fishes, and on the relations which they sustain to fossil forms found in other countries, and to living fishes. This seems the more necessary, as no summary of what is known of our fossil fishes has ever been given, and the literature of the subject is so scattered through scientific journals and the proceedings of learned societies, as to be practically inaccessible to most of those who will be readers of this report. I. THE ZOOLOGICAL RELATIONS OF OUR FOSSIL FISHES. To the common observer, the class of Fishes seems to be well defined and quite distin ct from all the other groups o f vertebrate animals; but the comparative anatomist finds in certain unusual and aberrant forms peculiarities of structure which link the Fishes to the Invertebrates below and Amphibians above, in such a way as to render it difficult, if not impossible, to draw the lines sharply between these great groups. -
Sequence Biostratigraphy of Carboniferous-Permian Boundary
Brigham Young University BYU ScholarsArchive Theses and Dissertations 2019-07-01 Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin Joshua Kerst Meibos Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Physical Sciences and Mathematics Commons BYU ScholarsArchive Citation Meibos, Joshua Kerst, "Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin" (2019). Theses and Dissertations. 7583. https://scholarsarchive.byu.edu/etd/7583 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin Joshua Kerst Meibos A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Scott M. Ritter, Chair Brooks B. Britt Sam Hudson Department of Geological Sciences Brigham Young University Copyright © 2019 Joshua Kerst Meibos All Rights Reserved ABSTRACT Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin Joshua Kerst Meibos Department of Geological Sciences, BYU Master of Science The stratal architecture of the upper Ely Limestone and Mormon Gap Formation (Pennsylvanian-early Permian) in western Utah reflects the interaction of icehouse sea-level change and tectonic activity in the distal Antler-Sonoma foreland basin. -
VOLUME 33 December 2017
VOLUME 33 December 2017 Volume 33 Table of Contents EXECUTIVE’S COLUMN…………………………………………………………………..…….. 2 OBITUARY……………………………………………………………………………………..…5 SCCS REPORTS………………………………………………………………………………….7 ANNUAL REPORT TO ICS FOR 2016-2017…………………………………………………..….7 TASK GROUP REPORTS FOR 2016-2017 AND WORK PLANS FOR 2017 FISCAL YEAR………….11 Report of the task group to establish a GSSP close to the existing Viséan-Serpukhovian boundary…………11 Report of the task group to establish a GSSP close to the existing Bashkirian-Moscovian boundary………16 Report of the task group to establish the Moscovian-Kasimovian and Kasimovian-Gzhelian boundaries…....18 SCCS DOCUMENTS (CONTRIBUTIONS BY MEMBERS)…………………………………...……21 SHALLOW-WATER SIPHONODELLIDS AND DEFINITION OF THE DEVONIAN-CARBONIFEROUS BOUNDARY…………………………………………………………………………………….21 REPORT FOR PROGRESS FOR 2017 ACTIVITIES IN THE CANTABRIAN MOUNTAINS, SPAIN AND THE AMAZONAS BASIN, BRAZIL……………………………………………...………………26 TAXONOMIC AND STRATIGRAPHIC PROBLEMS CONCERNING THE CONODONTS LOCHRIEA SENCKENBERGICA NEMIROVSKAYA, PERRET & MEISCHNER, 1994 AND LOCHRIEA ZIEGLERI NEMIROVSKAYA, PERRET & MEISHCNER, 1994-CONSEQUENCES FOR DEFINING THE VISÉAN- SERPUKHOVIAN BOUNDARY………………………………………………………………………………...28 PROGRESS ON THE VISÉAN-SERPUKHOVIAN BOUNDARY IN SOUTH CHINA AND GERMANY……………………………………………………………………………………..35 POTENTIAL FOR A MORE PRECISE CORRELATION OF THE BASHKIRIAN AMMONOID AND FORAMINIFERAL ZONES IN THE SOUTH URALS…………………………………………..……42 CHEMOMETRICS AND CARBONIFEROUS MEDULLOSALEAN FRONDS: IMPLICATIONS FOR CARBONIFEROUS PHYTOSTRATIGRAPHY…………………………………………………...…45 -
1 Supplementary Materials and Methods 1 S1 Expanded
1 Supplementary Materials and Methods 2 S1 Expanded Geologic and Paleogeographic Information 3 The carbonate nodules from Montañez et al., (2007) utilized in this study were collected from well-developed and 4 drained paleosols from: 1) the Eastern Shelf of the Midland Basin (N.C. Texas), 2) Paradox Basin (S.E. Utah), 3) Pedregosa 5 Basin (S.C. New Mexico), 4) Anadarko Basin (S.C. Oklahoma), and 5) the Grand Canyon Embayment (N.C. Arizona) (Fig. 6 1a; Richey et al., (2020)). The plant cuticle fossils come from localities in: 1) N.C. Texas (Lower Pease River [LPR], Lake 7 Kemp Dam [LKD], Parkey’s Oil Patch [POP], and Mitchell Creek [MC]; all representing localities that also provided 8 carbonate nodules or plant organic matter [POM] for Montañez et al., (2007), 2) N.C. New Mexico (Kinney Brick Quarry 9 [KB]), 3) S.E. Kansas (Hamilton Quarry [HQ]), 4) S.E. Illinois (Lake Sara Limestone [LSL]), and 5) S.W. Indiana (sub- 10 Minshall [SM]) (Fig. 1a, S2–4; Richey et al., (2020)). These localities span a wide portion of the western equatorial portion 11 of Euramerica during the latest Pennsylvanian through middle Permian (Fig. 1b). 12 13 S2 Biostratigraphic Correlations and Age Model 14 N.C. Texas stratigraphy and the position of pedogenic carbonate samples from Montañez et al., (2007) and cuticle were 15 inferred from N.C. Texas conodont biostratigraphy and its relation to Permian global conodont biostratigraphy (Tabor and 16 Montañez, 2004; Wardlaw, 2005; Henderson, 2018). The specific correlations used are (C. Henderson, personal 17 communication, August 2019): (1) The Stockwether Limestone Member of the Pueblo Formation contains Idiognathodus 18 isolatus, indicating that the Carboniferous-Permian boundary (298.9 Ma) and base of the Asselian resides in the Stockwether 19 Limestone (Wardlaw, 2005). -
GEOLOGIC TIME SCALE V
GSA GEOLOGIC TIME SCALE v. 4.0 CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST HIST. ANOM. (Ma) ANOM. CHRON. CHRO HOLOCENE 1 C1 QUATER- 0.01 30 C30 66.0 541 CALABRIAN NARY PLEISTOCENE* 1.8 31 C31 MAASTRICHTIAN 252 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 Lopin- 254 32 C32 72.1 635 2A C2A PIACENZIAN WUCHIAPINGIAN PLIOCENE 3.6 gian 33 260 260 3 ZANCLEAN CAPITANIAN NEOPRO- 5 C3 CAMPANIAN Guada- 265 750 CRYOGENIAN 5.3 80 C33 WORDIAN TEROZOIC 3A MESSINIAN LATE lupian 269 C3A 83.6 ROADIAN 272 850 7.2 SANTONIAN 4 KUNGURIAN C4 86.3 279 TONIAN CONIACIAN 280 4A Cisura- C4A TORTONIAN 90 89.8 1000 1000 PERMIAN ARTINSKIAN 10 5 TURONIAN lian C5 93.9 290 SAKMARIAN STENIAN 11.6 CENOMANIAN 296 SERRAVALLIAN 34 C34 ASSELIAN 299 5A 100 100 300 GZHELIAN 1200 C5A 13.8 LATE 304 KASIMOVIAN 307 1250 MESOPRO- 15 LANGHIAN ECTASIAN 5B C5B ALBIAN MIDDLE MOSCOVIAN 16.0 TEROZOIC 5C C5C 110 VANIAN 315 PENNSYL- 1400 EARLY 5D C5D MIOCENE 113 320 BASHKIRIAN 323 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 1500 CALYMMIAN 6 C6 APTIAN LATE 20 120 331 6A C6A 20.4 EARLY 1600 M0r 126 6B C6B AQUITANIAN M1 340 MIDDLE VISEAN MISSIS- M3 BARREMIAN SIPPIAN STATHERIAN C6C 23.0 6C 130 M5 CRETACEOUS 131 347 1750 HAUTERIVIAN 7 C7 CARBONIFEROUS EARLY TOURNAISIAN 1800 M10 134 25 7A C7A 359 8 C8 CHATTIAN VALANGINIAN M12 360 140 M14 139 FAMENNIAN OROSIRIAN 9 C9 M16 28.1 M18 BERRIASIAN 2000 PROTEROZOIC 10 C10 LATE