Bulletin 61, the Cretaceous Fossils of New Jersey -- Part II
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Upper Cretaceous Sequences and Sea-Level History, New Jersey Coastal Plain
Upper Cretaceous sequences and sea-level history, New Jersey Coastal Plain Kenneth G. Miller² Department of Geological Sciences, Rutgers University, Piscataway, New Jersey 08854, USA Peter J. Sugarman New Jersey Geological Survey, P.O. Box 427, Trenton, New Jersey 08625, USA James V. Browning Department of Geological Sciences, Rutgers University, Piscataway, New Jersey 08854, USA Michelle A. Kominz Department of Geosciences, Western Michigan University, Kalamazoo, Michigan 49008-5150, USA Richard K. Olsson Mark D. Feigenson John C. HernaÂndez Department of Geological Sciences, Rutgers University, Piscataway, New Jersey 08854, USA ABSTRACT pean sections, and Russian platform BACKGROUND outcrops points to a global cause. Because We developed a Late Cretaceous sea- backstripping, seismicity, seismic strati- Predictable, recurring sequences bracketed level estimate from Upper Cretaceous se- graphic data, and sediment-distribution by unconformities comprise the building quences at Bass River and Ancora, New patterns all indicate minimal tectonic ef- blocks of the stratigraphic record. Exxon Pro- Jersey (ODP [Ocean Drilling Program] Leg fects on the New Jersey Coastal Plain, we duction Research Company (EPR) de®ned a 174AX). We dated 11±14 sequences by in- interpret that we have isolated a eustatic depositional sequence as a ``stratigraphic unit tegrating Sr isotope and biostratigraphy signature. The only known mechanism composed of a relatively conformable succes- (age resolution 60.5 m.y.) and then esti- that can explain such global changesÐ sion of genetically related strata and bounded mated paleoenvironmental changes within glacio-eustasyÐis consistent with forami- at its top and base by unconformities or their the sequences from lithofacies and biofacies niferal d18O data. -
Detrital Zircon Provenance and Lithofacies Associations Of
geosciences Article Detrital Zircon Provenance and Lithofacies Associations of Montmorillonitic Sands in the Maastrichtian Ripley Formation: Implications for Mississippi Embayment Paleodrainage Patterns and Paleogeography Jennifer N. Gifford 1,*, Elizabeth J. Vitale 1, Brian F. Platt 1 , David H. Malone 2 and Inoka H. Widanagamage 1 1 Department of Geology and Geological Engineering, University of Mississippi, Oxford, MS 38677, USA; [email protected] (E.J.V.); [email protected] (B.F.P.); [email protected] (I.H.W.) 2 Department of Geography, Geology, and the Environment, Illinois State University, Normal, IL 61790, USA; [email protected] * Correspondence: jngiff[email protected]; Tel.: +1-(662)-915-2079 Received: 17 January 2020; Accepted: 15 February 2020; Published: 22 February 2020 Abstract: We provide new detrital zircon evidence to support a Maastrichtian age for the establishment of the present-day Mississippi River drainage system. Fieldwork conducted in Pontotoc County,Mississippi, targeted two sites containing montmorillonitic sand in the Maastrichtian Ripley Formation. U-Pb detrital zircon (DZ) ages from these sands (n = 649) ranged from Mesoarchean (~2870 Ma) to Pennsylvanian (~305 Ma) and contained ~91% Appalachian-derived grains, including Appalachian–Ouachita, Gondwanan Terranes, and Grenville source terranes. Other minor source regions include the Mid-Continent Granite–Rhyolite Province, Yavapai–Mazatzal, Trans-Hudson/Penokean, and Superior. This indicates that sediment sourced from the Appalachian Foreland Basin (with very minor input from a northern or northwestern source) was being routed through the Mississippi Embayment (MSE) in the Maastrichtian. We recognize six lithofacies in the field areas interpreted as barrier island to shelf environments. Statistically significant differences between DZ populations and clay mineralogy from both sites indicate that two distinct fluvial systems emptied into a shared back-barrier setting, which experienced volcanic ash input. -
A Fossiliferous Spherule-Rich Bed at the Cretaceous–Paleogene (K–Pg) Boundary in 1 Mississippi, USA: Implications for the K
1 A fossiliferous spherule-rich bed at the Cretaceous–Paleogene (K–Pg) boundary in 2 Mississippi, USA: implications for the K–Pg mass extinction event in the Mississippi 3 Embayment and Eastern Gulf Coastal Plain 4 James D. Witts1, Neil H. Landman1, Matthew P. Garb2, Caitlin Boas2, Ekaterina Larina3, 5 Remy Rovelli4, Lucy E. Edwards5, Robert M. Sherrell6,7, and J. Kirk Cochran8 6 1Division of Paleontology (Invertebrates), American Museum of Natural History, New York, 7 NY 10024, USA 8 2Department of Earth and Environmental Sciences, Brooklyn College, Brooklyn, NY 11210, 9 USA 10 3University of Southern California, Department of Earth Sciences, Los Angeles, CA 90018, 11 USA 12 4Department of Earth and Planetary Sciences, The University of New Mexico, Albuquerque, 13 NM 87131, USA 14 5U.S. Geological Survey, Mail Stop 926A, Reston, VA 20192, USA 15 6Department of Marine and Coastal Sciences, Rutgers University, Piscataway, NJ 08901, 16 USA 17 7 Department of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08901, 18 USA 19 8School of Marine and Atmospheric Science, Stony Brook University, Stony Brook, NY 11794, 20 USA 21 [The final, fully formatted version of this article is available online at Cretaceous Research: 22 https://doi.org/10.1016/j.cretres.2018.06.002 ] 23 Abstract 24 We describe an outcrop of the Cretaceous–Paleogene (K–Pg) boundary exposed due 25 to construction near New Albany, Union County, Mississippi. It consists of the Owl Creek 26 Formation and overlying Clayton Formation. The Owl Creek Formation is rich in the 27 ammonites Discoscaphites iris and Eubaculites carinatus, which, along with 28 biostratigraphically important dinoflagellate cysts and calcareous nannofossils, indicate 29 deposition occurred within the last 1 million years, most likely last 500 kyrs, of the 30 Cretaceous. -
Highly Diversified Late Cretaceous Fish Assemblage Revealed by Otoliths (Ripley Formation and Owl Creek Formation, Northeast Mississippi, Usa)
Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 126(1): 111-155. March 2020 HIGHLY DIVERSIFIED LATE CRETACEOUS FISH ASSEMBLAGE REVEALED BY OTOLITHS (RIPLEY FORMATION AND OWL CREEK FORMATION, NORTHEAST MISSISSIPPI, USA) GARY L. STRINGER1, WERNER SCHWARZHANS*2 , GEORGE PHILLIPS3 & ROGER LAMBERT4 1Museum of Natural History, University of Louisiana at Monroe, Monroe, Louisiana 71209, USA. E-mail: [email protected] 2Natural History Museum of Denmark, Zoological Museum, Universitetsparken 15, DK-2100, Copenhagen, Denmark. E-mail: [email protected] 3Mississippi Museum of Natural Science, 2148 Riverside Drive, Jackson, Mississippi 39202, USA. E-mail: [email protected] 4North Mississippi Gem and Mineral Society, 1817 CR 700, Corinth, Mississippi, 38834, USA. E-mail: [email protected] *Corresponding author To cite this article: Stringer G.L., Schwarzhans W., Phillips G. & Lambert R. (2020) - Highly diversified Late Cretaceous fish assemblage revealed by otoliths (Ripley Formation and Owl Creek Formation, Northeast Mississippi, USA). Riv. It. Paleontol. Strat., 126(1): 111-155. Keywords: Beryciformes; Holocentriformes; Aulopiformes; otolith; evolutionary implications; paleoecology. Abstract. Bulk sampling and extensive, systematic surface collecting of the Coon Creek Member of the Ripley Formation (early Maastrichtian) at the Blue Springs locality and primarily bulk sampling of the Owl Creek Formation (late Maastrichtian) at the Owl Creek type locality, both in northeast Mississippi, USA, have produced the largest and most highly diversified actinopterygian otolith (ear stone) assemblage described from the Mesozoic of North America. The 3,802 otoliths represent 30 taxa of bony fishes representing at least 22 families. In addition, there were two different morphological types of lapilli, which were not identifiable to species level. -
Vorkommen Und Häufigkeit Des Erdkäfers Trox Scaber L., 1758, Im Niederbayerischen Inntal Und in München
112. Bd. 2008 ©Naturwissenschaftlicher VereinBerichte für Schwaben, des Naturwissenschaftlichen download unter www.biologiezentrum.at Vereins für Schwaben e.V. Josef H. Reichholf Vorkommen und Häufigkeit des ErdkäfersTrox scaber L., 1758, im niederbayerischen Inntal und in München (Scarabaeoidea, Erdkäfer: Trogidae) Einleitung Die Erdkäfer, Trogidae, bilden innerhalb der Überfamilie der Scarabaeoidea eine eigene, kleine und gut abgegrenzte Familie, von der in Mitteleuropa nur 5 bis 8 Arten Vorkommen (Z a h r a d n ik 1985). Drei Angehörige der Gattung Trox gelten derzeit in Bayern als ausgestorben oder verschollen (J u n g w ir t h 2003). Zu den wenigen häufigen Arten finden sich in den gängigen Käferbüchern fast gleich lautende, sehr allgemeine Angaben, wie etwa für die hier behandelte Art Trox scaber bei S a u e r (1993): „Von April bis Oktober auf sandigen Feldern unter ausgetrockneten Kadavern. Die Käfer können zirpen und fliegen bei Nacht Lichtquellen an.“ Für Trox sabulosus führt er fast das Gleiche an: „In sandigen Gebieten unter trockenen Kadavern, Kno chen, Fellen und Horn“ Bei Z a h r a d n ik (1985) liest es sich für diesen Erdkäfer so: „Unter ausgetrockneten tierischen Überresten, vor allem auf Sandböden“ und dieser ergänzt „überwiegend in der Tiefebene“. Beide einander recht ähnliche Arten unter scheiden sich ein wenig in der Größe, zu der für T. scaber 5 -7 mm, für T. sabulosus 8-9 mm angegeben werden. Bei diesem sind die Fühler hell und die beiden innersten Glieder abstehend behaart, bei T. scaber aber rostbraun. Dieser trägt am Rand des Halsschildes eine deutliche Reihe heller Borsten und die Flügeldecken hält S a u e r (1993) für „sehr schwach buckelig“ Doch dies ist nicht leicht zu sehen, da sich diese Käfer mit einer mehr oder weniger ausgeprägten Schicht aus Lehm und Sekret bedecken (Z a h r a d n ik 1985), so dass sie auch häufig schmutziggrau und nicht schwarz aussehen. -
Quick Guide for the Identification Of
Quick Guide for the Identification of Maryland Scarabaeoidea Mallory Hagadorn Dr. Dana L. Price Department of Biological Sciences Salisbury University This document is a pictorial reference of Maryland Scarabaeoidea genera (and sometimes species) that was created to expedite the identification of Maryland Scarabs. Our current understanding of Maryland Scarabs comes from “An Annotated Checklist of the Scarabaeoidea (Coleoptera) of Maryland” (Staines 1984). Staines reported 266 species and subspecies using literature and review of several Maryland Museums. Dr. Price and her research students are currently conducting a bioinventory of Maryland Scarabs that will be used to create a “Taxonomic Guide to the Scarabaeoidea of Maryland”. This will include dichotomous keys to family and species based on historical reports and collections from all 23 counties in Maryland. This document should be cited as: Hagadorn, M.A. and D.L. Price. 2012. Quick Guide for the Identification of Maryland Scarabaeoidea. Salisbury University. Pp. 54. Questions regarding this document should be sent to: Dr. Dana L. Price - [email protected] **All pictures within are linked to their copyright holder. Table of Contents Families of Scarabaeoidea of Maryland……………………………………... 6 Geotrupidae……………………………………………………………………. 7 Subfamily Bolboceratinae……………………………………………… 7 Genus Bolbocerosoma………………………………………… 7 Genus Eucanthus………………………………………………. 7 Subfamily Geotrupinae………………………………………………… 8 Genus Geotrupes………………………………………………. 8 Genus Odonteus...……………………………………………… 9 Glaphyridae.............................................................................................. -
New Upper Cretaceous Amphineura (Mollusca)
New Upper Cretaceous Amphineura (Mollusca) GEOLOGICAL SURVEY PROFESSIONAL PAPER 593-G New Upper Cretaceous Amphineura (Mollusca) By ALLYN G. SMITH, NORMAN F. SOHL, and ELLIS L. YOCHELSON CONTRIBUTIONS TO PALEONTOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 593-G Description of chitons from the Gulf Coastal Plain and Puerto Rico UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 30 cents (paper cover) CONTENTS Page Abstract___________________________________________________________________ Gl Introduction_______________________________________________________________ 1 Geologic occurrence_ __ __ __ _ _ _ __ _ _ _ __ _ _ __ _ __ _ _ _ __ __ __ __ __ __ __ _ _ _ _ __ _ __ _ __ __ __ 1 Coastal Plain province____ _ _ _ __ _ __ __ __ _ _ _ _ _ __ _ _ _ __ _ _ _ _ _ __ __ __ _ _ _ _ _ _ __ __ _ _ 1 Caribbean province_____________________________________________________ 2 Previous reports of Cretaceous Amphineura (Polyplacophora) _ _ _ _ _ __ __ __ _ _ _ __ __ __ 3 Systematic paleontology_____________________________________________________ 3 References cited____ __ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ __ __ __ __ _ _ _ __ _ _ __ _ _ _ __ __ _ _ _ _ _ __ __ _ __ __ 7 Index_____________________________________________________________________ 8 ILLUSTRATIONS [Plate follows index] Page PLATE 1. Chiton (Chiton} and Aulachochiton. -
Uppermost Campanian–Maestrichtian Strontium Isotopic, Biostratigraphic, and Sequence Stratigraphic Framework of the New Jersey Coastal Plain
Uppermost Campanian–Maestrichtian strontium isotopic, biostratigraphic, and sequence stratigraphic framework of the New Jersey Coastal Plain Peter J. Sugarman New Jersey Geological Survey, CN 427, Trenton, New Jersey 08625, and Department of Geological Sciences, Rutgers University, New Brunswick, New Jersey 08903 Kenneth G. Miller Department of Geological Sciences, Rutgers University, New Brunswick, New Jersey 08903, and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964 David Bukry U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025 Mark D. Feigenson Department of Geological Sciences, Rutgers University, New Brunswick, New Jersey 08903 ABSTRACT boundaries elsewhere in the Atlantic Recent stratigraphic studies have concen- Coastal Plain (Owens and Gohn, 1985) and trated on the relationships between these se- Firm stratigraphic correlations are the inferred global sea-level record of Haq quences, their bounding surfaces (unconfor- needed to evaluate the global significance of et al. (1987); they support eustatic changes mities), and related sea-level changes. The unconformity bounded units (sequences). as the mechanism controlling depositional shoaling-upward sequences described by We correlate the well-developed uppermost history of this sequence. However, the latest Owens and Sohl (1969) have been related to Campanian and Maestrichtian sequences Maestrichtian record in New Jersey does recent sequence stratigraphic terminology of the New Jersey Coastal Plain to the geo- not agree with Haq et al. (1987); we at- (e.g., Van Wagoner et al., 1988) by Olsson magnetic polarity time scale (GPTS) by in- tribute this to correlation and time-scale (1991) and Sugarman et al. (1993). Glauco- tegrating Sr-isotopic stratigraphy and bio- differences near the Cretaceous/Paleogene nite beds are equivalent to the condensed stratigraphy. -
Coleoptera: Trogidae) on Insect Cadavers, Cow Dung, and Mushroom
NOTE Survival and Reproduction of Trox suberosus F. (Coleoptera: Trogidae) on Insect Cadavers, Cow Dung, and Mushroom Orrey P. Young United States Department of Agriculture, Agricultural Research Service, Southern Grain Insects Research Laboratory. P0 Box 748, Tifton, Georgia 31793 USA J. Entomol. Sci. 41(3): 271-276 (July 2006) Key Words Trox, Scarabaeoidea, Trogidae, dead insects, carrion, fungi, starvation, longev- ity, diet. progeny Trox suberosus F. (Coleoptera: Scarabaeoidea: Trogidae) has occasionally been collected at vertebrate feces (Fincher et al. 1970, J. Parasitol. 56: 378-383), but typical food choices for this and all other Trox species in eastern North America are the dried remains of vertebrates, such as fur, hair, feathers, skin, muscle, and bone (Vaurie 1955, Bull. Am. Mus. Nat. Hist. 106: 1-90). Although Trox species have been collected at dead insects (Baker 1968, Bull. U.S. Nat. Mus. 279: 1-79; Young 1984, Environ. Entomol. 13:1346-1351), only Young and Hamm (1985, J. Entomol. Sci. 20: 90-94) have demonstrated that adult Trox (T. suberosus) will consume some type of dead insect. Whereas Baker (1968) reared many Trox species from egg to adult on a moist diet mixture of cow hair, deer hair, sheeps wool, rabbit hair and skin, and pheasant, quail, and dove feathers and skin, there are no available data indicating that any adult Trox can survive or that immatures can develop on a diet of dead insects. The purpose of the experiment herein was to document the survival and reproduction of T. suberosus on various dead insects, dung, and fungi, as well as in the absence of food. -
Upper Cretaceous (Maestrichtian) Mollusca from the Haustator Bilira Assemblage Zone in the East Gulf Coastal Plain
UNITED STATES DEPARTMENT OF INTERIOR GEOLOGICAL SURVEY Upper Cretaceous (Maestrichtian) Mollusca from the Haustator bilira Assemblage Zone in the East Gulf Coastal Plain Norman F. So hi 1 and Carl F. Koch2 Open File Feport 83-451 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial Standards and stratigraphic nomenclature. Pages are numbered one to four and seven to 239. 1. Washington D.C. 2. Old Dominion University Norfolk, Va, 1983 CONTENTS Page Introduction 1 Explanation 1 Explanation of Annotation 4 References 9 Molluscan Faunal Lists 11 ILLUSTRATIONS Figure 1 Map showing location of collections 2 Relationships of stratigraphic units within the Haustator bilira Assemblage Zone, East Gulf Coastal Plain TABLE Table 1 U.S. Geological Survey numbers of collections for each location Upper Cretaceous (Maestrichtian) Mollusca from the Haustator bilira Assemblage Zone in the East Gulf Coastal Plain INTRODUCTION The following report contains lists of the molluscan fauna from 189 collections made at 161 localities or different levels at a locality in the rocks of the Haustator bilira Assemblage Zone as exposed in western Georgia, Alabama, Mississippi, and Tennessee (Figure 1). This compilation forms the data base for a series of studies published, in press or in preparation (Buzas, £t_ al. , 1982; Koch and Sohl, in press). The Haustator bilira Assemblage Zone was proposed by Sohl (1977) and traced through Late Cretaceous rocks of the Atlantic and Gulf Coastal Plains from New Jersey to Texas (Owens, et_jil_., 1977; Sohl and Smith, 1980). The base of the zone occurs above the base of the foraminiferid Globotruncana gansseri subzone of Pessagno (1967) and includes all subsequent younger Cretaceous deposits on the Coastal Plains (Figure 2). -
PSEG POWER, LLC (Environmental Report), Rev. 0
Occurrence in Formation/Unit Primary Lithologies Geologic Conditions Unit Thickness Site Area Quaternary Marsh deposits muck and peat; silt, sand and clay aggradation of Delaware Bay estuary variable thickness present over most of the site area in low lying areas Holocene ~~~~~~~~~~ unconformity ~~~~~~~~~~ DELAWARE NEW JERSEY Scotts Corners Formation outcrops in eastern and Cape May estuarine terrace deposits with coarse to fine sand and pebbles with Quaternary ~~ unconformity ~~ transgressive and regressive cycles western portions of the site concentrations of heavy minerals; peat; isolated fluvial deposits? variable thickness Formation area Group Lynch Heights Pleistocene Delaware Bay Formation ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ unconformity ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ regression and erosion CENOZOIC 90 feet at southern portions Kirkwood Formation clay silt and sand deposited in two or three marine cycles polycyclic transgression and regression phases subcrop only of site area; pinches out northward Upper Tertiary (Miocene) ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ unconformity ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ regression and erosion Shark River Formation glauconitic sand and mudstone low sediment input 70 feet (Reference 2.6-10) subcrop only ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ unconformity ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ regression and erosion Tertiary Manasquan Formation lower glauconitic member; upper clayey sand to silt member low sediment input and bioturbation 40 feet (Reference 2.6-10) subcrop only ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ -
Novitates PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET, NEW YORK, N.Y
AMERICANj MUSEUM Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 3186, 14 pp., 12 figures, 2 tables December 31, 1996 The Maastrichtian Ammonites Coahuilites sheltoni Btose, 1928, and Sphenodiscus pleurisepta (Conrad, 1857), from the Uppermost Pierre Shale and Basal Fox Hills Formation of Colorado and Wyoming W. J. KENNEDY,' N. H. LANDMAN,2 AND W. A. COBBAN3 ABSTRACT The Maastrichtian ammonites Coahuilites shel- birkelundi zone of Niobrara County, Wyoming, toni Bose, 1928, and Sphenodiscus pleurisepta and Weld County, Colorado. S. pleurisepta occurs (Conrad, 1857), are described from the Western in the H. birkelundi zone of Niobrara County, Interior where they are rare tethyan immigrants Wyoming; Weld County, Colorado; and Meade from Trans-Pecos Texas and adjacent parts of and Pennington counties, South Dakota. Mexico. C. sheltoni occurs in the Hoploscaphites INTRODUCTION Sphenodiscid ammonites dominate the known from the Western Interior: Sphenodis- ammonite faunas of the Escondido Forma- cus lobatus (Tuomey, 1856), Sphenodiscus tion and its correlatives in Trans-Pecos Texas pleurisepta (Conrad, 1857), and Coahuilites and adjacent parts of Mexico, and are also sheltoni Bose, 1928. known from other parts of the Gulf Coast The most common species in the Western and Atlantic Seaboard as far north as New Interior is Sphenodiscus lobatus. Examples Jersey. However, only three species are of this species are illustrated in Meek (1876: ' Curator, Geological Collections, University Museum, Parks Road, Oxford OXI 3PW, U.K. 2 Curator and Chairman, Department of Invertebrates, American Museum of Natural History. 370 Estes St., Lakewood, Colorado 80226.