Selenium Occurrence in Certain Soils in the United States, with a Discussion Of- .R Related Topics: Sixth Report'
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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. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
The Geology, Paleontology and Paleoecology of the Cerro Fortaleza Formation
The Geology, Paleontology and Paleoecology of the Cerro Fortaleza Formation, Patagonia (Argentina) A Thesis Submitted to the Faculty of Drexel University by Victoria Margaret Egerton in partial fulfillment of the requirements for the degree of Doctor of Philosophy November 2011 © Copyright 2011 Victoria M. Egerton. All Rights Reserved. ii Dedications To my mother and father iii Acknowledgments The knowledge, guidance and commitment of a great number of people have led to my success while at Drexel University. I would first like to thank Drexel University and the College of Arts and Sciences for providing world-class facilities while I pursued my PhD. I would also like to thank the Department of Biology for its support and dedication. I would like to thank my advisor, Dr. Kenneth Lacovara, for his guidance and patience. Additionally, I would like to thank him for including me in his pursuit of knowledge of Argentine dinosaurs and their environments. I am also indebted to my committee members, Dr. Gail Hearn, Dr. Jake Russell, Dr. Mike O‘Connor, Dr. Matthew Lamanna, Dr. Christopher Williams and Professor Hermann Pfefferkorn for their valuable comments and time. The support of Argentine scientists has been essential for allowing me to pursue my research. I am thankful that I had the opportunity to work with such kind and knowledgeable people. I would like to thank Dr. Fernando Novas (Museo Argentino de Ciencias Naturales) for helping me obtain specimens that allowed this research to happen. I would also like to thank Dr. Viviana Barreda (Museo Argentino de Ciencias Naturales) for her allowing me use of her lab space while I was visiting Museo Argentino de Ciencias Naturales. -
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. -
Publications Related to Stratigraphy, Sedimentology and Paleontology (All Featured Fossils in Publications Are Self-Collected.)
Publications Related to Stratigraphy, Sedimentology and Paleontology (All featured fossils in publications are self-collected.) 1) Becker, M., Slattery, W., and Chamberlain, J., 1996, Reworked Campanian and Maastrichtian Macrofossils in a Sequence Bounding Transgressive Lag Deposit, Monmouth County, New Jersey, Northeast Geology and Environmental Science, Vol. 18, pp. 234-252. 2) Becker, M., Slattery, W., and Chamberlain, J., 1998, Mixing of Santonian and Campanian Chondrichthyan and Ammonite Macrofossils along a Transgressive Lag Deposit, Greene County, Western Alabama, Southeastern Geology, Vol. 7, No. 1, pp. 1-12. 3) Becker, M., Meier, J., and Slattery, W., 1999, Spiral Coprolites from the Upper Cretaceous Wenonah-Mt. Laurel and Navesink Formations in the Northern Coastal Plain of New Jersey, Northeastern Geology and Environmental Science, Vol. 21, No. 3, pp. 181-187. 4) Becker, M., Chamberlain, J., and Stoffer, P., 2000, Pathological Tooth Deformities in Modern and Late Cretaceous Chondrichthyans: A Consequence of Feeding Related Injury, Lethaia, Vol. 36, No. 2, pp. 1-16. 5) Becker, M., and Chamberlain, J., 2001, Fossil Turtles from the Lowermost Navesink Formation (Maastrichtian) in Monmouth County New Jersey, Northeastern Geology and Environmental Science, Vol. 23, No. 4, pp. 332-339. 6) Chamberlain, J., Terry, D., Stoffer, P., and Becker, M., 2001, Paleontology of the K/T Boundary: Badlands National Park, South Dakota; in Santucci, V. L. and McClelland, L., eds., Proceedings of the 6th Fossil Resource Conference: National Park Service Geological Resource Division Technical Report, pp. 11-22. 7) Becker, M., Earley R., and Chamberlain, J., 2002, A Survey of Non-Tooth Chondrichthyan Hard-Parts from the Lower Navesink Formation (Maastrichtian) in Monmouth County, New Jersey, Northeastern Geology and Environmental Science, Vol. -
Jason P. Schein
Curriculum Vitae JASON P. SCHEIN EXECUTIVE DIRECTOR BIGHORN BASIN PALEONTOLOGICAL INSTITUTE 3959 Welsh Road, Ste. 208 Willow Grove, Pennsylvania 19090 Office: (406) 998-1390 Cell: (610) 996-1055 [email protected] EDUCATION Ph.D. Student Drexel University, Department of Biology, Earth and Environmental Science, 2005-2013 M.Sc., Auburn University, Department of Geology and Geography, 2004 B.Sc., Auburn University, Department of Geology and Geography, 2000 RESEARCH AND PROFESSIONAL INTERESTS Mesozoic vertebrate marine and terrestrial faunas, paleoecology, paleobiogeography, faunistics, taphonomy, biostratigraphy, functional morphology, sedimentology, general natural history, education and outreach, paleontological resource assessment, and entrepreneurial academic paleontology. ACADEMIC, PROFESSIONAL, & BOARD POSITIONS 2019-Present Member of the Board, Yellowstone-Bighorn Research Association 2017-Present Founding Executive Director, Bighorn Basin Paleontological Institute 2017-Present Member of the Board, Delaware Valley Paleontological Society 2016-Present Scientific and Educational Consultant, Field Station: Dinosaurs 2015-Present Graduate Research Associate, Academy of Natural Sciences of Drexel University 2007-2017 Assistant Curator of Natural History Collections and Exhibits, New Jersey State Museum 2015-2017 Co-founder, Co-leader, Bighorn Basin Dinosaur Project 2010-2015 International Research Associate, Palaeontology Research Team, University of Manchester 2010-2014 Co-leader, New Jersey State Museum’s Paleontology Field Camp 2007-2009 Interim Assistant Curator of Natural History, New Jersey State Museum 2006-2007 Manager, Dinosaur Hall Fossil Preparation Laboratory 2004-2005 Staff Environmental Geologist, Cobb Environmental and Technical Services, Inc. 1 FIELD EXPERIENCE 2010-2019 Beartooth Butte, Morrison, Lance, and Fort Union formations, Bighorn Basin, Wyoming and Montana, U.S.A. (Devonian, Jurassic, Late Cretaceous, and earliest Paleocene, respectively) 2010 Hell Creek Formation, South Dakota, U.S.A. -
Recent Mosasaur Discoveries from New Jersey and Delaware, USA: Stratigraphy, Taphonomy and Implications for Mosasaur Extinction
r fs| Netherlands Journal of Geosciences — Geologie en Mijnbouw | 84 - 3 | 241 - 245 | 2005 Recent mosasaur discoveries from New Jersey and Delaware, USA: stratigraphy, taphonomy and implications for mosasaur extinction W.B. Gallagher1' 1 Bureau of Natural History, New Jersey State Museum, Trenton, NJ 08625-0530, USA. Email: [email protected] 2 Department of Geological Sciences, Rutgers University, Piscataway, NJ 08855, USA. Manuscript received: December 2004; accepted: January 2005 Abstract The Upper Cretaceous deposits of New Jersey and Delaware produced the first mosasaur specimens collected in North America. Recent recovery of mosasaur specimens from streambank exposures and new excavation sites has increased our knowledge of the stratigraphic distribution of these animals in the northern Atlantic coastal plain. Reassessment of the source and age of mosasaur specimens from the Big Brook site and other localities in Monmouth County (NJ) has greatly increased the number of known Campanian mosasaur specimens from this region. Two main taphonomic occurrence modes are noted: 1 - single, worn and broken bones and isolated teeth in mixed faunal deposits probably accumulated due to current action in nearshore environments; 2 - partial skeletons, skulls and single bones in deeper-water settings were the aftermath of biological modification of carcasses and deadfalls. The mosasaurs of the New Egypt Formation represent some of the last (i.e., stratigraphically highest) mosasaur fossils in North America. Mosasaur extinction was due to the collapse of the rich Late Cretaceous marine food web at the K/T boundary. Subsequently in the early Paleocene, with the disappearance of the mosasaurs, crocodilians became the apical predators of the marine environment in this area. -
Cretaceous Fossils from the Chesapeake and Delaware Canal
Cretaceous S;cial Publication No. 18 Fossils from the Chesapeake and Delaware Canal A Guide for Students and Collectors Edward M. Lauginiger / /~ / CRETACEOUS FOSSILS FROM THE CHESAPEAKE AND DELAWARE CANAL: A GUIDE FOR STUDENTS AND COLLECTORS By Edward M. Lauginiger Biology Teacher Academy Park High School Sharon Hill, Pennsylvania September 1988 Reprinted 1997 CONTENTS Page INTRODUCTION. • 1 ACKNOWLEDGMENTS 2 PREVIOUS STUDIES. 3 FOSSILS AND FOSSILIZATION 5 Requirements for Fossilization 6 Types of Fossilization 7 GEOLOGY •• 10 CLASSIFICATON OF FOSSILS. 12 Kingdom Monera • 13 Kindgom Protista 1 3 Kingdom Plantae. 1 4 Kingdom Animalia 15 Phylum Porifera 15 Phylum Cnidaria (Coelenterata). 16 Phylum Bryozoa. 16 Phylum Brachiopoda. 17 Phylum Mollusca • 18 Phylum Annelida •. 22 Phylum Arthropoda • 23 Phylum Echinodermata. 24 Phylum Chordata 24 COLLECTING LOCALITIES 28 FOSSIL CHECK LIST 30 BIBLIOGRAPHY. 33 PLATES. ••• 39 iii FIGURES Page Figure 1 • Index map of the Chesapeake and Delaware Canal Area. .. .. 2 Figure 2. Generalized stratigraphic column of the formations exposed at the C & D Canal. 11 Figure 3. Foraminifera 14 Figure 4. Porifera 16 Figure 5. Cnidaria 16 Figure 6. Bryozoa. 17 Figure 7. Brachiopoda. 18 Figure 8. Mollusca-Gastropoda. 19 Figure 9. Mollusca-Pelecypoda. 21 Figure 10. Mollusca-Cephalopoda 22 Figure 11. Annelida . 22 Figure 12. Arthropoda 23 Figure 13. Echinodermata. 25 Figure 1 4. Chordata . 27 Figure 1 5. Collecting localities at the Chesapeake and Delaware Canal . ... .. 29 v CRETACEOUS FOSSILS FROM THE CHESAPEAKE AND DELAWARE CANAL: A GUIDE FOR STUDENTS AND COLLECTORS Edward M. Lauginiger INTRODUCTION Fossil collectors have been attracted to Delaware since the late 1820s when the excavation of the Chesapeake and Delaware (C&D) Canal first exposed marine fossils of Cretaceous age (Fig. -
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 ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ -
Short−Term Survival of Ammonites in New Jersey After the End−Cretaceous Bolide Impact
Short−term survival of ammonites in New Jersey after the end−Cretaceous bolide impact NEIL H. LANDMAN, MATTHEW P. GARB, REMY ROVELLI, DENTON S. EBEL, and LUCY E. EDWARDS Landman, N.H., Garb, M.P., Rovelli, R., Ebel, D.S., and Edwards, L.E. 2012. Short−term survival of ammonites in New Jersey after the end−Cretaceous bolide impact. Acta Palaeontologica Polonica 57 (4): 703–715. A section containing the Cretaceous/Paleogene (= Cretaceous/Tertiary) boundary in Monmouth County, New Jersey, pre− serves a record of ammonites extending from the end of the Cretaceous into possibly the beginning of the Danian. The sec− tion includes the upper part of the Tinton Formation and lower part of the Hornerstown Formation. The top of the Tinton Formation is represented by a richly fossiliferous unit (the Pinna Layer) that contains many bivalves in life position as well as ammonite jaws preserved inside body chambers. Ammonites include Pachydiscus (Neodesmoceras) mokotibensis, Sphenodiscus lobatus, Eubaculites carinatus, E. latecarinatus, Discoscaphites iris, D. sphaeroidalis, D. minardi,andD. jerseyensis.ThePinna Layer probably represents a relatively short interval of time lasting tens to hundreds of years; it is conformably overlain by the Burrowed Unit, which contains a single fragment of Discoscaphites sp. and several fragments of E. latecarinatus, as well as several isolated specimens of ammonite jaws including two of Eubaculites. Examination of the mode of preservation of the ammonites and jaws suggests that they were fossilized during deposition of the Burrowed Unit and were not reworked from older deposits. Based on the ammonites and dinoflagellates in the Pinna Layer and the Burrowed Unit, these strata traditionally would be assigned to the uppermost Maastrichtian, corresponding to calcareous nannofossil Subzone CC26b. -
Early Discoveries of Dinosaurs from North America and the Significance of the Springfield Armory Dinosaur Site
Early Discoveries of Dinosaurs From North America and the Significance of the Springfield Armory Dinosaur Site Vincent L. Santucci National Park Service, P.O. Box 592, Kemmerer, WY 83101 Abstract—Prior to the "Great American Dinosaur Rush" during the late 1800s, there were relatively few dinosaur sites recorded in North America. Hadrosaurus foulkii is recognized as the first articulated dinosaur collected, described and displayed in the New World. Most of the early discoveries consist of the fossil trackways from the Connecticut Valley and few partial dinosaur skeletons. The type specimen of the prosauropod dinosaur Anchisaurus polyzelus is recognized as one of the earliest dinosaur discoveries in North America. The fossil bones of Anchisaurus were uncovered during a blasting operation at the armory in Springfield, Massachusetts in the early 1800s. The excavation at this site is an important record in the early history of the science of dinosaur paleontology in North America. Introduction Prior to the 1870s and the "Great Era of Dinosaur Discoveries" there is a limited history for dinosaur paleontology in North America. Relatively few dinosaur specimens were recovered prior to the American Civil War. There appeared to be a general lack of interest in the petrifications of ancient life during the first half of the 19th century. The description and naming of the dinosaur remains often came long after their discovery. Early Disciveries Of Dinosaurs In North America 1802 — Dinosaur footprints.— In 1802, Pliny Figure 1—Late 1800s magazine illustration of the Moody, a student at Williams College, found the Springfield Armory Watershop main gate. Dinosaur bones footprint impressions near Moody's Corner, his South were discovered during the construction of this building. -
Matthew Carl Lamanna
Curriculum Vitae Matthew Carl Lamanna Assistant Curator Section of Vertebrate Paleontology Carnegie Museum of Natural History 4400 Forbes Avenue Pittsburgh, Pennsylvania 15213-4080 (412) 578-2696 (Office) (412) 622-8837 (Fax) Email: [email protected] Internet: http://www.carnegiemnh.org/vp/lamanna.html Education 2004 Ph.D., University of Pennsylvania, Department of Earth and Environmental Science. 1999 M.Sc., University of Pennsylvania, Department of Earth and Environmental Science. 1997 B.Sc., Hobart College, Departments of Geoscience and Biology, cum laude. Research Interests Mesozoic (principally Cretaceous) vertebrate faunas, paleoecology, and paleobiogeography; non-avian and avian dinosaur anatomy, systematics, and phylogeny. Academic and Professional Positions 2013–present Research Associate, Cleveland Museum of Natural History. 2012–present Principal Investigator and Project Director, Antarctic Peninsula Paleontology Project (AP3). 2005–present Adjunct Assistant Professor, Department of Geology and Planetary Science, University of Pittsburgh. 2004–present Assistant Curator, Section of Vertebrate Paleontology, Carnegie Museum of Natural History. 1999–present Paleontologist, Bahariya Dinosaur Project. 1997–present Research Associate, Academy of Natural Sciences of Drexel University (Philadelphia). 1997–1998 Exhibit Design Consultant, Dinosaur Hall, Academy of Natural Sciences (Philadelphia). 1995 Research Assistant, University of New Orleans Lance Dinosaur Project. Field Experience 2016 Unnamed formation, Robertson Island,