Geologic Map of New Jersey: Central Sheet
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
Triassic- Jurassic Stratigraphy Of
Triassic- Jurassic Stratigraphy of the <JF C7 JL / Culpfeper and B arbour sville Basins, VirginiaC7 and Maryland/ ll.S. PAPER Triassic-Jurassic Stratigraphy of the Culpeper and Barboursville Basins, Virginia and Maryland By K.Y. LEE and AJ. FROELICH U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1472 A clarification of the Triassic--Jurassic stratigraphic sequences, sedimentation, and depositional environments UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1989 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging in Publication Data Lee, K.Y. Triassic-Jurassic stratigraphy of the Culpeper and Barboursville basins, Virginia and Maryland. (U.S. Geological Survey professional paper ; 1472) Bibliography: p. Supt. of Docs. no. : I 19.16:1472 1. Geology, Stratigraphic Triassic. 2. Geology, Stratigraphic Jurassic. 3. Geology Culpeper Basin (Va. and Md.) 4. Geology Virginia Barboursville Basin. I. Froelich, A.J. (Albert Joseph), 1929- II. Title. III. Series. QE676.L44 1989 551.7'62'09755 87-600318 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Page Abstract.......................................................................................................... 1 Stratigraphy Continued Introduction... .......................................................................................... -
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. -
Bulletin 52. the Stratigraphy, Fauna and Correlation of The
52 -. BULLETIN~ .. _GEOLOGIC SERIES The Str:;ttigraphy, Fauna _ and Correlation of the Vincentown Formation ' \ I , I by KATHERINE FIEI;DING GREACE~ "· ' . ' DEPARTMENT OF ; .. CONSERVATION- AND DEVELOPMENT STATE OF NEW JERSEY' ' _,. CHARLES P. WrLBEJ!, Director and Chief of the Division of · · · - · ' Forests and Parks · 1 . ,MEipiDITH K JoHNSON,· Chief of the Division of Geology ' · and Topography _, Trenton,' N. J. 194i . ' NEW JERSEY GEOLOGICAL SURVEY BULLETIN 52 GEOLOGIC SERIES The Stratigraphy, Fauna and Correlation of the Vincentown Formation hy KATHERINE FIELDING GREAOEN DEPARTMENT OF CONSERVATION AND DEVELOPMENT STATE OF NEW JERSEY CHARLES P. WILBER, Director anrl Chief of the Division of Forests and Parks MEREDITH E . .TOW, SON, Chief of the Division of Geology and 'ropography Trenton, N. J. 1941 NEW JERSEY GEOLOGICAL SURVEY BOARD OF CONSERVATION AND DEVELOPMENT State House Annex, Trenton, N.J. CoT •. H. JJ. ?IIOELLER, Presldant . ....................... :Millburn A1n'HLlll J. CoLLrxs, JR., ........................... :;\loorestmrJJ \Vn1.1.-Ut C. COPE ...................... _ ........... Glen l{idge HciRRY L. DERRY ............•.........•..•.......... )fontclair JLIRTIN J. HoGENCAl!P .............................. Glen Rock \V. STEW.ART HOI.LJ)[GSHEAD .....•..•.................. Riverton CHARLES A. MEYER ..•.•.•••••..••.•..••.............. :\ndover OWEN WrNSTO" ...•...............•........•........ Mendham 2 NEW JERSEY GEOLOGICAL SURVEY ----------------------------------- LETTER OF TRANSMITTAL March 15, 1941. Mr. Charles P. -
A Dinosaur Track from New Jersey at the State Museum in Trenton
New Jersey Geological and Water Survey Information Circular What's in a Rock? A Dinosaur Track from New Jersey at the State Museum in Trenton Introduction a large dinosaur track (fig. 2) on the bottom. Most of the rock is sedimentary, sandstone from the 15,000-foot-thick Passaic A large, red rock in front of the New Jersey State Museum Formation. The bottom part is igneous, lava from the 525-foot- (NJSM) in Trenton (fig. 1) is more than just a rock. It has a thick Orange Mountain Basalt, which overspread the Passaic fascinating geological history. This three-ton slab, was excavated Formation. (The overspreading lava was originally at the top of from a construction site in Woodland Park, Passaic County. It the rock, but the rock is displayed upside down to showcase the was brought to Trenton in 2010 and placed upside down to show dinosaur footprint). The rock is about 200 million years old, from the Triassic footprints Period of geologic time. It formed in a rift valley, the Newark Passaic Formation Basin, when Africa, positioned adjacent to the mid-Atlantic states, began to pull eastward and North America began to pull westward contact to open the Atlantic Ocean. The pulling and stretching caused faults to move and the rift valley to subside along border faults including the Ramapo Fault of northeastern New Jersey, about 8 miles west of Woodland Park. Sediments from erosion of higher Collection site Orange Mountain Basalt top N Figure 1. Rock at the New Jersey State Museum. Photo by W. Kuehne Adhesion ripples DESCRIPTION OF MAP UNITS 0 1 2 mi Orange Mountain Basalt L 32 cm Jo (Lower Jurassic) 0 1 2 km W 25.4 cm contour interval 20 feet ^p Passaic Formation (Upper Triassic) Figure 3. -
Somerset County, New Jersey Geology
Natural and Cultural Resource Inventory & Guide Somerset County, New Jersey Geology 456659 456613 Peapack- Bernardsville ab206 456525 Gladstone Borough Borough 456661 456624 456512 456657 ab202 Far Hills Borough 456512 Bernards 456640 [^287 Township Bedminster Township 456622 456655 456523 NOTES 1. This map was prepared using GIS data produced & distributed 456531 456652 ¤£22 by the New Jersey Geological Survey. 456665 Watchung 2. Depiction of environmental features is for general information 456653 Borough purposes only, and shall not be construed to define the legal ¦¨§78 ¦¨§78 geographic jurisdiction associated with any statutes or rules. 456651 3. Somerset County uses the following map projection & coordinate system when presenting GIS data: 456620 - Horizontal: North American Datum 1983 (NAD83) ab206 - Vertical: North American Vertical Datum 1987 (NAVD87) [^287 - Coordinate System: New Jersey State Plane Feet ab202 456618 DATA SOURCES Warren Township NEW JERSEY GEOLOGICAL SURVEY 638 641 456 456 636 649 - Geological Formations 456529 456 456 - Fault Lines Bridgewater Township North Plainfield NEW JERSEY DEPARTMENT OF Green Brook Borough ENVIRONMENTAL PROTECTION (NJDEP) 456614 - Streams ¤£22 Township 456616 NEW JERSEY DEPARTMENT OF TRANSPORTATION (NJDOT) 456679 456651 - Major Roads 456634 SOMERSET COUNTY GIS ENTERPRISE 456673 - County Boundaries - Municipal Boundaries 456527 - Parcel Boundaries (!28 ¤£22 456525 Raritan 456644 456643 Branchburg Borough Somerville 456633 456626 Bound Brook Township (!28 Borough Borough 637 456635 456 -
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. -
New Decapods from the Navidad Formation (Miocene) of Chile
JOURNAL OF CRUSTACEAN BIOLOGY, 25(3): 427–449, 2005 NEW DECAPODS FROM THE NAVIDAD FORMATION (MIOCENE) OF CHILE Rodney M. Feldmann, Carrie E. Schweitzer, and Alfonso Encinas (RMF, correspondence) Department of Geology, Kent State University, Kent, Ohio 44242, U.S.A. ([email protected]); (CES) Department of Geology, Kent State University Stark Campus, Canton, Ohio 44720, U.S.A. ([email protected]); (AE) Universidad de Chile, Departamento de Geologı´a, Casilla 13518, Correo 21, Santiago, Chile ([email protected]) ABSTRACT A new Miocene decapod fauna is described from the Navidad Formation of coastal Chile. The fauna includes five callianassoid taxa, none of which is preserved sufficiently to identify to species level. New species include Calappilia? chilensis, Hepatus spinimarginatus, Proterocarcinus navidad, Pilumnus cucaoensis, and Pinnixa navidadensis. A possible rhizopine member of the Pilumnidae Samouelle, 1819, is described. Trichopeltarion levis Casadı´o et al., 2004, previously known from the late Oligocene of western Argentina, was also recovered from these rocks. Calappa circularis Beurlen, from the lower Miocene Pirabas Formation in Brazil, is herein referred to Calappilia. This report greatly increases the known number of fossil decapods from Chile and sets the stage for paleobiogeographic comparison of the decapod faunas of Chile and Argentina. The Neogene rock sequence in Chile is largely confined to M.S. thesis, added Callianassa sp. and a new species of crab about seven basins along the modern Pacific Ocean to the list. That material along with the newly collected (Ceccioni, 1980). These basins have been subject to extreme specimens will be discussed herein. vertical motion during the Neogene (Martı´nez-Pardo, 1990) so that rocks have been deposited at depths ranging from GEOLOGICAL SETTING shallow, inner shelf to bathyal. -
Evaluation of Groundwater Resources of Bernards Township, Somerset County, New Jersey
Evaluation of Groundwater Resources of Bernards Township, Somerset County, New Jersey M2 Associates Inc. 56 Country Acres Drive Hampton, New Jersey 08827 EVALUATION OF GROUNDWATER RESOURCES OF BERNARDS TOWNSHIP SOMERSET COUNTY, NEW JERSEY APRIL 11, 2008 Prepared for: Bernards Township 1 Collyer Lane Basking Ridge, NJ 07920 Prepared by: Matthew J. Mulhall, P.G. M2 Associates Inc. 56 Country Acres Drive Hampton, New Jersey 08827-4110 908-238-0827 Fax: 908-238-0830 EVALUATION OF GROUNDWATER RESOURCES OF BERNARDS TOWNSHIP SOMERSET COUNTY, NEW JERSEY TABLE OF CONTENTS INTRODUCTION............................................................................................................. 1 GEOLOGY ...................................................................................................................... 5 PHYSIOGRAPHIC PROVINCE ............................................................................................ 5 SURFACE WATER .......................................................................................................... 6 Watersheds............................................................................................................. 6 Stream Classifications........................................................................................... 7 Headwaters............................................................................................................. 9 SOILS ......................................................................................................................... 10 BEDROCK...................................................................................................................