Guide to the Mesozoic Redbeds of Central Connecticut

Total Page:16

File Type:pdf, Size:1020Kb

Guide to the Mesozoic Redbeds of Central Connecticut I I I Guide to the Mesozoic Redheds I of I Central Connecticut I JOHN F. HUBERT, ALAN A. REED, I WAYNE L. DOWDALL, and J. MICHAEL GILCHRIST I I I STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CONNECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION 1978 GUIDEBOOK NO. 4 On the cover: In the early morning along the shore of on East Berlin Lake, the 7-m phytosour Rutiodon snatches a Semionotus from the sho I lows. The tall horsetail Equisetum and cycad Otozomiles thrive in the wet mud of the lake strand. Stands of the conifer Aroucarioxylon tower 60 m high along the distant horizon on sandy soils of the well drained uplands. The dinosaur Eubronfes passed this way the previous evening. Sketch by Amy S. Hubert STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CONNECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION } } ] GUIDE TO THE MESOZOIC REDBEDS OF CENTRAL CONNECTICUT JOHN F. HUBERT J University of Massachusetts ALAN A. REED ) Chevron Oil Company WAYNE L • DOWDALL Weston Geophysical Resea:t>ch J. MICHAEL GILCHRIST Texaco Oil Company ,-------,_r-- -----------, i 1 i I 1 I ~ l ; .J J 1978 J GUIDEBOOK NO. 4 J J ii STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CONNECTICUT THE NATURAL RESOURCES CENTER DEPARTMENT OF ENVIRONMENTAL PROTECTION Honorable Ella Grasso, Governor of Connecticut Stanley J. Pac, Connnissioner of the Department of Environmental Protection STATE GEOLOGIST DIRECTOR, NATURAL RESOURCES CENTER Hugo F. Thomas, Ph.D. This guidebook is a reprint of "Guide to the Redbeds of Central Connecticut: 1978 Field Trip, Eastern Section of the Society of Economic Mineralogists and Paleontologists." It was originally published as Contribution No. 32, Department of Geology and Geography, University of Massachusetts; Amherst, Massachusetts. For information on ordering this guidebook and other publications of the Connecticut Geological and Natural History Survey, consult the List of Publications available from the Survey, Dept. of Environmental Protection, State Office Building, Hartford, Connecticut 06115. iii ) DEDICATION This guidebook is dedicated to the memory of Paul D• Krynine (1902-1964), superb teacher and researcher at The .l Pennsylvania State University and the foremost sedimentary petrographer of his day. His pioneering 1950 monograph . "Petrology, stratigraphy, and origin of the Triassic sedi- '1 mentary rocks of Connecticut" provides inspiration and a solid foundation for the subsequent advances in our under- standing of the sedimentology of the redbed sequence of the ) Connecticut Valley. J J J iv Special Note The fact that a locality is described in this guidebook does not imply that the public has access to the locality. Stopping ·on a limited access highway is forbidden by a regu­ lation of the State Traffic Commission, which prohibits all vehicles from stopping or parking on any part of the highway. These regulations also prohibit pedestrians on any limited access highway. Field trip features on these highways can be viewed from other ground. In other instances, stops on private property require permission of the owner. Anyone planning to go on this field trip should check carefully the suggested stops. Hugo F. Thomas State Geologist v TABLE OF CONTENTS DEDICATION.- • .••....•.........•. I • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • iii TABLE OF CONTENTS •••.••.•••.••••..•.••...•.••..•..••..•.• I • • • • • • • v LIST OF FIGURES. , • , , .• , , •••••.••.••. , , .....••..•.••.... , , • . • • • • • • viii ACKNOWLEDGMENTS , , •• , .••.••.••.•..• , . , . , • , •• , , , •• , •••. , , . • • • . • • xi OBJECTIVES OF THE TRIP •.••.••.••.••.• , ...••••.•• , •••• , . , ••••.• , • • 1 REGIONAL SETTING ••.•..•.. , , ••.••.••.•••..•••• , , ..•• , • • • . • • . • . • • 1 ABSTRACT OF THE PALEOGEOGRAPHIC HISTORY ..••••.••.••..••.••...•.•• 5 STOP 1. PORTLAND ARKO SE, DURHAM ••...•••.••••.•... , . • • . • . • • . • • • • 9 Location.................................................... 9 Introduction . ........................................... , . 9 Objective of Stop 1. ........................................ 10 Description of the Alluvial-fan Sequence .••.••..•.••.••.•.•. 10 STOP 2. NEW HAVEN ARKOSE, NORTH HAVEN ••••••..•..•......•.•..••.• 14 Location .................................................... 14 Objectives of Stop 2 ••••••••• ·-· ••••••••••.•••••••• , ••• , ••••• 14 Sedimentation on the Braided-river Alluvial Plain .••.•••••.. 17 Caliche Paleosol Profiles •••••.•••.•••••.•..••.••..•.•...••• 23 ) Description of the Caliche. • • • • • • • . • • • • • . • • • • • . • . • • • 23 j Soil Processes and Paleoclimate ••••..•.••.•••••.•..••.• 28 Broad Terrane Hypothesis .••.••.•.••.• , ••.••.••.••....•. , . • . • 32 Introduction ....... ,, ............... , ................... 32 J Modified Concept. • . • • . • • . • • . • . • • • • . • . • • . • • . • • . • . • . • 32 Isolated Basin Hypothesis ••••••.••••.•••••••..•••..•••• 37 J Pomperaug Outlier •• , • • . • • . • • • . • • • • • • • . • • • • • . • • . • • . • • . 39 J Regional Maps of Hartford Basin-Pomperaug Outlier •.••.. 39 J vi Page STOP 3. TALCOTT BASALT, MERIDEN. • • • • • • • • • • • . • • • • • . • • • • • • • • • • • • • • 4 7 Location ......... ................ , . 4 7 Objectives of Stop 3........................................ 47 Description of the Talcott Basalt at Stop 3 ••••••••••••..•.• 50 Paleogeography............. • • • • • • . • • • . • . • • • • • • • • . • • • • . • • 50 STOP 4. EAST PEAK OF THE HANGING HILLS OF MERIDEN ..••.••••••.••• 54 Location.................................................... 54 Objective of Stop 4......................................... 54 Geology Seen from the Stone Tower •...•••••.•.••••••.••.•..•• 54 STOP 5. NEW- HAVEN ARKO SE, MERIDEN............................... 59 Location.................................................... 59 Objectives of Stop 5...................... •. • • • • .. • . • • • . • • . 59 Descrip.tion of Stop 5....................................... 59 Interpretation of the River-channel Sandstones .•••••...••••• 63 STOP 6. SHUTTLE MEADOW FORMATION, PLAINVILLE •.••.••.•••.•.•••••. 65 Location... • • . • . • • . • . • • • • • . • • . • • • . • • • • • • • • • • • • • • • • . • • • • • 65 Objectives of Stop 6....... • • • . • • • • • • • • . • • . • • • • • • • • • • • • . • . • • 65 Evidence for Lacustrine Redbeds............................. 66 P aleos lopes ................. , . • • • • • . • .. • . • . • • .. • . .. • • • • . • • 70 Paleocurrents ••.••••••..•.••• , .••...••.•• , . • • • . • • . • • • • • • • . • . 72 Enigmatic Inclined Surfaces and Elongate Scour ••••••••.••.•• 73 Description of Inclined Surfaces .••••••••.•••••.•••.••• 73 Description of Elongate Scour ••..••••••.••••••.••.••••• 75 In terpre ta tion . ............•.................. ~ . 75 Limestone................................................... 76 '.,, ' ' vii 1 STOP 7. EAST BERLIN FORMATION, CROMWELL. • • • • • • . • . • • • • • • . • • • • • • • 77 Location........... 77 Introduction.............. 77 Lacustrine Black Shale, Gray Mudstone, 'll and Gray Sands tone. • . • • • • • • • • . • . • • • . • • • • • • • • • • • . • • . • • . • • • • . 79 ' l Symmetrical Lacustrine Cycles.......................... 79 P aleos lopes . 85 P aleocurrents. • • • • • • . • • • • • • • • • . • • • . • • • • • . • • • . • • • • . • • • . 85 Origin of Laminated Dolomite-Black Shale or Gray Mudstone Couplets ••.•••••.••.••....••••. 89 Size and Depth of the Perennial Lakes •••.••.•••.•.••••. 96 Burial Diagenesis. 99 Lacus trine Redbeds. • • • • . • . • • • • . • . • • • • • • • • • • • . • • • • • . • . • . • • • • 99 River-channel Sandstone ..................................... 102 Floodplain Red Muds tone .•.•••••••••••••.••.••.••••••••..•••. 104 Origin of the Color of the Redbeds •••••.••.•••••.•••••.••••. 104 In troduc tion. 104 J Colors in the East Berlin Formation •••••••••••••••••••• 107 J Genesis of Hematite Pigment ••.••••••••.••••••••.••••••• 107 REFERENCES CITED. • • • • • • • . • • • • • . • • • • • • . • • • • • • • • • . • • • • • • • • • . • . • • • • 110 J ROAD LOG •••••.•.•••••••••••.••.••••••••.•.••.••••.•••••.•••••••.• 123 'J J . I '' ,J viii LIST OF FIGURES Figure 1. Geologic map with location of field trip stops.................. 2 2. Map of basins of the Newark Supergroup.......................... 4 3. Stratigraphy of the Newark, Hartford, and Deerfield Basins and the Pomperaug Outlier.. • • . • • • • • • • . • . • • . • . • . • . • 6 4. Measured section of alluvial-fan facies of Portland Arkose, Durham........................................ 11 5. Measured section of New Haven Arkose, North. Haven............... 15 6. Braided-river sandstone and floodplain red mudstone in New Haven Arkose, North Haven............................... 16 7. Close-up of braid-bar complex in Figure 6.. • . • • . • • . • . • • • . • . • • . 16 8. Sketch of braid-bar complex in New Haven Arkose, North Haven •.•• 18 9. Thickness of cross-bed sets in New Haven Arkose ..••.••.•..•.••.• 19 10. Sketch of braided river with longitudinal bars ..••.••••.•.••••.. 21 11. Field and microscopic features of caliche in the New Haven Arkose........................................ 24 12. Caliche profile in New Haven Arkose, North Haven •••.•.•.•.••.•.. 26 13. Caliche profile in New Haven Arkose, North Haven •...•.•..•.•.••• 26 14. Measured section of New Haven Arkose along I-84, Southington •••• 27 15. Late Triassic paleoclimatic zones in Gondwanaland and Laurasia ...••.•..••.•••••...••...••...••.•.• ; . • . • • • • . • . • • • • 31 16. Newark and Hartford
Recommended publications
  • The Moenave Formation: Sedimentologic and Stratigraphic Context of the Triassic–Jurassic Boundary in the Four Corners Area, Southwestern U.S.A
    Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 111–125 www.elsevier.com/locate/palaeo The Moenave Formation: Sedimentologic and stratigraphic context of the Triassic–Jurassic boundary in the Four Corners area, southwestern U.S.A. ⁎ Lawrence H. Tanner a, , Spencer G. Lucas b a Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA b New Mexico Museum of Natural History, 1801 Mountain Road, N.W., Albuquerque, NM 87104, USA Received 20 February 2005; accepted 20 June 2006 Abstract The Moenave Formation was deposited during latest Triassic to earliest Jurassic time in a mosaic of fluvial, lacustrine, and eolian subenvironments. Ephemeral streams that flowed north-northwest (relative to modern geographic position) deposited single- and multi-storeyed trough cross-bedded sands on an open floodplain. Sheet flow deposited mainly silt across broad interchannel flats. Perennial lakes, in which mud, silt and carbonate were deposited, formed on the terminal floodplain; these deposits experienced episodic desiccation. Winds that blew dominantly east to south-southeast formed migrating dunes and sand sheets that were covered by low-amplitude ripples. The facies distribution varies greatly across the outcrop belt. The lacustrine facies of the terminal floodplain are limited to the northern part of the study area. In a southward direction along the outcrop belt (along the Echo Cliffs and Ward Terrace in Arizona), dominantly fluvial–lacustrine and subordinate eolian facies grade mainly to eolian dune and interdune facies. This transition records the encroachment of the Wingate erg. Moenave outcrops expose a north–south lithofacies gradient from distal, (erg margin) to proximal (erg interior). The presence of ephemeral stream and lake deposits, abundant burrowing and vegetative activity, and the general lack of strongly developed aridisols or evaporites suggest a climate that was seasonally arid both before and during deposition of the Moenave and the laterally equivalent Wingate Sandstone.
    [Show full text]
  • Perennial Lakes As an Environmental Control on Theropod Movement in the Jurassic of the Hartford Basin
    geosciences Article Perennial Lakes as an Environmental Control on Theropod Movement in the Jurassic of the Hartford Basin Patrick R. Getty 1,*, Christopher Aucoin 2, Nathaniel Fox 3, Aaron Judge 4, Laurel Hardy 5 and Andrew M. Bush 1,6 1 Center for Integrative Geosciences, University of Connecticut, 354 Mansfield Road, U-1045, Storrs, CT 06269, USA 2 Department of Geology, University of Cincinnati, 500 Geology Physics Building, P.O. Box 210013, Cincinnati, OH 45221, USA; [email protected] 3 Environmental Systems Graduate Group, University of California, 5200 North Lake Road, Merced, CA 95340, USA; [email protected] 4 14 Carleton Street, South Hadley, MA 01075, USA; [email protected] 5 1476 Poquonock Avenue, Windsor, CT 06095, USA; [email protected] 6 Department of Evolutionary Biology, University of Connecticut, 75 North Eagleville Road, U-3403, Storrs, CT 06269, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-413-348-6288 Academic Editors: Neil Donald Lewis Clark and Jesús Martínez Frías Received: 2 February 2017; Accepted: 14 March 2017; Published: 18 March 2017 Abstract: Eubrontes giganteus is a common ichnospecies of large dinosaur track in the Early Jurassic rocks of the Hartford and Deerfield basins in Connecticut and Massachusetts, USA. It has been proposed that the trackmaker was gregarious based on parallel trackways at a site in Massachusetts known as Dinosaur Footprint Reservation (DFR). The gregariousness hypothesis is not without its problems, however, since parallelism can be caused by barriers that direct animal travel. We tested the gregariousness hypothesis by examining the orientations of trackways at five sites representing permanent and ephemeral lacustrine environments.
    [Show full text]
  • Eolian Dune Field of Late Triassic Age, Fundy Basin, Nova Scotia'
    Comment and Reply on 'Eolian dune field of Late Triassic age, Fundy Basin, Nova Scotia' COMMENT sands occur in the Wolfville Formation and are Late Triassic in age (Figs. 1A and 1B). Hubert and Mertz suggested a regional Paul E. Olsen, Peabody Museum, Yale University, New Haven, south-to-north trend of increasing aridity during the deposition Connecticut 06511 of the Upper Triassic part of the Newark Supergroup. I agree with their interpretation of the Red Head and Clark Head locali- Hubert and Mertz's (1980) description of newly discovered ties as eolian dune fields, but I suggest that the localities repre- eolian dune sands in the lower Mesozoic Fundy Group of Nova sent two horizons of different ages; Red Head is Late Triassic Scotia provides the first definitive evidence of true aridity in the but Clark Head is Early Jurassic. This stratigraphic revision is Newark Supergroup. According to Hubert and Mertz, the dune crucial to the climatic framework for the whole of the Newark 1 3-6 2 c 1 2 3 4 5 6 CLARK HEAD- OLD WIFE POINT- WASSONS BLUFF - RED HEAD - MCKAY HEAD BLUE SAC-McKAY HEAD LOWER ECONOMY CLARK HEAD BLUE SAC CAPE BLOMIDON- OLD WIFE POINT- E,, E,, / covered ' 01 E /- ------ E ,/ faulted , CARNIAN ,/ORDOVICIAN TO CARBONIFEROUS ROCKS TO CARBONIFEROUS 1 ROCKS Figure 1. Diagrams of relationships of North Mountain Basalt to McKay Head Basalt of Klein (1962) and Wolfville, Blomidon, and Scots Bay Forma- tions. Note that both position of Triassic-Jurassic boundary and stage boundaries are approximate; lowermost North Mountain Basalt could be latest Triassic age.
    [Show full text]
  • Early Ornithischian Dinosaurs: the Triassic Record
    Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: https://www.tandfonline.com/loi/ghbi20 Early ornithischian dinosaurs: the Triassic record Randall B. Irmis , William G. Parker , Sterling J. Nesbitt & Jun Liu To cite this article: Randall B. Irmis , William G. Parker , Sterling J. Nesbitt & Jun Liu (2007) Early ornithischian dinosaurs: the Triassic record, Historical Biology, 19:1, 3-22, DOI: 10.1080/08912960600719988 To link to this article: https://doi.org/10.1080/08912960600719988 Published online: 10 Oct 2011. Submit your article to this journal Article views: 291 View related articles Citing articles: 70 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Historical Biology, 2007; 19(1): 3–22 Early ornithischian dinosaurs: the Triassic record RANDALL B. IRMIS1, WILLIAM G. PARKER2, STERLING J. NESBITT3,4, & JUN LIU3,4 1Museum of Paleontology and Department of Integrative Biology, University of California, 1101 Valley Life Sciences Building, Berkeley, CA, 94720-4780, USA, 2Division of Resource Management, Petrified Forest National Park, P.O. Box 2217, Petrified Forest, AZ, 86028, USA, 3Lamont–Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY, 10964, USA, and 4Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, NY, 10024, USA Abstract Ornithischian dinosaurs are one of the most taxonomically diverse dinosaur clades during the Mesozoic, yet their origin and early diversification remain virtually unknown. In recent years, several new Triassic ornithischian taxa have been proposed, mostly based upon isolated teeth.
    [Show full text]
  • Dinosaur Diversification Linked with the Carnian Pluvial Episode
    ARTICLE DOI: 10.1038/s41467-018-03996-1 OPEN Dinosaur diversification linked with the Carnian Pluvial Episode Massimo Bernardi 1,2, Piero Gianolla 3, Fabio Massimo Petti 1,4, Paolo Mietto5 & Michael J. Benton 2 Dinosaurs diversified in two steps during the Triassic. They originated about 245 Ma, during the recovery from the Permian-Triassic mass extinction, and then remained insignificant until they exploded in diversity and ecological importance during the Late Triassic. Hitherto, this 1234567890():,; Late Triassic explosion was poorly constrained and poorly dated. Here we provide evidence that it followed the Carnian Pluvial Episode (CPE), dated to 234–232 Ma, a time when climates switched from arid to humid and back to arid again. Our evidence comes from a combined analysis of skeletal evidence and footprint occurrences, and especially from the exquisitely dated ichnofaunas of the Italian Dolomites. These provide evidence of tetrapod faunal compositions through the Carnian and Norian, and show that dinosaur footprints appear exactly at the time of the CPE. We argue then that dinosaurs diversified explosively in the mid Carnian, at a time of major climate and floral change and the extinction of key herbivores, which the dinosaurs opportunistically replaced. 1 MUSE—Museo delle Scienze, Corso del Lavoro e della Scienza 3, 38122 Trento, Italy. 2 School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK. 3 Dipartimento di Fisica e Scienze della Terra, Università di Ferrara, via Saragat 1, 44100 Ferrara, Italy. 4 PaleoFactory, Dipartimento di Scienze della Terra, Sapienza Università di Roma, Piazzale Aldo Moro, 5, 00185 Rome, Italy. 5 Dipartimento di Geoscienze, Universitàdegli studi di Padova, via Gradenigo 6, I-35131 Padova, Italy.
    [Show full text]
  • Improving Hydric Soil Identification in Areas Containing Problematic Red Parent Materials: a Nationwide Collaborative Mapping Approach
    Wetlands https://doi.org/10.1007/s13157-018-1114-6 APPLIED WETLAND SCIENCE Improving Hydric Soil Identification in Areas Containing Problematic Red Parent Materials: a Nationwide Collaborative Mapping Approach Sara C. Mack1 & Jacob F. Berkowitz2 & Martin C. Rabenhorst1 Received: 9 July 2018 /Accepted: 18 November 2018 # The Author(s) 2018 Abstract Hydric soil identification utilizes diagnostic morphologic features, including iron transformations, resulting from anaerobic condi- tions. However, soils derived from some red parent materials (RPM) fail to develop characteristic hydric soils morphologies, confounding hydric soil and wetland delineation. Laboratory and field methods addressing resistant RPM soils exist, but application remains limited by uncertainty regarding problematic RPM distribution. In response, a collaborative effort (>50 participants) docu- mented problematic RPM distribution across the contiguous United States. Specifically, >1100 samples from >450 locations underwent laboratory analysis using the Color Change Propensity Index to identify problematic RPM soils. Geospatial analysis linked verified problematic soils with associated geologic units and soil series, generating maps of RPM distribution. Potential problematic RPM was identified in the Northeast and Mid-Atlantic, Great Lakes, South-central, and Desert Southwest-Western Mountains (problematic RPM regions herein), encompassing diverse groups of soils and parent materials. Despite the observed variability in soil characteristics, results suggest that problematic RPM was consistently derived from sedimentary, hematite-rich red bed formations developed where deposition of terrestrial sediments occurred in near-shore, marginal-marine environments. Understanding problematic RPM soils distribution promotes the appropriate application of existing hydric soil field indicators, including F21 – Red Parent Material, thus improving approaches to hydric soil identification and wetland management. Keywords Hydric soil .
    [Show full text]
  • Stratigraphic and Temporal Context and Faunal Diversity of Permian-Jurassic Continental Tetrapod Assemblages from the Fundy Rift Basin, Eastern Canada
    Stratigraphic and temporal context and faunal diversity of Permian-Jurassic continental tetrapod assemblages from the Fundy rift basin, eastern Canada Hans-Dieter Sues1* and Paul E. Olsen2 1. Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, P.O. Box 37012, Washington, DC 20013-7012, U.S.A. 2. Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, New York 10964-1000, U.S.A. *Corresponding author: <[email protected]> Date received 30 July 2014 ¶ Date accepted 25 November 2014 ABSTRacT The Fundy basin in Nova Scotia and New Brunswick is the largest exposed rift basin of the Newark Supergroup and also extends beneath the Bay of Fundy. Its strata can be divided into four tectonostratigraphic sequences (TS). TS I is represented by the probably Permian Honeycomb Point Formation and possibly the Lepreau Formation. TS II includes the Wolfville Formation with the probably Middle Triassic Economy Member and the early Late Triassic Evangeline Member. These members have yielded markedly different assemblages of continental tetrapods. TS III comprises most of the Blomidon Formation, which is Norian to Rhaetian in age. The Blomidon Formation has yielded few skeletal remains of tetrapods to date but many tetrapod tracks. TS IV includes the late Rhaetian top of the Blomidon Formation and the McCoy Brook Formation, which overlies the North Mountain Basalt and is latest Rhaetian and earliest Jurassic (Hettangian) in age. The McCoy Brook Formation has yielded a diversity of continental tetrapods and lacks any of the characteristic Late Triassic forms. Recent work has correlated the Global Boundary Stratotype Section and Point (GSSP) for the base of the Jurassic (Hettangian) to a level above the North Mountain Basalt.
    [Show full text]
  • Guidebook for Fieutrips In• Eastern Connecticut Arul the Hartford &Si,N
    Guidebook for FieUtrips in• Eastern Connecticut arul the Hartford &si,n HOLYOKE HAMPDEN EASTERN HI HIANDS DIKE/SILL ME :AMORPHIC BASEMENT ROCKS STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CoNNECTICUT THE NATURAL REsouRCES CENTER DEPARTMENT OF ENVIRONMENTAL PROTECTION MARCH 19, 20, 21, AND 22, 1995 Guidebook Number 7 NoJITHFAST SECTION, GEOLOGIO\L SOCIEIY OF AMERICA 30rn .ANNuAL MEETING CROMWEIL, CoNNECTICUT MARCH 19, 20, 21AND22, 1995 Guidebook far Piek/trips in &tern Connecticut and the Hartford Basin Editor Nancy W. McHone State Geological and Natural History Survey of Connecticut Guidebook Number 7 1995 State Geological and Narural History Survey of Connectirut The Natural Resources Center Department of Environmental Protection Governor of Connecticut HONORABLE JOHN ROWLAND Commissioner of the Deparment of Environmental Protection SIDNEY J. HOLBROOK State Geologist Director, Natural Resources Center RICHARD HYDE For information on ordering this guidebook and other publications of the Connecticut Geological and Natural History Survey, consult the List of Publications available from the survey, Department of Environmental Protection, 79 Flm Street, Hartford, CT 06106-5127 Telephone (203) 424-3555 Editors Preface I It has been twenty-four years since the last Northeast Section of the Geological Society of America meeting in Connecticut. Since that time our understanding of the geological history of northeastern USA and southeastern Canada has greatly increased. The fieldtrips described in this guide incorporate, and add to, our understanding of that history. Trip A examines metamorphic rocks, using mineral cooling ages to constrain the boundaries of terranes and the timing of i terrane assembly. The sedimentary and basalt units of the Hartford Basin are the subjects of trips B and D.
    [Show full text]
  • AGS#24 Fieldtripa5 Keighley Brown.Pdf (10.47Mb)
    GAC-MAC-CSPG-CSSS Pre-conference Field Trips A1 Contamination in the South Mountain Batholith and Port Mouton Pluton, southern Nova Scotia HALIFAX Building Bridges—across science, through time, around2005 the world D. Barrie Clarke and Saskia Erdmann A2 Salt tectonics and sedimentation in western Cape Breton Island, Nova Scotia Ian Davison and Chris Jauer A3 Glaciation and landscapes of the Halifax region, Nova Scotia Ralph Stea and John Gosse A4 Structural geology and vein arrays of lode gold deposits, Meguma terrane, Nova Scotia Rick Horne A5 Facies heterogeneity in lacustrine basins: the transtensional Moncton Basin (Mississippian) and extensional Fundy Basin (Triassic-Jurassic), New Brunswick and Nova Scotia David Keighley and David E. Brown A6 Geological setting of intrusion-related gold mineralization in southwestern New Brunswick Kathleen Thorne, Malcolm McLeod, Les Fyffe, and David Lentz A7 The Triassic-Jurassic faunal and floral transition in the Fundy Basin, Nova Scotia Paul Olsen, Jessica Whiteside, and Tim Fedak Post-conference Field Trips B1 Accretion of peri-Gondwanan terranes, northern mainland Nova Scotia Field Trip A5 and southern New Brunswick Sandra Barr, Susan Johnson, Brendan Murphy, Georgia Pe-Piper, David Piper, and Chris White Facies heterogeneity in lacustrine basins: B2 The Joggins Cliffs of Nova Scotia: Lyell & Co's "Coal Age Galapagos" J.H. Calder, M.R. Gibling, and M.C. Rygel the transtensional Moncton Basin (Mississippian) B3 Geology and volcanology of the Jurassic North Mountain Basalt, southern Nova Scotia Dan Kontak, Jarda Dostal, and John Greenough and extensional Fundy Basin (Triassic-Jurassic), B4 Stratigraphic setting of base-metal deposits in the Bathurst Mining Camp, New Brunswick New Brunswick and Nova Scotia Steve McCutcheon, Jim Walker, Pierre Bernard, David Lentz, Warna Downey, and Sean McClenaghan B5 Geology and environmental geochemistry of lode gold deposits in Nova Scotia Paul Smith, Michael Parsons, and Terry Goodwin David Keighley and David E.
    [Show full text]
  • A Long-Necked Tanystropheid from the Middle Triassic Moenkopi Formation (Anisian) Provides Insights Into the Ecology and Biogeography of Tanystropheids
    Palaeontologia Electronica palaeo-electronica.org A long-necked tanystropheid from the Middle Triassic Moenkopi Formation (Anisian) provides insights into the ecology and biogeography of tanystropheids Kiersten K. Formoso, Sterling J. Nesbitt, Adam C. Pritchard, Michelle R. Stocker, and William G. Parker ABSTRACT Archosauromorphs are a diverse and successful group of reptiles that radiated into a series of groups around the time of the end-Permian extinction. One of these groups of archosauromorphs, tanystropheids, consists of diverse forms, and some of the largest members of the group possessed extremely elongated cervical vertebrae (greater than five times longer than tall), resulting in a hyperelongate neck. These derived tanystropheids have been found in Tethyan marine deposits of Pangaea. Four partial cervical vertebrae from a hyperelongate-necked tanystropheid from the Middle Triassic Moenkopi Formation of Arizona and New Mexico are described in this paper. These cervical vertebrae are assigned to Tanystropheidae, specifically the clade that includes the hyperelongate-necked Tanystropheus based on character states, which include an elongate centrum (length to height ratio of 6.2), the presence of epipophy- ses, and an elongate axial centrum. The Moenkopi tanystropheid elements were found in lower latitude fluvial sequences without any marine influence, corresponding to western Pangaea, whereas Tanystropheus-like tanystropheids are typically associated with marginal marine environments in middle to high latitudes of eastern Pangaea. These fossils suggest that hyperelongate-necked, Tanystropheus-like tanystropheids were perhaps behaviorally bound to general semi-aquatic environments, both marine and freshwater, due to their unique morphology. These fossils also greatly extend the biogeographic range of large tanystropheids and increase the anatomical diversity of tanystropheids known from North America demonstrating that the clade persisted in a wide variety of environments throughout the Triassic Period.
    [Show full text]
  • Donald Baird and His Discoveries of Carboniferous and Early Mesozoic Vertebrates in Nova Scotia
    Donald Baird and his discoveries of Carboniferous and early Mesozoic vertebrates in Nova Scotia Hans-Dieter Sues1*, Robert W. Hook2, and Paul E. Olsen3 1. Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, MRC 121, P.O. Box 37012, Washington, DC 20013-7012, USA 2. Vertebrate Paleontology Laboratory, The University of Texas at Austin, Austin, Texas 78758, USA 3. Lamont-Doherty Earth Observatory of Columbia University, 61 Rt. 9W, Palisades, New York 10964-1000, USA *Corresponding author <[email protected]> Date received: 23 March 2013 ¶ Date accepted 08 April 2013 ABSTRacT Donald Baird (1926–2011), an influential and innovative vertebrate paleontologist with a scientific career spanning nearly 50 years, had an exceptional breadth of expertise in the study of late Paleozoic and Mesozoic vertebrates and their life traces. Beginning in 1956, Baird conducted fieldwork in the Carboniferous and Triassic-Jurassic of Nova Scotia, making a total of 21 trips in 30 years. His many scientific contributions include the discoveries of important assemblages of Carboniferous vertebrates as well as an unexpectedly diverse record of early Mesozoic tetrapods and their trackways in the province. Baird also encouraged and supported fieldwork by other vertebrate paleontologists as well as amateurs in Nova Scotia and elsewhere. His career-long commitment to the vertebrate paleontology of the province was instrumental in establishing it as an important source of fossils of Carboniferous and early Mesozoic continental vertebrates. RÉSUMÉ Donald Baird (1926–2011), paléontologiste des vertébrés influent et novateur dont la carrière scientifique s’est échelonnée sur près de 50 ans, a acquis un savoir-faire exceptionnel dans l’étude des vertébrés du Paléozoïque tardif et du Mésozoïque et des vestiges de leur vie.
    [Show full text]
  • Acadian Orogeny, 289-292, 311-315, 433- 439
    Index Acadian orogeny, 289-292, 311-315, 433- Cambrian Coal, 43-45, 412-413 439 Inwood Marble, 138 Coal seams, 31-32 magmatism, 293-300 Lower Coastal geology, 213-220 Adirondack-Champlain Valley boundary, Adeyton Group, 467-471 Coastlines, 213-220 151-154 Bomoseen Formation, 142 See also Shorelines Age Brigus Formation, 467-471 Columnar structures, 417 dates, 10, 16, 26 Browns Pond Formation, 233-237 Conglomerate, 311-315 Albee Formation, allochthon, 250-255 Dunham Dolomite, 229-232 Connecticut Alleghany orogeny, 55-58, 113-118, 187- East Passage Formation, 196-197 eastern, Willimantic fault, 169–173 190, 191-194 Lowerre Quartzite, 138 Farmington River gorge, Tariffville, 165- Allochthons, 66-69, 451-456 Middle Granville Slate, 233-237 168 Anchizone alteration, 62 Pirate Cave Formation, 195-196 northern, Hartford basin, 165–168 Annieopsquotch Complex, 441-444 Middle southeastern Antigonish Terrane, 421-426 Chamberlain’s Brook Formation, 467- Glacial Park, 175-180 Appalachian Basin, 113-118 471 Ledyard recessional moraine, 175-180 Appalachians Dutch Island Harbor Formation, 199 West Torrington 7½-minute Quadrangle, Birmingham window, 37-41 Fort Burnside Formation, 198-199 Cameron’s Line, 159-164 Canada, 363-368 Jamestown Formation, 197-198 Craig Harbor faultline scarp, 151-154 Piedmont, 77-80 Manuels River Formation, 467-471 Cretaceus Valley and Ridge province, 1-3, 5-8, Monkton Quartzite, 230-232 Magothy Formation, 88 37-41, 47-50, 55-58 West Castleton Formation, 233-237 Merchantville Formation, 88 Archean, komatiite, 317-322 Winooski
    [Show full text]