AGS#24 Fieldtripa5 Keighley Brown.Pdf (10.47Mb)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
ICMB-VIII Abstract Book
Program and Abstracts for the 8 th International Conference on Marine Bioinvasions (20-22 August 2013, Vancouver, Canada) Cover photography & design: Kimberley Seaward, NIWA Layout: Kimberley Seaward & Graeme Inglis, NIWA 8th International Conference on Marine Bioinvasions Vancouver 2013 8th International Conference on Marine Bioinvasions Dear Conference Participant On behalf of the Scientific Steering Committee (SSC) and our sponsors, we would like to welcome you to Vancouver for the 8th International Conference on Marine Bioinvasions. Vancouver is a culturally diverse metropolitan city serving as the western gateway to Canada. We hope you will spend some time to explore all this city has to offer. We are grateful for all of the efforts of the SSC and the local organizing committee as well as for the generous support of our sponsors: the Biodiversity Research Centre at the University of British Columbia for hosting the event; the Canadian Aquatic Invasive Species Network (CAISN), for providing additional funding by sponsoring one of the plenary presentations; The North Pacific Marine Science Organization (PICES), for providing travel awards to early career scientists; and the National Oceanographic and Atmospheric Administration (NOAA), for donating additional funds. Above all else, we are grateful for your participation and willingness to discuss your ideas, latest research results, and vision. Among the papers, posters, and plenary presentations that comprise the conference, we hope you will find many opportunities for discussion and -
Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna. -
Program and Abstracts
The Atlantic Geoscience Society (AGS) La Société Géoscientifique de l’Atlantique 45th Colloquium and Annual Meeting Special Sessions: • Special Session: In Memory of Dr. Trevor MacHattie (1974 - 2018) • Paleontology and Sedimentology in Atlantic Canada: In Memory of Dr. Ron Pickerill (1947 – 2018) • Current Research in Carboniferous Geology in the Atlantic Provinces • Minerals, metals, melts, and fluids associated with granitoid rocks: new insights from fundamental studies into the genesis, melt fertility, and ore-forming processes • Earth Science Outreach in the Maritime Provinces • Geohazards: Recent and Historical General Sessions: Current Research in the Atlantic Provinces February 7-9, 2019 Fredericton Inn, Fredericton, New Brunswick PROGRAM WITH ABSTRACTS We gratefully acknowledge sponsorship from the following companies and organizations: Department of Energy and Resource Development Geological Surveys Branch Department of Energy and Mines Department of Energy and Mines Geological Surveys Division Petroleum Resources Division Welcome to the 45th Colloquium and Annual Meeting of the Atlantic Geoscience Society in Fredericton, New Brunswick. This is a familiar place for AGS, having been a host several times over the years. We hope you will find something to interest you and generate discussion with old friends and new. AGS members are clearly pushing the boundaries of geoscience in all its branches! Be sure to take in the science on the posters and the displays from sponsors, and don’t miss the after-banquet jam and open mike on Saturday night. For social media types, please consider sharing updates on Facebook and Twitter (details in the program). We hope you will be able to use the weekend to renew old acquaintances, make new ones, and further the aims of your Atlantic Geoscience Society. -
A New Basal Sauropodomorph Dinosaur from the Lower Jurassic Navajo Sandstone of Southern Utah
A New Basal Sauropodomorph Dinosaur from the Lower Jurassic Navajo Sandstone of Southern Utah Joseph J. W. Sertich1*, Mark A. Loewen2 1 Department of Anatomical Sciences, Stony Brook University, Stony Brook, New York, United States of America, 2 Utah Museum of Natural History, Salt Lake City, Utah, United States of America Abstract Background: Basal sauropodomorphs, or ‘prosauropods,’ are a globally widespread paraphyletic assemblage of terrestrial herbivorous dinosaurs from the Late Triassic and Early Jurassic. In contrast to several other landmasses, the North American record of sauropodomorphs during this time interval remains sparse, limited to Early Jurassic occurrences of a single well- known taxon from eastern North America and several fragmentary specimens from western North America. Methodology/Principal Findings: On the basis of a partial skeleton, we describe here a new basal sauropodomorph dinosaur from the Lower Jurassic Navajo Sandstone of southern Utah, Seitaad ruessi gen. et sp. nov. The partially articulated skeleton of Seitaad was likely buried post-mortem in the base of a collapsed dune foreset. The new taxon is characterized by a plate-like medial process of the scapula, a prominent proximal expansion of the deltopectoral crest of the humerus, a strongly inclined distal articular surface of the radius, and a proximally and laterally hypertrophied proximal metacarpal I. Conclusions/Significance: Phylogenetic analysis recovers Seitaad as a derived basal sauropodomorph closely related to plateosaurid or massospondylid ‘prosauropods’ and its presence in western North America is not unexpected for a member of this highly cosmopolitan clade. This occurrence represents one of the most complete vertebrate body fossil specimens yet recovered from the Navajo Sandstone and one of the few basal sauropodomorph taxa currently known from North America. -
Selected Core from the Albert Formation (Mississippian), Moncton Basin, Southern New Brunswick
Selected Core from the Albert Formation (Mississippian), Moncton Basin, Southern New Brunswick Dave Keighley* University of New Brunswick, Fredericton, New Brunswick, Canada [email protected] and Clint St. Peter Hugh John Flemming Centre, Fredericton, New Brunswick, Canada Abstract Introduction The Moncton Basin is located in the southeastern part of New Brunswick (Fig. 1) and has a long history of petroleum activity. In the area ~25 km S of Moncton there has been mining of solid bitumen, Albertite, at Albert Mines (1850's); minor and intermittent production of oil/gas at Dover and Saint-Joseph (1859 to 1905); and oil and gas production at Stoney Creek (1911 to 1991 - gas was piped to the city for ~80 years). Stoney Creek gas is sweet, but wet, and the oil (total in place ~2.1 x 106 m3 with <5% recovered to date) is paraffinic with a pour point of over 7oC (45oF). Numerous appraisals of the oil shale in the area (e.g. Shell Albert Mines # 4 borehole) have also been undertaken periodically. In 2000, focus shifted 80 km west, where the McCully Gas Field (~1 TCF in place) was discovered, east of Sussex, by Corridor Resources Inc. and Potash Corporation of Saskatchewan (PCS). The A-67 discovery well (initial flow: 2.5 mcf p. day), and adjacent P-66 well currently produce gas for the PCS mill, but a link to the M&NE pipeline (Fig. 1) is planned to go into operation in late 2006. Approx. 17bcf (proven, ~120 bcf P2) remains in this production area (8% of the total joint venture area). -
Ecca Group) of South Africa: a Preliminary Review of Palaeoniscoid Fishes and Taphonomy
Records of the Western Australian Museum Supplement No. 57: 175-181 (1999). The Permian Whitehill Formation (Ecca Group) of South Africa: a preliminary review of palaeoniscoid fishes and taphonomy Fiona J. Evans 1 and Patrick A. Bender2 I Department of Zoology, University of Stellenbosch, Private Bag Xl, Matieland, 7602, South Africa; email: [email protected] 2 Museum of the Council for Geoscience, Private Bag Xl12, Pretoria, 0001, South Africa Abstract - The Permian (Artinskian) Whitehill Formation (Ecca Group) in South Africa and southern Namibia was deposited as part of a large stratified inland sea which extended from the southern margins of South Africa, and southern Namibia, northern Namibia (Aba-Huab Formation, Huab Basin) to the Iratl Formation of the Parana Basin in Brazil and parts of Uruguay. A common biota exists between these two continents, namely mesosaurid reptiles, pygocephalomorph crustacea, wood, palaeoniscoid fish and insects. The Whitehill Formation also contains plant stem fragments, palynomorphs, coprolites, a cephalochordate, rare sponge spicules and traces of arthropods and fish. The good preservation, particularly of the palaeoniscoid material, from the Whitehill Formation contrasts strongly with the disarticulated scales and spines from northern Namibia and Brazil. Recent collections in the Whitehill Formation near Calvinia and Louriesfontein (Northern Cape Province) of South Africa have demonstrated the necessity for a review of the palaeoniscoid taxa present in these units. Possible new species have also been collected, including a deep-bodied form. INTRODUCTION The extensive stratified inland sea in which the Whitehill Formation (Ecca Group, Karoo Supergroup; - - - - - Waterford Fm Figure 1) was deposited had limited or no access to ------------ the ocean according to reconstructions by Oelofsen Fort Brown Fm and Araujo (1987) and Pickford (1995). -
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. -
The Effects of Catchment Land Cover Change on Sedimentation in Back Lake, Merimbula, NSW.”
University of Wollongong Research Online Faculty of Science, Medicine & Health - Honours Theses University of Wollongong Thesis Collections 2013 “The Effects of Catchment Land Cover Change on Sedimentation in Back Lake, Merimbula, NSW.” Alison Borrell University of Wollongong Follow this and additional works at: https://ro.uow.edu.au/thsci University of Wollongong Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorise you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: This work is copyright. Apart from any use permitted under the Copyright Act 1968, no part of this work may be reproduced by any process, nor may any other exclusive right be exercised, without the permission of the author. Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. A court may impose penalties and award damages in relation to offences and infringements relating to copyright material. Higher penalties may apply, and higher damages may be awarded, for offences and infringements involving the conversion of material into digital or electronic form. Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong. Recommended Citation Borrell, Alison, “The Effects of Catchment Land Cover Change on Sedimentation in Back Lake, Merimbula, NSW.”, Bachelor of Environmental Science (Honours), School of Earth & Environmental Science, University of Wollongong, 2013. -
Internal Stratigraphy of the Jurassic North Mountain Basalt, Southern Nova Scotia
Report of Activities 2001 69 • Internal Stratigraphy of the Jurassic North Mountain Basalt, Southern Nova Scotia D. J. Kontak Introduction sediments are exposed, only 9 m of Scots Bay Formation remain as remnant inliers along the The Jurassic (201 Ma, Hodych and Dunning, 1992) Scots Bay coastline (De Wet and Hubert, 1989). North Mountain Basalt (NMB; also referred to as the North Mountain Fonnation) fonns a prominent The NMB outcrops along the Bay of Fundy in cuesta along the southern coastline of the Bay of southern mainland Nova Scotia and is Fundy. These continental, tholeiitic basalt flows exceptionally well exposed along the coastline and have played an important role in the geological inland along river valleys (Fig. 1). Topographic heritage of the province by: (l) hosting some ofthe relief of the area bounding the Bay of Fundy earliest mineral resources exploited (e.g. Cu, Fe), reflects the distribution of the underlying massive (2) contributing to the character of zeolite basalt flows. No more obvious is this than along mineralogy (e.g. type locality for mordenite; How, the Annapolis Valley area where the west side of 1864), (3) fonning part of the Fundy Rift Basin, an the valley is composed of massive, fresh basalt of important part of the Mesozoic evolution of eastern the lower flow unit of the NMB. The proximity of North America, and (4) filling an important niche the area on the north side of the Bay of Fundy to in the aggregate operations of the province. Despite the east-west Cobequid-Chedabucto Fault Zone has the importance of the NMB there has been resulted in structural modifications to the otherwise relatively little recent work devoted to defining and simple stratigraphy of the NMB. -
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. -
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. -
Stratigraphy, Sedimentary Facies and Diagenesis of the Ecca Group, Karoo Supergroup in the Eastern Cape, South Africa
STRATIGRAPHY, SEDIMENTARY FACIES AND DIAGENESIS OF THE ECCA GROUP, KAROO SUPERGROUP IN THE EASTERN CAPE, SOUTH AFRICA By Nonhlanhla Nyathi Dissertation submitted in fulfilment of the requirements for the degree of Master of Science In Geology FACULTY OF SCIENCE AND AGRICULTURE UNIVERSITY OF FORT HARE SUPERVISOR: PROFESSOR K. LIU CO-SUPERVISOR: PROFESSOR O. GWAVAVA APRIL 2014 DECLARATION I, Nonhlanhla Nyathi, hereby declare that the research described in this dissertation was carried out in the field and under the auspices of the Department of Geology, University of Fort Hare, under the supervision of Professor K. Liu and Prof. O. Gwavava. This dissertation and the accompanying photographs represent original work by the author, and have not been submitted, in whole or in part, to any other university for the purpose of a higher degree. Where reference has been made to the work of others, it has been dully acknowledged in the text. N. NYATHI Date signed: 12/04/2014 Place signed: Alice ACKNOWLEDGEMENTS The author is indebted to Professor K. Liu for his guidance, knowledge on all aspects of the project, constant supervision and help in doing field wok. Professor O. Gwavava is much appreciated for being my co-supervisor and helping me obtain financial support from the Goven Mbeki Research Development Centre. I am deeply grateful for the emotional support and encouragement from my parents and family. I express my profound gratitude to Mr Edwin Mutototwa and Mr Eric Madifor always taking time to read through my dissertation. The Rhodes University Geology laboratory technicians are thanked for their assistance in the making of thin sections.