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Facies Architecture and Stratigraphy of the Paleogene Huntingdon Formation at Abbotsford, British Columbia
Facies Architecture and Stratigraphy of the Paleogene Huntingdon Formation at Abbotsford, British Columbia Brett Hohs Tallentire Gilley B.Sc., Simon Fraser University, 1999 A THESIS SUBMInED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE In the DEPARTMENT OF EARTH SCIENCES O Brett Hollis Tallentire Gilley, 2003 SIMON FRASER UNIVERSITY December, 2003 All rights reserved. This work may not be reproduced in whole or part, by photocopy or other means, without the permission of the author. APPROVAL Name: Brett Hollis Tallentire Gilley Degree: Master of Science Title of Thesis: Facies Architecture and Stratigraphy of the Paleogene Huntingdon Formation at Abbotsford, British Columbia Examining Committee: Chair: Dr. Glyn Williams-Jones Assistant Professor Dr. Peter Mustard Senior Supervisor Associate Professor Dr. ames MacEachern SupJ rvisory Associate Profess - Fvpf.Michael ~ilhn Ex rnal Examiner Doua4 as Colleae. De~t.of Geolosv & Anthropology Date Approved: ne 4 , 2 csz aw PARTIAL COPYRIGHT LICENCE I hereby grant to Simon Fraser University the right to lend my thesis, project or extended essay (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this work for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this work for financial gain shall not be allowed without my written permission. -
1 Paleobotanical Proxies for Early Eocene Climates and Ecosystems in Northern North 2 America from Mid to High Latitudes 3 4 Christopher K
https://doi.org/10.5194/cp-2020-32 Preprint. Discussion started: 24 March 2020 c Author(s) 2020. CC BY 4.0 License. 1 Paleobotanical proxies for early Eocene climates and ecosystems in northern North 2 America from mid to high latitudes 3 4 Christopher K. West1, David R. Greenwood2, Tammo Reichgelt3, Alexander J. Lowe4, Janelle M. 5 Vachon2, and James F. Basinger1. 6 1 Dept. of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, 7 Saskatchewan, S7N 5E2, Canada. 8 2 Dept. of Biology, Brandon University, 270-18th Street, Brandon, Manitoba R7A 6A9, Canada. 9 3 Department of Geosciences, University of Connecticut, Beach Hall, 354 Mansfield Rd #207, 10 Storrs, CT 06269, U.S.A. 11 4 Dept. of Biology, University of Washington, Seattle, WA 98195-1800, U.S.A. 12 13 Correspondence to: C.K West ([email protected]) 14 15 Abstract. Early Eocene climates were globally warm, with ice-free conditions at both poles. Early 16 Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate biota, 17 but also with abundant thermophilic elements such as crocodilians, and mesothermic taxodioid 18 conifers and angiosperms. The globally warm early Eocene was punctuated by geologically brief 19 hyperthermals such as the Paleocene-Eocene Thermal Maximum (PETM), culminating in the 20 Early Eocene Climatic Optimum (EECO), during which the range of thermophilic plants such as 21 palms extended into the Arctic. Climate models have struggled to reproduce early Eocene Arctic 22 warm winters and high precipitation, with models invoking a variety of mechanisms, from 23 atmospheric CO2 levels that are unsupported by proxy evidence, to the role of an enhanced 24 hydrological cycle to reproduce winters that experienced no direct solar energy input yet remained 25 wet and above freezing. -
Amelanchierspp. Family: Rosaceae Serviceberry
Amelanchier spp. Family: Rosaceae Serviceberry The genus Amelanchier contains about 16 species native to North America [5], Mexico [2], and Eurasia to northern Africa [4]. The word amelanchier is derived from the French common name amelanche of the European serviceberry, Amelanchier ovalis. Amelanchier alnifolia-juneberry, Pacific serviceberry, pigeonberry, rocky mountain servicetree, sarvice, sarviceberry, saskatoon, saskatoon serviceberry, western service, western serviceberry , western shadbush Amelanchier arborea-Allegheny serviceberry, apple shadbush, downy serviceberry , northern smooth shadbush, shadblow, shadblown serviceberry, shadbush, shadbush serviceberry Amelanchier bartramiana-Bartram serviceberry Amelanchier canadensis-American lancewood, currant-tree, downy serviceberry, Indian cherry, Indian pear, Indian wild pear, juice plum, juneberry, may cherry, sugar plum, sarvice, servicetree, shadberry, shadblow, shadbush, shadbush serviceberry, shadflower, thicket serviceberry Amelanchier florida-Pacific serviceberry Amelanchier interior-inland serviceberry Amelanchier sanguinea-Huron serviceberry, roundleaf juneberry, roundleaf serviceberry , shore shadbush Amelanchier utahensis-Utah serviceberry Distribution In North America throughout upper elevations and temperate forests. The Tree Serviceberry is a shrub or tree that reaches a height of 40 ft (12 m) and a diameter of 2 ft (0.6 m). It grows in many soil types and occurs from swamps to mountainous hillsides. It flowers in early spring, producing delicate white flowers, making -
Outline of Angiosperm Phylogeny
Outline of angiosperm phylogeny: orders, families, and representative genera with emphasis on Oregon native plants Priscilla Spears December 2013 The following listing gives an introduction to the phylogenetic classification of the flowering plants that has emerged in recent decades, and which is based on nucleic acid sequences as well as morphological and developmental data. This listing emphasizes temperate families of the Northern Hemisphere and is meant as an overview with examples of Oregon native plants. It includes many exotic genera that are grown in Oregon as ornamentals plus other plants of interest worldwide. The genera that are Oregon natives are printed in a blue font. Genera that are exotics are shown in black, however genera in blue may also contain non-native species. Names separated by a slash are alternatives or else the nomenclature is in flux. When several genera have the same common name, the names are separated by commas. The order of the family names is from the linear listing of families in the APG III report. For further information, see the references on the last page. Basal Angiosperms (ANITA grade) Amborellales Amborellaceae, sole family, the earliest branch of flowering plants, a shrub native to New Caledonia – Amborella Nymphaeales Hydatellaceae – aquatics from Australasia, previously classified as a grass Cabombaceae (water shield – Brasenia, fanwort – Cabomba) Nymphaeaceae (water lilies – Nymphaea; pond lilies – Nuphar) Austrobaileyales Schisandraceae (wild sarsaparilla, star vine – Schisandra; Japanese -
Paleontological Resources at Grand Teton National Park, Northwestern Wyoming Vincent L
University of Wyoming National Park Service Research Center Annual Report Volume 22 22nd Annual Report, 1998 Article 7 1-1-1998 Paleontological Resources at Grand Teton National Park, Northwestern Wyoming Vincent L. Santucci National Park Service William P. Wall Georgia College and State University Follow this and additional works at: http://repository.uwyo.edu/uwnpsrc_reports Recommended Citation Santucci, Vincent L. and Wall, William P. (1998) "Paleontological Resources at Grand Teton National Park, Northwestern Wyoming," University of Wyoming National Park Service Research Center Annual Report: Vol. 22 , Article 7. Available at: http://repository.uwyo.edu/uwnpsrc_reports/vol22/iss1/7 This Grand Teton National Park Report is brought to you for free and open access by Wyoming Scholars Repository. It has been accepted for inclusion in University of Wyoming National Park Service Research Center Annual Report by an authorized editor of Wyoming Scholars Repository. For more information, please contact [email protected]. Santucci and Wall: Paleontological Resources at Grand Teton National Park, Northwest PALEONTOLOGICAL RESOURCES AT GRAND TETON NATIONAL PARK, NORTHWESTERN WYOMING + VINCENT L. SANTUCCI+ NATIONAL PARK SERVICE KEMMERER + WY WILLIAM P. WALL+ DEPARTMENT OF BIOLOGY GEORGIA COLLEGE AND STATE UNIVERSITY MILLEDGEVILLE + GA + ABSTRACT landscape, and though the last great ice masses melted 15 ,000 years ago, some re-established small Paleontological resources occur throughout glaciers still exist. the formations exposed in Grand Teton National Park. A comprehensive paleontological survey has This report provides a preliminary not been attempted previously at Grand Teton assessment of paleontological resources identified at National Park. Preliminary paleontologic resource Grand Teton National Park. data is given in this report in order to establish baseline data. -
Amelanchier Canadensis
AmelanchierAmelanchier canadensiscanadensis ShadblowShadblow serviceberry,serviceberry, CanadianCanadian serviceberry,serviceberry, DownyDowny serviceberry,serviceberry, Shadbush,Shadbush, Juneberry,Juneberry, ChuckleberryChuckleberry Amelanchier canadensis(Shadblow serviceberry) is native to South Canada and the eastern United States. The shrub was introduced in Europe in 1746. The Shadblow serviceberry grows up to 5 to 6 metres tall and wide with a finely branched, wide vase-shaped crown. Before the leaves start to sprout, the Amelanchier canadensisblooms bountifully racemes of white flowers that hang over slightly. In late July, it bears red-violet to blue-black fruits that are edible. The leaves are relatively large and bud in a lovely bronze-red. In the summer, the Shadblow serviceberry has green leaves with a grey-green underside. The autumn colours are yellow-orange to brown and less striking than those of other serviceberry shrubs. The species has a preference for sunlight and moist, humous, slightly acidic soil. It will tolerate a temporarily dry environment, as well as strong wind. That makes Amelanchier canadensis very suitable for use in containers and roof gardens. SEASONAL COLOURS jan feb mar apr mei jun jul aug sep okt nov dec TYPES OF PLANTING Tree types: fruit trees, solitary shrubs | Topiary on stem: multi-stem umbrella USE Location: park, central reservation, in containers, roof garden, large garden, small garden, patio, cemetery, countryside, ecological zone | Pavement: none, open | Planting concepts: Eco planting, -
Plant Collecting Expedition for Berry Crop Species Through Southeastern
Plant Collecting Expedition for Berry Crop Species through Southeastern and Midwestern United States June and July 2007 Glassy Mountain, South Carolina Participants: Kim E. Hummer, Research Leader, Curator, USDA ARS NCGR 33447 Peoria Road, Corvallis, Oregon 97333-2521 phone 541.738.4201 [email protected] Chad E. Finn, Research Geneticist, USDA ARS HCRL, 3420 NW Orchard Ave., Corvallis, Oregon 97330 phone 541.738.4037 [email protected] Michael Dossett Graduate Student, Oregon State University, Department of Horticulture, Corvallis, OR 97330 phone 541.738.4038 [email protected] Plant Collecting Expedition for Berry Crops through the Southeastern and Midwestern United States, June and July 2007 Table of Contents Table of Contents.................................................................................................................... 2 Acknowledgements:................................................................................................................ 3 Executive Summary................................................................................................................ 4 Part I – Southeastern United States ...................................................................................... 5 Summary.............................................................................................................................. 5 Travelog May-June 2007.................................................................................................... 6 Conclusions for part 1 ..................................................................................................... -
Origin and Beyond
EVOLUTION ORIGIN ANDBEYOND Gould, who alerted him to the fact the Galapagos finches ORIGIN AND BEYOND were distinct but closely related species. Darwin investigated ALFRED RUSSEL WALLACE (1823–1913) the breeding and artificial selection of domesticated animals, and learned about species, time, and the fossil record from despite the inspiration and wealth of data he had gathered during his years aboard the Alfred Russel Wallace was a school teacher and naturalist who gave up teaching the anatomist Richard Owen, who had worked on many of to earn his living as a professional collector of exotic plants and animals from beagle, darwin took many years to formulate his theory and ready it for publication – Darwin’s vertebrate specimens and, in 1842, had “invented” the tropics. He collected extensively in South America, and from 1854 in the so long, in fact, that he was almost beaten to publication. nevertheless, when it dinosaurs as a separate category of reptiles. islands of the Malay archipelago. From these experiences, Wallace realized By 1842, Darwin’s evolutionary ideas were sufficiently emerged, darwin’s work had a profound effect. that species exist in variant advanced for him to produce a 35-page sketch and, by forms and that changes in 1844, a 250-page synthesis, a copy of which he sent in 1847 the environment could lead During a long life, Charles After his five-year round the world voyage, Darwin arrived Darwin saw himself largely as a geologist, and published to the botanist, Joseph Dalton Hooker. This trusted friend to the loss of any ill-adapted Darwin wrote numerous back at the family home in Shrewsbury on 5 October 1836. -
HYDRANGEA CARE Hydrangeas Can Be Confusing When It Comes to Requirements and Especially Pruning
HYDRANGEA CARE Hydrangeas can be confusing when it comes to requirements and especially pruning. We’ve broken down the hydrangeas we carry into three basic groups to easily explain the differences. HYDRANGEA ARBORESCENS (SMOOTH HYDRANGEA) Smooth hydrangeas are some of the easiest to grow and lowest maintenance hydrangeas. They are known for their large flower heads, sturdy stems, and great cut flowers. They almost always bloom on new wood which means they should be pruned in late fall. Smooth hydrangeas can be cut back 6-8” from the ground in late fall if desired. Includes: Annabelle & Invincible Spirit II (and others) HYDRANGEA MACROPHYLLA (BIGLEAF HYDRANGEA) Bigleaf or “ever-blooming” hydrangeas are desired for their deep green leaves, numerous blooms, and easy care. Bigleaf hydrangeas bloom on both new and old wood, but most of their summer blooms occur on wood formed the previous summer. To encourage new blooms throughout the summer, remove spent blooms as soon as they’re done flowering. The sooner this is done, the longer the plant will be allowed to recover and set new buds for the next season. This will encourage larger and more numerous blooms. Bigleaf hydrangeas prefer a location where they receive morning sun (about 4 hours) but are shaded from the afternoon sun. If they are planted in an area with total shade, it is not likely that they will bloom. Includes: Endless Summer, Blushing Bride, Seaside Cape Cod, Grateful Red, & Bloomstruck (and others) HYDRANGEA PANICULATA (GRANDIFLORA HYDRANGEA) Grandiflora hydrangeas are some of the most commonly planted hydrangeas in this area. They are tolerant of numerous conditions and are easy to grow. -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. XVIII, NO. 13, pp. 205-227 (6 pls.) OCTOBER11, 1963 t i THE FERN GENUS ACROSTICHUM IN THE EOCENE CLARNO FORMATION OF OREGON BY CHESTER A. ARNOLD and LYMAN H. DAUGHERTY FROM THE EDWARD PULTENEY WRIGHT MEMORIAL VOLUME Publication of this paper is made possible by the Federal-Mogul-Bower Bearings, Inc. Paleontology Research Fund MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: LEWISB. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence v should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan. VOLS. 11-XVII. Parts of volumes may be obtained if available. VOLUMEXVIII 1. Morphology and Taxonomy of the Cystoid Cheirocrinus anatiformis (Hall), by Robert V. Kesling. Pages 1-21, with 4 plates. 2. Ordovician Streptelasmid Rugose Corals from Michigan, by Erwin C. Sturnm. Pages 23-31, with 2 plates. 3. Paraconularia newberryi (Winchell) and other Lower Mississippian Conulariids from Michigan, Ohio, Indiana, and Iowa, by Egbert G. Driscoll. Pages 33-46, with 3 plates. 4. Two New Genera of Stricklandid Brachiopods, by A. J. Boucot and G. M. Ehlers. Pages 47-66, with 5 plates. -
Geology and Tectonic Setting of the Kamloops Group, South
GEOLOGY AND TECTONIC SETTING OF THE KAMLOOPS GROUP, SOUTH- CENTRAL BRITISH COLUMBIA by THOMAS EDWARD EWING B.A., The Colorado College, 1975 M.S., New Mexico Institute of Mining and Technology, 1977 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES Department of Geological Sciences We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA February 1981 © Thomas Edward Ewing, 1981 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of r.pnlnpiVal Sri PTirp.S The University of British Columbia 2075 Wesbrook Place Vancouver, Canada V6T 1W5 Date February 17, 1981 ABSTRACT The Kamloops Group is a widespread assemblage of Eocene volcanic and sedimentary rocks in south-central British Columbia. Detailed mapping of the type area near Kamloops has resulted in its subdivision into two formations and thirteen formal and informal members. The Tranquille Formation, 0-450 metres thick, consists of lacustrine sediments which grade upward into pillowed flows, hyaloclastite breccia and aquagene tuff. The overlying Dewdrop Flats Formation, with nine members, consists of up to 1000 metres of basalt to andesite phreatic breccia, flow breccia and flat-lying flows. -
A Review of Vertebrate Track-Bearing Formations
5 Lockley, M.G. & Lucas, S.G., eds., 2014, Fossil footprints of western North America: NMMNHS Bulletin 62 A REVIEW OF VERTEBRATE TRACK-BEARING FORMATIONS FROM THE MESOZOIC AND EARLIEST CENOZOIC OF WESTERN CANADA WITH A DESCRIPTION OF A NEW THEROPOD ICHNOSPECIES AND REASSIGNMENT OF AN AVIAN ICHNOGENUS RICHARD T. MCCREA1, LISA G. BUCKLEY1, A. GUY PLINT2, PHILIP J. CURRIE3, JAMES W. HAGGART4, CHARLES W. HELM1 AND S. GEORGE PEMBERTON5 1Peace Region Palaeontology Research Centre; Box 1540; Tumbler Ridge, British Columbia; V0C 2W0; CANADA; 2Department of Earth Sciences; University of Western Ontario; London, Ontario; N6A 5B7; CANADA; 3Department of Biological Sciences; University of Alberta, Edmonton, Alberta; T6G 2E9; CANADA; 4Geological Survey of Canada; 1500-605 Robson Street; Vancouver, British Columbia; V6B 5J3; CANADA; 5Department of Earth and Atmospheric Sciences; University of Alberta; Edmonton, Alberta; T6G 2E3; CANADA Abstract—The past quarter century has seen a marked increase in the recognition of fossil vertebrate tracksites in western Canada. Most of these finds were made in Alberta and British Columbia, but the Yukon Territory can lay claim to at least one tracksite and probably has the potential to yield more sites. The record of dinosaur tracks with skin impressions has increased dramatically, and is now represented by specimens of ankylosaurs, large ornithopods, small theropods and tyrannosauroids. Notable new finds include the first record of sauropods in Canada, evidence of herding behavior in ankylosaurs and the first pterosaur tracks in Canada. First discoveries of track specimens from several formations in western Canada include the Mountain Park Member of the Gates Formation in Alberta, and the Boulder Creek, Goodrich, Kaskapau, Cardium and Marshybank formations in northeastern British Columbia.