A Revision of the Flora of the Latah Formation
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Pinus Sabiniana) in Oregon Frank Callahan PO Box 5531, Central Point, OR 97502
Discovering Gray Pine (Pinus sabiniana) in Oregon Frank Callahan PO Box 5531, Central Point, OR 97502 “Th e tree is remarkable for its airy, widespread tropical appearance, which suggest a region of palms rather than cool pine woods. Th e sunbeams sift through even the leafi est trees with scarcely any interruption, and the weary, heated traveler fi nds little protection in their shade.” –John Muir (1894) ntil fairly recently, gray pine was believed to be restricted to UCalifornia, where John Muir encountered it. But the fi rst report of it in Oregon dates back to 1831, when David Douglas wrote to the Linnaean Society of his rediscovery of Pinus sabiniana in California. In his letter from San Juan Bautista, Douglas claimed to have collected this pine in 1826 in Oregon while looking for sugar pine (Pinus lambertiana) between the Columbia and Umpqua rivers (Griffin 1962). Unfortunately, Douglas lost most of his fi eld notes and specimens when his canoe overturned in the Santiam River (Harvey 1947). Lacking notes and specimens, he was reluctant to report his original discovery of the new pine in Oregon until he found it again in California (Griffin 1962). Despite the delay in reporting it, Douglas clearly indicated that he had seen this pine before he found it in California, and the Umpqua region has suitable habitat for gray pine. John Strong Newberry1 (1857), naturalist on the 1855 Pacifi c Railroad Survey, described an Oregon distribution for Pinus sabiniana: “It was found by our party in the valleys of the coast ranges as far north as Fort Lane in Oregon.” Fort Lane was on the eastern fl ank of Blackwell Hill (between Central Point and Gold Hill in Jackson County), so his description may also include the Th e lone gray pine at Tolo, near the old Fort Lane site, displays the characteristic architecture of multiple Applegate Valley. -
Recommended Trees for Winnetka
RECOMMENDED TREES FOR WINNETKA SHADE TREES Common_Name Scientific_Name Ohio Buckeye Acer galbra Miyabe Maple Acer miyabei Black Maple Acer nigrum Norway Maple Acer plantanoides v. ___ Sugar Maple (many cultivars) Acer saccharum Shangtung Maple Acer truncatum Autumn Blaze or Marmo Maple Acer x freemanii Red Horsechestnut Aesculus x carnea 'Briotii' Horsechestnut Aesulus hippocastanum Alder Alnus glutinosa Yellowwood Caldrastis lutea Upright European Hornbeam Carpinus betulus “Fastigata” American Hornbeam Carpinus carolinians Hickory Carya ovata Catalpa Catalpa speciosa Hackberry Celtis occidentalis Katsuratree Cercidiphyllum japonicum Turkish Filbert Corylus colurna American Beech Fagus grandifolia Green Beech Fagus sylvatica European Beech Fagus sylvatica Ginkgo Ginkgo biloba Thornless Honeylocust Gleditsia triacanthos inermis Kentucky Coffeetree Gymnocladus dioica Goldenraintree Koelreuteria paniculata Sweetgum Liquidambar styraciflua Tulip Tree Liriodendron tulipfera Black gum, Tupelo Liriodendron tulipfera Hophornbeam Ostrya virginiana Corktree Phellodendron amurense Exclamation Plantree Plantanus x aceerifolia Quaking Aspen Populus tremuloides Swamp White Oak Quercus bicolor Shingle Oak Quercus imbricaria Bur Oak Quercus macrocarpa Chinkapin Oak Quercus muehlenbergii English Oak Quercus robur Red Oak Quercus rubra Schumard Oak Quercus shumardii Black Oak Quercus velutina May 2015 SHADE TREES Common_Name Scientific_Name Sassafras Sassafras albidum American Linden Tilia Americana Littleleaf Linden (many cultivars) Tilia cordata Silver -
Woodsia Obtusa
COSEWIC Assessment and Update Status Report on the blunt-lobed woodsia Woodsia obtusa in Canada THREATENED 2007 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the blunt-lobed woodsia Woodsia obtusa in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 17 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous report: COSEWIC 2000. COSEWIC assessment and status report on the blunt-lobed woodsia Woodsia obtusa in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-20 pp. Consaul, L.L. 1994. COSEWIC status report on the blunt-lobed woodsia Woodsia obtusa in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-20 pp. Production note: COSEWIC would like to acknowledge Matthew Wild for writing the status report on the blunt-lobed woodsia Woodsia obtusa in Canada, prepared under contract with Environment Canada, overseen and edited by Dr. Erich Haber, Co-chair, COSEWIC Plants and Lichens Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: 819-953-3215 Fax: 819-994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur la woodsie à lobes arrondis (Woodsia obtusa) au Canada – Mise à jour. -
Beyond the Fringe
Beyond the Fringe By Margaret Klein Wilson, Fairfax Master Gardener Intern The final flourish of native spring flowering trees belongs to fringe trees (Chionanthus virginicus). The measured parade of seasonal color — dogwoods and redbuds, flowering cherry and plum — is neatly capped by the fluttering grace of abundant white blossoms that engulf this small, often edge habitat tree beginning in mid-May. Encountering a fringe tree on a breezy spring day is to see masses of white corollas of petals casting their light perfume across the landscape. Is it any wonder Linnaeus named Yale ©2021 Copyright and noted this genus Chionanthus (chion = University snow; anthos = flower) as he compiled the photo: Genera Plantarum (1753)? Less poetically, fringe tree’s common names include Old Man’s Beard, Grancy graybeard, flowering ash and white fringe tree. Genus Chionanthus is a member of the Olive Family, the Olaceae, which includes 29 genera and over 600 species of trees and shrubs common in southeastern Asia and Australasia. Trees in this genus have uses both practical and ornamental: olive for food, ash for its lumber, and forsythia, gardenia and privets for sheer domestic beauty. In North America, ash trees in the genus Fraxinus, devilwood (Osmantus americanus) and Forestiera (swampprivet) are fringe tree’s near relatives. Only two species of fringe tree exist: C. virginicus in eastern North America and C. retusus, native to China. In his citation naming fringe tree the Virginia Native Plant Society 1997 Wildflower of the Year, C. F. Saachi explains this geographic disconnect: “This unusual biogeographic pattern, with different species within a genus … separated by several thousand miles, is a product of major geologic events including mountain building and the effects of glaciation. -
The Vascular Plants of Massachusetts
The Vascular Plants of Massachusetts: The Vascular Plants of Massachusetts: A County Checklist • First Revision Melissa Dow Cullina, Bryan Connolly, Bruce Sorrie and Paul Somers Somers Bruce Sorrie and Paul Connolly, Bryan Cullina, Melissa Dow Revision • First A County Checklist Plants of Massachusetts: Vascular The A County Checklist First Revision Melissa Dow Cullina, Bryan Connolly, Bruce Sorrie and Paul Somers Massachusetts Natural Heritage & Endangered Species Program Massachusetts Division of Fisheries and Wildlife Natural Heritage & Endangered Species Program The Natural Heritage & Endangered Species Program (NHESP), part of the Massachusetts Division of Fisheries and Wildlife, is one of the programs forming the Natural Heritage network. NHESP is responsible for the conservation and protection of hundreds of species that are not hunted, fished, trapped, or commercially harvested in the state. The Program's highest priority is protecting the 176 species of vertebrate and invertebrate animals and 259 species of native plants that are officially listed as Endangered, Threatened or of Special Concern in Massachusetts. Endangered species conservation in Massachusetts depends on you! A major source of funding for the protection of rare and endangered species comes from voluntary donations on state income tax forms. Contributions go to the Natural Heritage & Endangered Species Fund, which provides a portion of the operating budget for the Natural Heritage & Endangered Species Program. NHESP protects rare species through biological inventory, -
Kinematic Reconstruction of the Caribbean Region Since the Early Jurassic
Earth-Science Reviews 138 (2014) 102–136 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Kinematic reconstruction of the Caribbean region since the Early Jurassic Lydian M. Boschman a,⁎, Douwe J.J. van Hinsbergen a, Trond H. Torsvik b,c,d, Wim Spakman a,b, James L. Pindell e,f a Department of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands b Center for Earth Evolution and Dynamics (CEED), University of Oslo, Sem Sælands vei 24, NO-0316 Oslo, Norway c Center for Geodynamics, Geological Survey of Norway (NGU), Leiv Eirikssons vei 39, 7491 Trondheim, Norway d School of Geosciences, University of the Witwatersrand, WITS 2050 Johannesburg, South Africa e Tectonic Analysis Ltd., Chestnut House, Duncton, West Sussex, GU28 OLH, England, UK f School of Earth and Ocean Sciences, Cardiff University, Park Place, Cardiff CF10 3YE, UK article info abstract Article history: The Caribbean oceanic crust was formed west of the North and South American continents, probably from Late Received 4 December 2013 Jurassic through Early Cretaceous time. Its subsequent evolution has resulted from a complex tectonic history Accepted 9 August 2014 governed by the interplay of the North American, South American and (Paleo-)Pacific plates. During its entire Available online 23 August 2014 tectonic evolution, the Caribbean plate was largely surrounded by subduction and transform boundaries, and the oceanic crust has been overlain by the Caribbean Large Igneous Province (CLIP) since ~90 Ma. The consequent Keywords: absence of passive margins and measurable marine magnetic anomalies hampers a quantitative integration into GPlates Apparent Polar Wander Path the global circuit of plate motions. -
Delimiting Geologic Structures Affecting Water Movement of The
WRIA 54 Delimiting geologic structures affecting water movement and flow direction of the CRBG West Plains aquifer. DOE CONTRACT #11-1056 TECHNICAL MEMORANDUM TO ACCOMPANY THE STRUCTURAL GEOLOGY MAP OF THE WEST PLAINS REGION June 2012 Michael B. McCollum and Chad J. Pritchard Geology Department Eastern Washington University Cheney, Washington 99004-2439 I. INTRODUCTION The West Plains region is located just west of Spokane in Spokane and Lincoln Counties, Washington and is bounded to the north by the Spokane River, south by uplands and basalt scablands, east by Latah Creek and the Spokane Valley Aquifer, and to the west by loess covered hills and basalt lowlands. Increasing development and population growth in the eastern portion of the West Plains requires further understanding of the complex geohydrologic system. The complicated geologic history of eastern Washington and the West Plains spans billions of years and the rock types found in the region can be closely tied to the hydrology of the area. Geohydrology of the Spokane Area is strongly influenced by three major rock types 1) Pre- Neogene basement rock, 2) Miocene Columbia River Basalt Group (CRBG) and sedimentary interbeds (e.g. the Latah formation) that define the Columbia Plateau, and 3) Quaternary alluvium and glacial flood deposits that have molded the scablands of eastern Washington. This report begins with a brief overview of the regional geology and structural history of the mountainous areas adjacent to the West Plains region of the Columbia Plateau region, followed by a summary of our original scientific research on the pre-Neogene rocks and structures exposed in the isolated hills and ridges located in the West Plains as well as high density fracture zones, such as the Cheney Fracture Zone. -
The Jurassic Fossil Wood Diversity from Western Liaoning, NE China
Jiang et al. Journal of Palaeogeography (2019) 8:1 https://doi.org/10.1186/s42501-018-0018-y Journal of Palaeogeography RESEARCH Open Access The Jurassic fossil wood diversity from western Liaoning, NE China Zi-Kun Jiang1,2, Yong-Dong Wang2,3*, Ning Tian4,5, Ao-Wei Xie2,6, Wu Zhang7, Li-Qin Li2 and Min Huang1 Abstract Western Liaoning is a unique region in China that bears diverse types of Jurassic plants, including leaves, fern rhizomes, and wood, providing significant proxy for vegetation and palaeoenvironment reconstruction of the well-known Yanliao Flora in East Asia. In particular, the silicified wood is very abundant in the fossil Lagerstätte of the Jurassic Tiaojishan Formation in Beipiao, western Liaoning. Previous and recent systematic investigations documented a high diversity of the Jurassic wood assemblages. These assemblages are dominated by conifers, followed by cycads and ginkgoaleans. In total, about 30 species belonging to 21 genera of fossil wood have been recorded so far, which are represented by Cycadopsida, Ginkgopsida, Coniferopsida, and Gymnospermae incertae sedis. The evolutionary implications of several distinctive fossil wood taxa as well as palaeoclimate implications are summarized based on their anatomical structures and growth ring patterns. This work approaches the vegetation development and evolutionary significances of the wood taxa and their relatives, and provides clues for the further understanding of the diversity of the Jurassic Yanliao Flora in East Asia. Keywords: Fossil wood, Diversity, Evolution, Tiaojishan Formation, Jurassic 1 Introduction 2004;Wangetal.,2009). Among these localities, western Fossil floras are a significant record for the vegetation Liaoning is a well-known fossil Lagerstätte with diverse and for the palaeoenvironment reconstructions of the and well-preserved fossil plant foliages and wood (Zhang Mesozoic. -
Köppen Signatures” of Fossil Plant Assemblages for Effective Heat Transport of Gulf Stream to Subarctic North Atlantic During Miocene Cooling
Biogeosciences, 10, 7927–7942, 2013 Open Access www.biogeosciences.net/10/7927/2013/ doi:10.5194/bg-10-7927-2013 Biogeosciences © Author(s) 2013. CC Attribution 3.0 License. Evidence from “Köppen signatures” of fossil plant assemblages for effective heat transport of Gulf Stream to subarctic North Atlantic during Miocene cooling T. Denk1, G. W. Grimm1, F. Grímsson2, and R. Zetter2 1Swedish Museum of Natural History, Department of Palaeobiology, Box 50007, 10405 Stockholm, Sweden 2University of Vienna, Department of Palaeontology, Althanstrasse 14, 1090 Vienna, Austria Correspondence to: T. Denk ([email protected]) Received: 8 July 2013 – Published in Biogeosciences Discuss.: 15 August 2013 Revised: 29 October 2013 – Accepted: 2 November 2013 – Published: 6 December 2013 Abstract. Shallowing of the Panama Sill and the closure 1 Introduction of the Central American Seaway initiated the modern Loop Current–Gulf Stream circulation pattern during the Miocene, The Mid-Miocene Climatic Optimum (MMCO) at 17–15 but no direct evidence has yet been provided for effec- million years (Myr) was the last phase of markedly warm cli- tive heat transport to the northern North Atlantic during mate in the Cenozoic (Zachos et al., 2001). The MMCO was that time. Climatic signals from 11 precisely dated plant- followed by the Mid-Miocene Climate Transition (MMCT) bearing sedimentary rock formations in Iceland, spanning at 14.2–13.8 Myr correlated with the growth of the East 15–0.8 million years (Myr), resolve the impacts of the devel- Antarctic Ice Sheet (Shevenell et al., 2004). In the Northern oping Miocene global thermohaline circulation on terrestrial Hemisphere this cooling is reflected by continuous sea ice in vegetation in the subarctic North Atlantic region. -
5.0 Torrey Pine Forest
Volume 2C: Goals and Objectives for Vegetation Focus Management Species 5.0 Torrey Pine Forest 5.0 TORREY PINE FOREST 5.1 OVERVIEW OF THE TORREY PINE FOREST VEGETATION COMMUNITY The Torrey pine forest vegetation community has a very limited distribution in the MSPA, occurring almost exclusively in MU7 on 175 acres and with 1 acre in MU6 (SANDAG 2012; Table V2C.5-1, Figure V2C.5-1, or view an online map at: https://portal.sdmmp.com/map_vegetation.php?taxaid=SDMMP_vegcom_8). Distribution of Torrey Pines Forest Vegetation). Over 97% of Torrey pine forest is conserved, primarily at Torrey Pines State Natural Reserve, where 5,394 trees were mapped in 2006 (Franklin and Santos 2011). Torrey pine forest is the only native coastal southern California forest and is the rarest pine in North America (CDPR 2017). The forest is a remnant population from a period over 10,000 years ago when the climate was wetter and pines were more widespread on the southern California coast. Winter to spring precipitation is most important in annual growth (Biondi et al. 1997). This vegetation community is found only at Torrey Pines State Natural Reserve and on Santa Rosa Island (Sproul et al. 2011). Torrey pines occur on rocky sandstone soils immediately adjacent to the coast (Oberbauer et al. 2008). Torrey pine forest is classified as Pinus torreyana Special Stands, similar to an alliance but dominated by a rare, special-status species (Sproul et al. 2011). It is an open forest with trees <15 meters and with coastal sage scrub and chaparral understories. The stands are associated with many different species and Torrey pines are not diagnostic of a specific floristic composition. -
Skye: a Landscape Fashioned by Geology
SCOTTISH NATURAL SKYE HERITAGE A LANDSCAPE FASHIONED BY GEOLOGY SKYE A LANDSCAPE FASHIONED BY GEOLOGY SCOTTISH NATURAL HERITAGE Scottish Natural Heritage 2006 ISBN 1 85397 026 3 A CIP record is held at the British Library Acknowledgements Authors: David Stephenson, Jon Merritt, BGS Series editor: Alan McKirdy, SNH. Photography BGS 7, 8 bottom, 10 top left, 10 bottom right, 15 right, 17 top right,19 bottom right, C.H. Emeleus 12 bottom, L. Gill/SNH 4, 6 bottom, 11 bottom, 12 top left, 18, J.G. Hudson 9 top left, 9 top right, back cover P&A Macdonald 12 top right, A.A. McMillan 14 middle, 15 left, 19 bottom left, J.W.Merritt 6 top, 11 top, 16, 17 top left, 17 bottom, 17 middle, 19 top, S. Robertson 8 top, I. Sarjeant 9 bottom, D.Stephenson front cover, 5, 14 top, 14 bottom. Photographs by Photographic Unit, BGS Edinburgh may be purchased from Murchison House. Diagrams and other information on glacial and post-glacial features are reproduced from published work by C.K. Ballantyne (p18), D.I. Benn (p16), J.J. Lowe and M.J.C. Walker. Further copies of this booklet and other publications can be obtained from: The Publications Section, Cover image: Scottish Natural Heritage, Pinnacle Ridge, Sgurr Nan Gillean, Cullin; gabbro carved by glaciers. Battleby, Redgorton, Perth PH1 3EW Back page image: Tel: 01783 444177 Fax: 01783 827411 Cannonball concretions in Mid Jurassic age sandstone, Valtos. SKYE A Landscape Fashioned by Geology by David Stephenson and Jon Merritt Trotternish from the south; trap landscape due to lavas dipping gently to the west Contents 1. -
New Nomenclature Combinations in the Green Alder Species Complex
A peer-reviewed open-access journal PhytoKeys 56:New 1–6 nomenclature(2015) combinations in the green alder species complex (Betulaceae) 1 doi: 10.3897/phytokeys.56.5225 RESEARCH ARTICLE http://phytokeys.pensoft.net Launched to accelerate biodiversity research New nomenclature combinations in the green alder species complex (Betulaceae) Joyce Chery1 1 Department of Integrative Biology, University of California, Berkeley, California 94720 Corresponding author: Joyce Chery ([email protected]) Academic editor: Hugo De Boer | Received 1 May 2015 | Accepted 10 June 2015 | Published 14 August 2015 Citation: Chery J (2015) New nomenclature combinations in the green alder species complex (Betulaceae). PhytoKeys 56: 1–6. doi: 10.3897/phytokeys.56.5225 Abstract The name Alnus viridis (Chaix) DC., based on Betula viridis Chaix (1785), has traditionally been attributed to green alders although it is based on a later basionym. Alnus alnobetula (Ehrh.) K. Koch based on Betula alnobetula Ehrh. (1783) is the correct name for green alders. In light of the increasing use and recognition of the name Alnus alnobetula (Ehrh.) K. Koch in the literature. I herein propose new nomenclatural combinations to account for the Japanese and Chinese subspecies respectively: Alnus alnobetula subsp. maximowiczii (Callier ex C.K. Schneid.) J. Chery and Alnus alnobetula subsp. mandschurica (Callier ex C.K. Schneid.) J. Chery. Recent phylogenetic analyses place these two taxa in the green alder species complex, suggesting that they should be treated as infraspecific taxa under the polymorphic Alnus alnobetula. Keywords Green alders, Alnus viridis, Alnus alnobetula, Betulaceae Introduction Characteristic to the genus, Alnus alnobetula (Ehrh.) K. Koch is an anemophilous shrub with carpellate catkins that develop into woody strobili.