Copper River Delta
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Translocation and Transport
Glime, J. M. 2017. Nutrient Relations: Translocation and Transport. Chapt. 8-5. In: Glime, J. M. Bryophyte Ecology. Volume 1. 8-5-1 Physiological Ecology. Ebook sponsored by Michigan Technological University and the International Association of Bryologists. Last updated 17 July 2020 and available at <http://digitalcommons.mtu.edu/bryophyte-ecology/>. CHAPTER 8-5 NUTRIENT RELATIONS: TRANSLOCATION AND TRANSPORT TABLE OF CONTENTS Translocation and Transport ................................................................................................................................ 8-5-2 Movement from Older to Younger Tissues .................................................................................................. 8-5-6 Directional Differences ................................................................................................................................ 8-5-8 Species Differences ...................................................................................................................................... 8-5-8 Mechanisms of Transport .................................................................................................................................... 8-5-9 Source to Sink? ............................................................................................................................................ 8-5-9 Enrichment Effects ..................................................................................................................................... 8-5-10 Internal Transport -
Geomorphic Classification of Rivers
9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations. -
Inferences Based on ITS Molecular Phylogenetic Analyses
Korean J. Pl. Taxon. (2011) Vol. 41 No. 3, pp.209-214 The taxonomic status of Angelica purpuraefolia and its allies in Korea : Inferences based on ITS molecular phylogenetic analyses Byoung Yoon Lee1,2*, Myounghai Kwak1, Jeong Eun Han1,3 and Se-Jung Kim1,4 1Wildlife Genetic Resources Center, National Institute of Biological Resources, Incheon 404-170, Korea 2Division of Microorganism, National Institute of Biological Resources, Incheon 404-170, Korea 3Department of Biology, Inha University, Incheon 402-751, Korea 4Genome analyses center, National Instrumentation Center for Environmental Management, Seoul 151-921, Korea (Received 29 August 2011; Revised 08 September 2011; Accepted 13 September 2011) ABSTRACT: The taxonomy of the umbelliferous species Angelica amurensis and its allies was reviewed on the basis of molecular phylogenies derived from sequences of nuclear ribosomal DNA internal transcribed spacer (ITS) regions. Strict consensus of six minimal length 119-step trees derived from equally weighted maximum parsimony analysis of combined nuclear rDNA ITS1 and ITS2 sequences from 29 accessions of Angelica and outgroups indicated that Angelica purpuraefolia, known to be endemic to Korea, is the same species as A. amurensis. Comparisons of sequence pairs across both spacer regions revealed identity or 1-2 bp differences between A. purpuraefolia and A. amurensis. These results indicated that the two taxa are not distinguished taxonomically. Also, nuclear rDNA ITS regions are discussed as potential barcoding loci for identifying Korean Angelica. Keywords: Apiaceae, Angelica purpuraefolia, Angelica amurensis, DNA barcode The Korean endemic Angelica purpuraefolia Chung grows bioactivities have been protected by Korean patent law (Lee in mountainous areas in Gangwondo, Gyeongsangbugdo, and et al., 2005). -
Fishing in the Cordova Area
Southcentral Region Department of Fish and Game Fishing in the Cordova Area About Cordova Cordova is a small commercial fishing town (pop. 2,500) on the southeastern side of Prince William Sound, 52 air miles southeast of Valdez and 150 air miles southeast of Anchorage. The town can be reached only by air or by ferries. Check the Alaska Marine Highway website for more informa- tion about the ferries: www.dot.state.ak.us/amhs Alaska Natives originally settled the area around the Copper River Delta. The town of Cordova changed its name from Puerto Cordova in 1906 when the railroad was built to move copper ore. Commercial fishing has been a major industry The Scott River for Cordova since the 1940s, so please be careful around their boats and nets. The Division of Commercial Hotels, fishing charters, camping Fisheries offers a wealth of information on their website, For information about fishing charters, accommoda- including in-season harvest information at www.adfg. tions and other services in Cordova, contact the Chamber alaska.gov . of Commerce and Visitor’s Center at P.O. Box 99, Cordova, Bears are numerous in the Cordova area and anglers Alaska, 99574, (907) 424-7260 or cordovachamber.com. The should use caution when fishing salmon spawning areas. City of Cordova also runs an excellent website at www. Check the ADF&G website for the “Bear Facts” brochure, cityofcordova.net . or request one from the ADF&G Anchorage regional of- fice. Anglers who fillet fish along a river are encouraged to chop up the fish carcass and throw the pieces into fast Management of Alaska’s flowing water. -
Regulation Summary and Access for the Chitina
Regulation Summary & you have fished or not, and whether you harvested Recording & Marking Catch fish or not. ONLINE HARVEST REPORTING: Both tips of the tail must be removed and all salmon Access for the Chitina http://fish.alaska.gov/PU. Failure to report is in taken must be recorded on the permit immediately Subdistrict Personal violation of 5 AAC 77.015(c), and is subject to a $200 with the date fished and catch by species, prior fine and loss of future personal use fishing privileges. to leaving the fishing site and before fish are Use Salmon Fishery concealed from plain view (5 AAC 77.591 (d)). For the purposes of this fishery, immediately“ ” Where Is the Chitina Subdistrict? Online permits and harvest reporting: means before concealing the fish from plain view The fishery is restricted to the waters of the mainstem http://fish.alaska.gov/PU or transporting the salmon from the fishing site. Copper River between the downstream edge of the “Fishing site” means the location where the fish Fishery opening recordings: Chitina-McCarthy Bridge and ADF&G regulatory is removed from the water and becomes part of the markers located about 200 yards upstream of Haley Glennallen: (907) 822-5224 permit holder’s bag limit. Creek. All tributaries of the Copper River in this area, Fairbanks: (907) 459-7382 including the Chitina River, are closed to personal use Personal Use Harvested Fish Anchorage: (907) 267-2511 fishing(map on reverse). Personal use harvested fish (including eggs) cannot ADF&G Chitina dip net website: be bought, sold, traded or bartered. -
Safe Boating Through the St. Lucie Inlet
Information: Florida Fish & Wildlife Commission 850-488-4676 SAFE BOATING US Coast Guard - Ft. Pierce 772-461-7606 THROUGH THE ST. LUCIE INLET US Coast Guard Auxiliary 772-465-8128 US Army Corps of Engineers 772-221-3349 St. Lucie Inlet Coastal 772-225-2300 Weather Station HERE ARE SOME THINGS TO REMEMBER: • Listen to the most recent weather forecast for the times you plan to go out AND come back in the inlet. • Look in the Tide Tables or local newspapers for the times St. Lucie Inlet of predicted high and low tides for the day you plan to go out. Remember the outgoing (ebb) tital current at low Newcomers tide is the worst time to make a passage through the St. Lucie Inlet. If you are a boater new to this area, it is highly • Safe boating practices are even more important in inlets. recommended that you make your first passage of Check your boat before you head out. Life preservers the St. Lucie Inlet as an observer. An experienced should be worn when going through inlets. boater with local knowledge at the helm can point • Expect the unexpected. Watch the clouds to anticipate out various hazards and conditions to avoid. This is severe weather such as thunderstorms. Be on the lookout for shifting shoals and changing channels. especially important if you have no prior experience • Engine failure is common in small boats in rough seas. with any ocean inlets. The extra roughness agitates gasoline and settled dirt or water in the fuel system, which can cause engine failure Notes on Navigation at Night at a crtical time. -
State of New York City's Plants 2018
STATE OF NEW YORK CITY’S PLANTS 2018 Daniel Atha & Brian Boom © 2018 The New York Botanical Garden All rights reserved ISBN 978-0-89327-955-4 Center for Conservation Strategy The New York Botanical Garden 2900 Southern Boulevard Bronx, NY 10458 All photos NYBG staff Citation: Atha, D. and B. Boom. 2018. State of New York City’s Plants 2018. Center for Conservation Strategy. The New York Botanical Garden, Bronx, NY. 132 pp. STATE OF NEW YORK CITY’S PLANTS 2018 4 EXECUTIVE SUMMARY 6 INTRODUCTION 10 DOCUMENTING THE CITY’S PLANTS 10 The Flora of New York City 11 Rare Species 14 Focus on Specific Area 16 Botanical Spectacle: Summer Snow 18 CITIZEN SCIENCE 20 THREATS TO THE CITY’S PLANTS 24 NEW YORK STATE PROHIBITED AND REGULATED INVASIVE SPECIES FOUND IN NEW YORK CITY 26 LOOKING AHEAD 27 CONTRIBUTORS AND ACKNOWLEGMENTS 30 LITERATURE CITED 31 APPENDIX Checklist of the Spontaneous Vascular Plants of New York City 32 Ferns and Fern Allies 35 Gymnosperms 36 Nymphaeales and Magnoliids 37 Monocots 67 Dicots 3 EXECUTIVE SUMMARY This report, State of New York City’s Plants 2018, is the first rankings of rare, threatened, endangered, and extinct species of what is envisioned by the Center for Conservation Strategy known from New York City, and based on this compilation of The New York Botanical Garden as annual updates thirteen percent of the City’s flora is imperiled or extinct in New summarizing the status of the spontaneous plant species of the York City. five boroughs of New York City. This year’s report deals with the City’s vascular plants (ferns and fern allies, gymnosperms, We have begun the process of assessing conservation status and flowering plants), but in the future it is planned to phase in at the local level for all species. -
Morphologic Characteristics of the Blow River Delta, Yukon Territory, Canada
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1969 Morphologic Characteristics of the Blow River Delta, Yukon Territory, Canada. James Murl Mccloy Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Mccloy, James Murl, "Morphologic Characteristics of the Blow River Delta, Yukon Territory, Canada." (1969). LSU Historical Dissertations and Theses. 1605. https://digitalcommons.lsu.edu/gradschool_disstheses/1605 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. This dissertation has been microfilmed exactly as received 70-252 McCLOY, James Murl, 1934- MORPHOLOGIC CHARACTERISTICS OF THE BLOW RIVER DELTA, YUKON TERRITORY, CANADA. The Louisiana State University and Agricultural and Mechanical College, Ph.D., 1969 Geography University Microfilms, Inc., Ann Arbor, Michigan Morphologic Characteristics of the Blow River Belta, Yukon Territory, Canada A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography and Anthropology by James Murl McCloy B.A., State College at Los Angeles, 1961 May, 1969 ACKNOWLEDGEMENTS Research culminating in this dissertation was conducted under the auspices of the Arctic Institute of North America. The major portion of the financial support was received from the United States Army under contract no. BA-ARO-D-3I-I2I4.-G832, "Arctic Environmental Studies." Additional financial assistance during part of the writing stage was received in the form of a research assistantship from the Coastal Studies Institute, Louisi ana State University. -
Population Ecology of Eriophorum Latifolium, a Clonal Species in Rich Fen Vegetation
Anders Lyngstad Population Ecology of Eriophorum latifolium, a Clonal Species in Rich Fen Vegetation Thesis for the degree of Philosophiae Doctor Trondheim, October 2010 Norwegian University of Science and Technology Faculty of Natural Sciences and Technology Department of Biology NTNU Norwegian University of Science and Technology Thesis for the degree of Philosophiae Doctor Faculty of Natural Sciences and Technology Department of Biology © Anders Lyngstad ISBN 978-82-471-2332-4 (printed ver.) ISBN 978-82-471-2333-1 (electronic ver.) ISSN 1503-8181 Doctoral theses at NTNU, 2010:179 Printed by NTNU-trykk Synopsis PREFACE It was the spring of 2005, and it was the right time to move onwards. A position as a research fellow working with long-term time series at the Museum of Natural History and Archaeology at the Norwegian University of Science and Technology (NTNU) was announced, and a PhD-project was developed with the studies of former haymaking lands at Sølendet and Tågdalen nature reserves as a starting point. Work began in earnest in January 2006, and continued at an ever increasing pace until July 2010, when all the parts of the thesis were finally completed and assembled. The study was financed by NTNU, and was carried out at the Museum of Natural History and Archaeology and the Institute of Biology, both NTNU. I am deeply grateful to my main supervisor Professor Asbjørn Moen at the Museum of Natural History and Archaeology, and my co-supervisor Associate Professor Bård Pedersen at the Institute of Biology. This project rests on the long-term studies of rich hayfens that were initiated by Asbjørn 40 years ago, and that are still ongoing, much due to his continuous effort. -
1 the Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration
1 The Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration 2 of Soft Cliff Coastlines 3 4 Sally Brown1*, Max Barton1, Robert J Nicholls1 5 6 1. Faculty of Engineering and the Environment, University of Southampton, 7 University Road, Highfield, Southampton, UK. S017 1BJ. 8 9 * Sally Brown ([email protected], Telephone: +44(0)2380 594796). 10 11 Abstract: Building defences, such as groynes, on eroding soft cliff coastlines alters the 12 sediment budget, changing the shoreline configuration adjacent to defences. On the 13 down-drift side, the coastline is set-back. This is often believed to be caused by increased 14 erosion via the ‘terminal groyne effect’, resulting in rapid land loss. This paper examines 15 whether the terminal groyne effect always occurs down-drift post defence construction 16 (i.e. whether or not the retreat rate increases down-drift) through case study analysis. 17 18 Nine cases were analysed at Holderness and Christchurch Bay, England. Seven out of 19 nine sites experienced an increase in down-drift retreat rates. For the two remaining sites, 20 retreat rates remained constant after construction, probably as a sediment deficit already 21 existed prior to construction or as sediment movement was restricted further down-drift. 22 For these two sites, a set-back still evolved, leading to the erroneous perception that a 23 terminal groyne effect had developed. Additionally, seven of the nine sites developed a 24 set back up-drift of the initial groyne, leading to the defended sections of coast acting as 1 25 a hard headland, inhabiting long-shore drift. -
3.13 Paleontological Resources
Gateway West Transmission Line Draft EIS 3.13 PALEONTOLOGICAL RESOURCES This section addresses the potential impacts from the Proposed Route and Route Alternatives on the known paleontological resources during construction, operation, and decommissioning. The Proposed Route and Route Alternatives pass through areas where paleontological resources are known to exist. The routes, their potential impacts, and mitigation methods to minimize or eliminate impacts are discussed in this section. 3.13.1 Affected Environment This section describes the mapped geology and known paleontological resources near the Proposed Action. It also describes and compares potential impacts of the Proposed Action and Action Alternatives to paleontological resources. Fossils are important scientific and educational resources because of their use in: 1) documenting the presence and evolutionary history of particular groups of now extinct organisms, 2) reconstructing the environments in which these organisms lived, and 3) determining the relative ages of the strata in which they occur. Fossils are also important in determining the geologic events that resulted in the deposition of the sediments in which they were buried. 3.13.1.1 Analysis Area The Project area in Wyoming and Idaho consists of predominantly north-south trending mountain ranges separated by structural basins. The eastern portion of the Project (Segments 1 and 2) would be located within the Laramie Mountains and the Shirley Mountains, which consist predominantly of Precambrian granite and gneisses. Moving west in Wyoming, the Project would cross major structural basins created during the Laramide Orogeny, including the Hanna Basin in Carbon County (Segment 2), and the Greater Green River Basin in Sweetwater County (Segments 3 and 4). -
Experiments on Patterns of Alluvial Cover and Bedrock Erosion in a Meandering Channel Roberto Fernández1, Gary Parker1,2, Colin P
Earth Surf. Dynam. Discuss., https://doi.org/10.5194/esurf-2019-8 Manuscript under review for journal Earth Surf. Dynam. Discussion started: 27 February 2019 c Author(s) 2019. CC BY 4.0 License. Experiments on patterns of alluvial cover and bedrock erosion in a meandering channel Roberto Fernández1, Gary Parker1,2, Colin P. Stark3 1Ven Te Chow Hydrosystems Laboratory, Department of Civil and Environmental Engineering, University of Illinois at 5 Urbana-Champaign, Urbana, IL 61801, USA 2Department of Geology, University of Illinois at Urbana-Champaign, Urbana, IL 61801, USA 3Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA Correspondence to: Roberto Fernández ([email protected]) Abstract. 10 In bedrock rivers, erosion by abrasion is driven by sediment particles that strike bare bedrock while traveling downstream with the flow. If the sediment particles settle and form an alluvial cover, this mode of erosion is impeded by the protection offered by the grains themselves. Channel erosion by abrasion is therefore related to the amount and pattern of alluvial cover, which are functions of sediment load and hydraulic conditions, and which in turn are functions of channel geometry, slope and sinuosity. This study presents the results of alluvial cover experiments conducted in a meandering channel flume of high fixed 15 sinuosity. Maps of quasi-instantaneous alluvial cover were generated from time-lapse imaging of flows under a range of below- capacity bedload conditions. These maps were used to infer patterns