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Patterns and Drivers of Recent Disturbances Across the Temperate Forest Biome
ARTICLE DOI: 10.1038/s41467-018-06788-9 OPEN Patterns and drivers of recent disturbances across the temperate forest biome Andreas Sommerfeld 1, Cornelius Senf 1,2, Brian Buma 3, Anthony W. D’Amato 4, Tiphaine Després 5,6, Ignacio Díaz-Hormazábal7, Shawn Fraver8, Lee E. Frelich 9, Álvaro G. Gutiérrez 7, Sarah J. Hart10, Brian J. Harvey11, Hong S. He12, Tomáš Hlásny5, Andrés Holz 13, Thomas Kitzberger14, Dominik Kulakowski 15, David Lindenmayer 16, Akira S. Mori17, Jörg Müller18,19, Juan Paritsis 14, George L. W. Perry 20, Scott L. Stephens21, Miroslav Svoboda5, Monica G. Turner 22, Thomas T. Veblen23 & Rupert Seidl 1 1234567890():,; Increasing evidence indicates that forest disturbances are changing in response to global change, yet local variability in disturbance remains high. We quantified this considerable variability and analyzed whether recent disturbance episodes around the globe were con- sistently driven by climate, and if human influence modulates patterns of forest disturbance. We combined remote sensing data on recent (2001–2014) disturbances with in-depth local information for 50 protected landscapes and their surroundings across the temperate biome. Disturbance patterns are highly variable, and shaped by variation in disturbance agents and traits of prevailing tree species. However, high disturbance activity is consistently linked to warmer and drier than average conditions across the globe. Disturbances in protected areas are smaller and more complex in shape compared to their surroundings affected by human land use. This signal disappears in areas with high recent natural disturbance activity, underlining the potential of climate-mediated disturbance to transform forest landscapes. 1 University of Natural Resources and Life Sciences (BOKU) Vienna, Institute of Silviculture, Peter Jordan Straße 82, 1190 Wien, Austria. -
Biome-Specific Scaling of Ocean Productivity, Temperature, and Carbon Export Efficiency
UC Irvine UC Irvine Previously Published Works Title Biome-specific scaling of ocean productivity, temperature, and carbon export efficiency Permalink https://escholarship.org/uc/item/9vk7r4v9 Journal Geophysical Research Letters, 43(10) ISSN 0094-8276 Authors Britten, GL Primeau, FW Publication Date 2016 DOI 10.1002/2016GL068778 License https://creativecommons.org/licenses/by/4.0/ 4.0 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PUBLICATIONS Geophysical Research Letters RESEARCH LETTER Biome-specific scaling of ocean productivity, 10.1002/2016GL068778 temperature, and carbon export efficiency Key Points: Gregory L. Britten1 and François W. Primeau1 • Optimized models predict carbon fi export ef ciency from net primary 1Department of Earth System Science, University of California, Irvine, USA production and sea surface temperature • Biome-specific relationships impact global export inferred from Abstract Mass conservation and metabolic theory place constraints on how marine export production (EP) satellite-derived variables scales with net primary productivity (NPP) and sea surface temperature (SST); however, little is empirically • Individual biomes respond differently known about how these relationships vary across ecologically distinct ocean biomes. Here we compiled in to simulated net primary production fi and sea surface temperature changes situ observations of EP, NPP, and SST and used statistical model selection theory to demonstrate signi cant biome-specific scaling relationships among these variables. Multiple statistically similar models yield a À threefold variation in the globally integrated carbon flux (~4–12 Pg C yr 1) when applied to climatological Supporting Information: • Supporting Information S1 satellite-derived NPP and SST. Simulated NPP and SST input variables from a 4×CO2 climate model experiment • Data Set S1 further show that biome-specific scaling alters the predicted response of EP to simulated increases of • Data Set S2 atmospheric CO2. -
2019 Data Report for Oneida Lake, Livingston County
Michigan Lakes– Ours to Protect 2019 Data Report for Oneida Lake, Livingston County Site ID: 470573 42.4676°N, 83.8488°W The CLMP is brought to you by: 1 About this report: This report is a summary of the data that have been collected through the Cooperative Lakes Monitoring Program. The contents have been customized for your lake. The first page is a summary of the Trophic Status Indicators of your lake (Secchi Disk Transparency, Chlorophyll-a, Spring Total Phosphorus, and Summer Total Phosphorus). Where data are available, they have been summarized for the most recent field season, five years prior to the most recent field season, and since the first year your lake has been enrolled in the program. If you did not take 8 or more Secchi disk measurements or 4 or more chlorophyll measurements, there will not be summary data calculated for these parameters. These numbers of measurements are required to ensure that the results are indicative of overall summer conditions. If you enrolled in Dissolved Oxygen/Temperature, the summary page will have a graph of one of the profiles taken during the late summer (typically August or September). If your lake stratifies, we will use a graph showing the earliest time of stratification, because identifying the timing of this condition and the depth at which it occurs is typically the most important use of dissolved oxygen measurements. The back of the summary page will be an explanation of the Trophic Status Index and where your lake fits on that scale. The rest of the report will be aquatic plant summaries, Score the Shore results, and larger graphs, including all Dissolved Oxygen/Temperature Profiles that you recorded. -
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 -
Current Insights Into the Effectiveness of Riparian Management, Attainment of Multiple Benefits, and Potential Technical Enhancements
Published March 8, 2019 Journal of Environmental Quality SPECIAL SECTION RIPARIAN BUFFER MANAGEMENT Current Insights into the Effectiveness of Riparian Management, Attainment of Multiple Benefits, and Potential Technical Enhancements Marc Stutter,* Brian Kronvang, Daire Ó hUallacháin, and Joachim Rozemeijer iparian buffers have been one of the most widely Abstract used management options worldwide when dealing Buffer strips between land and waters are widely applied with protection of surface waters from agricultural dif- measures in diffuse pollution management, with desired Rfuse pollution. Appropriately managed riparian areas offer mul- outcomes across other factors. There remains a need for tiple functions related to improving water quality, biodiversity, evidence of pollution mitigation and wider habitat and societal benefits across scales. This paper synthesizes a collection of 16 and climate adaptation. First, riparian areas offer possibilities new primary studies and review papers to provide the latest for protecting watercourses and lakes from inputs of sediments, insights into riparian management. We focus on the following nutrients, pesticides, and other contaminants by intercepting areas: (i) diffuse pollution removal efficiency of conventional surface runoff, tile drainage, and groundwater from adjoining and saturated buffer strips, (ii) enhancing biodiversity of buffers, agricultural fields. Second, riparian areas also offer unique bio- (iii) edge-of-field technologies for improving nutrient retention, and (iv) potential reuse of nutrients and biomass from buffers. diversity (in turn affecting in-field and in-stream biodiversity) Although some topics represent emerging areas, for other including structurally complex layers of vegetation, making well-studied topics (e.g., diffuse pollution), it remains that them attractive to many wildlife species (Naiman et al., 1993). -
Grasslands 4/16/03 3:46 PM
Ecoregion: Grasslands 4/16/03 3:46 PM Grasslands INTRODUCTION About 25% of Earth’s land surface is covered by temperate grassland. These large expanses of flat or hilly country cover much of North America, as well as large areas of Europe, Asia, and South America. Most grasslands are found in the interiors of continents, where there is too little rainfall for a forest but too much rain for a desert. Art Explosion Art Explosion Rolling hills covered with grasses and very few trees A few scattered trees are found on savannas, are typical of North American grassland prairies. tropical grasslands of Africa. Temperate grasslands have subtle differences and different names throughout the world. Prairies and plains of North America are grasslands with tall grasses, while the steppes of Russia are grasslands with short grasses. Veldts are found in South Africa, the puszta in Hungary, and the pampas in Argentina and Uruguay. Savannas are tropical grasslands that support scattered trees and shrubs. They often form a transitional biome file:///Ecoregion/grass/content.html Page 1 of 6 Ecoregion: Grasslands 4/16/03 3:46 PM between deserts and rain forests. Some temperate grasslands are also called savannas. The word savanna comes from the Spanish word zavanna, meaning “treeless plain.” Savannas cover almost half of Africa (mostly central Africa) and large areas of Australia and South America. ABIOTIC DATA The grassland climate is rather dry, averaging about 20 to 100 centimeters (8–40 inches) of precipitation a year. Summers are very hot and may reach 45°C (113°F). Winter temperatures often fall below freezing, which is 0°C (32°F). -
Assessment of Land Use Change and Riparian Zone Status in the Barnegat Bay and Little Egg Harbor Watershed: 1995-2002-2006
Assessment of Land Use Change and Riparian Zone Status in the Barnegat Bay and Little Egg Harbor Watershed: 1995-2002-2006 Intact forested riparian zone along the upper reaches of the Forked River. Richard G. Lathrop¹ Scott M. Haag² October 2007 ¹Grant F. Walton Center for Remote Sensing and Spatial Analysis ²Institute of Marine and Coastal Science School of Environmental & Biological Sciences-Rutgers University New Brunswick, NJ 08901 1 Assessment of Land Use Change and Riparian Zone Status in the Barnegat Bay and Little Egg Harbor Watershed: 1995-2002-2006 Executive Summary The Barnegat Bay/Little Egg Harbor (BB/LEH) estuary is suffering from eutrophication issues due to nutrient, most importantly nitrogen, loading from both atmospheric as well as watershed sources (Kennish et al, 2007). Urban and agricultural land uses can be an important source of nitrogen loading. As part of our ongoing monitoring efforts, the Grant F. Walton Center for Remote Sensing & Spatial Analysis, with funding provided by the Barnegat Bay National Estuary Program, undertook to map and assess recent land use change in the Barnegat Bay-Little Egg Harbor watershed. Our updated mapping reveals that urban land use increased from approximately 25% in 1995 to approximately 30% of the BB/LEH watershed in 2006. Including all altered land uses (i.e., agriculture and barren lands) puts the percentage of altered land in the BB-LEH watershed at over 33% in 2006. The BB/LEH estuary system is continuing to experience a significant conversion of forested and wetland habitats to urban land cover and thereby exacerbating nutrient loading to the BB-LEH estuary. -
Chapter Vii Table of Contents
CHAPTER VII TABLE OF CONTENTS VII. APPENDICES AND REFERENCES CITED........................................................................1 Appendix 1: Description of Vegetation Databases......................................................................1 Appendix 2: Suggested Stocking Levels......................................................................................8 Appendix 3: Known Plants of the Desolation Watershed.........................................................15 Literature Cited............................................................................................................................25 CHAPTER VII - APPENDICES & REFERENCES - DESOLATION ECOSYSTEM ANALYSIS i VII. APPENDICES AND REFERENCES CITED Appendix 1: Description of Vegetation Databases Vegetation data for the Desolation ecosystem analysis was stored in three different databases. This document serves as a data dictionary for the existing vegetation, historical vegetation, and potential natural vegetation databases, as described below: • Interpretation of aerial photography acquired in 1995, 1996, and 1997 was used to characterize existing (current) conditions. The 1996 and 1997 photography was obtained after cessation of the Bull and Summit wildfires in order to characterize post-fire conditions. The database name is: 97veg. • Interpretation of late-1930s and early-1940s photography was used to characterize historical conditions. The database name is: 39veg. • The potential natural vegetation was determined for each polygon in the analysis -
The New York Botanical Garden
Vol. XV DECEMBER, 1914 No. 180 JOURNAL The New York Botanical Garden EDITOR ARLOW BURDETTE STOUT Director of the Laboratories CONTENTS PAGE Index to Volumes I-XV »33 PUBLISHED FOR THE GARDEN AT 41 NORTH QUBKN STRHBT, LANCASTER, PA. THI NEW ERA PRINTING COMPANY OFFICERS 1914 PRESIDENT—W. GILMAN THOMPSON „ „ _ i ANDREW CARNEGIE VICE PRESIDENTS J FRANCIS LYNDE STETSON TREASURER—JAMES A. SCRYMSER SECRETARY—N. L. BRITTON BOARD OF- MANAGERS 1. ELECTED MANAGERS Term expires January, 1915 N. L. BRITTON W. J. MATHESON ANDREW CARNEGIE W GILMAN THOMPSON LEWIS RUTHERFORD MORRIS Term expire January. 1916 THOMAS H. HUBBARD FRANCIS LYNDE STETSON GEORGE W. PERKINS MVLES TIERNEY LOUIS C. TIFFANY Term expire* January, 1917 EDWARD D. ADAMS JAMES A. SCRYMSER ROBERT W. DE FOREST HENRY W. DE FOREST J. P. MORGAN DANIEL GUGGENHEIM 2. EX-OFFICIO MANAGERS THE MAYOR OP THE CITY OF NEW YORK HON. JOHN PURROY MITCHEL THE PRESIDENT OP THE DEPARTMENT OP PUBLIC PARES HON. GEORGE CABOT WARD 3. SCIENTIFIC DIRECTORS PROF. H. H. RUSBY. Chairman EUGENE P. BICKNELL PROF. WILLIAM J. GIES DR. NICHOLAS MURRAY BUTLER PROF. R. A. HARPER THOMAS W. CHURCHILL PROF. JAMES F. KEMP PROF. FREDERIC S. LEE GARDEN STAFF DR. N. L. BRITTON, Director-in-Chief (Development, Administration) DR. W. A. MURRILL, Assistant Director (Administration) DR. JOHN K. SMALL, Head Curator of the Museums (Flowering Plants) DR. P. A. RYDBERG, Curator (Flowering Plants) DR. MARSHALL A. HOWE, Curator (Flowerless Plants) DR. FRED J. SEAVER, Curator (Flowerless Plants) ROBERT S. WILLIAMS, Administrative Assistant PERCY WILSON, Associate Curator DR. FRANCIS W. PENNELL, Associate Curator GEORGE V. -
The Riparian Zone
Land-Water Interactions: The Riparian Zone F J. Swanson, S. V Gregory, J. R. Sedell,and A. G.Campbell INTRODUCTION The interface between aquatic and terrestrial environments in coniferous structure, composition, and function of the riparian zone had received little consideration in ecosystem level research, because this zone forms the interface between scientific disci- plines as well as ecosystem components. In some climate-vegetation zones particular aspects of riparian zones have received much study. ñparinpiant communities in arid lands have been studied extensive!y, primar- ily in terms o TdfeTbiiatJohnson and Jones 1977 Thomas et al 1979) Research on riparian 'egetation along major rivers has dealt mainly with forest composition and dynamics (for example, Lindsey et al. 1961; Sigafoos 1964; Bell 1974; Johnson et al. 1976). Riparian vegetation research has been largely neglected in forested mountain land, where it tends to have smaller areal extent and economic value than upslope vegetation. yre!pian zone is an integral part of the forest/stream ecosystem complex. This chapter synthesizes general concepts about the riparian zone in north- west coniferous forests and the results of coniferous forest biome research on: (1) structure and composition of riparian vegetation and its variation in time and space; and (2) functional aspects of the riparian zone in terms of physical, biological, and chemical terrestrial/aquatic interactions. We emphasize condi- tions observed in mountain streams and small rivers. The riparian zone may be defined in a variety of ways, based on factors such as vegetation type, groundwater and surface water hydrology, topogra- phy, and ecosystem function. These factors have so many complex interactions that defining the riparian zone in one sense integrates elements of the other factors. -
A Database of Plant Traits Spanning the Tundra Biome
Received: 15 November 2017 | Revised: 11 July 2018 | Accepted: 20 July 2018 DOI: 10.1111/geb.12821 DATA PAPER Tundra Trait Team: A database of plant traits spanning the tundra biome Anne D. Bjorkman1,2,3 | Isla H. Myers‐Smith1 | Sarah C. Elmendorf4,5,6 | Signe Normand2,7,8 | Haydn J. D. Thomas1 | Juha M. Alatalo9 | Heather Alexander10 | Alba Anadon‐Rosell11,12,13 | Sandra Angers‐Blondin1 | Yang Bai14 | Gaurav Baruah15 | Mariska te Beest16,17 | Logan Berner18 | Robert G. Björk19,20 | Daan Blok21 | Helge Bruelheide22,23 | Agata Buchwal24,25 | Allan Buras26 | Michele Carbognani27 | Katherine Christie28 | Laura S. Collier29 | Elisabeth J. Cooper30 | J. Hans C. Cornelissen31 | Katharine J. M. Dickinson32 | Stefan Dullinger33 | Bo Elberling34 | Anu Eskelinen35,23,36 | Bruce C. Forbes37 | Esther R. Frei38,39 | Maitane Iturrate‐Garcia15 | Megan K. Good40 | Oriol Grau41,42 | Peter Green43 | Michelle Greve44 | Paul Grogan45 | Sylvia Haider22,23 | Tomáš Hájek46,47 | Martin Hallinger48 | Konsta Happonen49 | Karen A. Harper50 | Monique M. P. D. Heijmans51 | Gregory H. R. Henry39 | Luise Hermanutz29 | Rebecca E. Hewitt52 | Robert D. Hollister53 | James Hudson54 | Karl Hülber33 | Colleen M. Iversen55 | Francesca Jaroszynska56,57 | Borja Jiménez‐Alfaro58 | Jill Johnstone59 | Rasmus Halfdan Jorgesen60 | Elina Kaarlejärvi14,61 | Rebecca Klady62 | Jitka Klimešová46 | Annika Korsten32 | Sara Kuleza59 | Aino Kulonen57 | Laurent J. Lamarque63 | Trevor Lantz64 | Amanda Lavalle65 | Jonas J. Lembrechts66 | Esther Lévesque63 | Chelsea J. Little15,67 | Miska Luoto49 | Petr Macek47 | Michelle C. Mack52 | Rabia Mathakutha44 | Anders Michelsen34,68 | Ann Milbau69 | Ulf Molau70 | John W. Morgan43 | Martin Alfons Mörsdorf30 | Jacob Nabe‐Nielsen71 | Sigrid Schøler Nielsen2 | Josep M. Ninot11,12 | Steven F. Oberbauer72 | Johan Olofsson16 | Vladimir G. Onipchenko73 | Alessandro Petraglia27 | Catherine Pickering74 | Janet S. -
The Buffer Capacity of Riparian Vegetation to Control Water Quality
water Article The Buffer Capacity of Riparian Vegetation to Control Water Quality in Anthropogenic Catchments from a Legally Protected Area: A Critical View over the Brazilian New Forest Code Carlos Alberto Valera 1,2,3, Teresa Cristina Tarlé Pissarra 2,3 , Marcílio Vieira Martins Filho 2,3 , Renato Farias do Valle Júnior 3,4, Caroline Fávaro Oliveira 3,4, João Paulo Moura 5 , Luís Filipe Sanches Fernandes 3,5 and Fernando António Leal Pacheco 3,6,* 1 Coordenadoria Regional das Promotorias de Justiça do Meio Ambiente das Bacias dos Rios Paranaíba e Baixo Rio Grande, Rua Coronel Antônio Rios, 951, Uberaba MG 38061-150, Brazil; [email protected] 2 Universidade Estadual Paulista, Faculdade de Ciências Agrárias e Veterinárias, Via de Acesso Prof. Paulo Donato Castellane, s/n, Jaboticabal SP 14884-900, Brazil; [email protected] (T.C.T.P.); marcilio.martins-fi[email protected] (M.V.M.F.) 3 POLUS—Grupo de Política de Uso do Solo, Universidade Estadual Paulista (UNESP), Via de Acesso Prof. Paulo Donato Castellane, s/n, Jaboticabal SP 14884-900, Brazil; [email protected] (R.F.d.V.J.); [email protected] (C.F.O.); lfi[email protected] (L.F.S.F.) 4 Instituto Federal do Triângulo Mineiro, Campus Uberaba, Laboratório de Geoprocessamento, Uberaba MG 38064-790, Brazil 5 Centro de Investigação e Tecnologias Agroambientais e Biológicas, Universidade de Trás-os-Montes e Alto Douro, Ap. 1013, 5001-801 Vila Real, Portugal; [email protected] 6 Centro de Química de Vila Real, Universidade de Trás-os-Montes e Alto Douro, Ap. 1013, 5001-801 Vila Real, Portugal * Correspondence: [email protected]; Tel.: +55-351-917519833 Received: 10 February 2019; Accepted: 12 March 2019; Published: 16 March 2019 Abstract: The riparian buffer width on watersheds has been modified over the last decades.