Considering Forest and Grassland Carbon in Land Management
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Foliar and Ecosystem Respiration in an Old-Growth Tropical Rain Forest
Plant, Cell and Environment (2008) 31, 473–483 doi: 10.1111/j.1365-3040.2008.01775.x Foliar and ecosystem respiration in an old-growth tropical rain forest MOLLY A. CAVALERI1,2, STEVEN F. OBERBAUER3,4 & MICHAEL G. RYAN5,6 1Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO 80523, USA, 2Botany Department, University of Hawaii, Manoa, 3190 Maile Way, Honolulu, HI 96826, USA, 3Department of Biological Sciences, Florida International University, 11200 SW 8th Street, Miami, FL 33199, USA, 4Fairchild Tropical Botanic Garden, 11935 Old Cutler Road, Miami, FL 33156, USA, 5United States Department of Agriculture Forest Service, Rocky Mountain Research Station, 240 West Prospect RD, Fort Collins, CO 80526, USA and 6Graduate Degree Program in Ecology, Department of Forest, Rangeland, and Watershed Stewardship, Colorado State University, Fort Collins, CO 80523, USA ABSTRACT Chambers et al. 2004). Results vary widely about whether tropical forests are presently acting as carbon sources or Foliar respiration is a major component of ecosystem res- sinks, or how this may be affected by global warming. piration, yet extrapolations are often uncertain in tropical Several eddy flux studies have concluded that tropical rain forests because of indirect estimates of leaf area index forests are primarily acting as carbon sinks (Fan et al. 1990; (LAI). A portable tower was used to directly measure LAI Grace et al. 1995; Malhi et al. 1998; Loescher et al. 2003, and night-time foliar respiration from 52 vertical transects but see Saleska et al. 2003). Many atmosphere–biosphere throughout an old-growth tropical rain forest in Costa Rica. modelling studies, on the other hand, predict that tropical In this study, we (1) explored the effects of structural, func- forests will be an increased carbon source with global tional and environmental variables on foliar respiration; (2) warming (Kindermann, Würth & Kohlmaier 1996; Braswell extrapolated foliar respiration to the ecosystem; and (3) et al. -
Drought and Ecosystem Carbon Cycling
Agricultural and Forest Meteorology 151 (2011) 765–773 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Review Drought and ecosystem carbon cycling M.K. van der Molen a,b,∗, A.J. Dolman a, P. Ciais c, T. Eglin c, N. Gobron d, B.E. Law e, P. Meir f, W. Peters b, O.L. Phillips g, M. Reichstein h, T. Chen a, S.C. Dekker i, M. Doubková j, M.A. Friedl k, M. Jung h, B.J.J.M. van den Hurk l, R.A.M. de Jeu a, B. Kruijt m, T. Ohta n, K.T. Rebel i, S. Plummer o, S.I. Seneviratne p, S. Sitch g, A.J. Teuling p,r, G.R. van der Werf a, G. Wang a a Department of Hydrology and Geo-Environmental Sciences, Faculty of Earth and Life Sciences, VU-University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands b Meteorology and Air Quality Group, Wageningen University and Research Centre, P.O. box 47, 6700 AA Wageningen, The Netherlands c LSCE CEA-CNRS-UVSQ, Orme des Merisiers, F-91191 Gif-sur-Yvette, France d Institute for Environment and Sustainability, EC Joint Research Centre, TP 272, 2749 via E. Fermi, I-21027 Ispra, VA, Italy e College of Forestry, Oregon State University, Corvallis, OR 97331-5752 USA f School of Geosciences, University of Edinburgh, EH8 9XP Edinburgh, UK g School of Geography, University of Leeds, Leeds LS2 9JT, UK h Max Planck Institute for Biogeochemistry, PO Box 100164, D-07701 Jena, Germany i Department of Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, PO Box 80115, 3508 TC Utrecht, The Netherlands j Institute of Photogrammetry and Remote Sensing, Vienna University of Technology, Gusshausstraße 27-29, 1040 Vienna, Austria k Geography and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA 02215, USA l Department of Global Climate, Royal Netherlands Meteorological Institute, P.O. -
Grassland to Shrubland State Transitions Enhance Carbon Sequestration in the Northern Chihuahuan Desert
Global Change Biology Global Change Biology (2015) 21, 1226–1235, doi: 10.1111/gcb.12743 Grassland to shrubland state transitions enhance carbon sequestration in the northern Chihuahuan Desert M. D. PETRIE1 ,S.L.COLLINS1 ,A.M.SWANN2 ,P.L.FORD3 andM.E. LITVAK1 1Department of Biology, University of New Mexico, Albuquerque, New Mexico, USA, 2Department of Biology, Sevilleta LTER, University of New Mexico, Albuquerque, New Mexico, USA, 3USDA Forest Service, Rocky Mountain Research Station, Albuquerque, New Mexico, USA Abstract The replacement of native C4-dominated grassland by C3-dominated shrubland is considered an ecological state tran- sition where different ecological communities can exist under similar environmental conditions. These state transi- tions are occurring globally, and may be exacerbated by climate change. One consequence of the global increase in woody vegetation may be enhanced ecosystem carbon sequestration, although the responses of arid and semiarid ecosystems may be highly variable. During a drier than average period from 2007 to 2011 in the northern Chihuahuan À2 À1 Desert, we found established shrubland to sequester 49 g C m yr on average, while nearby native C4 grassland À À was a net source of 31 g C m 2 yr 1 over this same period. Differences in C exchange between these ecosystems were pronounced – grassland had similar productivity compared to shrubland but experienced higher C efflux via ecosys- tem respiration, while shrubland was a consistent C sink because of a longer growing season and lower ecosystem respiration. At daily timescales, rates of carbon exchange were more sensitive to soil moisture variation in grassland than shrubland, such that grassland had a net uptake of C when wet but lost C when dry. -
Model-Based Analysis of the Impact of Diffuse
Agricultural and Forest Meteorology 249 (2018) 377–389 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Model-based analysis of the impact of diffuse radiation on CO2 exchange in a T temperate deciduous forest Min S. Leea, David Y. Hollingerb, Trevor F. Keenanc, Andrew P. Ouimetted, Scott V. Ollingerd, ⁎ Andrew D. Richardsona,e,f, a Harvard University, Department of Organismic and Evolutionary Biology, 26 Oxford Street, Cambridge, MA 02138, USA b USDA Forest Service, Northern Research Station, 271 Mast Rd, Durham, NH 03824, USA c Climate and Ecosystem Sciences Division, Lawrence Berkeley National Lab., 1 Cyclotron Rd., Berkeley, CA 94720, USA d University of New Hampshire, Earth Systems Research Center, 8 College Rd, Durham, NH 03824, USA e Northern Arizona University, School of Informatics, Computing and Cyber Systems, PO Box 5693, Flagstaff, AZ 86011, USA f Northern Arizona University, Center for Ecosystem Science and Society, PO Box 5620, Flagstaff, AZ 86011, USA ARTICLE INFO ABSTRACT Keywords: Clouds and aerosols increase the fraction of global solar irradiance that is diffuse light. This phenomenon is Diffuse radiation known to increase the photosynthetic light use efficiency (LUE) of closed-canopy vegetation by redistributing Light use efficiency photosynthetic photon flux density (400–700 nm) from saturated, sunlit leaves at the top of the canopy, to Eddy covariance shaded leaves deeper in the canopy. We combined a process-based carbon cycle model with 10 years of eddy Net ecosystem exchange covariance carbon flux measurements and other ancillary data sets to assess 1) how this LUE enhancement Deciduous forest influences interannual variation in carbon uptake, and 2) how errors in modeling diffuse fraction affect pre- Canopy photosynthesis dictions of carbon uptake. -
Respiration from a Tropical Forest Ecosystem: Partitioning of Sources and Low Carbon Use Efficiency
Ecological Applications, 14(4) Supplement, 2004, pp. S72±S88 q 2004 by the Ecological Society of America RESPIRATION FROM A TROPICAL FOREST ECOSYSTEM: PARTITIONING OF SOURCES AND LOW CARBON USE EFFICIENCY JEFFREY Q. CHAMBERS,1,2,4 EDGARD S. TRIBUZY,2 LIGIA C. TOLEDO,2 BIANCA F. C RISPIM,2 NIRO HIGUCHI,2 JOAQUIM DOS SANTOS,2 ALESSANDRO C. ARAUÂ JO,2 BART KRUIJT,3 ANTONIO D. NOBRE,2 AND SUSAN E. TRUMBORE1 1University of California, Earth System Sciences, Irvine, California 92697 USA 2Instituto Nacional de Pesquisas da AmazoÃnia, C.P. 478, Manaus, Amazonas, Brazil, 69011-970 3Alterra, University of Wageningen, Alterra, 6700 AA Wageningen, The Netherlands Abstract. Understanding how tropical forest carbon balance will respond to global change requires knowledge of individual heterotrophic and autotrophic respiratory sources, together with factors that control respiratory variability. We measured leaf, live wood, and soil respiration, along with additional environmental factors over a 1-yr period in a Central Amazon terra ®rme forest. Scaling these ¯uxes to the ecosystem, and combining our data with results from other studies, we estimated an average total ecosystem respiration (Reco) of 7.8 mmol´m22´s21. Average estimates (per unit ground area) for leaf, wood, soil, total heterotrophic, and total autotrophic respiration were 2.6, 1.1, 3.2, 5.6, and 2.2 mmol´m22´s21, respectively. Comparing autotrophic respiration with net primary production (NPP) esti- mates indicated that only ;30% of carbon assimilated in photosynthesis was used to con- struct new tissues, with the remaining 70% being respired back to the atmosphere as autotrophic respiration. -
Interpreting, Measuring, and Modeling Soil Respiration
Biogeochemistry (2005) 73: 3–27 Ó Springer 2005 DOI 10.1007/s10533-004-5167-7 -1 Interpreting, measuring, and modeling soil respiration MICHAEL G. RYAN1,2,* and BEVERLY E. LAW3 1US Department of Agriculture-Forest Service, Rocky Mountain Research Station, 240 West Pros- pect Street, Fort Collins, CO 80526, USA; 2Affiliate Faculty, Department of Forest, Rangeland and Watershed Stewardship and Graduate Degree Program in Ecology, Colorado State University Fort Collins, CO 80523, USA; 3Department of Forest Science, Oregon State University, 328 Richardson Hall, Corvallis, OR 97331, USA; *Author for correspondence (e-mail: [email protected]) Key words: Belowground carbon allocation, Carbon cycling, Carbon dioxide, CO2, Infrared gas analyzers, Methods, Soil carbon, Terrestrial ecosystems Abstract. This paper reviews the role of soil respiration in determining ecosystem carbon balance, and the conceptual basis for measuring and modeling soil respiration. We developed it to provide background and context for this special issue on soil respiration and to synthesize the presentations and discussions at the workshop. Soil respiration is the largest component of ecosystem respiration. Because autotrophic and heterotrophic activity belowground is controlled by substrate availability, soil respiration is strongly linked to plant metabolism, photosynthesis and litterfall. This link dominates both base rates and short-term fluctuations in soil respiration and suggests many roles for soil respiration as an indicator of ecosystem metabolism. However, the strong links between above and belowground processes complicate using soil respiration to understand changes in ecosystem carbon storage. Root and associated mycorrhizal respiration produce roughly half of soil respiration, with much of the remainder derived from decomposition of recently produced root and leaf litter. -
Ecosystem Diversity Report George Washington National Forest Draft EIS April 2011
Appendix E Ecosystem Diversity Report George Washington National Forest Draft EIS April 2011 U.S. Department of Agriculture Forest Service Southern Region Ecosystem Diversity Report George Washington National Forest April 2011 Appendix E Ecosystem Diversity Report George Washington National Forest Draft EIS April 2011 Table of Contents TABLE OF CONTENTS .............................................................................................................. I 1.0 INTRODUCTION.................................................................................................................. 1 2.0 ECOLOGICAL SUSTAINABILITY EVALUATION PROCESS ................................... 3 3.0 ECOLOGICAL SYSTEMS .................................................................................................. 7 3.1 Background and Distribution of Ecosystems ..................................................................................................... 7 North-Central Appalachian Acidic Swamp ............................................................................................................ 10 3.2 Descriptions of the Ecological Systems ............................................................................................................ 10 3.2.1 Spruce Forest: Central and Southern Appalachian Spruce-Fir Forest .......................................................... 10 3.2.2 Northern Hardwood Forest : Appalachian (Hemlock)- Northern Hardwood Forest ..................................... 11 3.2.3 Cove Forest: Southern and Central -
5Th Grade Life Science: Ecosystems Unit
5th Grade Life Science: Ecosystems Unit Developed for Chapel Hill Carrboro City Schools Northside Elementary School Outdoor Wonder & Learning (OWL) Initiative Unless otherwise noted, activities written by: Lauren Greene, Sarah Yelton, Dana Haine, & Toni Stadelman Center for Public Engagement with Science UNC Institute for the Environment In collaboration with 5th grade teachers at Northside Elementary School: Michelle Gay, Daila Patrick, & Elizabeth Symons ACKNOWLEDGEMENTS Many thanks to Dan Schnitzer, Coretta Sharpless, Kirtisha Jones and the many wonderful teachers and support staff at Northside Elementary for their participation in and support of the Northside OWL Initiative. Thanks also to Shelby Brown for her invaluable assistance compiling, editing, and proofreading the curriculum. Instructional materials and supplies to promote STEM-based outdoor learning were instrumental to the successful implementation of this curriculum. The purchase of these materials was made possible with funding provided by the Duke Energy Foundation to Chapel Hill-Carrboro City Schools. Curriculum developed June 2018 – July 2019 For more information, contact: Sarah Yelton, Environmental Education & Citizen Science Program Manager UNC Institute for the Environment Center for Public Engagement with Science [email protected] 5th Grade Ecosystems Unit Northside Outdoor Wonder & Learning Initiative Overarching Unit Question How and why do organisms (including humans) interact with their environment, and what are the effects of these interactions? Essential Questions Arc 1: How can I describe and compare different ecosystems? Arc 2: How is energy transferred through an ecosystem? How can I explain the interconnected relationships between organisms and their environments? Transfer Goals o Use scientific thinking to understand the relationships and complexities of the world around them. -
Global Satellite-Driven Estimates of Heterotrophic Respiration
Biogeosciences, 16, 2269–2284, 2019 https://doi.org/10.5194/bg-16-2269-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Global satellite-driven estimates of heterotrophic respiration Alexandra G. Konings1, A. Anthony Bloom2, Junjie Liu2, Nicholas C. Parazoo2, David S. Schimel2, and Kevin W. Bowman2 1Department of Earth System Science, Stanford University, Stanford, CA 94305, USA 2NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA Correspondence: Alexandra G. Konings ([email protected]) Received: 31 October 2018 – Discussion started: 15 November 2018 Revised: 4 April 2019 – Accepted: 10 May 2019 – Published: 4 June 2019 Abstract. While heterotrophic respiration (Rh) makes up to bottom-up estimates of annual heterotrophic respiration, about a quarter of gross global terrestrial carbon fluxes, using new uncertainty estimates that partially account for it remains among the least-observed carbon fluxes, partic- sampling and model errors. Top-down heterotrophic respira- ularly outside the midlatitudes. In situ measurements col- tion estimates are higher than those from bottom-up upscal- lected in the Soil Respiration Database (SRDB) number only ing everywhere except at high latitudes and are 30 % greater a few hundred worldwide. Similarly, only a single data- overall (43.6 Pg C yr−1 vs. 33.4 Pg C yr−1). The uncertainty driven wall-to-wall estimate of annual average heterotrophic ranges of both methods are comparable, except poleward of respiration exists, based on bottom-up upscaling of SRDB 45◦ N, where bottom-up uncertainties are greater. The ra- measurements using an assumed functional form to account tio of top-down heterotrophic to total ecosystem respiration for climate variability. -
Ecosystem Ecology Living Organisms and Their Non Living (Abiotic) Environment Are Interrelated and Interact with Each Other
1 | P a g e Ecosystem Ecology Living organisms and their non living (abiotic) environment are interrelated and interact with each other. The term ‘ecosystem’ was proposed by A. G. Tansley and it was defined as the system resulting from the integration of all living and non living factors of the environment. Some parallel terms such as biocoenosis, microcosm, geobiocoenosis, holecoen, biosystem, bioenert body and ecosom were used for each ecological systems. However, the term ‘ecosystem’ is most preferred, where ‘eco’ stands for the environment, and ‘system’ stands for an interacting, interdependent complex. Any unit that includes all the organisms, i.e. communities, in a given area, interacts with the physical environment so that a flow of energy leads to a clearly defined trophic structure, biotic diversity and material cycle within the system, is known as an ecological system or ecosystem. It is usually an open system with regular but variable influx and loss of materials and energy. It is a basic functional unit with unlimited boundaries. Types of ecosystems The ecosystems can be broadly divided into the following two types; 1. Natural ecosystems 2. Artificial (man cultured ecosystems Natural ecosystems The ecosystems which are self-operating under natural conditions with any interference by man, are known as natural ecosystems. These ecosystems may be classified as follows: 1. Terrestrial ecosystems, e.g. Forests, grasslands and deserts 2. Aquatic ecosystems, which may be further classified as i) Freshwater: ecosystem, which in turn is divided into lentic (running water like streams, springs, rivers, etc.) and lentic (standing water like lakes, bonds, pools, swamps, ditches, etc.) ii) Marine ecosystem, e.g. -
Distribution Mapping of World Grassland Types A
Journal of Biogeography (J. Biogeogr.) (2014) SYNTHESIS Distribution mapping of world grassland types A. P. Dixon1*, D. Faber-Langendoen2, C. Josse2, J. Morrison1 and C. J. Loucks1 1World Wildlife Fund – United States, 1250 ABSTRACT 24th Street NW, Washington, DC 20037, Aim National and international policy frameworks, such as the European USA, 2NatureServe, 4600 N. Fairfax Drive, Union’s Renewable Energy Directive, increasingly seek to conserve and refer- 7th Floor, Arlington, VA 22203, USA ence ‘highly biodiverse grasslands’. However, to date there is no systematic glo- bal characterization and distribution map for grassland types. To address this gap, we first propose a systematic definition of grassland. We then integrate International Vegetation Classification (IVC) grassland types with the map of Terrestrial Ecoregions of the World (TEOW). Location Global. Methods We developed a broad definition of grassland as a distinct biotic and ecological unit, noting its similarity to savanna and distinguishing it from woodland and wetland. A grassland is defined as a non-wetland type with at least 10% vegetation cover, dominated or co-dominated by graminoid and forb growth forms, and where the trees form a single-layer canopy with either less than 10% cover and 5 m height (temperate) or less than 40% cover and 8 m height (tropical). We used the IVC division level to classify grasslands into major regional types. We developed an ecologically meaningful spatial cata- logue of IVC grassland types by listing IVC grassland formations and divisions where grassland currently occupies, or historically occupied, at least 10% of an ecoregion in the TEOW framework. Results We created a global biogeographical characterization of the Earth’s grassland types, describing approximately 75% of IVC grassland divisions with ecoregions. -
Chapter 10. Amphibians of the Palaearctic Realm
CHAPTER 10. AMPHIBIANS OF THE PALAEARCTIC REALM Figure 1. Summary of Red List categories Brandon Anthony, J.W. Arntzen, Sherif Baha El Din, Wolfgang Böhme, Dan Palaearctic Realm contains 6% of all globally threatened amphibians. The Palaearctic accounts for amphibians in the Palaearctic Realm. CogĄlniceanu, Jelka Crnobrnja-Isailovic, Pierre-André Crochet, Claudia Corti, for only 3% of CR species and 5% of the EN species, but 9% of the VU species. Hence, on the The percentage of species in each category Richard Griffiths, Yoshio Kaneko, Sergei Kuzmin, Michael Wai Neng Lau, basis of current knowledge, threatened Palaearctic amphibians are more likely to be in a lower is also given. Pipeng Li, Petros Lymberakis, Rafael Marquez, Theodore Papenfuss, Juan category of threat, when compared with the global distribution of threatened species amongst Manuel Pleguezuelos, Nasrullah Rastegar, Benedikt Schmidt, Tahar Slimani, categories. The percentage of DD species, 13% (62 species), is also much less than the global Max Sparreboom, ùsmail Uøurtaû, Yehudah Werner and Feng Xie average of 23%, which is not surprising given that parts of the region have been well surveyed. Red List Category Number of species Nevertheless, the percentage of DD species is much higher than in the Nearctic. Extinct (EX) 2 Two of the world’s 34 documented amphibian extinctions have occurred in this region: the Extinct in the Wild (EW) 0 THE GEOGRAPHIC AND HUMAN CONTEXT Hula Painted Frog Discoglossus nigriventer from Israel and the Yunnan Lake Newt Cynops Critically Endangered (CR) 13 wolterstorffi from around Kunming Lake in Yunnan Province, China. In addition, one Critically Endangered (EN) 40 The Palaearctic Realm includes northern Africa, all of Europe, and much of Asia, excluding Endangered species in the Palaearctic Realm is considered possibly extinct, Scutiger macu- Vulnerable (VU) 58 the southern extremities of the Arabian Peninsula, the Indian Subcontinent (south of the latus from central China.