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Fernández-Martínez M, Barquín J, Bonada N, Cantonati M, Churro C, Corbera J, Delgado C, Dulsat-Masvidal M, Garcia G, Margalef O, Pascual R, Peñuelas J, Preece C, Sabater F, Seiler H, Zamora-Marín JM, Romero E. Mediterranean springs: Keystone ecosystems and biodiversity refugia threatened by global change. Glob Chang Biol 2024; 30:e16997. [PMID: 37937346 DOI: 10.1111/gcb.16997] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/02/2023] [Revised: 09/29/2023] [Accepted: 10/09/2023] [Indexed: 11/09/2023]
Abstract
Mediterranean spring ecosystems are unique habitats at the interface between surface water and groundwater. These ecosystems support a remarkable array of biodiversity and provide important ecological functions and ecosystem services. Spring ecosystems are influenced by abiotic, biotic, and anthropogenic factors such as the lithology of their draining aquifers, their climate, and the land use of their recharge area, all of which affect the water chemistry of the aquifer and the spring discharges. One of the most relevant characteristics of spring ecosystems is the temporal stability of environmental conditions, including physicochemical features of the spring water, across seasons and years. This stability allows a wide range of species to benefit from these ecosystems (particularly during dry periods), fostering an unusually high number of endemic species. However, global change poses important threats to these freshwater ecosystems. Changes in temperature, evapotranspiration, and precipitation patterns can alter the water balance and chemistry of spring water. Eutrophication due to agricultural practices and emergent pollutants, such as pharmaceuticals, personal care products, and pesticides, is also a growing concern for the preservation of spring biodiversity. Here, we provide a synthesis of the main characteristics and functioning of Mediterranean spring ecosystems. We then describe their ecological value and biodiversity patterns and highlight the main risks these ecosystems face. Moreover, we identify existing knowledge gaps to guide future research in order to fully uncover the hidden biodiversity within these habitats and understand the main drivers that govern them. Finally, we provide a brief summary of recommended actions that should be taken to effectively manage and preserve Mediterranean spring ecosystems for future generations. Even though studies on Mediterranean spring ecosystems are still scarce, our review shows there are sufficient data to conclude that their future viability as functional ecosystems is under severe threat.
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Affiliation(s)
- M Fernández-Martínez
- CREAF, Campus de Bellaterra (UAB), Cerdanyola del Vallès, Spain
- Delegació de la Serralada Litoral Central - ICHN, Mataró, Spain
- Department of Evolutionary Biology, Ecology and Environmental Sciences (BEECA-UB), University of Barcelona, Barcelona, Spain
| | - J Barquín
- Instituto de Hidráulica Ambiental de la Universidad de Cantabria (IHCantabria), Santander, Spain
| | - N Bonada
- Freshwater Ecology, Hydrology and Management Research Group (FEHM), Department of Evolutionary Biology, Ecology and Environmental Sciences, University of Barcelona, Barcelona, Spain
- Institut de Recerca de la Biodiversitat (IRBio), University of Barcelona, Barcelona, Spain
| | - M Cantonati
- BIOME Lab, Department of Biological, Geological and Environmental Sciences - BiGeA, Alma Mater Studiorum - University of Bologna, Bologna, Italy
| | - C Churro
- Laboratory of Virology and Molecular Biology and Laboratory of Phytoplankton, Department of the Sea and Marine Resources, Portuguese Institute for the Sea and Atmosphere (IPMA), Lisbon, Portugal
- Blue Biotechnology and Ecotoxicology (BBE), CIIMAR - Centro Interdisciplinar de Investigação Marinha e Ambiental, Universidade do Porto, Matosinhos, Portugal
| | - J Corbera
- Delegació de la Serralada Litoral Central - ICHN, Mataró, Spain
| | - C Delgado
- Departamento de Ecoloxía e Bioloxía Animal, Facultade de Ciencias, Universidade de Vigo, Vigo, Spain
| | - M Dulsat-Masvidal
- IDAEA-CSIC, Institute of Environmental Assessment and Water Research, Barcelona, Spain
| | - G Garcia
- BioSciCat, The Catalan Society of Sciences for the Conservation of Biodiversity, Tarragona, Spain
| | - O Margalef
- CREAF, Campus de Bellaterra (UAB), Cerdanyola del Vallès, Spain
- Departament de Dinàmica de la Terra i de l'Oceà, GRC RISKNAT, UB-Geomodels, Facultat de Ciències de la Terra, University of Barcelona, Barcelona, Spain
| | - R Pascual
- BioSciCat, The Catalan Society of Sciences for the Conservation of Biodiversity, Tarragona, Spain
| | - J Peñuelas
- CREAF, Campus de Bellaterra (UAB), Cerdanyola del Vallès, Spain
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Barcelona, Spain
| | - C Preece
- Institute of Agrifood Research and Technology (IRTA), Sustainability in Biosystems Programme, Barcelona, Spain
| | - F Sabater
- CREAF, Campus de Bellaterra (UAB), Cerdanyola del Vallès, Spain
- Delegació de la Serralada Litoral Central - ICHN, Mataró, Spain
- Department of Evolutionary Biology, Ecology and Environmental Sciences (BEECA-UB), University of Barcelona, Barcelona, Spain
| | - H Seiler
- Vegetation Ecology, Institute of Natural Resource Sciences (IUNR), Zurich University of Applied Sciences (ZHAW), Wädenswil, Switzerland
| | - J M Zamora-Marín
- Department of Applied Biology, Centro de Investigación e Innovación Agroalimentaria (CIAGRO-UMH), Miguel Hernández University of Elche, Elche, Spain
| | - E Romero
- CREAF, Campus de Bellaterra (UAB), Cerdanyola del Vallès, Spain
- Department of Evolutionary Biology, Ecology and Environmental Sciences (BEECA-UB), University of Barcelona, Barcelona, Spain
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2
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Fernández-Martínez M, Sardans J, Sayol F, LaMontagne JM, Bogdziewicz M, Collalti A, Hacket-Pain A, Vacchiano G, Espelta JM, Peñuelas J, Janssens IA. Reply to: Nutrient scarcity cannot cause mast seeding. Nat Plants 2020; 6:763-765. [PMID: 32572211 DOI: 10.1038/s41477-020-0703-6] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/15/2020] [Accepted: 05/20/2020] [Indexed: 06/11/2023]
Affiliation(s)
- M Fernández-Martínez
- Research Group PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Antwerp, Belgium.
| | - J Sardans
- Global Ecology Unit, CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | - F Sayol
- Department of Biological and Environmental Sciences, University of Gothenburg, Gothenburg, Sweden
- Gothenburg Global Biodiversity Centre, Gothenburg, Sweden
| | - J M LaMontagne
- Department of Biological Sciences, DePaul University, Chicago, IL, USA
| | - M Bogdziewicz
- Department of Systematic Zoology, Faculty of Biology, Adam Mickiewicz University, Poznań, Poland
| | - A Collalti
- Institute for Agriculture and Forestry Systems in the Mediterranean, National Research Council of Italy (CNR-ISAFOM), Perugia, Italy
- Department of Innovation in Biological, Agro-food and Forest Systems, University of Tuscia, Viterbo, Italy
| | - A Hacket-Pain
- Department of Geography and Planning, School of Environmental Sciences, University of Liverpool, Liverpool, UK
| | | | | | - J Peñuelas
- Global Ecology Unit, CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | - I A Janssens
- Research Group PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Antwerp, Belgium
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3
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Thomas HJD, Bjorkman AD, Myers-Smith IH, Elmendorf SC, Kattge J, Diaz S, Vellend M, Blok D, Cornelissen JHC, Forbes BC, Henry GHR, Hollister RD, Normand S, Prevéy JS, Rixen C, Schaepman-Strub G, Wilmking M, Wipf S, Cornwell WK, Beck PSA, Georges D, Goetz SJ, Guay KC, Rüger N, Soudzilovskaia NA, Spasojevic MJ, Alatalo JM, Alexander HD, Anadon-Rosell A, Angers-Blondin S, Te Beest M, Berner LT, Björk RG, Buchwal A, Buras A, Carbognani M, Christie KS, Collier LS, Cooper EJ, Elberling B, Eskelinen A, Frei ER, Grau O, Grogan P, Hallinger M, Heijmans MMPD, Hermanutz L, Hudson JMG, Johnstone JF, Hülber K, Iturrate-Garcia M, Iversen CM, Jaroszynska F, Kaarlejarvi E, Kulonen A, Lamarque LJ, Lantz TC, Lévesque E, Little CJ, Michelsen A, Milbau A, Nabe-Nielsen J, Nielsen SS, Ninot JM, Oberbauer SF, Olofsson J, Onipchenko VG, Petraglia A, Rumpf SB, Shetti R, Speed JDM, Suding KN, Tape KD, Tomaselli M, Trant AJ, Treier UA, Tremblay M, Venn SE, Vowles T, Weijers S, Wookey PA, Zamin TJ, Bahn M, Blonder B, van Bodegom PM, Bond-Lamberty B, Campetella G, Cerabolini BEL, Chapin FS, Craine JM, Dainese M, Green WA, Jansen S, Kleyer M, Manning P, Niinemets Ü, Onoda Y, Ozinga WA, Peñuelas J, Poschlod P, Reich PB, Sandel B, Schamp BS, Sheremetiev SN, de Vries FT. Global plant trait relationships extend to the climatic extremes of the tundra biome. Nat Commun 2020; 11:1351. [PMID: 32165619 PMCID: PMC7067758 DOI: 10.1038/s41467-020-15014-4] [Citation(s) in RCA: 28] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/17/2018] [Accepted: 02/11/2020] [Indexed: 11/09/2022] Open
Abstract
The majority of variation in six traits critical to the growth, survival and reproduction of plant species is thought to be organised along just two dimensions, corresponding to strategies of plant size and resource acquisition. However, it is unknown whether global plant trait relationships extend to climatic extremes, and if these interspecific relationships are confounded by trait variation within species. We test whether trait relationships extend to the cold extremes of life on Earth using the largest database of tundra plant traits yet compiled. We show that tundra plants demonstrate remarkably similar resource economic traits, but not size traits, compared to global distributions, and exhibit the same two dimensions of trait variation. Three quarters of trait variation occurs among species, mirroring global estimates of interspecific trait variation. Plant trait relationships are thus generalizable to the edge of global trait-space, informing prediction of plant community change in a warming world.
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Affiliation(s)
- H J D Thomas
- School of Geosciences, University of Edinburgh, Edinburgh, EH9 3FF, Scotland, UK.
| | - A D Bjorkman
- School of Geosciences, University of Edinburgh, Edinburgh, EH9 3FF, Scotland, UK
- Department of Biological and Environmental Sciences, University of Gothenburg, Medicinaregatan 18, 40530, Gothenburg, Sweden
- Gothenburg Global Biodiversity Centre, Carl Skottsbergs gata 22B, 41319, Gothenburg, Sweden
| | - I H Myers-Smith
- School of Geosciences, University of Edinburgh, Edinburgh, EH9 3FF, Scotland, UK
| | - S C Elmendorf
- Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, 80309-0450, USA
| | - J Kattge
- Max Planck Institute for Biogeochemistry, 07701, Jena, Germany
- German Centre for Integrative Biodiversity Research (iDiv), Halle-Jena-Leipzig, Deutscher Platz 5e, 04103, Leipzig, Germany
| | - S Diaz
- Instituto Multidisciplinario de Biología Vegetal (IMBIV), CONICET, Av.Velez Sarsfield 299, Cordoba, Argentina
- FCEFyN, Universidad Nacional de Córdoba, Av. Vélez Sarsfield 299, X5000JJC, Córdoba, Argentina
| | - M Vellend
- Département de Biologie, Université de Sherbrooke, 2500, boul. de l'Université Sherbrooke, Québec, J1K 2R1, Canada
| | - D Blok
- Dutch Research Council, (NWO), Postbus 93460, 2509 AL, Den Haag, The Netherlands
| | - J H C Cornelissen
- Systems Ecology, Department of Ecological Science, Vrije Universiteit, De Boelelaan 1085, 1081 HV, Amsterdam, The Netherlands
| | - B C Forbes
- Arctic Centre, University of Lapland, 96101, Rovaniemi, Finland
| | - G H R Henry
- Department of Geography, University of British Columbia, 1984 West Mall, Vancouver, V6T 1Z2, Canada
| | - R D Hollister
- Biology Department, Grand Valley State University, 1 Campus Drive, 3300a Kindschi Hall of Science, Allendale, Michigan, USA
| | - S Normand
- Department of Biology, Aarhus University, Ny Munkegade 114-116, DK-8000, Aarhus C, Denmark
| | - J S Prevéy
- U.S. Geological Survey, Fort Collins Science Center, Fort Collins, CO, 80526, USA
- WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260, Davos Dorf, Switzerland
| | - C Rixen
- WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260, Davos Dorf, Switzerland
| | - G Schaepman-Strub
- Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland
| | - M Wilmking
- Institute of Botany and Landscape Ecology, Greifswald University, Soldmannstraße 15, 17487, Greifswald, Germany
| | - S Wipf
- WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260, Davos Dorf, Switzerland
- Swiss National Park, Runatsch 124, Chastè Planta-Wildenberg, 7530, Zernez, Switzerland
| | - W K Cornwell
- Ecology and Evolution Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, 2052, Australia
| | - P S A Beck
- European Commission, Joint Research Centre, Via Enrico Fermi, 2749, Ispra, 21027, Italy
| | - D Georges
- School of Geosciences, University of Edinburgh, Edinburgh, EH9 3FF, Scotland, UK
- International Agency for Research in Cancer, 150 Cours Albert Thomas, 69372, Lyon, France
| | - S J Goetz
- School of Informatics, Computing and Cyber Systems, Northern Arizona University, Flagstaff, 1295S Knoles Dr, AZ, 86011, USA
| | - K C Guay
- Bigelow Laboratory for Ocean Sciences, 60 Bigelow Dr, East Boothbay, Maine, 04544, USA
| | - N Rüger
- German Centre for Integrative Biodiversity Research (iDiv), Halle-Jena-Leipzig, Deutscher Platz 5e, 04103, Leipzig, Germany
- Smithsonian Tropical Research Institute, Luis Clement Avenue, Bldg. 401 Tupper, Balboa Ancón, Panama
| | - N A Soudzilovskaia
- Environmental Biology Department, Institute of Environmental Sciences, Leiden University, 2300 RA, Leiden, The Netherlands
| | - M J Spasojevic
- Department of Evolution, Ecology, and Organismal Biology, University of California Riverside, Life Sciences Building, Eucalyptus Dr #2710, Riverside, CA, 92521, USA
| | - J M Alatalo
- Department of Biological and Environmental Sciences, College of Arts and Sciences, Qatar University, P.O. Box 2713, Doha, Qatar
- Environmental Science Center, Qatar University, Doha, Qatar
| | - H D Alexander
- Department of Forestry, Forest and Wildlife Research Center, Mississippi State University, Mississippi, MS, 39762, USA
| | - A Anadon-Rosell
- Institute of Botany and Landscape Ecology, Greifswald University, Soldmannstraße 15, 17487, Greifswald, Germany
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of Barcelona, Diagonal, 643, 08028, Barcelona, Spain
- Biodiversity Research Institute, University of Barcelona, Av. Diagonal, 645, 08028, Barcelona, Spain
| | - S Angers-Blondin
- School of Geosciences, University of Edinburgh, Edinburgh, EH9 3FF, Scotland, UK
| | - M Te Beest
- Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, Heidelberglaan 8, 3584 CS, Utrecht, The Netherlands
- Department of Ecology and Environmental Science Umeå University, SE-901 87, Umeå, Sweden
| | - L T Berner
- School of Informatics, Computing and Cyber Systems, Northern Arizona University, Flagstaff, 1295S Knoles Dr, AZ, 86011, USA
| | - R G Björk
- Department of Earth Sciences, University of Gothenburg, 405 30, Gothenburg, Sweden
- Gothenburg Global Biodiversity Centre, SE-405 30, Gothenburg, Sweden
| | - A Buchwal
- Adam Mickiewicz University, Institute of Geoecology and Geoinformation, B. Krygowskiego 10, 61-680, Poznan, Poland
- University of Alaska Anchorage, 3211 Providence Dr, Anchorage, AK, 99508, USA
| | - A Buras
- Land Surface-Atmosphere Interactions, Technische Universität München, Hans-Carl-von-Carlowitz Platz 2, 85354, Freising, Germany
| | - M Carbognani
- Deptartment of Chemistry, Life Sciences and Environmental Sustainability, University of Parma, Parco Area delle Scienze, 11/a, 43124, Parma, Italy
| | - K S Christie
- Alaska Department of Fish and Game, 333 Raspberry Rd, Anchorage, AK, 99518, USA
| | - L S Collier
- Department of Biology, Memorial University, St. John's, Newfoundland and Labrador, A1C 5S7, Canada
| | - E J Cooper
- Deptartment of Arctic and Marine Biology, Faculty of Bioscences Fisheries and Economics, UiT-The Arctic University of Norway, Tromsø, Norway
| | - B Elberling
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark
| | - A Eskelinen
- German Centre for Integrative Biodiversity Research (iDiv), Halle-Jena-Leipzig, Deutscher Platz 5e, 04103, Leipzig, Germany
- Department of Physiological Diversity, Helmholtz Centre for Environmental Research-UFZ, Deutscher Platz 5e, 04103, Leipzig, Germany
- Department of Ecology and Genetics, University of Oulu, Pentti Kaiteran katu 1, Linnanmaa, Oulu, Finland
| | - E R Frei
- Department of Geography, University of British Columbia, 1984 West Mall, Vancouver, V6T 1Z2, Canada
- Swiss Federal Research Institute WSL, Zürcherstrasse 111, 8903, Birmensdorf, Switzerland
| | - O Grau
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, 08193 Cerdanyola del Vallès Bellaterra, Catalonia, Spain
- CREAF, 08193 Cerdanyola del Vallès, Catalonia, Spain
- Cirad, UMR EcoFoG (AgroParisTech, CNRS, Inra, Univ Antilles, Univ Guyane), Campus Agronomique, 97310, Kourou, French Guiana
| | - P Grogan
- Department of Biology, Queen's University, Biosciences Complex, 116 Barrie St., Kingston, ON, K7L 3N6, Canada
| | - M Hallinger
- Biology Department, Swedish Agricultural University (SLU), SE-750 07, Uppsala, Sweden
| | - M M P D Heijmans
- Plant Ecology and Nature Conservation Group, Wageningen University and Research, 6700 AA, Wageningen, The Netherlands
| | - L Hermanutz
- Department of Biology, Memorial University, St. John's, Newfoundland and Labrador, A1C 5S7, Canada
| | - J M G Hudson
- British Columbia Public Service, Vancouver, Canada
| | - J F Johnstone
- Department of Biology, University of Saskatchewan, Saskatoon, SK, S7N 5E2, Canada
| | - K Hülber
- Department of Botany and Biodiversity Research, University of Vienna, Rennweg 14, 1030, Vienna, Austria
| | - M Iturrate-Garcia
- Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland
| | - C M Iversen
- Climate Change Science Institute and Environmental Sciences Division, Oak Ridge National Laboratory, 1 Bethel Valley Road, Oak Ridge, TN, 37831-6134, USA
| | - F Jaroszynska
- WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260, Davos Dorf, Switzerland
- Department of Biological Sciences and Bjerknes Centre for Climate Research, University of Bergen, N-5020, Bergen, Norway
- Institute of Biological and Environmental Sciences, University of Aberdeen, Aberdeen, AB24 3FX, Scotland, UK
| | - E Kaarlejarvi
- Biodiversity Research Institute, University of Barcelona, Av. Diagonal, 645, 08028, Barcelona, Spain
- Department of Biology, Vrije Universiteit Brussel (VUB), Pleinlaan 2, 1050, Elsene, Brussles, Belgium
- Organismal and Evolutionary Biology Research Programme, University of Helsinki, PO Box, 65, FI-00014, Helsinki, Finland
| | - A Kulonen
- WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260, Davos Dorf, Switzerland
| | - L J Lamarque
- Département des Sciences de l'environnement et Centre d'études nordiques, Université du Québec à Trois-Rivières, 3351, boul. des Forges, Québec, Canada
| | - T C Lantz
- School of Environmental Studies, University of Victoria, David Turpin Building, B243, Victoria, BC, Canada
| | - E Lévesque
- Département des Sciences de l'environnement et Centre d'études nordiques, Université du Québec à Trois-Rivières, 3351, boul. des Forges, Québec, Canada
| | - C J Little
- Department of Evolutionary Biology and Environmental Studies, University of Zurich, Winterthurerstrasse 190, 8057, Zurich, Switzerland
- Department of Aquatic Ecology, Eawag, the Swiss Federal Institute for Aquatic Science and Technology, Überlandstrasse 133, CH-8600, Duebendorf, Switzerland
| | - A Michelsen
- Center for Permafrost (CENPERM), Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350, Copenhagen K, Denmark
- Department of Biology, University of Copenhagen, Terrestrial Ecology Section, Universitetsparken 15, DK-2100, Copenhagen Ø, Denmark
| | - A Milbau
- Research Institute for Nature and Forest (INBO), Havenlaan 88 bus 73, 1000, Brussels, Belgium
| | - J Nabe-Nielsen
- Department of Bioscience, Aarhus University, Frederiksborgvej 399, 4000, Roskilde, Denmark
| | - S S Nielsen
- Department of Biology, Aarhus University, Ny Munkegade 114-116, DK-8000, Aarhus C, Denmark
| | - J M Ninot
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of Barcelona, Diagonal, 643, 08028, Barcelona, Spain
- Biodiversity Research Institute, University of Barcelona, Av. Diagonal, 645, 08028, Barcelona, Spain
| | - S F Oberbauer
- Department of Biological Sciences, Florida International University, 11200S.W. 8th Street, Miami, FL, 33199, USA
| | - J Olofsson
- Department of Ecology and Environmental Science Umeå University, SE-901 87, Umeå, Sweden
| | - V G Onipchenko
- Department of Ecology and Plant Geography, Moscow State Lomonosov University, 119234, Moscow, 1-12 Leninskie Gory, Russia
| | - A Petraglia
- Deptartment of Chemistry, Life Sciences and Environmental Sustainability, University of Parma, Parco Area delle Scienze, 11/a, 43124, Parma, Italy
| | - S B Rumpf
- Department of Botany and Biodiversity Research, University of Vienna, Rennweg 14, 1030, Vienna, Austria
- Department of Ecology and Evolution, University of Lausanne, Bâtiment Biophore, Quartier UNIL-Sorge, 1015, Lausanne, Switzerland
| | - R Shetti
- Institute of Botany and Landscape Ecology, Greifswald University, Soldmannstraße 15, 17487, Greifswald, Germany
| | - J D M Speed
- Department of Natural History, NTNU University Museum, Norwegian University of Science and Technology, NO-7491, Trondheim, Norway
| | - K N Suding
- Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, 80309-0450, USA
| | - K D Tape
- Institute of Northern Engineering, University of Alaska, Engineering Learning and Innovation Facility (ELIF), Suite 240, 1764 Tanana Loop, Fairbanks, AK, 99775-5910, USA
| | - M Tomaselli
- Deptartment of Chemistry, Life Sciences and Environmental Sustainability, University of Parma, Parco Area delle Scienze, 11/a, 43124, Parma, Italy
| | - A J Trant
- School of Environment, Resources and Sustainability, University of Waterloo, 200 University Avenue West, Waterloo, ON, N2L 3G1, Canada
| | - U A Treier
- Department of Biology, Aarhus University, Ny Munkegade 114-116, DK-8000, Aarhus C, Denmark
| | - M Tremblay
- Département des Sciences de l'environnement et Centre d'études nordiques, Université du Québec à Trois-Rivières, 3351, boul. des Forges, Québec, Canada
| | - S E Venn
- Centre for Integrative Ecology, School of Life and Environmental Sciences, Deakin University, 75 Pigdons Rd, Waurn Ponds Victoria, 3216, Australia
| | - T Vowles
- Department of Earth Sciences, University of Gothenburg, 405 30, Gothenburg, Sweden
| | - S Weijers
- Department of Geography, University of Bonn, Meckenheimer Allee 166, D-53115, Bonn, Germany
| | - P A Wookey
- Biological and Environmental Sciences, Faculty of Natural Sciences, University of Stirling, Stirling, FK9 4LA, Scotland, UK
| | - T J Zamin
- Department of Biology, Queen's University, Biosciences Complex, 116 Barrie St., Kingston, ON, K7L 3N6, Canada
| | - M Bahn
- Department of Ecology, University of Innsbruck, Innrain 52, 6020, Innsbruck, Austria
| | - B Blonder
- Environmental Change Institute, School of Geography and the Environment, University of Oxford, 3 South Parks Road, Oxford, OX1 3QY, UK
- Rocky Mountain Biological Laboratory, 8000 Co Rd 317, Crested Butte, CO, 81224, USA
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, CA, 94706, USA
| | - P M van Bodegom
- Environmental Biology Department, Institute of Environmental Sciences, Leiden University, 2300 RA, Leiden, The Netherlands
| | - B Bond-Lamberty
- Pacific Northwest National Laboratory, Joint Global Change Research Institute, 5825 University Research Ct, College Park, MD, 20740, USA
| | - G Campetella
- School of Biosciences and Veterinary Medicine-Plant Diversity and Ecosystems Management Unit, Univeristy of Camerino, Via Gentile III Da Varano, 62032, Camerino, Italy
| | - B E L Cerabolini
- DBSV-University of Insubria, Via Dunant, 3, 21100, Varese, Italy
| | - F S Chapin
- Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, AK, 99775, USA
| | - J M Craine
- Jonah Ventures, 1600 Range Street Suite 201, Boulder, CO, 80301, USA
| | - M Dainese
- Department of Animal Ecology and Tropical Biology, University of Würzburg, Am Hubland, 97074, Würzburg, Germany
- Institute for Alpine Environment, EURAC Research, Viale Druso, 1, 39100, Bolzano, Italy
| | - W A Green
- Department of Organismic and Evolutionary Biology, Harvard University, 52 Oxford Street, Cambridge, MA, 02138, USA
| | - S Jansen
- Institute of Systematic Botany and Ecology, Ulm University, Albert-Einstein-Allee 11, D-89081, Ulm, Germany
| | - M Kleyer
- Institute of Biology and Environmental Sciences, University of Oldenburg, Carl-von-Ossietzky-Strasse 9-11, 26129, Oldenburg, Germany
| | - P Manning
- Senckenberg Biodiversity and Climate Research Centre, 60325, Frankfurt, Germany
| | - Ü Niinemets
- Institute of Agricultural and Environmental Sciences, Estonian University of Life Sciences, Fr.R.Kreutzwaldi 1, 51006, Tartu, Estonia
| | - Y Onoda
- Graduate School of Agriculture, Kyoto University, Sakyo-ku, Kyoto, 606-8502, Japan
| | - W A Ozinga
- Vegetation, Forest and Landscape Ecology, Wageningen University and Research, P.O. Box 47, NL-6700 AA, Wageningen, The Netherlands
| | - J Peñuelas
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, 08193 Cerdanyola del Vallès Bellaterra, Catalonia, Spain
- CREAF, 08193 Cerdanyola del Vallès, Catalonia, Spain
| | - P Poschlod
- Ecology and Conservation Biology, Institute of Plant Sciences, University of Regensburg, Regensburg, Germany
| | - P B Reich
- Department of Forest Resources, University of Minnesota, 115 Green Hall, 1530 Cleveland Ave. N., St. Paul, MN, 55108, USA
- Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, 2751, Australia
| | - B Sandel
- Department of Biology, Santa Clara University, 500 El Camino Real, Santa Clara, CA, 95053, USA
| | - B S Schamp
- Department of Biology, Algoma University, 1520 Queen Street East, Sault Ste., Marie, ON, P6A 2G4, Canada
| | - S N Sheremetiev
- Komarov Botanical Institute, Professor Popova Street, 2, St Petersburg, Russia
| | - F T de Vries
- Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Postbus 94240, 1090 GE, Amsterdam, Netherlands
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4
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Sperlich D, Chang CT, Peñuelas J, Sabaté S. Responses of photosynthesis and component processes to drought and temperature stress: are Mediterranean trees fit for climate change? Tree Physiol 2019; 39:1783-1805. [PMID: 31553458 DOI: 10.1093/treephys/tpz089] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/22/2019] [Revised: 03/19/2019] [Accepted: 08/15/2019] [Indexed: 05/24/2023]
Abstract
Global warming is raising concerns about the acclimatory capacity of trees and forests, especially in Mediterranean-type ecosystems. The sensitivity of photosynthesis to temperature is a key uncertainty for projecting the magnitude of terrestrial feedbacks on future climate change. While boreal, temperate and tropical species have been comparatively well investigated, our study provides the first comprehensive overview of the seasonal acclimatory responses of photosynthesis and its component processes to temperature in four Mediterranean climax species under natural conditions. We quantified seasonal changes in the responses of net photosynthesis (Anet), stomatal conductance (gs), mesophyllic conductance (gm) and electron-transport rate (Jcf), and investigated their sensitivity to drought and temperature stress in sunlit and shaded leaves of four Mediterranean tree species (Quercus ilex L., Pinus halepensis Mill., Arbutus unedo L. and Quercus pubescens Willd.). Sunlit leaves, but not shaded leaves, showed a pronounced seasonality in the temperature responses of Anet, gs, gm and Jcf. All four species and variables showed a remarkably dynamic and consistent acclimation of the thermal optimum (Topt), reaching peaks in summer ~29-32 °C. Changes in the shape of the response curves were, however, highly species-specific. Under severe drought, Topt of all variables were on average 22-29% lower. This was accompanied by narrower response curves above all in P. halepensis, reducing the optimal range for photosynthesis to the cooler morning or evening periods. Wider temperature-response curves and less strict stomatal control under severe drought were accompanied by wilting and drought-induced leaf shedding in Q. ilex and Q. pubescens and by additional branch dieback in A. unedo. Mild winter conditions led to a high Topt (~19.1-22.2 °C), benefitting the evergreen species, especially P. halepensis. Seasonal acclimation of Anet was explained better by gs and gm being less pronounced in Jcf. Drought was thus a key factor, in addition to growth temperature, to explain seasonal acclimation of photosynthesis. Severe drought periods may exceed more frequently the high acclimatory capacity of Mediterranean trees to high ambient temperatures, which could lead to reduced growth, increased leaf shedding and, for some species such as A. unedo, increased mortality risk.
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Affiliation(s)
- D Sperlich
- Chair of Forestry Economics and Forest Planning, Faculty of Environment and Natural Resources, University of Freiburg, 79085 Freiburg im Breisgau, Tennenbacherstr. 4, Germany
| | - C T Chang
- Department of Evolutionary Biology, Ecology and Environmental Sciences (BEECA), University of Barcelona (UB), Av. Diagonal 643, 08028 Barcelona
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - J Peñuelas
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
- Global Ecology Unit CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - S Sabaté
- Department of Evolutionary Biology, Ecology and Environmental Sciences (BEECA), University of Barcelona (UB), Av. Diagonal 643, 08028 Barcelona
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
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5
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Fernández-Martínez M, Pearse I, Sardans J, Sayol F, Koenig WD, LaMontagne JM, Bogdziewicz M, Collalti A, Hacket-Pain A, Vacchiano G, Espelta JM, Peñuelas J, Janssens IA. Nutrient scarcity as a selective pressure for mast seeding. Nat Plants 2019; 5:1222-1228. [PMID: 31792395 DOI: 10.1038/s41477-019-0549-y] [Citation(s) in RCA: 21] [Impact Index Per Article: 4.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/08/2019] [Accepted: 10/08/2019] [Indexed: 06/10/2023]
Abstract
Mast seeding is one of the most intriguing reproductive traits in nature. Despite its potential drawbacks in terms of fitness, the widespread existence of this phenomenon suggests that it should have evolutionary advantages under certain circumstances. Using a global dataset of seed production time series for 219 plant species from all of the continents, we tested whether masting behaviour appears predominantly in species with low foliar nitrogen and phosphorus concentrations when controlling for local climate and productivity. Here, we show that masting intensity is higher in species with low foliar N and P concentrations, and especially in those with imbalanced N/P ratios, and that the evolutionary history of masting behaviour has been linked to that of nutrient economy. Our results support the hypothesis that masting is stronger in species growing under limiting conditions and suggest that this reproductive behaviour might have evolved as an adaptation to nutrient limitations and imbalances.
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Affiliation(s)
- M Fernández-Martínez
- PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Antwerp, Belgium.
- Global Ecology Unit, CREAF-CSIC-UAB, Barcelona, Spain.
| | - I Pearse
- US Geological Survey, Fort Collins Science Center, Fort Collins, CO, USA
| | - J Sardans
- Global Ecology Unit, CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | - F Sayol
- Department of Biological and Environmental Sciences, University of Gothenburg, Gothenburg, Sweden
- Gothenburg Global Biodiversity Centre, Gothenburg, Sweden
| | - W D Koenig
- Cornell Lab of Ornithology, Cornell University, Ithaca, NY, USA
| | - J M LaMontagne
- Department of Biological Sciences, DePaul University, Chicago, IL, USA
| | - M Bogdziewicz
- Department of Systematic Zoology, Faculty of Biology, Adam Mickiewicz University in Poznań, Poznań, Poland
| | - A Collalti
- Institute for Agriculture and Forestry Systems in the Mediterranean, National Research Council of Italy (CNR-ISAFOM), Rende, Italy
- Department of Innovation in Biological, Agro-food and Forest Systems, University of Tuscia, Viterbo, Italy
| | - A Hacket-Pain
- Department of Geography and Planning, School of Environmental Sciences, University of Liverpool, Liverpool, UK
| | | | | | - J Peñuelas
- Global Ecology Unit, CREAF-CSIC-UAB, Barcelona, Spain
- CREAF, Barcelona, Spain
| | - I A Janssens
- PLECO (Plants and Ecosystems), Department of Biology, University of Antwerp, Antwerp, Belgium
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6
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Thomas HJD, Myers‐Smith IH, Bjorkman AD, Elmendorf SC, Blok D, Cornelissen JHC, Forbes BC, Hollister RD, Normand S, Prevéy JS, Rixen C, Schaepman‐Strub G, Wilmking M, Wipf S, Cornwell WK, Kattge J, Goetz SJ, Guay KC, Alatalo JM, Anadon‐Rosell A, Angers‐Blondin S, Berner LT, Björk RG, Buchwal A, Buras A, Carbognani M, Christie K, Siegwart Collier L, Cooper EJ, Eskelinen A, Frei ER, Grau O, Grogan P, Hallinger M, Heijmans MMPD, Hermanutz L, Hudson JMG, Hülber K, Iturrate‐Garcia M, Iversen CM, Jaroszynska F, Johnstone JF, Kaarlejärvi E, Kulonen A, Lamarque LJ, Lévesque E, Little CJ, Michelsen A, Milbau A, Nabe‐Nielsen J, Nielsen SS, Ninot JM, Oberbauer SF, Olofsson J, Onipchenko VG, Petraglia A, Rumpf SB, Semenchuk PR, Soudzilovskaia NA, Spasojevic MJ, Speed JDM, Tape KD, te Beest M, Tomaselli M, Trant A, Treier UA, Venn S, Vowles T, Weijers S, Zamin T, Atkin OK, Bahn M, Blonder B, Campetella G, Cerabolini BEL, Chapin III FS, Dainese M, de Vries FT, Díaz S, Green W, Jackson RB, Manning P, Niinemets Ü, Ozinga WA, Peñuelas J, Reich PB, Schamp B, Sheremetev S, van Bodegom PM. Traditional plant functional groups explain variation in economic but not size-related traits across the tundra biome. Glob Ecol Biogeogr 2019; 28:78-95. [PMID: 31007605 PMCID: PMC6472633 DOI: 10.1111/geb.12783] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/20/2017] [Revised: 05/24/2018] [Accepted: 05/29/2018] [Indexed: 06/01/2023]
Abstract
AIM Plant functional groups are widely used in community ecology and earth system modelling to describe trait variation within and across plant communities. However, this approach rests on the assumption that functional groups explain a large proportion of trait variation among species. We test whether four commonly used plant functional groups represent variation in six ecologically important plant traits. LOCATION Tundra biome. TIME PERIOD Data collected between 1964 and 2016. MAJOR TAXA STUDIED 295 tundra vascular plant species. METHODS We compiled a database of six plant traits (plant height, leaf area, specific leaf area, leaf dry matter content, leaf nitrogen, seed mass) for tundra species. We examined the variation in species-level trait expression explained by four traditional functional groups (evergreen shrubs, deciduous shrubs, graminoids, forbs), and whether variation explained was dependent upon the traits included in analysis. We further compared the explanatory power and species composition of functional groups to alternative classifications generated using post hoc clustering of species-level traits. RESULTS Traditional functional groups explained significant differences in trait expression, particularly amongst traits associated with resource economics, which were consistent across sites and at the biome scale. However, functional groups explained 19% of overall trait variation and poorly represented differences in traits associated with plant size. Post hoc classification of species did not correspond well with traditional functional groups, and explained twice as much variation in species-level trait expression. MAIN CONCLUSIONS Traditional functional groups only coarsely represent variation in well-measured traits within tundra plant communities, and better explain resource economic traits than size-related traits. We recommend caution when using functional group approaches to predict tundra vegetation change, or ecosystem functions relating to plant size, such as albedo or carbon storage. We argue that alternative classifications or direct use of specific plant traits could provide new insights for ecological prediction and modelling.
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Affiliation(s)
- H. J. D. Thomas
- School of GeosciencesUniversity of EdinburghEdinburghUnited Kingdom
| | | | - A. D. Bjorkman
- School of GeosciencesUniversity of EdinburghEdinburghUnited Kingdom
- Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus UniversityAarhusDenmark
- Senckenberg Gesellschaft für Naturforschung, Biodiversity and Climate Research Centre (SBiK‐F)FrankfurtGermany
| | - S. C. Elmendorf
- Institute of Arctic and Alpine Research, University of ColoradoBoulderColorado
| | - D. Blok
- Department of Physical Geography and Ecosystem Science, Lund UniversityLundSweden
| | | | - B. C. Forbes
- Arctic Centre, University of LaplandRovaniemiFinland
| | - R. D. Hollister
- Biology Department, Grand Valley State UniversityAllendaleMichigan
| | - S. Normand
- Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus UniversityAarhusDenmark
| | - J. S. Prevéy
- WSL Institute for Snow and Avalanche Research SLFDavosSwitzerland
| | - C. Rixen
- WSL Institute for Snow and Avalanche Research SLFDavosSwitzerland
| | - G. Schaepman‐Strub
- Department of Evolutionary Biology and Environmental Studies, University of ZurichZurichSwitzerland
| | - M. Wilmking
- Institute for Botany and Landscape Ecology, Greifswald UniversityGreifswaldGermany
| | - S. Wipf
- WSL Institute for Snow and Avalanche Research SLFDavosSwitzerland
| | - W. K. Cornwell
- School of Biological Earth and Environmental Sciences, University of New South WalesSydneyNew South WalesAustralia
| | - J. Kattge
- Max Planck Institute for BiogeochemistryJenaGermany
- German Centre for Integrative Biodiversity Research (iDiv)Halle‐Jena‐LeipzigGermany
| | - S. J. Goetz
- School of Informatics, Computing, and Cyber Systems, Northern Arizona UniversityFlagstaffArizona
| | - K. C. Guay
- Bigelow Laboratory for Ocean SciencesBoothbayMaine
| | - J. M. Alatalo
- Department of Biological and Environmental Sciences, Qatar UniversityDohaQatar
| | - A. Anadon‐Rosell
- Institute for Botany and Landscape Ecology, Greifswald UniversityGreifswaldGermany
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of BarcelonaBarcelonaSpain
- Biodiversity Research InstituteUniversity of BarcelonaBarcelonaSpain
| | | | - L. T. Berner
- School of Informatics, Computing, and Cyber Systems, Northern Arizona UniversityFlagstaffArizona
| | - R. G. Björk
- Department of Earth Sciences, University of GothenburgGothenburgSweden
- Gothenburg Global Biodiversity CentreGothenburgSweden
| | - A. Buchwal
- Institute of Geoecology and Geoinformation, Adam Mickiewicz UniversityPoznanPoland
- Department of Biological Sciences, University of Alaska AnchorageAnchorageAlaska
| | - A. Buras
- Forest Ecology and Forest Management, Wageningen University and Research, WageningenNetherlands
| | - M. Carbognani
- Department of Chemistry, Life Sciences and Environmental Sustainability, University of ParmaParmaItaly
| | - K. Christie
- The Alaska Department of Fish and GameJuneauAlaska
| | - L. Siegwart Collier
- Department of Biology, Memorial UniversitySt John’s, Newfoundland and LabradorCanada
| | - E. J. Cooper
- Department of Arctic and Marine Biology, UiT‐The Arctic University of NorwayTromsøNorway
| | - A. Eskelinen
- German Centre for Integrative Biodiversity Research (iDiv)Halle‐Jena‐LeipzigGermany
- Department of Physiological Diversity, Helmholtz Centre for Environmental Research – UFZLeipzigGermany
- Department of Ecology and Genetics, University of OuluOuluFinland
| | - E. R. Frei
- Department of Geography, University of British ColumbiaVancouverBritish ColumbiaCanada
| | - O. Grau
- Global Ecology Unit, CREAF‐CSIC‐UAB‐UBBellaterraSpain
| | - P. Grogan
- Department of Biology, Queen's UniversityKingston, OntarioCanada
| | - M. Hallinger
- Biology Department, Swedish Agricultural University (SLU)UppsalaSweden
| | - M. M. P. D. Heijmans
- Plant Ecology and Nature Conservation Group, Wageningen University & ResearchWageningenThe Netherlands
| | - L. Hermanutz
- Department of Biology, Memorial UniversitySt John’s, Newfoundland and LabradorCanada
| | | | - K. Hülber
- Department of Botany and Biodiversity Research, University of ViennaViennaAustria
| | - M. Iturrate‐Garcia
- Department of Evolutionary Biology and Environmental Studies, University of ZurichZurichSwitzerland
| | - C. M. Iversen
- Climate Change Science Institute and Environmental Sciences Division, Oak Ridge National LaboratoryOak RidgeTennessee
| | | | - J. F. Johnstone
- Department of Biology, University of SaskatchewanSaskatoonCanada
| | - E. Kaarlejärvi
- Department of Ecology and Environmental Sciences, Umeå UniversityUmeåSweden
- Department of Biology, Vrije Universiteit Brussel (VUB)BrusselsBelgium
- Faculty of Biological and Environmental Sciences, University of HelsinkiHelsinkiFinland
| | - A. Kulonen
- WSL Institute for Snow and Avalanche Research SLFDavosSwitzerland
- Department of Biology, University of BergenBergenNorway
| | - L. J. Lamarque
- Département des Sciences de l'Environnement and Centres d'études nordiques, Université du Québec à Trois‐RivièresTrois‐RivièresQuebecCanada
| | - E. Lévesque
- Département des Sciences de l'Environnement and Centres d'études nordiques, Université du Québec à Trois‐RivièresTrois‐RivièresQuebecCanada
| | - C. J. Little
- Department of Evolutionary Biology and Environmental Studies, University of ZurichZurichSwitzerland
- Eawag Swiss Federal Institute of Aquatic Science & TechnologyDubendorfSwitzerland
| | - A. Michelsen
- Department of Biology, University of CopenhagenCopenhagenDenmark
- Center for Permafrost (CENPERM), University of CopenhagenCopenhagenDenmark
| | - A. Milbau
- Research Institute for Nature and Forest (INBO)BrusselsBelgium
| | - J. Nabe‐Nielsen
- Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus UniversityAarhusDenmark
| | - S. S. Nielsen
- Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus UniversityAarhusDenmark
| | - J. M. Ninot
- Department of Evolutionary Biology, Ecology and Environmental Sciences, University of BarcelonaBarcelonaSpain
- Biodiversity Research InstituteUniversity of BarcelonaBarcelonaSpain
| | - S. F. Oberbauer
- Department of Biological Sciences, Florida International UniversityMiamiFlorida
| | - J. Olofsson
- Department of Ecology and Environmental Sciences, Umeå UniversityUmeåSweden
| | - V. G. Onipchenko
- Department of Geobotany, Lomonosov Moscow State UniversityMoscowRussia
| | - A. Petraglia
- Department of Chemistry, Life Sciences and Environmental Sustainability, University of ParmaParmaItaly
| | - S. B. Rumpf
- Department of Botany and Biodiversity Research, University of ViennaViennaAustria
| | - P. R. Semenchuk
- Department of Arctic and Marine Biology, UiT‐The Arctic University of NorwayTromsøNorway
- Department of Botany and Biodiversity Research, University of ViennaViennaAustria
| | - N. A. Soudzilovskaia
- Environmental Biology, Department Institute of Environmental Sciences, CML, Leiden UniversityLeidenThe Netherlands
| | - M. J. Spasojevic
- Department of Biology, University of California RiversideRiversideCalifornia
| | - J. D. M. Speed
- NTNU University Museum, Norwegian University of Science and TechnologyTrondheimNorway
| | - K. D. Tape
- Water and Environmental Research Center, University of AlaskaFairbanksAlaska
| | - M. te Beest
- Department of Ecology and Environmental Sciences, Umeå UniversityUmeåSweden
- Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht UniversityUtrechtThe Netherlands
| | - M. Tomaselli
- Department of Chemistry, Life Sciences and Environmental Sustainability, University of ParmaParmaItaly
| | - A. Trant
- Department of Biology, Memorial UniversitySt John’s, Newfoundland and LabradorCanada
- School of Environment, Resources and Sustainability, University of WaterlooWaterlooOntarioCanada
| | - U. A. Treier
- Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus UniversityAarhusDenmark
| | - S. Venn
- Research School of Biology, Australian National UniversityActon, ACTAustralia
- Centre for Integrative Ecology, School of Life and Environmental Sciences, Deakin UniversityBurwoodVictoriaAustralia
| | - T. Vowles
- Department of Earth Sciences, University of GothenburgGothenburgSweden
| | - S. Weijers
- Department of Geography, University of BonnBonnGermany
| | - T. Zamin
- Department of Biology, Queen's UniversityKingston, OntarioCanada
| | - O. K. Atkin
- Research School of Biology, Australian National UniversityActon, ACTAustralia
| | - M. Bahn
- Department of Ecology, University of InnsbruckInnsbruckAustria
| | - B. Blonder
- Environmental Change Institute, School of Geography and the Environment, University of OxfordOxfordUnited Kingdom
- Rocky Mountain Biological LaboratoryCrested ButteColorado
| | - G. Campetella
- School of Biosciences & Veterinary Medicine ‐ Plant Diversity and Ecosystems Management Unit, University of CamerinoCamerinoItaly
| | | | - F. S. Chapin III
- Institute of Arctic Biology, University of AlaskaFairbanksAlaska
| | - M. Dainese
- Department of Animal Ecology and Tropical Biology, University of WürzburgWürzburgGermany
| | - F. T. de Vries
- School of Earth and Environmental Sciences, The University of ManchesterManchesterUnited Kingdom
| | - S. Díaz
- Instituto Multidisciplinario de Biología Vegetal (IMBIV), CONICET and FCEFyN, Universidad Nacional de CórdobaCórdobaArgentina
| | - W. Green
- Department of Organismic and Evolutionary Biology, Harvard University Cambridge, Massachusetts
| | - R. B. Jackson
- Department of Earth System Science, Stanford UniversityStanford, California
| | - P. Manning
- Senckenberg Gesellschaft für Naturforschung, Biodiversity and Climate Research Centre (SBiK‐F)FrankfurtGermany
| | - Ü. Niinemets
- Institute of Agricultural and Environmental Sciences, Estonian University of Life SciencesTartuEstonia
| | - W. A. Ozinga
- Plant Ecology and Nature Conservation Group, Wageningen University & ResearchWageningenThe Netherlands
| | - J. Peñuelas
- Global Ecology Unit, CREAF‐CSIC‐UAB‐UBBellaterraSpain
- CREAFCerdanyola del VallèsSpain
| | - P. B. Reich
- Department of Forest Resources, University of MinnesotaSt. Paul, MinneapolisMinnesota
- Hawkesbury Institute for the Environment, Western Sydney UniversityPenrith, NSWAustralia
| | - B. Schamp
- Department of Biology, Algoma UniversitySault Ste. MarieOntarioCanada
| | | | - P. M. van Bodegom
- Environmental Biology, Department Institute of Environmental Sciences, CML, Leiden UniversityLeidenThe Netherlands
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7
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Fernández-Martínez M, Vicca S, Janssens IA, Ciais P, Obersteiner M, Bartrons M, Sardans J, Verger A, Canadell JG, Chevallier F, Wang X, Bernhofer C, Curtis PS, Gianelle D, Grünwald T, Heinesch B, Ibrom A, Knohl A, Laurila T, Law BE, Limousin JM, Longdoz B, Loustau D, Mammarella I, Matteucci G, Monson RK, Montagnani L, Moors EJ, Munger JW, Papale D, Piao SL, Peñuelas J. Atmospheric deposition, CO 2, and change in the land carbon sink. Sci Rep 2017; 7:9632. [PMID: 28851977 PMCID: PMC5574890 DOI: 10.1038/s41598-017-08755-8] [Citation(s) in RCA: 44] [Impact Index Per Article: 6.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/25/2017] [Accepted: 07/18/2017] [Indexed: 11/20/2022] Open
Abstract
Concentrations of atmospheric carbon dioxide (CO2) have continued to increase whereas atmospheric deposition of sulphur and nitrogen has declined in Europe and the USA during recent decades. Using time series of flux observations from 23 forests distributed throughout Europe and the USA, and generalised mixed models, we found that forest-level net ecosystem production and gross primary production have increased by 1% annually from 1995 to 2011. Statistical models indicated that increasing atmospheric CO2 was the most important factor driving the increasing strength of carbon sinks in these forests. We also found that the reduction of sulphur deposition in Europe and the USA lead to higher recovery in ecosystem respiration than in gross primary production, thus limiting the increase of carbon sequestration. By contrast, trends in climate and nitrogen deposition did not significantly contribute to changing carbon fluxes during the studied period. Our findings support the hypothesis of a general CO2-fertilization effect on vegetation growth and suggest that, so far unknown, sulphur deposition plays a significant role in the carbon balance of forests in industrialized regions. Our results show the need to include the effects of changing atmospheric composition, beyond CO2, to assess future dynamics of carbon-climate feedbacks not currently considered in earth system/climate modelling.
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Affiliation(s)
- M Fernández-Martínez
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain. .,CREAF, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain.
| | - S Vicca
- Centre of Excellence PLECO (Plant and Vegetation Ecology), Department of Biology, University of Antwerp, 2610, Wilrijk, Belgium
| | - I A Janssens
- Centre of Excellence PLECO (Plant and Vegetation Ecology), Department of Biology, University of Antwerp, 2610, Wilrijk, Belgium
| | - P Ciais
- Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, 91191, Gif-sur-Yvette, France
| | - M Obersteiner
- International Institute for Applied Systems Analysis, Schlossplatz 1, 2361, Laxenburg, Austria
| | - M Bartrons
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain.,CREAF, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain
| | - J Sardans
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain.,CREAF, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain
| | - A Verger
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain.,CREAF, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain
| | - J G Canadell
- Global Carbon Project, CSIRO Oceans and Atmosphere, Canberra, ACT 2601, Australia
| | - F Chevallier
- Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS UVSQ, 91191, Gif-sur-Yvette, France
| | - X Wang
- Sino-French Institute of Earth System Sciences, College of Urban and Environmental Sciences, Peking University, Beijing, 100871, China.,Laboratoire de Météorologie Dynamique, Université Pierre et Marie Curie, Paris, 75005, France
| | - C Bernhofer
- TU Dresden, Institut für Hydrologie und Meteorologie, LS Meteorologie, Pienner Str. 23, 01737, Tharandt, Germany
| | - P S Curtis
- Department of Evolution, Ecology, and Organismal Biology, The Ohio State University, Columbus, Ohio, 43210, USA
| | - D Gianelle
- Foxlab Joint CNR-FEM Initiative, Via E. Mach 1, 38010 San Michele all'Adige, Italy.,Department of Sustainable Agro-Ecosystems and Bioresources, Research and Innovation Center, Fondazione Edmund Mach, 38010 S, Michele all' Adige Trento, Italy
| | - T Grünwald
- TU Dresden, Institut für Hydrologie und Meteorologie, LS Meteorologie, Pienner Str. 23, 01737, Tharandt, Germany
| | - B Heinesch
- Department of Biosystem Engineering (BioSE), Gembloux Agro-Bio Tech, University of Liege, Liège, 4000, Belgium
| | - A Ibrom
- Department of Environmental Engineering, Technical University of Denmark (DTU), Lyngby, Denmark
| | - A Knohl
- Bioclimatology, Faculty of Forest Sciences and Forest Ecology, University of Göttingen, Büsgenweg 2, 37077, Göttingen, Germany
| | - T Laurila
- Finnish Meteorological Institute, Erik Palménin aukio 1, FI-00560, Helsinki, Finland
| | - B E Law
- Department of Forest Ecosystems & Society, Oregon State University, Corvallis, OR, 97331, USA
| | - J M Limousin
- Centre d'Ecologie Fonctionelle et Evolutive CEFE, UMR 5175, CNRS, Université de Montpellier, Université Paul-Valery Montpellier, EPHE, 1919 route de Mende, 34293, Montpellier 5, France
| | - B Longdoz
- UMR Ecologie et Ecophysiologie Forestières, UMR1137, Inra-Université de Lorraine, Champenoux (F-54280)-Vandoeuvre Les Nancy (F-54500), France
| | - D Loustau
- INRA, UMR 1391 ISPA, Centre de Bordeaux Aquitaine, Villenave-d'Ornon, France
| | - I Mammarella
- Department of Physics, University of Helsinki, P.O. Box 48, FIN-00014, Helsinki, Finland
| | - G Matteucci
- IBAF - National Research Council of Italy, I-00015, Monterotondo (RM), Italy.,ISAFOM - National Research Council of Italy, I-87036, Rende (CS), Italy
| | - R K Monson
- School of Natural Resources and the Environment and Laboratory of Tree Ring Research, University of Arizona, Tucson, Arizona, USA
| | - L Montagnani
- Forest Services, Autonomous Province of Bolzano, Via Brennero 6, 39100, Bolzano, Italy.,Faculty of Science and Technology, Free University of Bolzano, Piazza Università 5, 39100, Bolzano, Italy
| | - E J Moors
- Alterra Wageningen UR, PO Box 47, 6700 AA, Wageningen, Netherlands.,VU University Amsterdam, Boelelaan 1085, Amsterdam, Netherlands
| | - J W Munger
- School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, 02138, USA
| | - D Papale
- DIBAF, University of Tuscia, 01100, Viterbo, Italy
| | - S L Piao
- Sino-French Institute of Earth System Sciences, College of Urban and Environmental Sciences, Peking University, Beijing, 100871, China.,Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China
| | - J Peñuelas
- CSIC, Global Ecology Unit, CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain.,CREAF, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain
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8
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Margalef O, Sardans J, Fernández-Martínez M, Molowny-Horas R, Janssens IA, Ciais P, Goll D, Richter A, Obersteiner M, Asensio D, Peñuelas J. Global patterns of phosphatase activity in natural soils. Sci Rep 2017; 7:1337. [PMID: 28465504 PMCID: PMC5431046 DOI: 10.1038/s41598-017-01418-8] [Citation(s) in RCA: 106] [Impact Index Per Article: 15.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/06/2016] [Accepted: 03/28/2017] [Indexed: 11/25/2022] Open
Abstract
Soil phosphatase levels strongly control the biotic pathways of phosphorus (P), an essential element for life, which is often limiting in terrestrial ecosystems. We investigated the influence of climatic and soil traits on phosphatase activity in terrestrial systems using metadata analysis from published studies. This is the first analysis of global measurements of phosphatase in natural soils. Our results suggest that organic P (Porg), rather than available P, is the most important P fraction in predicting phosphatase activity. Structural equation modeling using soil total nitrogen (TN), mean annual precipitation, mean annual temperature, thermal amplitude and total soil carbon as most available predictor variables explained up to 50% of the spatial variance in phosphatase activity. In this analysis, Porg could not be tested and among the rest of available variables, TN was the most important factor explaining the observed spatial gradients in phosphatase activity. On the other hand, phosphatase activity was also found to be associated with climatic conditions and soil type across different biomes worldwide. The close association among different predictors like Porg, TN and precipitation suggest that P recycling is driven by a broad scale pattern of ecosystem productivity capacity.
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Affiliation(s)
- O Margalef
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, 08193, Catalonia, Spain.
- CREAF, Cerdanyola del Vallès, 08193, Catalonia, Spain.
| | - J Sardans
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, 08193, Catalonia, Spain
- CREAF, Cerdanyola del Vallès, 08193, Catalonia, Spain
| | - M Fernández-Martínez
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, 08193, Catalonia, Spain
- CREAF, Cerdanyola del Vallès, 08193, Catalonia, Spain
| | | | - I A Janssens
- Department of Biology, University of Antwerp, Universiteitsplein 1, B‑2610, Wilrijk, Belgium
| | - P Ciais
- Laboratoire des Sciences du Climat et de l'Environnement, IPSL-LSCE CEA CNRS UVSQ UPSaclay, 91190, Gif-sur-Yvette, France
| | - D Goll
- Laboratoire des Sciences du Climat et de l'Environnement, IPSL-LSCE CEA CNRS UVSQ UPSaclay, 91190, Gif-sur-Yvette, France
| | - A Richter
- Department of Microbiology and Ecosystem Science, University of Vienna, Vienna, A‑1090, Austria
| | - M Obersteiner
- International Institute for Applied Systems Analysis (IIASA), Ecosystem s Services and Management, Schlossplatz 1, A-2361, Laxenburg, Austria
| | - D Asensio
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, 08193, Catalonia, Spain
- CREAF, Cerdanyola del Vallès, 08193, Catalonia, Spain
| | - J Peñuelas
- CSIC, Global Ecology Unit CREAF-CSIC-UAB, Bellaterra, 08193, Catalonia, Spain
- CREAF, Cerdanyola del Vallès, 08193, Catalonia, Spain
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9
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Campioli M, Malhi Y, Vicca S, Luyssaert S, Papale D, Peñuelas J, Reichstein M, Migliavacca M, Arain MA, Janssens IA. Evaluating the convergence between eddy-covariance and biometric methods for assessing carbon budgets of forests. Nat Commun 2016; 7:13717. [PMID: 27966534 PMCID: PMC5171944 DOI: 10.1038/ncomms13717] [Citation(s) in RCA: 72] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/19/2015] [Accepted: 10/27/2016] [Indexed: 11/13/2022] Open
Abstract
The eddy-covariance (EC) micro-meteorological technique and the ecology-based biometric methods (BM) are the primary methodologies to quantify CO2 exchange between terrestrial ecosystems and the atmosphere (net ecosystem production, NEP) and its two components, ecosystem respiration and gross primary production. Here we show that EC and BM provide different estimates of NEP, but comparable ecosystem respiration and gross primary production for forest ecosystems globally. Discrepancies between methods are not related to environmental or stand variables, but are consistently more pronounced for boreal forests where carbon fluxes are smaller. BM estimates are prone to underestimation of net primary production and overestimation of leaf respiration. EC biases are not apparent across sites, suggesting the effectiveness of standard post-processing procedures. Our results increase confidence in EC, show in which conditions EC and BM estimates can be integrated, and which methodological aspects can improve the convergence between EC and BM.
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Affiliation(s)
- M. Campioli
- Centre of Excellence PLECO (Plant and Vegetation Ecology), Department of Biology, University of Antwerp, 2610 Wilrijk, Belgium
| | - Y. Malhi
- Environmental Change Institute, School of Geography and the Environment, University of Oxford, Oxford OX1 3QY, UK
| | - S. Vicca
- Centre of Excellence PLECO (Plant and Vegetation Ecology), Department of Biology, University of Antwerp, 2610 Wilrijk, Belgium
| | - S. Luyssaert
- LSCE CEA-CNRS-UVSQ, Orme des Merisiers, F-91191 Gif-sur-Yvette, France
| | - D. Papale
- DIBAF, University of Tuscia, 01100 Viterbo, Italy
- Euro-Mediterranean Center on Climate Change, CMCC, 73100 Lecce, Italy
| | - J. Peñuelas
- CSIC, Global Ecology Unit, CREAF-CEAB-CSIC-UAB, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - M. Reichstein
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
| | - M. Migliavacca
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
| | - M. A. Arain
- School of Geography & Earth Sciences, McMaster University, Hamilton, Ontario, Canada L8S 4K1
| | - I. A. Janssens
- Centre of Excellence PLECO (Plant and Vegetation Ecology), Department of Biology, University of Antwerp, 2610 Wilrijk, Belgium
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10
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Jiang LL, Wang SP, Meng FD, Duan JC, Niu HS, Xu GP, Zhu XX, Zhang ZH, Luo CY, Cui SJ, Li YM, Li XE, Wang Q, Zhou Y, Bao XY, Li YN, Dorji T, Piao SL, Ciais P, Peñuelas J, Du MY, Zhao XQ, Zhao L, Zhang FW, Wang GJ. Relatively stable response of fruiting stage to warming and cooling relative to other phenological events. Ecology 2016; 97:1961-1969. [DOI: 10.1002/ecy.1450] [Citation(s) in RCA: 29] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Submit a Manuscript] [Subscribe] [Scholar Register] [Received: 08/18/2015] [Revised: 02/23/2016] [Accepted: 03/04/2016] [Indexed: 11/11/2022]
Affiliation(s)
- L. L. Jiang
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
- Naqu Integrated Observation and Research Station of Ecology and Environment; Tibet University and Institute of Tibetan Plateau Research of the Chinese Academy of Sciences; Lasa 850012 China
| | - S. P. Wang
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
- Naqu Integrated Observation and Research Station of Ecology and Environment; Tibet University and Institute of Tibetan Plateau Research of the Chinese Academy of Sciences; Lasa 850012 China
- CAS Center for Excellence in Tibetan Plateau Earth Science; Chinese Academy of Sciences; Beijing 100101 China
| | - F. D. Meng
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
- University of Chinese Academy of Sciences; Beijing 100049 China
| | - J. C. Duan
- Binhai Research Institute in Tianjin; Tianjin 300457 China
| | - H. S. Niu
- University of Chinese Academy of Sciences; Beijing 100049 China
| | - G. P. Xu
- Guangxi Institute of Botany; Guangxi Zhuang Autonomous Region and Chinese Academy of Sciences; Guangxi 541006 China
| | - X. X. Zhu
- Naqu Integrated Observation and Research Station of Ecology and Environment; Tibet University and Institute of Tibetan Plateau Research of the Chinese Academy of Sciences; Lasa 850012 China
- Key Laboratory of Adaptation and Evolution of Plateau Biota; Northwest Institute of Plateau Biology; Chinese Academy of Sciences; Xining 810008 China
| | - Z. H. Zhang
- Key Laboratory of Adaptation and Evolution of Plateau Biota; Northwest Institute of Plateau Biology; Chinese Academy of Sciences; Xining 810008 China
| | - C. Y. Luo
- Key Laboratory of Adaptation and Evolution of Plateau Biota; Northwest Institute of Plateau Biology; Chinese Academy of Sciences; Xining 810008 China
| | - S. J. Cui
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
- Naqu Integrated Observation and Research Station of Ecology and Environment; Tibet University and Institute of Tibetan Plateau Research of the Chinese Academy of Sciences; Lasa 850012 China
| | - Y. M. Li
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
| | - X. E. Li
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
| | - Q. Wang
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
- University of Chinese Academy of Sciences; Beijing 100049 China
| | - Y. Zhou
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
- University of Chinese Academy of Sciences; Beijing 100049 China
| | - X. Y. Bao
- University of Chinese Academy of Sciences; Beijing 100049 China
| | - Y. N. Li
- Key Laboratory of Adaptation and Evolution of Plateau Biota; Northwest Institute of Plateau Biology; Chinese Academy of Sciences; Xining 810008 China
| | - T. Dorji
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
- Naqu Integrated Observation and Research Station of Ecology and Environment; Tibet University and Institute of Tibetan Plateau Research of the Chinese Academy of Sciences; Lasa 850012 China
| | - S. L. Piao
- Key Laboratory of Alpine Ecology and Biodiversity; Institute of Tibetan Plateau Research; Chinese Academy of Sciences; Beijing 100101 China
| | - P. Ciais
- Laboratoire des Sciences du Climat et de l'Environnement; CEA CNRS UVSQ; 91191 Gif-sur-Yvette France
| | - J. Peñuelas
- CREAF; Cerdanyola del Valles Barcelona 08193 Catalonia, Spain
- CSIC; Global Ecology Unit CREAF-CEAB-CSIC-UAB; Cerdanyola del Vallès Barcelona 08193 Catalonia Spain
| | - M. Y. Du
- National Institute for Agro-Environment Sciences; Tsukuba 305-8604 Japan
| | - X. Q. Zhao
- Key Laboratory of Adaptation and Evolution of Plateau Biota; Northwest Institute of Plateau Biology; Chinese Academy of Sciences; Xining 810008 China
| | - L. Zhao
- Key Laboratory of Adaptation and Evolution of Plateau Biota; Northwest Institute of Plateau Biology; Chinese Academy of Sciences; Xining 810008 China
| | - F. W. Zhang
- Key Laboratory of Adaptation and Evolution of Plateau Biota; Northwest Institute of Plateau Biology; Chinese Academy of Sciences; Xining 810008 China
| | - G. J. Wang
- Oregon State University Agriculture and Natural Resource Program at Eastern Oregon University; La Grande Oregon 97850 USA
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11
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Rivas-Ubach A, Sardans J, Hódar JA, Garcia-Porta J, Guenther A, Oravec M, Urban O, Peñuelas J. Similar local, but different systemic, metabolomic responses of closely related pine subspecies to folivory by caterpillars of the processionary moth. Plant Biol (Stuttg) 2016; 18:484-494. [PMID: 26642818 DOI: 10.1111/plb.12422] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/27/2015] [Accepted: 11/25/2015] [Indexed: 06/05/2023]
Abstract
Plants respond locally and systemically to herbivore attack. Most of the research conducted on plant-herbivore relationships at element and molecular levels have focused on the elemental composition or/and certain molecular compounds or specific families of defence metabolites showing that herbivores tend to select plant individuals or species with higher nutrient concentrations and avoid those with higher levels of defence compounds. We performed stoichiometric and metabolomics, both local and systemic, analyses in two subspecies of Pinus sylvestris under attack from caterpillars of the pine processionary moth, an important pest in the Mediterranean Basin. Both pine subspecies responded locally to folivory mainly by increasing relative concentrations of terpenes and some phenolics. Systemic responses differed between pine subspecies, and most of the metabolites presented intermediate concentrations between those of the affected parts and unattacked trees. Our results support the hypothesis that foliar nutrient concentrations are not a key factor for plant selection by adult female processionary moths for oviposition, since folivory was not associated with any of the elements analysed. Phenolic compounds generally did not increase in the attacked trees, questioning the suggestion of induction of phenolics following folivory attack and the anti-feeding properties of phenolics. Herbivory attack produced a general systemic shift in pines, in both primary and secondary metabolism, which was less intense and chemically different from the local responses. Local pine responses were similar between pine subspecies, while systemic responses were more distant.
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Affiliation(s)
- A Rivas-Ubach
- Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, WA, USA
- CSIC, Global Ecology Unit CREAF-CEAB-CSIC-UAB, Cerdanyola del Vallès, Catalonia, Spain
- Cerdanyola del Vallès, CREAF, Catalonia, Spain
| | - J Sardans
- CSIC, Global Ecology Unit CREAF-CEAB-CSIC-UAB, Cerdanyola del Vallès, Catalonia, Spain
- Cerdanyola del Vallès, CREAF, Catalonia, Spain
| | - J A Hódar
- Grupo de Ecología Terrestre, Departamento de Biología Animal y Ecología, Facultad de Ciencias, Universidad de Granada, Granada, Spain
| | - J Garcia-Porta
- Institute of Evolutionary Biology, CSIC-Universitat Pompeu Fabra, Barcelona, Spain
| | - A Guenther
- Department of Earth System Science, University of California, Irvine, CA, USA
- Global Change Research Centre, Academy of Sciences of the Czech Republic, Brno, Czech Republic
| | - M Oravec
- Global Change Research Centre, Academy of Sciences of the Czech Republic, Brno, Czech Republic
| | - O Urban
- Global Change Research Centre, Academy of Sciences of the Czech Republic, Brno, Czech Republic
| | - J Peñuelas
- CSIC, Global Ecology Unit CREAF-CEAB-CSIC-UAB, Cerdanyola del Vallès, Catalonia, Spain
- Cerdanyola del Vallès, CREAF, Catalonia, Spain
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12
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Sperlich D, Barbeta A, Ogaya R, Sabaté S, Peñuelas J. Balance between carbon gain and loss under long-term drought: impacts on foliar respiration and photosynthesis in Quercus ilex L. J Exp Bot 2016; 67:821-33. [PMID: 26552882 PMCID: PMC4737074 DOI: 10.1093/jxb/erv492] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/05/2023]
Abstract
Terrestrial carbon exchange is a key process of the global carbon cycle consisting of a delicate balance between photosynthetic carbon uptake and respiratory release. We have, however, a limited understanding how long-term decreases in precipitation induced by climate change affect the boundaries and mechanisms of photosynthesis and respiration. We examined the seasonality of photosynthetic and respiratory traits and evaluated the adaptive mechanism of the foliar carbon balance of Quercus ilex L. experiencing a long-term rainfall-exclusion experiment. Day respiration (Rd) but not night respiration (Rn) was generally higher in the drought treatment leading to an increased Rd/Rn ratio. The limitation of mesophyll conductance (gm) on photosynthesis was generally stronger than stomatal limitation (gs) in the drought treatment, reflected in a lower gm/gs ratio. The peak photosynthetic activity in the drought treatment occurred in an atypical favourable summer in parallel with lower Rd/Rn and higher gm/gs ratios. The plant carbon balance was thus strongly improved through: (i) higher photosynthetic rates induced by gm; and (ii) decreased carbon losses mediated by Rd. Interestingly, photosynthetic potentials (Vc,max, Jmax, and TPU) were not affected by the drought treatment, suggesting a dampening effect on the biochemical level in the long term. In summary, the trees experiencing a 14-year-long drought treatment adapted through higher plasticity in photosynthetic and respiratory traits, so that eventually the atypical favourable growth period was exploited more efficiently.
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Affiliation(s)
- D Sperlich
- Departament d'Ecologia, Facultat de Biologia, Universitat de Barcelona, Diagonal 645, 08028 Barcelona, Spain CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - A Barbeta
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain CSIC, Global Ecology Unit CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - R Ogaya
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain CSIC, Global Ecology Unit CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - S Sabaté
- Departament d'Ecologia, Facultat de Biologia, Universitat de Barcelona, Diagonal 645, 08028 Barcelona, Spain CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - J Peñuelas
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain CSIC, Global Ecology Unit CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
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13
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Sperlich D, Chang CT, Peñuelas J, Gracia C, Sabaté S. Seasonal variability of foliar photosynthetic and morphological traits and drought impacts in a Mediterranean mixed forest. Tree Physiol 2015; 35:501-20. [PMID: 25836361 DOI: 10.1093/treephys/tpv017] [Citation(s) in RCA: 17] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/14/2014] [Accepted: 01/29/2015] [Indexed: 05/24/2023]
Abstract
The Mediterranean region is a hot spot of climate change vulnerable to increased droughts and heat waves. Scaling carbon fluxes from leaf to landscape levels is particularly challenging under drought conditions. We aimed to improve the mechanistic understanding of the seasonal acclimation of photosynthesis and morphology in sunlit and shaded leaves of four Mediterranean trees (Quercus ilex L., Pinus halepensis Mill., Arbutus unedo L. and Quercus pubescens Willd.) under natural conditions. Vc,max and Jmax were not constant, and mesophyll conductance was not infinite, as assumed in most terrestrial biosphere models, but varied significantly between seasons, tree species and leaf position. Favourable conditions in winter led to photosynthetic recovery and growth in the evergreens. Under moderate drought, adjustments in the photo/biochemistry and stomatal/mesophyllic diffusion behaviour effectively protected the photosynthetic machineries. Severe drought, however, induced early leaf senescence mostly in A. unedo and Q. pubescens, and significantly increased leaf mass per area in Q. ilex and P. halepensis. Shaded leaves had lower photosynthetic potentials but cushioned negative effects during stress periods. Species-specificity, seasonal variations and leaf position are key factors to explain vegetation responses to abiotic stress and hold great potential to reduce uncertainties in terrestrial biosphere models especially under drought conditions.
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Affiliation(s)
- D Sperlich
- Departament d'Ecologia, Facultat de Biologia, Universitat de Barcelona, Diagonal 645, 08028 Barcelona, Spain CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - C T Chang
- Departament d'Ecologia, Facultat de Biologia, Universitat de Barcelona, Diagonal 645, 08028 Barcelona, Spain CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - J Peñuelas
- CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain CSIC, global Ecology Unit CREAF-CSIC-UAB, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - C Gracia
- Departament d'Ecologia, Facultat de Biologia, Universitat de Barcelona, Diagonal 645, 08028 Barcelona, Spain CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
| | - S Sabaté
- Departament d'Ecologia, Facultat de Biologia, Universitat de Barcelona, Diagonal 645, 08028 Barcelona, Spain CREAF, Cerdanyola del Vallès, 08193 Barcelona, Catalonia, Spain
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Abstract
AIM Phosphorus (P) tends to become limiting in aging terrestrial ecosystems, and its resorption efficiency is higher than for other elements such as nitrogen (N). We thus hypothesized that trees should store more P than those other elements such as N when tree size increases and that this process should be enhanced in slow-growing late successional trees. LOCATION Catalan forests. METHODS We have used data from the Catalan Forest Inventory that contains field data of the P and N contents of total aboveground, foliar and woody biomasses of the diverse Mediterranean, temperate and alpine forests of Catalonia (1018 sites). We used correlation and general lineal models (GLM) to analyze the allometric relationships between nutrient contents of different aboveground biomass fractions (foliar, branches and stems) and total aboveground biomass. RESULTS Aboveground forest P content increases proportionally more than aboveground forest N content with increasing aboveground biomass. Two mechanisms underlie this. First, woody biomass increases proportionally more than foliar biomass having woody biomass higher P:N ratio than foliar biomass. Second, wood P:N ratio increases with tree size. These results are consistent with the generally higher foliar resorption of P than of N. Slow-growing species accumulate more P in total aboveground with size than fast-growing species mainly as a result of their large capacity to store P in wood. MAIN CONCLUSIONS Trees may have thus developed long-term adaptive mechanisms to store P in biomass, mainly in wood, thereby slowing the loss of P from the ecosystems, reducing its availability for competitors, and implying an increase in the P:N ratio in forest biomass with aging. This trend to accumulate more P than N with size is more accentuated in slow-growing, large, long-living species of late successional stages. This way they partly counterbalance the gradual decrease of P in the soil.
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Affiliation(s)
- J Sardans
- CSIC, Global Ecology Unit CREAF-CEAB-CSIC-UAB, Cerdanyola del Vallés, 08193 Barcelona, Catalonia, Spain
- CREAF, Cerdanyola del Vallés, 08193 Barcelona, Catalonia, Spain
- Jordi Sardans. . Tel 34 93 581 29 34. Fax: 34 93 581 41 51
| | - J. Peñuelas
- CSIC, Global Ecology Unit CREAF-CEAB-CSIC-UAB, Cerdanyola del Vallés, 08193 Barcelona, Catalonia, Spain
- CREAF, Cerdanyola del Vallés, 08193 Barcelona, Catalonia, Spain
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15
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Wang SP, Meng FD, Duan JC, Wang YF, Cui XY, Piao SL, Niu HS, Xu GP, Luo CY, Zhang ZH, Zhu XX, Shen MG, Li YN, Du MY, Tang YH, Zhao XQ, Ciais P, Kimball B, Peñuelas J, Janssens IA, Cui SJ, Zhao L, Zhang FW. Asymmetric sensitivity of first flowering date to warming and cooling in alpine plants. Ecology 2014. [DOI: 10.1890/13-2235.1] [Citation(s) in RCA: 56] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Submit a Manuscript] [Subscribe] [Scholar Register] [Indexed: 02/01/2023]
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16
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Wang W, Sardans J, Zeng C, Zhong C, Li Y, Peñuelas J. Responses of soil nutrient concentrations and stoichiometry to different human land uses in a subtropical tidal wetland. Geoderma 2014; 232-234:459-470. [PMID: 25821240 PMCID: PMC4374112 DOI: 10.1016/j.geoderma.2014.06.004] [Citation(s) in RCA: 31] [Impact Index Per Article: 3.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/25/2023]
Abstract
We studied the impacts of anthropogenic changes in land use on the stoichiometric imbalance of soil carbon (C), nitrogen (N), phosphorus (P) and potassium (K) in Phragmites australis wetlands in the Minjiang River estuary. We compared five areas with different land uses: P. australis wetland (control), grassland, a mudskipper breeding flat, pond aquaculture and rice cropland. Human activity has affected the elemental and stoichiometric compositions of soils through changes in land use. In general, soil C and N concentrations were lower and total soil K concentrations were higher at the sites under human land uses relative to the control site, and total soil P concentrations were generally not significantly different. The close relationship between total soil C and N concentrations in all cases, including fertilization with N, suggested that N was the most limiting nutrient in these wetlands. Lower soil N concentrations and similar soil P concentrations and higher soil K concentrations under human land-use activities suggest that human activity has increased the role of N limitation in these wetlands. Only grassland use increases soil N contents (only in the 0-10 cm of soil). Despite N fertilization, lower soil N concentrations were also observed in the rice cropland, indicating the difficulty of avoiding N limitation in these wetlands. The observed lower soil N:P ratio, together with higher soil P and K availabilities in rice croplands, is consistent with the tendency of human activity to change the competitive relationships of plants, in this case favoring species adapted to high rates of growth (low N:P ratio) and/or favoring plants with high demands for P and K. Both, soil C storage and respiration were higher in grasslands, likely due to the introduction of grasses, which led to a high density of plants, increased grazing activity and soil compaction. Soil C storage and respiration were lower under human land uses, except in the rice cropland, with respect to natural wetland. Using overall data, soil C storage and respiration were correlated, indicating that soil respiration was correlated with plant productivity. In this wetland area the impacts of different human land-uses on soil stoichiometry and C-cycle can be very different depending on the activity. Further regeneration of natural communities can be determined by the previous type of land-use.
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Affiliation(s)
- W. Wang
- Institute of Geography, Fujian Normal University, Fuzhou 350007, China
| | - J. Sardans
- CSIC, Global Ecology CREAF-CEAB-CSIC-UAB, Cerdanyola del Valles, 08193 Barcelona, Catalonia, Spain
- CREAF, Cerdanyola del Valles, 08193 Barcelona, Catalonia, Spain
| | - C. Zeng
- Institute of Geography, Fujian Normal University, Fuzhou 350007, China
| | - C. Zhong
- Institute of Geography, Fujian Normal University, Fuzhou 350007, China
| | - Y. Li
- Key Laboratory of Agro-ecological Process in the Subtropical Region, Chinese Academy of Sciences, Hunan 410125, China
| | - J. Peñuelas
- CSIC, Global Ecology CREAF-CEAB-CSIC-UAB, Cerdanyola del Valles, 08193 Barcelona, Catalonia, Spain
- CREAF, Cerdanyola del Valles, 08193 Barcelona, Catalonia, Spain
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Peñuelas J, Asensio D, Tholl D, Wenke K, Rosenkranz M, Piechulla B, Schnitzler JP. Biogenic volatile emissions from the soil. Plant Cell Environ 2014; 37:1866-91. [PMID: 24689847 DOI: 10.1111/pce.12340] [Citation(s) in RCA: 146] [Impact Index Per Article: 14.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/16/2013] [Revised: 03/10/2014] [Accepted: 03/14/2014] [Indexed: 05/18/2023]
Abstract
Volatile compounds are usually associated with an appearance/presence in the atmosphere. Recent advances, however, indicated that the soil is a huge reservoir and source of biogenic volatile organic compounds (bVOCs), which are formed from decomposing litter and dead organic material or are synthesized by underground living organism or organs and tissues of plants. This review summarizes the scarce available data on the exchange of VOCs between soil and atmosphere and the features of the soil and particle structure allowing diffusion of volatiles in the soil, which is the prerequisite for biological VOC-based interactions. In fact, soil may function either as a sink or as a source of bVOCs. Soil VOC emissions to the atmosphere are often 1-2 (0-3) orders of magnitude lower than those from aboveground vegetation. Microorganisms and the plant root system are the major sources for bVOCs. The current methodology to detect belowground volatiles is described as well as the metabolic capabilities resulting in the wealth of microbial and root VOC emissions. Furthermore, VOC profiles are discussed as non-destructive fingerprints for the detection of organisms. In the last chapter, belowground volatile-based bi- and multi-trophic interactions between microorganisms, plants and invertebrates in the soil are discussed.
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Affiliation(s)
- J Peñuelas
- Global Ecology Unit CREAF-CEAB-CSIC-UAB, CSIC, Catalonia, Spain; CREAF, Catalonia, Spain
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Rico L, Ogaya R, Terradas J, Peñuelas J. Community structures of N2 -fixing bacteria associated with the phyllosphere of a Holm oak forest and their response to drought. Plant Biol (Stuttg) 2014; 16:586-93. [PMID: 23952768 DOI: 10.1111/plb.12082] [Citation(s) in RCA: 36] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/18/2013] [Accepted: 06/26/2013] [Indexed: 05/22/2023]
Abstract
Biological nitrogen (N) fixation is a key pathway in terrestrial ecosystems and is therefore critical for understanding the responses of ecosystems to global environmental changes. The free-living diazotrophic community is distributed along the canopy-to-soil profile, but the ecological significance of epiphyllic N2 fixers, despite their functional relevance, on plant foliar surfaces remains very poorly understood compared with the N2 -fixing community in forest litter and soils. We assessed the community structure of N2 fixers and overall bacteria by genetic fingerprinting (t-RFLP) to explore the seasonal successional patterns of the microbial community in the natural phyllosphere of a Holm oak (Quercus ilex) forest submitted to 12-year field experiment of rain exclusion mimicking the conditions of drought projected for the coming decades. Leaves of Holm oak were analysed in different seasons over a period of 1.5 years. The bacterial community of the phyllosphere did not correspond to the surrounding soil biome in the same area. These analyses provided field evidence for the presence of free-living diazotrophs associated with the tissues of leaves of Holm oak, the dominant tree species of many Mediterranean forests. The results also revealed that the community composition is affected seasonally and inter-annually by the environment, and that the composition shifts in response to climate change. Drought treatment increased the richness of the epiphyllic microbial community, especially during the summer. These changes were associated with higher C:N ratios of leaves observed in response to drought in semiarid areas. This epiphyllic microbiota that can potentially fix N2 extends the capacity of plants to adapt to the environment.
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Affiliation(s)
- L Rico
- CSIC, Global Ecology Unit CREAF-CEAB-UAB, Cerdanyola del Vallès, Catalonia, Spain; CREAF, Cerdanyola del Vallès, Catalonia, Spain
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Sardans J, Peñuelas J. Climate and taxonomy underlie different elemental concentrations and stoichiometries of forest species: the optimum "biogeochemical niche". Plant Ecol 2014; 215:441-455. [PMID: 25983614 PMCID: PMC4430814 DOI: 10.1007/s11258-014-0314-2] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/31/2023]
Abstract
We previously hypothesised the existence of a "biogeochemical niche" occupied by each plant species. Different species should have a specific elemental composition, stoichiometry and allocation as a consequence of their particular metabolism, physiology and structure (morphology) linked to their optimal functioning under the environmental (abiotic and biotic) conditions where they have evolved. We tested this hypothesis using data from the Catalan Forestry Inventory that covers different forest groups growing under a large climatic gradient. Mediterranean species that occupy hotter-drier environments have lower leaf N, P and K concentrations than non-Mediterranean forest species. Within a determined climatic biome, different species competing in the same space have different elemental compositions and allocations linked to their taxonomical differences and their phenotypic plasticity. Gymnosperms have a proportionally higher elemental allocation to leaves than to wood, higher C concentrations, and lower N, P and K concentrations mainly in the stem and branches than angiosperms. The differences among species are linked to asymmetrical use of different elements, suggesting that the biogeochemical niche is a final expression and consequence of long-term species adaptation to particular abiotic factors, ecological role (stress tolerant, ruderal, competitor), different soil occupation and use of resources to avoid interspecific competition, and finally of a certain degree of flexibility to adapt to current environmental shifts.
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Affiliation(s)
- J Sardans
- CSIC, Global Ecology Unit (CREAF-CEAB-CSIC-UAB), Universitat Autonoma de Barcelona, 08913 Cerdanyola del Vallès, Catalonia, Spain ; CREAF, 08913 Cerdanyola del Vallès, Catalonia, Spain
| | - J Peñuelas
- CSIC, Global Ecology Unit (CREAF-CEAB-CSIC-UAB), Universitat Autonoma de Barcelona, 08913 Cerdanyola del Vallès, Catalonia, Spain ; CREAF, 08913 Cerdanyola del Vallès, Catalonia, Spain
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Rico L, Ogaya R, Barbeta A, Peñuelas J. Changes in DNA methylation fingerprint of Quercus ilex trees in response to experimental field drought simulating projected climate change. Plant Biol (Stuttg) 2014; 16:419-27. [PMID: 23889779 DOI: 10.1111/plb.12049] [Citation(s) in RCA: 33] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/23/2013] [Accepted: 04/11/2013] [Indexed: 05/22/2023]
Abstract
Rapid genetic changes in plants have been reported in response to current climate change. We assessed the capacity of trees in a natural forest to produce rapid acclimation responses based on epigenetic modifications. We analysed natural populations of Quercus ilex, the dominant tree species of Mediterranean forests, using the methylation-sensitive amplified polymorphism (MSAP) technique to assess patterns and levels of methylation in individuals from unstressed forest plots and from plots experimentally exposed to drought for 12 years at levels projected for the coming decades. The percentage of hypermethylated loci increased, and the percentage of fully methylated loci clearly decreased in plants exposed to drought. Multivariate analyses exploring the status of methylation at MSAP loci also showed clear differentiation depending on stress. The PCA scores for the MSAP profiles clearly separated the genetic from the epigenetic structure, and also significantly separated the samples within each group in response to drought. Changes in DNA methylation highlight the large capacity of plants to rapidly acclimate to changing environmental conditions, including trees with long life spans, and our results demonstrate those changes. These changes, although unable to prevent the decreased growth and higher mortality associated with this experimental drought, occurred together with a dampening in such decreases as the long-term treatment progressed.
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Affiliation(s)
- L Rico
- CSIC, Global Ecology Unit CREAF-CEAB-UAB, Catalonia, Spain; CREAF, Cerdanyola del Vallès, Catalonia, Spain
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Sardans J, Gargallo-Garriga A, Pérez-Trujillo M, Parella TJ, Seco R, Filella I, Peñuelas J. Metabolic responses of Quercus ilex seedlings to wounding analysed with nuclear magnetic resonance profiling. Plant Biol (Stuttg) 2014; 16:395-403. [PMID: 23590498 DOI: 10.1111/plb.12032] [Citation(s) in RCA: 17] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/15/2013] [Accepted: 03/01/2013] [Indexed: 06/02/2023]
Abstract
Plants defend themselves against herbivory at several levels. One of these is the synthesis of inducible chemical defences. Using NMR metabolomic techniques, we studied the metabolic changes of plant leaves after a wounding treatment simulating herbivore attack in the Mediterranean sclerophyllous tree Quercus ilex. First, an increase in glucose content was observed in wounded plants. There was also an increase in the content of C-rich secondary metabolites such as quinic acid and quercitol, both related to the shikimic acid pathway and linked to defence against biotic stress. There was also a shift in N-storing amino acids, from leucine and isoleucine to asparagine and choline. The observed higher content of asparagine is related to the higher content of choline through serine that was proved to be the precursor of choline. Choline is a general anti-herbivore and pathogen deterrent. The study shows the rapid metabolic response of Q. ilex in defending its leaves, based on a rapid increase in the production of quinic acid, quercitol and choline. The results also confirm the suitability of (1)H NMR-based metabolomic profiling studies to detect global metabolome shifts after wounding stress in tree leaves, and therefore its suitability in ecometabolomic studies.
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Affiliation(s)
- J Sardans
- CREAF, Cerdanyola del Vallés, Catalonia, Spain; Global Ecology Unit CREAF-CEAB-UAB, CSIC, Bellaterra, Catalonia, Spain
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Abstract
BACKGROUND In the Mediterranean climate, plants have evolved under conditions of low soil-water and nutrient availabilities and have acquired a series of adaptive traits that, in turn exert strong feedback on soil fertility, structure, and protection. As a result, plant-soil systems constitute complex interactive webs where these adaptive traits allow plants to maximize the use of scarce resources. SCOPE It is necessary to review the current bibliography to highlight the most know characteristic mechanisms underlying Mediterranean plant-soil feed-backs and identify the processes that merit further research in order to reach an understanding of the plant-soil feed-backs and its capacity to cope with future global change scenarios. In this review, we characterize the functional and structural plant-soil relationships and feedbacks in Mediterranean regions. We thereafter discuss the effects of global change drivers on these complex interactions between plants and soil. CONCLUSIONS The large plant diversity that characterizes Mediterranean ecosystems is associated to the success of coexisting species in avoiding competition for soil resources by differential exploitation in space (soil layers) and time (year and daily). Among plant and soil traits, high foliar nutrient re-translocation and large contents of recalcitrant compounds reduce nutrient cycling. Meanwhile increased allocation of resources to roots and soil enzymes help to protect against soil erosion and to improve soil fertility and capacity to retain water. The long-term evolutionary adaptation to drought of Mediterranean plants allows them to cope with moderate increases of drought without significant losses of production and survival in some species. However, other species have proved to be more sensitive decreasing their growth and increasing their mortality under moderate rising of drought. All these increases contribute to species composition shifts. Moreover, in more xeric sites, the desertification resulting from synergic interactions among some related process such as drought increases, torrential rainfall increases and human driven disturbances is an increasing concern. A research priority now is to discern the effects of long-term increases in atmospheric CO2 concentrations, warming, and drought on soil fertility and water availability and on the structure of soil communities (e.g. shifts from bacteria to fungi) and on patching vegetation and root-water uplift (from soil to plant and from soil deep layers to soil superficial layers) roles in desertification.
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Affiliation(s)
- J Sardans
- CSIC Global Ecology Unit CREAF-CEAB-UAB. 08913 Cerdanyola del Vallés. Catalonia, Spain
- CREAF, 08913 Cerdanyola del Vallés. Catalonia, Spain
| | - J Peñuelas
- CSIC Global Ecology Unit CREAF-CEAB-UAB. 08913 Cerdanyola del Vallés. Catalonia, Spain
- CREAF, 08913 Cerdanyola del Vallés. Catalonia, Spain
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Peñuelas J, Rico L, Ogaya R, Jump AS, Terradas J. Summer season and long-term drought increase the richness of bacteria and fungi in the foliar phyllosphere of Quercus ilex in a mixed Mediterranean forest. Plant Biol (Stuttg) 2012; 14:565-575. [PMID: 22289059 DOI: 10.1111/j.1438-8677.2011.00532.x] [Citation(s) in RCA: 68] [Impact Index Per Article: 5.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/31/2023]
Abstract
We explored the changes in richness, diversity and evenness of epiphytic (on the leaf surface) and endophytic (within leaf tissues) bacteria and fungi in the foliar phyllosphere of Quercus ilex, the dominant tree species of Mediterranean forests. Bacteria and fungi were assessed during ontogenic development of the leaves, from the wet spring to the dry summer season in control plots and in plots subjected to drought conditions mimicking those projected for future decades. Our aim was to monitor succession in microbiota during the colonisation of plant leaves and its response to climate change. Ontogeny and seasonality exerted a strong influence on richness and diversity of the microbial phyllosphere community, which decreased in summer in the whole leaf and increased in summer in the epiphytic phyllosphere. Drought precluded the decrease in whole leaf phyllosphere diversity and increased the rise in the epiphytic phyllosphere. Both whole leaf bacterial and fungal richness decreased with the decrease in physiological activity and productivity of the summer season in control trees. As expected, the richness of epiphytic bacteria and fungi increased in summer after increasing time of colonisation. Under summer dry conditions, there was a positive relationship between TRF (terminal restriction fragments) richness and drought, both for whole leaf and epiphytic phyllosphere, and especially for fungal communities. These results demonstrate that changes in climate are likely to significantly alter microbial abundance and composition of the phyllosphere. Given the diverse functions and large number of phyllospheric microbes, the potential functional implications of such community shifts warrant exploration.
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Affiliation(s)
- J Peñuelas
- Global Ecology Unit, Center for Ecological Research and Forestry Applications, Universitat Autònoma Barcelona, Bellaterra, Spain.
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Reche C, Viana M, Amato F, Alastuey A, Moreno T, Hillamo R, Teinilä K, Saarnio K, Seco R, Peñuelas J, Mohr C, Prévôt ASH, Querol X. Biomass burning contributions to urban aerosols in a coastal Mediterranean city. Sci Total Environ 2012; 427-428:175-190. [PMID: 22554530 DOI: 10.1016/j.scitotenv.2012.04.012] [Citation(s) in RCA: 19] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/23/2011] [Revised: 02/22/2012] [Accepted: 04/02/2012] [Indexed: 05/31/2023]
Abstract
Mean annual biomass burning contributions to the bulk particulate matter (PM(X)) load were quantified in a southern-European urban environment (Barcelona, Spain) with special attention to typical Mediterranean winter and summer conditions. In spite of the complexity of the local air pollution cocktail and the expected low contribution of biomass burning emissions to PM levels in Southern Europe, the impact of these emissions was detected at an urban background site by means of tracers such as levoglucosan, K(+) and organic carbon (OC). The significant correlation between levoglucosan and OC (r(2)=0.77) and K(+) (r(2)=0.65), as well as a marked day/night variability of the levoglucosan levels and levoglucosan/OC ratios was indicative of the contribution from regional scale biomass burning emissions during night-time transported by land breezes. In addition, on specific days (21-22 March), the contribution from long-range transported biomass burning aerosols was detected. Quantification of the contribution of biomass burning aerosols to PM levels on an annual basis was possible by means of the Multilinear Engine (ME). Biomass burning emissions accounted for 3% of PM(10) and PM(2.5) (annual mean), while this percentage increased up to 5% of PM(1). During the winter period, regional-scale biomass burning emissions (agricultural waste burning) were estimated to contribute with 7±4% of PM(2.5) aerosols during night-time (period when emissions were clearly detected). Long-range transported biomass burning aerosols (possibly from forest fires and/or agricultural waste burning) accounted for 5±2% of PM(2.5) during specific episodes. Annually, biomass burning emissions accounted for 19%-21% of OC levels in PM(10), PM(2.5) and PM(1). The contribution of this source to K(+) ranged between 48% for PM(10) and 97% for PM(1) (annual mean). Results for K(+) from biomass burning evidenced that this tracer is mostly emitted in the fine fraction, and thus coarse K(+) could not be taken as an appropriate tracer of biomass burning.
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Affiliation(s)
- C Reche
- Institute of Environmental Assessment and Water Research, IDAEA, CSIC, c/ Jordi Girona 18-26, Barcelona, Spain.
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Vicca S, Luyssaert S, Peñuelas J, Campioli M, Chapin FS, Ciais P, Heinemeyer A, Högberg P, Kutsch WL, Law BE, Malhi Y, Papale D, Piao SL, Reichstein M, Schulze ED, Janssens IA. Fertile forests produce biomass more efficiently. Ecol Lett 2012; 15:520-6. [DOI: 10.1111/j.1461-0248.2012.01775.x] [Citation(s) in RCA: 229] [Impact Index Per Article: 19.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
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Blanch JS, Sampedro L, Llusià J, Moreira X, Zas R, Peñuelas J. Effects of phosphorus availability and genetic variation of leaf terpene content and emission rate in Pinus pinaster seedlings susceptible and resistant to the pine weevil, Hylobius abietis. Plant Biol (Stuttg) 2012; 14 Suppl 1:66-72. [PMID: 21972958 DOI: 10.1111/j.1438-8677.2011.00492.x] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/31/2023]
Abstract
We studied the effects of phosphorus fertilisation on foliar terpene concentrations and foliar volatile terpene emission rates in six half-sib families of Pinus pinaster Ait. seedlings. Half of the seedlings were resistant to attack of the pine weevil Hylobius abietis L., a generalist phloem feeder, and the remaining seedlings were susceptible to this insect. We hypothesised that P stress could modify the terpene concentration in the needles and thus lead to altered terpene emission patterns relevant to plant-insect signalling. The total concentration and emission rate ranged between 5732 and 13,995 μg·g(-1) DW and between 2 and 22 μg·g(-1) DW·h(-1), respectively. Storage and emission were dominated by the isomers α- and β-pinene (77.2% and 84.2% of the total terpene amount amassed and released, respectively). In both resistant and susceptible families, P stress caused an increase of 31% in foliar terpene concentration with an associated 5-fold decrease in terpene emission rates. A higher terpene content in the leaves implies that the 'excess carbon', available under limiting growth conditions (P scarcity), is allocated to terpene production. Sensitive families showed a greater increase in terpene emission rates with increasing P concentrations, which could explain their susceptibility to H. abietis.
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Affiliation(s)
- J-S Blanch
- Global Ecology Unit CREAF-CEAB-CSIC, Universitat Autònoma de Barcelona, Bellaterra, Spain.
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Jump AS, Rico L, Coll M, Peñuelas J. Wide variation in spatial genetic structure between natural populations of the European beech (Fagus sylvatica) and its implications for SGS comparability. Heredity (Edinb) 2012; 108:633-9. [PMID: 22354112 DOI: 10.1038/hdy.2012.1] [Citation(s) in RCA: 23] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022] Open
Abstract
Identification and quantification of spatial genetic structure (SGS) within populations remains a central element of understanding population structure at the local scale. Understanding such structure can inform on aspects of the species' biology, such as establishment patterns and gene dispersal distance, in addition to sampling design for genetic resource management and conservation. However, recent work has identified that variation in factors such as sampling methodology, population characteristics and marker system can all lead to significant variation in SGS estimates. Consequently, the extent to which estimates of SGS can be relied on to inform on the biology of a species or differentiate between experimental treatments is open to doubt. Following on from a recent report of unusually extensive SGS when assessed using amplified fragment length polymorphisms in the tree Fagus sylvatica, we explored whether this marker system led to similarly high estimates of SGS extent in other apparently similar populations of this species. In the three populations assessed, SGS extent was even stronger than this previously reported maximum, extending up to 360 m, an increase in up to 800% in comparison with the generally accepted maximum of 30-40 m based on the literature. Within this species, wide variation in SGS estimates exists, whether quantified as SGS intensity, extent or the Sp parameter. Consequently, we argue that greater standardization should be applied in sample design and SGS estimation and highlight five steps that can be taken to maximize the comparability between SGS estimates.
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Affiliation(s)
- A S Jump
- Biological and Environmental Sciences, School of Natural Sciences, University of Stirling, Stirling, UK.
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Ogaya R, Llorens L, Peñuelas J. Density and length of stomatal and epidermal cells in "living fossil" trees grown under elevated CO2 and a polar light regime. Acta Oecologica 2011. [DOI: 10.1016/j.actao.2011.04.010] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 10/18/2022]
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Peñuelas J, Sardans J, Llusia J, Owen SM, Niinemets Ü. Lower P contents and more widespread terpene presence in old Bornean than in young Hawaiian tropical plant species guilds. Ecosphere 2011. [DOI: 10.1890/es10-00185.1] [Citation(s) in RCA: 10] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
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Abstract
Current climate projections predict drier and warmer conditions in the Mediterranean basin over the next century. While advanced spring growth due to warming has been described in the literature, few data are available on the effects of drought on phenology. Hence, the phenology and growth of two Mediterranean shrubs, Erica multiflora and Globularia alypum, was studied in a rainfall exclusion field experiment to simulate spring drought in a natural shrubland. We estimated the onset of growth in spring by monitoring the appearance of new stems, and the end of growth in summer by following the elongation of stems. Drought treatment caused earlier onset of the spring growing season in E. multiflora, whereas no advance was observed in G. alypum. However, growth cessation was not affected in E. multiflora. Drought reduced the growth of both shrubs, as reflected in less stem elongation. The results show that a drier climate might affect not only growth but also spring phenology of some Mediterranean species. We suggest that a reduction in the cooling effect of transpiration may have analogous effects to warming and might advance the start of growth in E. multiflora, a species whose phenology has been described as warming-sensitive. The lengthening of the growing season resulting from advanced growth did not imply higher productivity, as growth was restricted by drought.
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Affiliation(s)
- M Bernal
- Global Ecology Unit CSIC-CEAB-CREAF, Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, Bellaterra, Spain
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Abstract
Fumana thymifolia (Cistaceae) is an insect-pollinated, gravity-dispersed evergreen shrub, which is a common component of fire-prone Mediterranean shrubland ecosystems. Despite the availability of basic knowledge on its ecology, little is known of its breeding system and no information is available on its population genetic structure. We explored the within-population genetic structure of this species using amplified fragment length polymorphism (AFLP) molecular markers and related this to predictions based on its breeding system, pollen and seed dispersal. Existing information on the reproductive ecology of F. thymifolia was supplemented by artificial pollination experiments. We determined that self-fertilisation can occur in F. thymifolia but results in reduced fruit set. Significant genetic structuring was detected within the population, a likely consequence of localised seed dispersal in combination with a mixed mating system. In a study site covering approximately 0.5 ha, amova revealed that approximately 9% of genetic variability was distributed among population subsamples. Significant spatial genetic structure was detected, with kinship coefficients being significantly elevated above the null expectation in the first six distance classes (maximum 5 m), and a value of Sp of up to 0.0342, comparable with species having similar ecological characteristics. Weak isolation by distance at the plot scale was detected, suggesting that insect-mediated pollen flow is non-random, despite being more extensive than seed dispersal. Fumana thymifolia provides a promising model for the investigation of both short- and long-term population dynamics in relation to fire frequency within this plant community.
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Affiliation(s)
- A S Jump
- Unitat d'Ecofisiologia i Canvi Global CSIC-CEAB-CREAF, CREAF (Centre de Recerca Ecològica i Aplicacions Forestals), Universitat Autònoma de Barcelona, Bellaterra (Barcelona), Spain.
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Llorens L, Llusià J, Murchie EH, Peñuelas J, Beerling DJ. Monoterpene emissions and photoinhibition of “living fossil” trees grown under CO2enrichment in a simulated Cretaceous polar environment. ACTA ACUST UNITED AC 2009. [DOI: 10.1029/2008jg000802] [Citation(s) in RCA: 10] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Beier C, Emmett BA, Peñuelas J, Schmidt IK, Tietema A, Estiarte M, Gundersen P, Llorens L, Riis-Nielsen T, Sowerby A, Gorissen A. Carbon and nitrogen cycles in European ecosystems respond differently to global warming. Sci Total Environ 2008; 407:692-697. [PMID: 18930514 DOI: 10.1016/j.scitotenv.2008.10.001] [Citation(s) in RCA: 49] [Impact Index Per Article: 3.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/26/2023]
Abstract
The global climate is predicted to become significantly warmer over the next century. This will affect ecosystem processes and the functioning of semi natural and natural ecosystems in many parts of the world. However, as various ecosystem processes may be affected to a different extent, balances between different ecosystem processes as well as between different ecosystems may shift and lead to major unpredicted changes. In this study four European shrubland ecosystems along a north-south temperature gradient were experimentally warmed by a novel nighttime warming technique. Biogeochemical cycling of both carbon and nitrogen was affected at the colder sites with increased carbon uptake for plant growth as well as increased carbon loss through soil respiration. Carbon uptake by plant growth was more sensitive to warming than expected from the temperature response across the sites while carbon loss through soil respiration reacted to warming in agreement with the overall Q10 and response functions to temperature across the sites. Opposite to carbon, the nitrogen mineralization was relatively insensitive to the temperature increase and was mainly affected by changes in soil moisture. The results suggest that C and N cycles respond asymmetrically to warming, which may lead to progressive nitrogen limitation and thereby acclimation in plant production. This further suggests that in many temperate zones nitrogen deposition has to be accounted for, not only with respect to the impact on water quality through increased nitrogen leaching where N deposition is high, but also in predictions of carbon sequestration in terrestrial ecosystems under future climatic conditions. Finally the results indicate that on the short term the above-ground processes are more sensitive to temperature changes than the below ground processes.
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Affiliation(s)
- C Beier
- RISØ National Laboratory for Sustainable Energy, Risø DTU, P. O. Box 49, DK-4000 Roskilde, Denmark.
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Sardans J, Peñuelas J, Prieto P, Estiarte M. Changes in Ca, Fe, Mg, Mo, Na, and S content in a Mediterranean shrubland under warming and drought. ACTA ACUST UNITED AC 2008. [DOI: 10.1029/2008jg000795] [Citation(s) in RCA: 27] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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Rapparini F, Llusià J, Peñuelas J. Effect of arbuscular mycorrhizal (AM) colonization on terpene emission and content of Artemisia annua L. Plant Biol (Stuttg) 2008; 10:108-22. [PMID: 18211551 DOI: 10.1055/s-2007-964963] [Citation(s) in RCA: 42] [Impact Index Per Article: 2.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/10/2023]
Abstract
Plant roots interact with a wide variety of rhizospheric microorganisms, including bacteria and the symbiontic arbuscular mycorrhizal (AM) fungi. The mycorrhizal symbiosis represents a series of complex feedbacks between plant and fungus regulated by their physiology and nutrition. Despite the widespread distribution and ecological significance of AM symbiosis, little is known about the potential of AM fungi to affect plant VOC metabolism. The purpose of this study was to investigate whether colonization of plant roots by AM fungi and associated soil microorganisms affects VOC emission and content of Artemisia annua L. plants (Asteraceae). Two inoculum types were evaluated: one consisted of only an arbuscular mycorrhizal (AM) fungus species (Glomus spp.), and the other was a mixture of different Glomus species and associated soil bacteria. Inoculated plants were compared with non-inoculated plants and with plants supplemented with extra phosphorus (P) to obtain plants of the same size as mycorrhizal plants, thus excluding potentially-confounding mycorrhizal effects on shoot growth. VOC emissions of Artemisia annua plants were analyzed by leaf cuvette sampling followed by off-line measurements with pre-concentration and gas chromatography mass spectrometry (GC-MS). Measurements of CO(2) and H(2)O exchanges were conducted simultaneously. Several volatile monoterpenes were identified and characterized from leaf emissions of Artemisia annua L. by GC-MS analysis. The main components identified belong to different monoterpene structures: alpha-pinene, beta-pinene, camphor, 1,8-cineole, limonene, and artemisia ketone. A good correlation between monoterpene leaf concentration and leaf emission was found. Leaf extracts included also several sesquiterpenes. Total terpene content and emission was not affected by AM inoculation with or without bacteria, while emission of limonene and artemisia ketone was stimulated by this treatment. No differences were found among treatments for single monoterpene content, while accumulation of specific sesquiterpenes in leaves was altered in mycorrhizal plants compared to control plants. Growth conditions seemed to have mainly contributed to the outcome of the symbiosis and influenced the magnitude of the plant response. These results highlight the importance of considering the below-ground interaction between plant and soil for estimating VOC emission rates and their ecological role at multitrophic levels.
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Affiliation(s)
- F Rapparini
- Biometeorology Institute, IBIMET-CNR, Via P. Gobetti 101, 40129 Bologna, Italy.
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Alessio GA, Peñuelas J, De Lillis M, Llusià J. Implications of foliar terpene content and hydration on leaf flammability of Quercus ilex and Pinus halepensis. Plant Biol (Stuttg) 2008; 10:123-8. [PMID: 18211552 DOI: 10.1111/j.1438-8677.2007.00011.x] [Citation(s) in RCA: 8] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/04/2023]
Abstract
We investigated the implications of foliar hydration and terpene content on leaf flammability in two widely distributed forest species of the Mediterranean basin, Quercus ilex, which does not store terpenes, and Pinus halepensis, a terpene-storing species. The experiments were carried out in plants grown under different water regimes that generated a wide range of foliar hydration and terpene contents. We monitored the temperatures and time elapsed to reach the smoke, pyrolysis and flame phases. Smoke appeared much earlier (37 versus 101 s) and at lower temperatures (96 versus 139 degrees C) in Quercus ilex than in Pinus halepensis. Quercus ilex reached pyrolysis earlier than Pinus halepensis (278 versus 338 s) but at the same temperature (365-371 degrees C). There were no significant differences in time elapsed nor in temperature for flammability (386-422 s; 505-487 degrees C in both species). Quercus ilex had lower water hydration than Pinus halepensis (41 versus 100%) and the leaf content of terpenes in Quercus was three orders of magnitude lower. The results of this study show no differences in the flame phase between the two species and the absence of a significant relationship between temperature and elapsed time of the different flammability phases in relation to monoterpene content; thus indicating that the role of monoterpenes in flammability phases is smaller than that of the water content. This, however, does not exclude the effects of terpene content on plant combustibility and fire propagation once fires start.
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Affiliation(s)
- G A Alessio
- Unitat d'Ecofisiologia i Canvi Global CREAF-CSIC-CEAB, Universitat Autònoma de Barcelona, Barcelona, Spain.
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Sardans J, Peñuelas J, Estiarte M. Warming and drought change trace element bioaccumulation patterns in a Mediterranean shrubland. Chemosphere 2008; 70:874-85. [PMID: 17709128 DOI: 10.1016/j.chemosphere.2007.06.085] [Citation(s) in RCA: 22] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/20/2007] [Revised: 06/27/2007] [Accepted: 06/30/2007] [Indexed: 05/16/2023]
Abstract
A field experiment consisting of drought and warming manipulation was conducted in a Mediterranean shrubland dominated by the shrubs Erica multiflora and Globularia alypum. The aim was to investigate the effects of the climatic changes predicted by IPCC models for the coming decades on trace element concentration and accumulation in aboveground biomass, plant litter, and soil. Warming increased concentrations and aboveground accumulation of some trace elements related to plant root uptake, such as Al, As, Cr, Cu, and partially Pb. This effect was more general in E. multiflora than in G. alypum. The stronger effects were increases in Al leaf concentrations (42%) and aboveground accumulation (500gha(-1)) in E. multiflora, in As stem biomass accumulation (0.2gha(-1)) in E. multiflora, and in Cr leaf concentrations (51%) in G. alypum and stem aboveground accumulation in E. multiflora (1.1gha(-1)). These species-specific increases were related to greater retranslocation, photosynthetic capacity and growth in E. multiflora than in G. alypum. Warming decreased the concentrations of some trace elements in leaf litter, implying the existence of an increased leaf retranslocation. Drought increased As (40%) and Cd (55%) in E. multiflora stems, whereas it decreased Cu (50%) in leaves, Ni (28%) in stems and Pb (32%) in leaf litter of G. alypum. The increasing concentrations of some trace elements in E. multiflora and not in G. alypum were related to a greater growth reduction in E. multiflora than in G. alypum. Warming increased As soil solubility (67%) and decreased total soil As (21%). Those changes were related to a greater Fe mobilization in warming plot and to a greater plant capture. Drought increased Hg (350%) concentrations in soils but had no significant effects on trace element accumulation in aboveground biomass. The different response to warming and drought in the two dominant species implies uneven changes in the quality of the plant tissues that may have implications for herbivores. This may be specially important for the performance of the studied Mediterranean ecosystems under the warmer and drier conditions predicted by the next decades by the GCM and ecophysiological models.
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Affiliation(s)
- J Sardans
- Universitat Autònoma de Barcelona, E-08193 Bellaterra, Spain.
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Abstract
Research on biogenic volatile organic compound (BVOC) emissions has mainly focused on native species in natural ecosystems. However, much of the ozone and aerosol formation occurs in city atmospheres due to BVOC emissions by local urban vegetation. Plant composition of urban habitats is often dominated by non-native ornamental plant species, for which only limited data on BVOC emissions are available. To gain insight into the influence of ornamental vegetation on the urban atmospheric reactivity in Barcelona, Spain, we studied volatile isoprenoid emissions in 11 widespread ornamental tree species (three conifers and nine angiosperms). We found significant monoterpene emissions in all studied species, with normalized emission potentials (T=30 degrees C, photosynthetic photon flux density (PPFD)=1000 micromol x m(-2) x s(-1)) ranging between 0.2 to 110 microg x g(-1) (dry weight) h(-1). Depending on species, the emissions were dominated by alpha- and beta-pinene, myrcene, alpha- and beta-phellandrene, carene, limonene and eucalyptol. These data demonstrate that ornamental plants may significantly contribute to the BVOC load in urban atmospheres and also underscore the importance of broadleaf angiosperms as significant monoterpene emitters.
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Affiliation(s)
- S M Noe
- Department of Plant Physiology, University of Tartu, Tartu, Estonia.
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Sutton MA, Nemitz E, Erisman JW, Beier C, Bahl KB, Cellier P, de Vries W, Cotrufo F, Skiba U, Di Marco C, Jones S, Laville P, Soussana JF, Loubet B, Twigg M, Famulari D, Whitehead J, Gallagher MW, Neftel A, Flechard CR, Herrmann B, Calanca PL, Schjoerring JK, Daemmgen U, Horvath L, Tang YS, Emmett BA, Tietema A, Peñuelas J, Kesik M, Brueggemann N, Pilegaard K, Vesala T, Campbell CL, Olesen JE, Dragosits U, Theobald MR, Levy P, Mobbs DC, Milne R, Viovy N, Vuichard N, Smith JU, Smith P, Bergamaschi P, Fowler D, Reis S. Challenges in quantifying biosphere-atmosphere exchange of nitrogen species. Environ Pollut 2007; 150:125-39. [PMID: 17604887 DOI: 10.1016/j.envpol.2007.04.014] [Citation(s) in RCA: 15] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/16/2006] [Revised: 02/19/2007] [Accepted: 04/15/2007] [Indexed: 05/16/2023]
Abstract
Recent research in nitrogen exchange with the atmosphere has separated research communities according to N form. The integrated perspective needed to quantify the net effect of N on greenhouse-gas balance is being addressed by the NitroEurope Integrated Project (NEU). Recent advances have depended on improved methodologies, while ongoing challenges include gas-aerosol interactions, organic nitrogen and N(2) fluxes. The NEU strategy applies a 3-tier Flux Network together with a Manipulation Network of global-change experiments, linked by common protocols to facilitate model application. Substantial progress has been made in modelling N fluxes, especially for N(2)O, NO and bi-directional NH(3) exchange. Landscape analysis represents an emerging challenge to address the spatial interactions between farms, fields, ecosystems, catchments and air dispersion/deposition. European up-scaling of N fluxes is highly uncertain and a key priority is for better data on agricultural practices. Finally, attention is needed to develop N flux verification procedures to assess compliance with international protocols.
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Affiliation(s)
- M A Sutton
- Centre for Ecology and Hydrology, Edinburgh Research Station, Bush Estate, Penicuik, EH26 0QB, UK.
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Sardans J, Peñuelas J. Drought changes the dynamics of trace element accumulation in a Mediterranean Quercus ilex forest. Environ Pollut 2007; 147:567-83. [PMID: 17137692 DOI: 10.1016/j.envpol.2006.10.008] [Citation(s) in RCA: 15] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/20/2006] [Revised: 10/03/2006] [Accepted: 10/06/2006] [Indexed: 05/08/2023]
Abstract
We conducted a field drought manipulation experiment in an evergreen oak Mediterranean forest from 1999 to 2005 to investigate the effects of the increased drought predicted for the next decades on the accumulation of trace elements that can be toxic for animals, in stand biomass, litter and soil. Drought increased concentrations of As, Cd, Ni, Pb and Cr in roots of the dominant tree species, Quercus ilex, and leaf Cd concentrations in Arbutus unedo and of Phillyrea latifolia codominant shrubs. The increased concentration of As and Cd can aggravate the toxic capacity of those two elements, which are already next or within the levels that have been shown to be toxic for herbivores. The study also showed a great reduction in Pb biomass content (100-135 gha(-1)) during the studied period (1999-2005) showing the effectiveness of the law that prohibited leaded fuel after 2001. The results also indicate that drought increases the exportation of some trace elements to continental waters.
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Affiliation(s)
- J Sardans
- Unitat d'Ecofisiologia CSIC-CEAB-CREAF, CREAF (Centre de Recerca Ecològica d'Aplicacions Forestals) Edifici C, Universitat Autònoma Barcelona, Bellaterra, Barcelona, Spain.
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Munné-Bosch S, Peñuelas J. Photo- and antioxidative protection during summer leaf senescence in Pistacia lentiscus L. grown under Mediterranean field conditions. Ann Bot 2003; 92:385-91. [PMID: 12871848 PMCID: PMC4257514 DOI: 10.1093/aob/mcg152] [Citation(s) in RCA: 21] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/20/2023]
Abstract
Summer leaf senescence in Pistacia lentiscus L. plants serves to remobilize nutrients from the oldest leaves to the youngest ones, and therefore contributes to plant survival during the adverse climatic conditions typical of Mediterranean summers, i.e. water deficit superimposed on high solar radiation and high temperatures. To evaluate the extent of photo- and antioxidative protection during leaf senescence of this species, changes in carotenoids, including xanthophyll cycle pigments, and in the levels of ascorbate and alpha-tocopherol were measured prior to and during summer leaf senescence in 3-year-old plants grown under Mediterranean field conditions. Although a chlorophyll loss of approx. 20% was observed during the first stages of leaf senescence, no damage to the photosynthetic apparatus occurred as indicated by constant maximum efficiencies of photosystem II photochemistry. During this period the de-epoxidation state of the xanthophyll cycle, and lutein, neoxanthin and ascorbate levels were kept constant. At the same time beta-carotene and alpha-tocopherol levels increased by approx. 9 and 70%, respectively, presumably conferring photo- and antioxidative protection to the photosynthetic apparatus. By contrast, during the later stages of leaf senescence, characterized by severe chlorophyll loss, carotenoids were moderately degraded (neoxanthin by approx. 20%, and both lutein and beta-carotene by approx. 35%), ascorbate decreased by approx. 80% and alpha-tocopherol was not detected in senescing leaves. This study demonstrates that mechanisms of photo- and antioxidative protection may play a major role in maintaining chloroplast function during the first stages of leaf senescence, while antioxidant defences are lost during the latest stages of senescence.
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Affiliation(s)
- S Munné-Bosch
- Unitat d'Ecofisiologia CSIC-CEAB-CREAF, Facultat de Ciències, Universitat Autònoma de Barcelona, 08193 Bellaterra, Barcelona, Spain.
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Klumpp A, Ansel W, Klumpp G, Belluzzo N, Calatayud V, Chaplin N, Garrec JP, Gutsche HJ, Hayes M, Hentze HW, Kambezidis H, Laurent O, Peñuelas J, Rasmussen S, Ribas A, Ro-Poulsen H, Rossi S, Sanz MJ, Shang H, Sifakis N, Vergne P. EuroBionet: a pan-European biomonitoring network for urban air quality assessment. Environ Sci Pollut Res Int 2002; 9:199-203. [PMID: 12094534 DOI: 10.1007/bf02987489] [Citation(s) in RCA: 13] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/23/2023]
Abstract
EuroBionet, the 'European Network for the Assessment of Air Quality by the Use of Bioindicator Plants', is an EU-funded cooperative project currently consisting of public authorities and scientific institutes from 12 cities in 8 countries. In 2000, the bioindicator plants tobacco (Nicotiana tabacum Bel W3), poplar (Populus nigra 'Brandaris'), spiderwort (Tradescantia sp. clone 4430), Italian rye grass (Lolium multiflorum italicum) and curly kale (Brassica oleracea acephala) were exposed to ambient air at 90 monitoring sites according to standardised methods. Visible injuries and growth parameters were assessed and the accumulation of toxic substances in leaves determined. The exposure of tobacco resulted in a gradient with low levels of ozone-induced foliar injury in N and NW Europe, and medium to high values in the southern and central regions. The results of heavy metal and sulphur analyses in rye grass samples generally showed low to very low sulphur and low to medium heavy metal concentrations in leaves. In some cities, however, local hot spots of heavy metal contamination were detected. Analyses of the PAH contents in curly kale leaves gave low to medium values, with locally elevated levels at traffic-exposed sites.
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Affiliation(s)
- A Klumpp
- Institute for Landscape and Plant Ecology (320), University of Hohenheim, 70593 Stuttgart, Germany.
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Affiliation(s)
- J Peñuelas
- Unitat Ecofisiologia CSIC-CREAF, Center for Ecological Research and Forestry Applications (CREAF), Edifici C, Universitat Autònoma de Barcelona, 08193 Bellaterra (Barcelona), Spain.
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Abstract
The seasonal pattern of non-terpenoid C6-C10 VOC emission by seven Mediterranean woody species (Bupleurum fruticosum, Cistus albidus, Pinus halepensis, Arbutus unedo, Erica arborea, Quercus coccifera, and Q. ilex) was studied under field conditions. Branch chamber samples were sorbed on carbotrap and analyzed by thermal desorption in combination with GC-MS. These non-terpenoid C6-C10 VOC emissions were large, almost of similar magnitude to those of terpenes. Overall, maximum values were recorded in spring and summer (up to 12 microg g(-1) DM h(-1) in Q. ilex) and minimum values in autumn and winter (up to 5 microg g(-1) DM h(-1) in Q. ilex). These C6-C10 VOC emissions represented 2.82% of the photosynthetic C fixation in summer and 0.22% in winter. Some compounds such as 2-ethoxyethyl acetate were emitted by most species, others such as 3-hexen-1-ol, phenol or decanal were significantly emitted only by few species. The greatest diversity of emitted non-terpenoid C6-C10 VOCs was observed in spring and in Q. ilex. Temperature seemed a strong driver of these seasonal changes but other species-specific and seasonal factors seem involved. These results indicate that C6-C10 non-terpenoid VOCs contribute a rather significant fraction of the total biogenic VOC flux from these Mediterranean species, especially in spring and summer, and therefore should be considered in VOC emission inventories and in model predictions of tropospheric chemistry.
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Affiliation(s)
- J Peñuelas
- Centre de Recerca Ecològica i Aplicacions Forestals, Facultat de Ciències, Universitat Autònoma de Barcelona, Bellaterra (Barcelona), Catalonia, Spain.
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Llusià J, Peñuelas J. Emission of volatile organic compounds by apple trees under spider mite attack and attraction of predatory mites. Exp Appl Acarol 2001; 25:65-77. [PMID: 11508530 DOI: 10.1023/a:1010659826193] [Citation(s) in RCA: 15] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/09/2023]
Abstract
Emission rates of volatile organic compounds (VOCs) from Pirus malus L. subsp. mitis (Wallr.) var. Golden Delicious and var. Starking attacked by the phytophagous mite Panonychus ulmi Koch, and their attractiveness to the predatory mites Amblyseius andersoni Chant and Amblyseius californicus McGregor, were studied during three years. A large variability was found in the emission of individual VOCs depending on the infestation, the apple tree variety and the date. There were larger total VOC emission rates and larger total VOC leaf concentrations in apple trees attacked by phytophagous mites, especially in the var. Starking. In infested trees of this variety, there were also more predatory mites. An olfactometer assay showed that predatory mites preferentially chose branches infested by Panonychus ulmi (85% went to infested branches vs 15% to uninfested control branches) indicating that volatiles may be used as cues to find their prey.
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Affiliation(s)
- J Llusià
- Unitat Ecofisiologia CSIC, Centre de Recerca Ecològica i Aplicacions Forestals, Facultat de Ciències, Universitat Autònoma de Barcelona, Bellaterra, Catalonia, Spain.
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Tognetti R, Minnocci A, Peñuelas J, Raschi A, Jones MB. Comparative field water relations of three Mediterranean shrub species co-occurring at a natural CO(2) vent. J Exp Bot 2000; 51:1135-1146. [PMID: 10948241 DOI: 10.1093/jexbot/51.347.1135] [Citation(s) in RCA: 8] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/23/2023]
Abstract
Annual variations in the water relations and stomatal response of Erica arborea, Myrtus communis and Juniperus communis occurring at a natural CO(2) vent were analysed under Mediterranean field conditions. A distinct gradient of CO(2)concentration ([CO(2)]) exists between two sites near a natural CO(2)-emitting vent, with higher [CO(2)] (700 micromol mol(-1)) in the proximity of the CO(2) spring. Plants at the CO(2) spring site have been growing for generations at elevated [CO(2)]. At both sites, maximum leaf conductance was related to predawn shoot water potential. The effects of water deficits during the summer drought were severe. Leaf conductance and water potential recovered after major rainfalls in September to predrought values. Strong relationships between leaf conductance, predawn water potential, and leaf-specific hydraulic resistance are consistent with the role of stomata in regulating plant water status. Considerable between-species variation in sensitivity of water potentials and stomatal characters to elevated [CO(2)] were observed. Common to all the shrubs were a reduction in leaf conductance and an increase in water potentials in response to elevated [CO(2)]. Elevated [CO(2)] decreased the sensitivity of leaf conductance to vapour pressure deficit. Morphological characters (including stomatal density and degree of sclerophylly) showed site-dependent variations, but degree and sign of such changes varied with the species and/or the season. Measurements of discrimination against (13)C provided evidence for long-term decreases of water use efficiency in CO(2) spring plants. Analysis of C isotope composition suggested that a downward adjustment of photosynthetic capacity may have occurred under elevated [CO(2)]. Elevated [CO(2)] effects on water relations and leaf morphology persisted in the long term, but the three shrubs growing in the same environment showed species-specific responses.
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Affiliation(s)
- R Tognetti
- Dipartimento di Coltivazione e Difesa delle Species Legnose-Sezione Coltivazioni Arboree, Università di Pisa, Italy.
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Llusià J, Peñuelas J. Seasonal patterns of terpene content and emission from seven Mediterranean woody species in field conditions. Am J Bot 2000; 87:133-140. [PMID: 10636836 DOI: 10.2307/2656691] [Citation(s) in RCA: 72] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
The seasonal pattern of terpene content and emission by seven Mediterranean woody species was studied under field conditions. Emission rates were normalized at 30°C and 1000 μmol·m·s PFD (photosynthetic photon flux density). Bupleurum fruticosum, Pinus halepensis, and Cistus albidus stored large amounts of terpenes (0.01-1.77% [dry matter]) with maximum values in autumn and minimum values in spring. They emitted large amounts of terpenes (2-40 μg·g DM·h), but with no clear seasonal trend except for Cistus albidus, which had maximum values in spring and minimum values in autumn. The nonstoring species Arbutus unedo, Erica arborea, Quercus coccifera and Quercus ilex also emitted large amounts of terpenes (0-40 μg·g DM·h) and also tended to present maximum emission rates in spring, although this trend was significant only for A. unedo. At the seasonal scale, emission rates did not follow changes in photosynthetic rates; instead, they mostly followed changes in temperature. From autumn to spring, the least volatile monoterpenes such as limonene were emitted at highest rates, whereas the most volatile monoterpenes such as α-pinene and β-pinene were the most emitted in summer. The monoterpene emission rates represented a greater percentage of the photosynthetic carbon fixation in summer (from 0.51% in Arbutus unedo to 5.64% in Quercus coccifera) than in the rest of the seasons. All these seasonality trends must be considered when inventorying and modeling annual emission rates in Mediterranean ecosystems.
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Affiliation(s)
- J Llusià
- CREAF (Centre de Recerca Ecològica i Aplicacions Forestals), Facultat de Ciències, Universitat Autònoma de Barcelona, 08193 Bellaterra (Barcelona), Catalonia, Spain
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48
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Llusià J, Peñuelas J. Changes in terpene content and emission in potted Mediterranean woody plants under severe drought. ACTA ACUST UNITED AC 1998. [DOI: 10.1139/b98-141] [Citation(s) in RCA: 32] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/22/2022]
Abstract
Terpene concentration and emission were studied in potted plants of some of the most common Mediterranean woody species (Pinus halepensis L., Pistacia lentiscus L., Cistus albidus L., Cistus monspeliensis L., Quercus ilex L., Quercus coccifera L., Phillyrea latifolia L., Phillyrea angustifolia L., and Arbutus unedo L.) under irrigation and under severe drought conditions that dropped relative water content to a range between 40% in Q. ilex and 85% in Phillyrea latifolia after withholding watering for one dry summer week. Terpene concentrations were detected in Pinus halepensis, Pistacia lentiscus, C. albidus, and C. monspeliensis, and they increased after withholding watering except in C. albidus. Terpene emission was detected in all species except Phillyrea angustifolia and A. unedo. Pinus halepensis showed the highest diurnal terpene emission rates of 86 µg·g-1 dry wt.·h-1 followed by C. albidus, Pistacia lentiscus, Q. ilex, Q. coccifera, Phillyrea latifolia, and C. monspeliensis (4 µg·g-1 dry wt.·h-1). Emitted terpenes represented from 0.33% of C fixed in C. monspeliensis to 10% in C. albidus. All species severely decreased their terpene emission rates under severe drought conditions. Emission by terpene-storing species (e.g., Pinus halepensis) was more related to temperature than in nonstoring species (e.g., Q. ilex), which showed emission relationships with photosynthetic rates. The monoterpenes alpha-pinene, beta-pinene, beta-phellandrene, and limonene and the sesquiterpene caryophyllene were the most abundant terpenes stored and emitted by these Mediterranean plant species.Key words: drought, Mediterranean conditions, terpene concentration, terpene emission, woody plants.
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Llusià J, Peñuelas J. Changes in terpene content and emission in potted Mediterranean woody plants under severe drought. ACTA ACUST UNITED AC 1998. [DOI: 10.1139/cjb-76-8-1366] [Citation(s) in RCA: 29] [Impact Index Per Article: 1.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/22/2022]
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Abstract
Atmospheric CO2 concentration has increased by 25% over the preindustrial level. A parallel increase in C concentration and decreases in N concentration and δ13C of plants grown throughout this century have been observed in plant specimens stored in herbaria. We tested our previous results in a study of 12 more species collected in the western Mediterranean throughout this century (1920-1930, 1945-1955, and 1985-1990) and tree rings of Quercus pubescens from the same area. These changes were accompanied by apparent increases in condensed tannin concentration. A decreasing trend in δ15N both in herbarium material and tree rings was also found, indicating that ecosystems might cope with higher plant N demand by decreasing N losses and increasing N fixation and mineralization. These results may contribute to a better understanding of the effects of global change on carbon and nitrogen cycling.
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Affiliation(s)
- J Peñuelas
- Centre de Recerca Ecològica i Aplicacions Forestals, Facultat de Ciències, Universitat Autònoma, 08193 Bellaterra, Barcelona, Spain, , , , , , ES
| | - Marc Estiarte
- Centre de Recerca Ecològica i Aplicacions Forestals, Facultat de Ciències, Universitat Autònoma, 08193 Bellaterra, Barcelona, Spain, , , , , , ES
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