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Ericoid shrub encroachment shifts aboveground-belowground linkages in three peatlands across Europe and Western Siberia.
Buttler, Alexandre; Bragazza, Luca; Laggoun-Défarge, Fatima; Gogo, Sebastien; Toussaint, Marie-Laure; Lamentowicz, Mariusz; Chojnicki, Bogdan H; Slowinski, Michal; Slowinska, Sandra; Zielinska, Malgorzata; Reczuga, Monika; Barabach, Jan; Marcisz, Katarzyna; Lamentowicz, Lukasz; Harenda, Kamila; Lapshina, Elena; Gilbert, Daniel; Schlaepfer, Rodolphe; Jassey, Vincent E J.
Afiliación
  • Buttler A; School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL), Lausanne, Switzerland.
  • Bragazza L; Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Lausanne, Switzerland.
  • Laggoun-Défarge F; Agroscope, Field-Crop Systems and Plant Nutrition, Nyon, Switzerland.
  • Gogo S; CNRS, BRGM, ISTO, UMR 7327, Université d'Orléans, Orléans, France.
  • Toussaint ML; UMR-CNRS 6553 ECOBIO, Université de Rennes, Rennes, France.
  • Lamentowicz M; Laboratoire de Chrono-Environnement, UMR, CNRS 6249, UFR des Sciences et Techniques, Université de Franche-Comté, Besançon, France.
  • Chojnicki BH; Climate Change Ecology Research Unit, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Poznan, Poland.
  • Slowinski M; Laboratory of Bioclimatology, Department of Ecology and Environmental Protection, Faculty of Environmental and Mechanical Engineering, Poznan University of Life Sciences, Poznan, Poland.
  • Slowinska S; Past Landscape Dynamic Laboratory, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Warsaw, Poland.
  • Zielinska M; Climate Research Department, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Warsaw, Poland.
  • Reczuga M; Climate Change Ecology Research Unit, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Poznan, Poland.
  • Barabach J; Climate Change Ecology Research Unit, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Poznan, Poland.
  • Marcisz K; Department of Land Improvement, Environmental Development and Spatial Management, Poznan University of Life Sciences, Poznan, Poland.
  • Lamentowicz L; Climate Change Ecology Research Unit, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Poznan, Poland.
  • Harenda K; Climate Change Ecology Research Unit, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Poznan, Poland.
  • Lapshina E; Laboratory of Bioclimatology, Department of Ecology and Environmental Protection, Faculty of Environmental and Mechanical Engineering, Poznan University of Life Sciences, Poznan, Poland.
  • Gilbert D; Yugra State University, Khanty-Mansiysk, Russia.
  • Schlaepfer R; Laboratoire de Chrono-Environnement, UMR, CNRS 6249, UFR des Sciences et Techniques, Université de Franche-Comté, Besançon, France.
  • Jassey VEJ; School of Architecture, Civil and Environmental Engineering (ENAC), Ecole Polytechnique Fédérale de Lausanne (EPFL), Lausanne, Switzerland.
Glob Chang Biol ; 29(23): 6772-6793, 2023 Dec.
Article en En | MEDLINE | ID: mdl-37578632
In northern peatlands, reduction of Sphagnum dominance in favour of vascular vegetation is likely to influence biogeochemical processes. Such vegetation changes occur as the water table lowers and temperatures rise. To test which of these factors has a significant influence on peatland vegetation, we conducted a 3-year manipulative field experiment in Linje mire (northern Poland). We manipulated the peatland water table level (wet, intermediate and dry; on average the depth of the water table was 17.4, 21.2 and 25.3 cm respectively), and we used open-top chambers (OTCs) to create warmer conditions (on average increase of 1.2°C in OTC plots compared to control plots). Peat drying through water table lowering at this local scale had a larger effect than OTC warming treatment per see on Sphagnum mosses and vascular plants. In particular, ericoid shrubs increased with a lower water table level, while Sphagnum decreased. Microclimatic measurements at the plot scale indicated that both water-level and temperature, represented by heating degree days (HDDs), can have significant effects on the vegetation. In a large-scale complementary vegetation gradient survey replicated in three peatlands positioned along a transitional oceanic-continental and temperate-boreal (subarctic) gradient (France-Poland-Western Siberia), an increase in ericoid shrubs was marked by an increase in phenols in peat pore water, resulting from higher phenol concentrations in vascular plant biomass. Our results suggest a shift in functioning from a mineral-N-driven to a fungi-mediated organic-N nutrient acquisition with shrub encroachment. Both ericoid shrub encroachment and higher mean annual temperature in the three sites triggered greater vascular plant biomass and consequently the dominance of decomposers (especially fungi), which led to a feeding community dominated by nematodes. This contributed to lower enzymatic multifunctionality. Our findings illustrate mechanisms by which plants influence ecosystem responses to climate change, through their effect on microbial trophic interactions.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Sphagnopsida / Tracheophyta País/Región como asunto: Asia / Europa Idioma: En Revista: Glob Chang Biol Año: 2023 Tipo del documento: Article País de afiliación: Suiza Pais de publicación: Reino Unido

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Sphagnopsida / Tracheophyta País/Región como asunto: Asia / Europa Idioma: En Revista: Glob Chang Biol Año: 2023 Tipo del documento: Article País de afiliación: Suiza Pais de publicación: Reino Unido