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1. Mosses modify effects of warmer and wetter conditions on tree seedlings at the alpine treeline

Author

Marie-Charlotte Nilsson, Laurenz M. Teuber, Anders Michelsen, Johan Olofsson, David A. Wardle, Eveline J. Krab, Ellen Dorrepaal, and Signe Lett

Subjects
RECRUITMENT, 0106 biological sciences, 010504 meteorology & atmospheric sciences, Climate change, Bryophyta, Betulapubescens, precipitation, SUB-ARCTIC BRYOPHYTE, 010603 evolutionary biology, 01 natural sciences, treeline expansion, Trees, LITTER DECOMPOSITION, Betula pubescens, Arctic, bryophytes, Environmental Chemistry, Precipitation, 0105 earth and related environmental sciences, General Environmental Science, Sweden, Ekologi, Global and Planetary Change, CLIMATE-CHANGE, Ecology, biology, Arctic Regions, FUNCTIONAL-GROUP LOSS, Global warming, Pinus sylvestris, Vegetation, plant interactions, biology.organism_classification, CARBON BALANCE, Tundra, climate change, Seedlings, Seedling, GROWTH, Environmental science, VEGETATION, Pinussylvestris, TRAITS, RESPONSES
Abstract

Climate warming enables tree seedling establishment beyond the current alpine treeline, but to achieve this, seedlings have to establish within existing tundra vegetation. In tundra, mosses are a prominent feature, known to regulate soil temperature and moisture through their physical structure and associated water retention capacity. Moss presence and species identity might therefore modify the impact of increases in temperature and precipitation on tree seedling establishment at the arctic‐alpine treeline. We followed Betula pubescens and Pinus sylvestris seedling survival and growth during three growing seasons in the field. Tree seedlings were transplanted along a natural precipitation gradient at the subarctic‐alpine treeline in northern Sweden, into plots dominated by each of three common moss species and exposed to combinations of moss removal and experimental warming by open‐top chambers (OTCs). Independent of climate, the presence of feather moss, but not Sphagnum , strongly supressed survival of both tree species. Positive effects of warming and precipitation on survival and growth of B. pubescens seedlings occurred in the absence of mosses and as expected, this was partly dependent on moss species. P. sylvestris survival was greatest at high precipitation, and this effect was more pronounced in Sphagnum than in feather moss plots irrespective of whether the mosses had been removed or not. Moss presence did not reduce the effects of OTCs on soil temperature. Mosses therefore modified seedling response to climate through other mechanisms, such as altered competition or nutrient availability. We conclude that both moss presence and species identity pose a strong control on seedling establishment at the alpine treeline, and that in some cases mosses weaken climate‐change effects on seedling establishment. Changes in moss abundance and species composition therefore have the potential to hamper treeline expansion induced by climate warming.

Published
2020

2. SoilTemp: A global database of near-surface temperature

Author

Juha M. Alatalo, Ilya M. D. Maclean, Ivan Nijs, Pascal Boeckx, Ronja E. M. Wedegärtner, Josefine Walz, Sergiy Medinets, Jonas Ardö, Martin Wilmking, Aníbal Pauchard, Onur Candan, Joseph Okello, Miguel Portillo-Estrada, Christian Rossi, Francesco Malfasi, Robert G. Björk, Tim Seipel, Pekka Niittynen, Kristoffer Hylander, Simone Cesarz, Michael B. Ashcroft, Dany Ghosn, T'Ai Gladys Whittingham Forte, Andrew D. Thomas, Nina Buchmann, Pavel Dan Turtureanu, Marcello Tomaselli, Martin Svátek, Luca Vitale, Christian Rixen, Valter Di Cecco, Pascal Vittoz, Jan Wild, Hans J. De Boeck, M. Rosa Fernández Calzado, Khatuna Gigauri, Haydn J.D. Thomas, Josef Brůna, Patrice Descombes, Robert Kanka, Roman Plichta, Julia Boike, Juan J. Jiménez, Mihai Pușcaș, James D. M. Speed, Tudor-Mihai Ursu, Maaike Y. Bader, Jian Zhang, Shengwei Zong, Marko Smiljanic, Ben Somers, Toke T. Høye, Martin Macek, Rebecca Finger Higgens, Jürgen Homeier, Fatih Fazlioglu, Ana Clara Mazzolari, Katja Tielbörger, Marek Čiliak, Sanne Govaert, Matěj Man, Loïc Pellissier, Bente J. Graae, Mana Gharun, Juan Lorite, Jhonatan Sallo Bravo, Thomas Scholten, Ian Klupar, Jonathan Lenoir, Martin Kopecký, Angela Stanisci, Joseph J. Bailey, Stuart W. Smith, Gergana N. Daskalova, Andrej Varlagin, Radim Matula, Meelis Pärtel, Ann Milbau, Peter Barančok, Jörg G. Stephan, Marijn Bauters, Jan Dick, Zuzana Sitková, Alistair S. Jump, Felix Gottschall, Fernando Moyano, Mario Trouillier, Filip Hrbáček, Eduardo Fuentes-Lillo, Nicoletta Cannone, Koenraad Van Meerbeek, Miska Luoto, Christopher Andrews, Charly Geron, Lisa J. Rew, Michael Stemkovski, Rafaella Canessa, Lucia Hederová, Peter Haase, Klaus Steinbauer, Keith W. Larson, Mats P. Björkman, Edoardo Cremonese, Lore T. Verryckt, Aud H. Halbritter, Jiri Dolezal, František Máliš, William D. Pearse, Zhaochen Zhang, Christian D. Larson, Sylvia Haider, Robert Weigel, Harald Pauli, Romina D. Dimarco, Nico Eisenhauer, Agustina Barros, Shyam S. Phartyal, Liesbeth van den Brink, Edmund W. Basham, Adrian V. Rocha, Mauro Guglielmin, Rafael A. García, Andrej Palaj, Josef Urban, Austin Koontz, Brett R. Scheffers, Mia Vedel Sørensen, Isla H. Myers-Smith, Camille Meeussen, Lena Muffler, Krystal Randall, Volodymyr I. Medinets, Sonia Merinero, Laurenz M. Teuber, Salvatore R. Curasi, José Luis Benito Alonso, Pieter De Frenne, Kamil Láska, Jonas Schmeddes, Martin A. Nuñez, Amanda Ratier Backes, Alessandro Petraglia, Miroslav Svoboda, Ellen Dorrepaal, Sonja Wipf, Juha Aalto, Masahito Ueyama, Benjamin Blonder, Jonas J. Lembrechts, Esther R. Frei, Lukas Siebicke, Bernard Heinesch, C. Johan Dahlberg, Juergen Kreyling, Camille Pitteloud, Florian Zellweger, Rebecca A. Senior, David H. Klinges, Miguel Ángel de Pablo, Elizabeth G. Simpson, George Kazakis, Jozef Kollár, Pallieter De Smedt, Olivier Roupsard, Jan Altman, Michele Carbognani, Julia Kemppinen, Manuela Winkler, Valeria Aschero, Pieter Vangansbeke, Andrea Lamprecht, Stef Haesen, University of Antwerp (UA), Finnish Meteorological Institute (FMI), Helsingin yliopisto = Helsingfors universitet = University of Helsinki, University of Wollongong [Australia], Australian Museum [Sydney], Universiteit Gent = Ghent University (UGENT), Institute of Botany of the Czech Academy of Sciences (IB / CAS), Czech Academy of Sciences [Prague] (CAS), Czech University of Life Sciences Prague (CZU), Ecologie et Dynamique des Systèmes Anthropisés - UMR CNRS 7058 (EDYSAN), Université de Picardie Jules Verne (UPJV)-Centre National de la Recherche Scientifique (CNRS), University of Exeter, Ecologie fonctionnelle et biogéochimie des sols et des agro-écosystèmes (UMR Eco&Sols), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Institut de Recherche pour le Développement (IRD)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut Agro - Montpellier SupAgro, Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro), LMI IESOL Intensification Ecologique des Sols Cultivés en Afrique de l’Ouest [Dakar] (IESOL), Institut de recherche pour le développement (IRD [Sénégal]), Universidad de Concepción - University of Concepcion [Chile], Instituto de Ecología y Biodiversidad (IEB), Universidad Adventista de Chile - Adventist University of Chile (UNACH), Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich), Qatar University, Norwegian University of Science and Technology [Trondheim] (NTNU), Norwegian University of Science and Technology (NTNU), Nanyang Technological University [Singapour], University of Gothenburg (GU), Universität Greifswald - University of Greifswald, Georg-August-University = Georg-August-Universität Göttingen, Martin-Luther-University Halle-Wittenberg, German Centre for Integrative Biodiversity Research (iDiv), Leipzig University, Mountains of the Moon University, Laboratory of Applied Physical Chemistry - ISOFYS (Gent, Belgium), Mendel University in Brno (MENDELU), Siberian Federal University (SibFU), Nalanda University, Hemvati Nandan Bahuguna Garhwal University (HNBGU), Babes-Bolyai University [Cluj-Napoca] (UBB), A.N. Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences [Moscow] (RAS), Instituto de Investigaciones Forestales y Agropecuarias Bariloche (IFAB), Consejo Nacional de Investigaciones Científicas y Técnicas [Buenos Aires] (CONICET)-Instituto Nacional de Tecnología Agropecuaria (INTA), University of Stirling, Umeå University, Istituto per i Sistemi Agricoli e Forestali del Mediterraneo (ISAFOM), National Research Council of Italy | Consiglio Nazionale delle Ricerche (CNR), Dartmouth College [Hanover], University of Bergen (UiB), University of Notre Dame [Indiana] (UND), Utah State University (USU), Imperial College London, Arctic Research Centre [Aarhus] (ARC), Aarhus University [Aarhus], Universidad de Granada = University of Granada (UGR), Università degli studi di Parma = University of Parma (UNIPR), Catholic University of Leuven - Katholieke Universiteit Leuven (KU Leuven), Stockholm University, University of South Bohemia, Aberystwyth University, York St John University, Centre International de Hautes Etudes Agronomiques Méditerranéennes - Institut Agronomique Méditerranéen de Chania (CIHEAM-IAMC), Centre International de Hautes Études Agronomiques Méditerranéennes (CIHEAM), Universidad de Alcalá - University of Alcalá (UAH), Montana State University (MSU), Lund University [Lund], Universitá degli Studi dell’Insubria = University of Insubria [Varese] (Uninsubria), Philipps Universität Marburg = Philipps University of Marburg, Università degli Studi del Molise = University of Molise (UNIMOL), Universidad Nacional de Cuyo [Mendoza] (UNCUYO), Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales [Mendoza] (CONICET-IANIGLA), Consejo Nacional de Investigaciones Científicas y Técnicas [Buenos Aires] (CONICET)-Universidad Nacional de Cuyo [Mendoza] (UNCUYO), Technical University in Zvolen (TUZVO), Georgian Institute of Public Affairs (GIPA), Austrian Academy of Sciences (OeAW), Universität für Bodenkultur Wien = University of Natural Resources and Life [Vienne, Autriche] (BOKU), Osaka Prefecture University, Instituto Nacional de Investigaciones en Biodiversidad y Medioambiente [Bariloche] (INIBIOMA-CONICET), Consejo Nacional de Investigaciones Científicas y Técnicas [Buenos Aires] (CONICET)-Universidad Nacional del Comahue [Neuquén] (UNCOMA), National Institute of Research and Development for Biological Sciences [Bucarest] (INCDSB), Université de Lausanne = University of Lausanne (UNIL), University of Tartu, Institute of Landscape Ecology of the Slovak Academy of Sciences, Slovak Academy of Sciences (SAS), Jolube Consultor Botánico, Northeast Normal University, Majella National Park - Parco Nazionale della Majella, National Forest Centre - Národné lesnícke centrum [Zvolen], University of Tübingen, County Administrative Board of Västra Götaland, Odessa National I.I.Mechnikov University, Research Institute for Nature and Forest (INBO), University of Edinburgh, University of California [Berkeley] (UC Berkeley), University of California (UC), Arizona State University [Tempe] (ASU), Swedish University of Agricultural Sciences (SLU), Gembloux Agro-Bio Tech [Gembloux], Université de Liège, Centre for Ecology and Hydrology [Bangor] (CEH), Natural Environment Research Council (NERC), Princeton University, Fundación Agencia Aragonesa para la Investigación y el Desarrollo (ARAID), Alfred Wegener Institute [Potsdam], Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Humboldt University Of Berlin, University of Florida [Gainesville] (UF), East China Normal University [Shangaï] (ECNU), Ordu University - Ordu Üniversitesi, Universidad Nacional de San Antonio Abad del Cusco (UNSAAC), Masaryk University [Brno] (MUNI), Aosta Valley Regional Environmental Protection Agency (ARPA), Senckenberg – Leibniz Institution for Biodiversity and Earth System Research - Senckenberg Gesellschaft für Naturforschung, Leibniz Association, Universität Duisburg-Essen = University of Duisburg-Essen [Essen], Swiss National Park - Parc Naziunal Svizzer, Universität Zürich [Zürich] = University of Zurich (UZH), ANR-19-CE32-0005,IMPRINT,IMpacts des PRocessus mIcroclimatiques sur la redistributioN de la biodiversiTé forestière en contexte de réchauffement du macroclimat(2019), University of Helsinki, Universiteit Gent = Ghent University [Belgium] (UGENT), Centre National de la Recherche Scientifique (CNRS)-Université de Picardie Jules Verne (UPJV), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Institut de Recherche pour le Développement (IRD)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro), Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), Georg-August-University [Göttingen], Consiglio Nazionale delle Ricerche [Roma] (CNR), University of Granada [Granada], University of Parma = Università degli studi di Parma [Parme, Italie], Universitá degli Studi dell’Insubria, Philipps University of Marburg, Università degli Studi del Molise (Unimol), Universität für Bodenkultur Wien [Vienne, Autriche] (BOKU), University of Lausanne (UNIL), University of California [Berkeley], University of California, Humboldt-Universität zu Berlin, and University of Duisburg-Essen

Subjects
0106 biological sciences, 010504 meteorology & atmospheric sciences, Biome, Biodiversity & Conservation, Microclimate, computer.software_genre, 01 natural sciences, topoclimate, Snow, HETEROGENEITY, SCALE, database, General Environmental Science, [SDV.EE]Life Sciences [q-bio]/Ecology, environment, Global and Planetary Change, CLIMATE-CHANGE, Database, Ecology, Spatial database, Vegetation, Biological Sciences, Chemistry, soil climate, climate change, species distributions, Biodiversity Conservation, ecosystem processes, microclimate, temperature, Life Sciences & Biomedicine, Biologie, [SDE.MCG]Environmental Sciences/Global Changes, Climate change, Environmental Sciences & Ecology, [SDV.BID]Life Sciences [q-bio]/Biodiversity, MOISTURE, 010603 evolutionary biology, soil, LITTER DECOMPOSITION, species 19 distributions, Environmental Chemistry, DISTRIBUTIONS, SCALE SOIL, Biology, climate, Ecosystem, 0105 earth and related environmental sciences, Science & Technology, Global warming, SPECIES DISTRIBUTION MODELS, 15. Life on land, Radiative forcing, MACROCLIMATE, Agriculture and Soil Science, 13. Climate action, SNOW, Earth and Environmental Sciences, Environmental science, [SDE.BE]Environmental Sciences/Biodiversity and Ecology, computer, Environmental Sciences
Abstract

Current analyses and predictions of spatially explicit patterns and processes in ecology most often rely on climate data interpolated from standardized weather stations. This interpolated climate data represents long-term average thermal conditions at coarse spatial resolutions only. Hence, many climate-forcing factors that operate at fine spatiotemporal resolutions are overlooked. This is particularly important in relation to effects of observation height (e.g. vegetation, snow and soil characteristics) and in habitats varying in their exposure to radiation, moisture and wind (e.g. topography, radiative forcing or cold-air pooling). Since organisms living close to the ground relate more strongly to these microclimatic conditions than to free-air temperatures, microclimatic ground and near-surface data are needed to provide realistic forecasts of the fate of such organisms under anthropogenic climate change, as well as of the functioning of the ecosystems they live in. To fill this critical gap, we highlight a call for temperature time series submissions to SoilTemp, a geospatial database initiative compiling soil and near-surface temperature data from all over the world. Currently, this database contains time series from 7,538 temperature sensors from 51 countries across all key biomes. The database will pave the way toward an improved global understanding of microclimate and bridge the gap between the available climate data and the climate at fine spatiotemporal resolutions relevant to most organisms and ecosystem processes. ispartof: GLOBAL CHANGE BIOLOGY vol:26 issue:11 pages:6616-6629 ispartof: location:England status: published

Published
2020

3. Meshes in mesocosms control solute and biota exchange in soils:A step towards disentangling (a)biotic impacts on the fate of thawing permafrost

Author

Konstantin Gavazov, James T. Weedon, Frida Keuper, Ellen Dorrepaal, Eveline J. Krab, Maria Väisänen, Sylvain Monteux, Laurenz M. Teuber, and Systems Ecology

Subjects
0106 biological sciences, Nitrogen, Soil Science, chemistry.chemical_element, Permafrost, 01 natural sciences, Faunal inoculation, Mesocosm, Nutrient, Soil functions, skin and connective tissue diseases, Abiotic component, Ecology, Biota, Lateral soil connection, 04 agricultural and veterinary sciences, Agricultural and Biological Sciences (miscellaneous), Field incubation, chemistry, Root, Environmental chemistry, Soil water, 040103 agronomy & agriculture, 0401 agriculture, forestry, and fisheries, Environmental science, sense organs, Bacterial community, Carbon, 010606 plant biology & botany
Abstract

Environmental changes feedback to climate through their impact on soil functions such as carbon (C) and nutrient sequestration. Abiotic conditions and the interactions between above- and belowground biota drive soil responses to environmental change but these (a)biotic interactions are challenging to study. Nonetheless, better understanding of these interactions would improve predictions of future soil functioning and the soil-climate feedback and, in this context, permafrost soils are of particular interest due to their vast soil C-stores. We need new tools to isolate abiotic (microclimate, chemistry) and biotic (roots, fauna, microorganisms) components and to identify their respective roles in soil processes. We developed a new experimental setup, in which we mimic thermokarst (permafrost thaw-induced soil subsidence) by fitting thawed permafrost and vegetated active layer sods side by side into mesocosms deployed in a subarctic tundra over two growing seasons. In each mesocosm, the two sods were separated from each other by barriers with different mesh sizes to allow varying degrees of physical connection and, consequently, (a)biotic exchange between active layer and permafrost. We demonstrate that our mesh-approach succeeded in controlling 1) lateral exchange of solutes between the two soil types, 2) colonization of permafrost by microbes but not by soil fauna, and 3) ingrowth of roots into permafrost. In particular, experimental thermokarst induced a ~60% decline in permafrost nitrogen (N) content, a shift in soil bacteria and a rapid buildup of root biomass (+33.2 g roots m−2 soil). This indicates that cascading plant-soil-microbe linkages are at the heart of biogeochemical cycling in thermokarst events. We propose that this novel setup can be used to explore the effects of (a)biotic ecosystem components on focal biogeochemical processes in permafrost soils and beyond.

Published
2020

4. From Understanding to Sustainable Use of Peatlands: The WETSCAPES Approach

Author

Ralf Bill, Almut Mrotzek, Haitao Wang, Franziska Schmacka, John Couwenberg, Wakene Negassa, Dierk Michaelis, Laurenz M. Teuber, Peter Leinweber, Franziska Tanneberger, Micha Weil, Gerald Jurasinski, Sandra Schenk, Nicole Wrage-Mönnig, Tim Urich, Martin Wilmking, Bernd Lennartz, Marko Smiljanic, Dominik Zak, Anke Günther, Gesche Blume-Werry, J. Berendt, Sarah Schwieger, Alba Anadon-Rosell, Franziska Koebsch, Florian Beyer, Haojie Liu, Hans Joosten, Nils Koldrack, Daniel Köhn, Sate Ahmad, and Jürgen Kreyling

Subjects
Peat, 010504 meteorology & atmospheric sciences, fen, Soil Science, Climate change, 01 natural sciences, Ecosystem services, lcsh:Chemistry, agricultural_sciences_agronomy, Environmental protection, Ecosystem, Greenhouse effect, lcsh:Physical geography, 0105 earth and related environmental sciences, Earth-Surface Processes, Water transport, rewetting, matter fluxes, Vegetation, 04 agricultural and veterinary sciences, Miljövetenskap, lcsh:QD1-999, Greenhouse gas, interdisciplinary, 040103 agronomy & agriculture, 0401 agriculture, forestry, and fisheries, Terrestrial ecosystem, paludiculture, lcsh:GB3-5030, Environmental Sciences, drainage
Abstract

Of all terrestrial ecosystems, peatlands store carbon most effectively in long-term scales of millennia. However, many peatlands have been drained for peat extraction or agricultural use. This converts peatlands from sinks to sources of carbon, causing approx. 5% of the anthropogenic greenhouse effect and additional negative effects on other ecosystem services. Rewetting peatlands can mitigate climate change and may be combined with management in the form of paludiculture. Rewetted peatlands, however, do not equal their pristine ancestors and their ecological functioning is not understood. This holds true especially for groundwater-fed fens. Their functioning results from manifold interactions and can only be understood following an integrative approach of many relevant fields of science, which we merge in the interdisciplinary project WETSCAPES. Here, we address interactions among water transport and chemistry, primary production, peat formation, matter transformation and transport, microbial community, and greenhouse gas exchange using state of the art methods. We record data on six study sites spread across three common fen types (Alder forest, percolation fen, and coastal fen), each in drained and rewetted states. First results revealed that indicators reflecting more long-term effects like vegetation and soil chemistry showed a stronger differentiation between drained and rewetted states than variables with a more immediate reaction to environmental change, like greenhouse gas (GHG) emissions. Variations in microbial community composition explained differences in soil chemical data as well as vegetation composition and GHG exchange. We show the importance of developing an integrative understanding of managed fen peatlands and their ecosystem functioning.

Published
2020

5. The role of bryophytes for tree seedling responses to winter climate change: Implications for the stress gradient hypothesis

Author

Signe Lett, Marie-Charlotte Nilsson, David A. Wardle, Ellen Dorrepaal, Laurenz M. Teuber, Chen, Han, and Asian School of the Environment

Subjects
0106 biological sciences, Ecology, biology, Global warming, Climate change, Plant Science, Vegetation, Geology [Science], Alpine, biology.organism_classification, 010603 evolutionary biology, 01 natural sciences, Subarctic climate, Tundra, Arctic, Seedling, Environmental science, B. pubescens, Ecology, Evolution, Behavior and Systematics, Tree line, 010606 plant biology & botany
Abstract

1. When tree seedlings establish beyond the current tree line due to climate warming, they encounter existing vegetation, such as bryophytes that often dominate in arctic and alpine tundra. The stress gradient hypothesis (SGH) predicts that plant interactions in tundra become increasingly negative as climate warms and conditions become less harsh. However, for seedlings, climate warming might not result in lower winter stress, if insulating snow cover is reduced. 2. We aimed to understand if bryophytes facilitate seedling survival in a changing winter climate and if these effects of bryophytes on tree seedlings comply with the SGH along elevational gradients under contrasting snow conditions. 3. In the Swedish subarctic, we transplanted intact bryophyte cores covered by each of three bryophyte species and bryophyte‐free control soil from above the tree line to two field common garden sites, representing current and future tree line air temperature conditions (i.e. current tree line elevation and a lower, warmer, elevation below the tree line). We planted seedlings of Betula pubescens and Pinus sylvestris into these cores and subjected them to experimental manipulation of snow cover during one winter. 4. In agreement with the SGH, milder conditions caused by increased snow cover enhanced the generally negative or neutral effects of bryophytes on seedlings immediately after winter. Furthermore, survival of P. sylvestris seedlings after one full year was higher at lower elevation, especially when snow cover was thinner. However, in contrast with the SGH, impacts of bryophytes on over‐winter survival of seedlings did not differ between elevations, and impacts on survival of B. pubescens seedlings after 1 year was more negative at lower elevation. Bryophyte species differed in their effect on seedling survival after winter, but these differences were not related to their insulating capacity. 5. Synthesis. Our study demonstrates that interactions from bryophytes can modify the impacts of winter climate change on tree seedlings, and vice versa. These responses do not always comply with SGH, but could ultimately have consequences for large‐scale ecological processes such as tree line shifts. These new insights need to be taken into account in predictions of plant species responses to climate change. Accepted version

Published
2017

6. Dwelling in the deep - strongly increased root growth and rooting depth enhance plant interactions with thawing permafrost soil

Author

Ann Milbau, Laurenz M. Teuber, Margareta Johansson, Ellen Dorrepaal, and Gesche Blume-Werry

Subjects
0106 biological sciences, 0301 basic medicine, Root growth, Peat, Physiology, Nitrogen, chemistry.chemical_element, Permafrost, Plant Science, 01 natural sciences, Plant Roots, 03 medical and health sciences, Soil, Fertilizers, biology, fungi, food and beverages, Eriophorum, biology.organism_classification, Tundra, Active layer, 030104 developmental biology, chemistry, Agronomy, Environmental science, Carbon, 010606 plant biology & botany
Abstract

Climate-warming-induced permafrost thaw exposes large amounts of carbon and nitrogen in soil at considerable depths, below the seasonally thawing active layer. The extent to which plant roots can reach and interact with these hitherto detached, deep carbon and nitrogen stores remains unknown. We aimed to quantify how permafrost thaw affects root dynamics across soil depths and plant functional types compared with above-ground abundance, and potential consequences for plant-soil interactions. A decade of experimental permafrost thaw strongly increased total root length and growth in the active layer, and deep roots invaded the newly thawed permafrost underneath. Root litter input to soil across all depths was 10 times greater with permafrost thaw. Root growth timing was unaffected by experimental permafrost thaw but peaked later in deeper soil, reflecting the seasonally receding thaw front. Deep-rooting species could sequester

Published
2018

7. Understory plant functional groups and litter species identity are stronger drivers of litter decomposition than warming along a boreal forest post-fire successional gradient

Author

David A. Wardle, Jonathan R. De Long, Paul Kardol, Laurenz M. Teuber, Marie-Charlotte Nilsson, and Ellen Dorrepaal

Subjects
0106 biological sciences, Ecology, Taiga, Global warming, Soil Science, Climate change, 04 agricultural and veterinary sciences, Understory, Plant litter, 010603 evolutionary biology, 01 natural sciences, Microbiology, Litter decomposition, Nutrient, 040103 agronomy & agriculture, Litter, 0401 agriculture, forestry, and fisheries, Environmental science, sense organs
Abstract

Increasing surface temperatures due to climate change have the potential to alter plant litter mass loss and nutrient release during decomposition. However, a great deal of uncertainty remains conc ...

Published
2016

8. Contrasting Responses of Soil Microbial and Nematode Communities to Warming and Plant Functional Group Removal Across a Post-fire Boreal Forest Successional Gradient

Author

Paul Kardol, Marie-Charlotte Nilsson, Ellen Dorrepaal, Jonathan R. De Long, Laurenz M. Teuber, and David A. Wardle

Subjects
0106 biological sciences, Ecology, biology, Global warming, Taiga, Post fire succession, 04 agricultural and veterinary sciences, biology.organism_classification, 010603 evolutionary biology, 01 natural sciences, Nematode, 040103 agronomy & agriculture, 0401 agriculture, forestry, and fisheries, Environmental Chemistry, Environmental science, Functional group (ecology), Ecology, Evolution, Behavior and Systematics
Abstract

Global warming is causing increases in surface temperatures and has the potential to influence the structure of soil microbial and faunal communities. However, little is known about how warming int ...

Published
2015

9. Livestock grazing in intermountain depressional wetlands—Effects on plant strategies, soil characteristics and biomass

Author

Laurenz M. Teuber, Norbert Hölzel, and Lauchlan H. Fraser

Subjects
Biomass (ecology), geography, Soil salinity, geography.geographical_feature_category, Ecology, business.industry, Agroforestry, media_common.quotation_subject, Wildlife, Wetland, Competition (biology), Habitat, Environmental science, Ruderal species, Animal Science and Zoology, Livestock, business, Agronomy and Crop Science, media_common
Abstract

Prairie wetlands are considered valuable habitat for plants, birds, and wildlife. Livestock use of these wetlands can create conflicts with conservation issues. To achieve proper management, patter ...

Published
2013

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