{"type": "FeatureCollection", "features": [{"id": "10.1016/j.foreco.2022.120396", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:16:11Z", "type": "Journal Article", "created": "2022-07-04", "title": "Tree species identity is the predominant modulator of the effects of soil fauna on leaf litter decomposition", "description": "Open AccessLa faune du sol est l'un des principaux moteurs de la d\u00e9composition de la liti\u00e8re \u00e0 l'\u00e9chelle locale et mondiale, mais le r\u00f4le des esp\u00e8ces d'arbres dans la m\u00e9diation des effets de la faune du sol sur la d\u00e9composition de la liti\u00e8re reste insaisissable. Nous avons men\u00e9 une exp\u00e9rience sur le terrain en utilisant des sacs de liti\u00e8re avec trois tailles de maille diff\u00e9rentes qui ont permis l'acc\u00e8s \u00e0 la microfaune (0,1 mm), \u00e0 la micro et m\u00e9sofaune (2 mm) et \u00e0 la faune totale du sol (5 mm) pour \u00e9valuer la d\u00e9composition de la liti\u00e8re foliaire de deux esp\u00e8ces d'arbres associ\u00e9es \u00e0 des champignons mycorhiziens arbusculaires (MA) et de trois esp\u00e8ces d'arbres associ\u00e9es \u00e0 des champignons ectomycorhiziens (ECM) dans six sites de jardins communs danois. Nous avons \u00e9galement \u00e9valu\u00e9 comment les diff\u00e9rences dans la qualit\u00e9 initiale de la liti\u00e8re, les propri\u00e9t\u00e9s du sol et la composition de la communaut\u00e9 microbienne parmi les esp\u00e8ces d'arbres peuvent affecter la d\u00e9composition de la liti\u00e8re ainsi que les effets de la faune du sol sur la d\u00e9composition de la liti\u00e8re. Les r\u00e9sultats ont montr\u00e9 que (1) la perte de masse de la liti\u00e8re variait consid\u00e9rablement selon la taille des mailles et les esp\u00e8ces d'arbres, avec des taux de d\u00e9composition de la liti\u00e8re (k) allant de 0,273 \u00e0 3,482\u00a0; (2) l'acc\u00e8s \u00e0 la m\u00e9sofaune augmentait significativement la liti\u00e8re k de 0,658 pour la MA et de 0,396 pour les esp\u00e8ces d'arbres ECM sans acc\u00e8s \u00e0 la faune du sol, respectivement de 255 et 92%, tandis que l'acc\u00e8s \u00e0 la fois \u00e0 la m\u00e9so- et \u00e0 la macrofaune augmentait k de 265 et 108% pour les arbres AM et ECM, respectivement\u00a0; (3) l'identit\u00e9 des esp\u00e8ces d'arbres, l'association mycorhizienne, la qualit\u00e9 initiale de la liti\u00e8re, les propri\u00e9t\u00e9s du sol, la composition des communaut\u00e9s microbiennes et la biomasse de la faune du sol ambiant \u00e9taient tous des facteurs influen\u00e7ant significativement la d\u00e9composition de la liti\u00e8re, mais l'identit\u00e9 des esp\u00e8ces d'arbres \u00e9tait le facteur dominant ind\u00e9pendamment de la taille des mailles des sacs de liti\u00e8re\u00a0; et (4) les effets de la m\u00e9sofaune sur la d\u00e9composition de la liti\u00e8re \u00e9taient principalement contr\u00f4l\u00e9s par l'identit\u00e9 des esp\u00e8ces d'arbres, la concentration initiale en Mg de la liti\u00e8re et le rapport lignine\u00a0:N, tandis que le petit impact suppl\u00e9mentaire de l'acc\u00e8s \u00e0 la macrofaune n'\u00e9tait pas bien expliqu\u00e9 par aucun des facteurs \u00e9valu\u00e9s. Dans l'ensemble, nos r\u00e9sultats sugg\u00e8rent que les esp\u00e8ces d'arbres affectent la d\u00e9composition de la liti\u00e8re via une stimulation diff\u00e9rente du fonctionnement de la faune du sol, et que les esp\u00e8ces d'arbres associ\u00e9es \u00e0 la MA et \u00e0 la mec diff\u00e8rent dans le degr\u00e9 auquel la faune du sol stimule la d\u00e9composition de la liti\u00e8re. Cependant, le mod\u00e8le n'\u00e9tait pas enti\u00e8rement coh\u00e9rent car les taux de d\u00e9composition de la liti\u00e8re pour la chaux associ\u00e9e \u00e0 la mec \u00e9taient stimul\u00e9s dans la m\u00eame mesure que les taux pour les esp\u00e8ces d'arbres associ\u00e9es \u00e0 la MA, le fr\u00eane et l'\u00e9rable. Dans l'ensemble, nos r\u00e9sultats sugg\u00e8rent que les communaut\u00e9s de m\u00e9so- et de macrofaune du sol peuvent am\u00e9liorer les effets des esp\u00e8ces d'arbres sur la d\u00e9composition de la liti\u00e8re ainsi que l'incorporation de la liti\u00e8re C dans le sol min\u00e9ral.", "keywords": ["Biomass (ecology)", "0106 biological sciences", "Litter quality", "Microfauna", "Plant Science", "Soil mesofauna", "01 natural sciences", "Plant litter", "Soil fauna", "Agricultural and Biological Sciences", "Biodiversity Conservation and Ecosystem Management", "Soil biology", "Microbial community", "Mycorrhizal Fungi and Plant Interactions", "Litter", "Soil water", "Wood Decomposition", "Saproxylic Insect Ecology and Forest Management", "Plant Interactions", "Biology", "Ecosystem", "Nature and Landscape Conservation", "Ecology", "Soil property", "Life Sciences", "04 agricultural and veterinary sciences", "15. Life on land", "Fauna", "Insect Science", "FOS: Biological sciences", "Environmental Science", "Physical Sciences", "Common garden", "0401 agriculture", " forestry", " and fisheries", "Litterbag mesh size"]}, "links": [{"href": "https://doi.org/10.1016/j.foreco.2022.120396"}, {"rel": "related", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/Forest%20Ecology%20and%20Management", "name": "related record", "description": "related record", "type": "application/json"}, {"rel": "self", "type": "application/geo+json", "title": "10.1016/j.foreco.2022.120396", "name": "item", "description": "10.1016/j.foreco.2022.120396", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main/items/10.1016/j.foreco.2022.120396"}, {"rel": "collection", "type": "application/json", "title": "Collection", "name": "collection", "description": "Collection", "href": "https://repository.soilwise-he.eu/cat/collections/metadata:main"}], "time": {"date": "2022-09-01T00:00:00Z"}}, {"id": "10.1002/ecm.1507", "type": "Feature", "geometry": null, "properties": {"updated": "2026-05-25T16:13:53Z", "type": "Journal Article", "created": "2022-01-09", "title": "Lessons learned from a long\u2010term irrigation experiment in a dry Scots pine forest: Impacts on traits and functioning", "description": "Abstract

Climate change exposes ecosystems to strong and rapid changes in their environmental boundary conditions mainly due to the altered temperature and precipitation patterns. It is still poorly understood how fast interlinked ecosystem processes respond to altered environmental conditions, if these responses occur gradually or suddenly when thresholds are exceeded, and if the patterns of the responses will reach a stable state. We conducted an irrigation experiment in the Pfynwald, Switzerland from 2003\uffe2\uff80\uff932018. A naturally dry Scots pine (Pinus sylvestris L.) forest was irrigated with amounts that doubled natural precipitation, thus releasing the forest stand from water limitation. The aim of this study was to provide a quantitative understanding on how different traits and functions of individual trees and the whole ecosystem responded to increased water availability, and how the patterns and magnitudes of these responses developed over time. We found that the response magnitude, the temporal trajectory of responses, and the length of initial lag period prior to significant response largely varied across traits. We detected rapid and stronger responses from aboveground tree traits (e.g., tree\uffe2\uff80\uff90ring width, needle length, and crown transparency) compared to belowground tree traits (e.g., fine\uffe2\uff80\uff90root biomass). The altered aboveground traits during the initial years of irrigation increased the water demand and trees adjusted by increasing root biomass during the later years of irrigation, resulting in an increased survival rate of Scots pine trees in irrigated plots. The irrigation also stimulated ecosystem\uffe2\uff80\uff90level foliar decomposition rate, fungal fruit body biomass, and regeneration abundances of broadleaved tree species. However, irrigation did not promote the regeneration of Scots pine trees, which are reported to be vulnerable to extreme droughts. Our results provide extensive evidence that tree\uffe2\uff80\uff90 and ecosystem\uffe2\uff80\uff90level responses were pervasive across a number of traits on long\uffe2\uff80\uff90term temporal scales. However, after reaching a peak, the magnitude of these responses either decreased or reached a new stable state, providing important insights into how resource alterations could change the system functioning and its boundary conditions.The relationship between the spatial variability of soil multifunctionality (i.e., the capacity of soils to conduct multiple functions; SVM) and major climatic drivers, such as temperature and aridity, has never been assessed globally in terrestrial ecosystems. We surveyed 236 dryland ecosystems from six continents to evaluate the relative importance of aridity and mean annual temperature, and of other abiotic (e.g., texture) and biotic (e.g., plant cover) variables as drivers of SVM, calculated as the averaged coefficient of variation for multiple soil variables linked to nutrient stocks and cycling. We found that increases in temperature and aridity were globally correlated to increases in SVM. Some of these climatic effects on SVM were direct, but others were indirectly driven through reductions in the number of vegetation patches and increases in soil sand content. The predictive capacity of our structural equation\uffc2\uffa0modelling was clearly higher for the spatial variability of N\uffe2\uff80\uff90 than for C\uffe2\uff80\uff90 and P\uffe2\uff80\uff90related soil variables. In the case of N cycling, the effects of temperature and aridity were both direct and indirect via changes in soil properties. For C and P, the effect of climate was mainly indirect via changes in plant attributes. These results suggest that future changes in climate may decouple the spatial availability of these elements for plants and microbes in dryland soils. Our findings significantly advance our understanding of the patterns and mechanisms driving SVM in drylands across the globe, which is critical for predicting changes in ecosystem functioning in response to climate change.The relationship between the spatial variability of soil multifunctionality (i.e., the capacity of soils to conduct multiple functions; SVM) and major climatic drivers, such as temperature and aridity, has never been assessed globally in terrestrial ecosystems. We surveyed 236 dryland ecosystems from six continents to evaluate the relative importance of aridity and mean annual temperature, and of other abiotic (e.g., texture) and biotic (e.g., plant cover) variables as drivers of SVM, calculated as the averaged coefficient of variation for multiple soil variables linked to nutrient stocks and cycling. We found that increases in temperature and aridity were globally correlated to increases in SVM. Some of these climatic effects on SVM were direct, but others were indirectly driven through reductions in the number of vegetation patches and increases in soil sand content. The predictive capacity of our structural equation\uffc2\uffa0modelling was clearly higher for the spatial variability of N\uffe2\uff80\uff90 than for C\uffe2\uff80\uff90 and P\uffe2\uff80\uff90related soil variables. In the case of N cycling, the effects of temperature and aridity were both direct and indirect via changes in soil properties. For C and P, the effect of climate was mainly indirect via changes in plant attributes. These results suggest that future changes in climate may decouple the spatial availability of these elements for plants and microbes in dryland soils. Our findings significantly advance our understanding of the patterns and mechanisms driving SVM in drylands across the globe, which is critical for predicting changes in ecosystem functioning in response to climate change.Climate change exposes ecosystems to strong and rapid changes in their environmental boundary conditions mainly due to the altered temperature and precipitation patterns. It is still poorly understood how fast interlinked ecosystem processes respond to altered environmental conditions, if these responses occur gradually or suddenly when thresholds are exceeded, and if the patterns of the responses will reach a stable state. We conducted an irrigation experiment in the Pfynwald, Switzerland from 2003\uffe2\uff80\uff932018. A naturally dry Scots pine (Pinus sylvestris L.) forest was irrigated with amounts that doubled natural precipitation, thus releasing the forest stand from water limitation. The aim of this study was to provide a quantitative understanding on how different traits and functions of individual trees and the whole ecosystem responded to increased water availability, and how the patterns and magnitudes of these responses developed over time. We found that the response magnitude, the temporal trajectory of responses, and the length of initial lag period prior to significant response largely varied across traits. We detected rapid and stronger responses from aboveground tree traits (e.g., tree\uffe2\uff80\uff90ring width, needle length, and crown transparency) compared to belowground tree traits (e.g., fine\uffe2\uff80\uff90root biomass). The altered aboveground traits during the initial years of irrigation increased the water demand and trees adjusted by increasing root biomass during the later years of irrigation, resulting in an increased survival rate of Scots pine trees in irrigated plots. The irrigation also stimulated ecosystem\uffe2\uff80\uff90level foliar decomposition rate, fungal fruit body biomass, and regeneration abundances of broadleaved tree species. However, irrigation did not promote the regeneration of Scots pine trees, which are reported to be vulnerable to extreme droughts. Our results provide extensive evidence that tree\uffe2\uff80\uff90 and ecosystem\uffe2\uff80\uff90level responses were pervasive across a number of traits on long\uffe2\uff80\uff90term temporal scales. However, after reaching a peak, the magnitude of these responses either decreased or reached a new stable state, providing important insights into how resource alterations could change the system functioning and its boundary conditions.