{"type": "FeatureCollection", "features": [{"id": "10.1126/science.aay5958", "type": "Feature", "geometry": null, "properties": {"updated": "2026-10-06T16:18:22Z", "type": "Journal Article", "created": "2020-02-14", "title": "Global ecosystem thresholds driven by aridity", "description": "Thresholds of aridity           <p>             Increasing aridity due to climate change is expected to affect multiple ecosystem structural and functional attributes in global drylands, which cover \uffe2\uff88\uffbc45% of the terrestrial globe. Berdugo             et al.             show that increasing aridity promotes thresholds on the structure and functioning of drylands (see the Perspective by Hirota and Oliveira). Their database includes 20 variables summarizing multiple aspects and levels of ecological organization. They found evidence for a series of abrupt ecological events occurring sequentially in three phases, culminating with a shift to low-cover ecosystems that are nutrient- and species-poor at high aridity values. They estimate that more than 20% of land surface will cross at least one of the thresholds by 2100, which can potentially lead to widespread land degradation and desertification worldwide.           </p>           <p>             Science             , this issue p.             787             ; see also p.             739           </p", "keywords": ["[SDE] Environmental Sciences", "0301 basic medicine", "570", "Increasing aridity", "[SDE.MCG]Environmental Sciences/Global Changes", "Climate Change", "availability", "Promotes sequential", "vegetation cover", "Systemic thresholds", "soil", "forest", "Soil", "03 medical and health sciences", "https://purl.org/becyt/ford/1.6", "XXXXXX - Unknown", "Climate change", "functional traits", "https://purl.org/becyt/ford/1", "climate", "Climatical change", "Ecosystem", "Dryland ecosystems", "Aridity", "2. Zero hunger", "regime shifts", "drylands", "0303 health sciences", "500", "Abrupt thresholds", "Ecolog\u00eda", "15. 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Despite their  important contribution to the global land C sink, we have a poor  mechanistic understanding of the processes that drive C cycling patterns  in drylands. In this study in eastern Utah, we examined the natural  variation of soil C pools and fluxes along semiorthogonal gradients of  climate and soil texture in order to determine the pertinent environmental  controls on soil C cycling dynamics. Our study revealed a high degree of  collinearity among C stocks and fluxes, which were related to climate,  vegetation, and soil clay content. Soil C pools were positively correlated  with both soil clay content and precipitation, which in turn was linked to  aboveground plant biomass. By contrast, enzyme activities were negatively  associated with temperature. We observed a strong decoupling of C pools  and fluxes (for example, total C, DOC, microbial biomass C, and  respiration) from the enzyme activities involved in organic matter  decomposition. Overall, our findings indicate that the within- and  between-site variation of soil C pools across diverse dryland ecosystems  was strongly linked to both climate and edaphic characteristics, but the  high degree of local variability within sites could challenge  interpretations of environmental controls at broader scales.", "keywords": ["soil organic carbon", "dryland ecosystems", "microbial biomass", "13. Climate action", "clay", "15. 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Berdugo             et al.             show that increasing aridity promotes thresholds on the structure and functioning of drylands (see the Perspective by Hirota and Oliveira). Their database includes 20 variables summarizing multiple aspects and levels of ecological organization. They found evidence for a series of abrupt ecological events occurring sequentially in three phases, culminating with a shift to low-cover ecosystems that are nutrient- and species-poor at high aridity values. 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