Publications by authors named "Miguel Berdugo"

It is unclear how much land use intensification ecosystems can withstand before undergoing abrupt changes in their structure and dynamics. Here we assess how the functional structure, diversity and temporal stability of 150 agricultural grasslands responded to large variations in land use intensification, namely, different intensities of fertilization, grazing and mowing. Using multi-site time series (2008-2020) of plant trait distributions, we identify two thresholds where the functional structure, diversity and stability of grasslands changed dramatically.

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Montane ecosystems are crucial for maintaining global biodiversity and function that sustain life on our planet. Yet, these ecosystems are highly vulnerable to changing temperatures and may undergo critical transitions under ongoing climate change. What we do not know is to what extent montane biodiversity and ecosystem services will respond to local temperature variations in a gradual versus abrupt manner across global environments.

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Resilience is a key feature of ecosystem dynamics reflecting a system's ability to resist and recover from environmental perturbations. Slowing down in the rate of recovery has been used as an early-warning signal for abrupt transitions. Recent advances in Earth observation (EO) vegetation data provide the capability to capture broad-scale resilience patterns and identify regions experiencing resilience loss.

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Fires alter the stability of organic matter and promote soil erosion which threatens the fundamental coupling of soil biogeochemical cycles. Yet, how soil biogeochemistry and its environmental drivers respond to fire remain virtually unknown globally. Here, we integrate experimental observations and random forest model, and reveal significant divergence in the responses of soil biogeochemical attributes to fire, including soil carbon (C), nitrogen (N), and phosphorus (P) contents worldwide.

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Article Synopsis
  • Global soil biodiversity and functions face threats due to water availability thresholds, which are not well understood.
  • Analyzing data from 383 global sites shows that these thresholds change how climate, vegetation, and soil properties impact soil biodiversity and functions.
  • In areas with less aridity, vegetation and soil properties play a key role, but in more arid regions, climate becomes the main factor influencing soil biodiversity, particularly affecting soil multidiversity more than multifunctionality.
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Earth harbours an extraordinary plant phenotypic diversity that is at risk from ongoing global changes. However, it remains unknown how increasing aridity and livestock grazing pressure-two major drivers of global change-shape the trait covariation that underlies plant phenotypic diversity. Here we assessed how covariation among 20 chemical and morphological traits responds to aridity and grazing pressure within global drylands.

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Climate change will affect the way biodiversity influences the stability of plant communities. Although biodiversity, associated species asynchrony, and species stability could enhance community stability, the understanding of potential nonlinear shifts in the biodiversity-stability relationship across a wide range of aridity (measured as the aridity index, the precipitation/potential evapotranspiration ratio) gradients and the underlying mechanisms remain limited. Using an 8-year dataset from 687 sites in Mongolia, which included 5496 records of vegetation and productivity, we found that the temporal stability of plant communities decreased more rapidly in more arid areas than in less arid areas.

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The emergence of alternative stable states in forest systems has significant implications for the functioning and structure of the terrestrial biosphere, yet empirical evidence remains scarce. Here, we combine global forest biodiversity observations and simulations to test for alternative stable states in the presence of evergreen and deciduous forest types. We reveal a bimodal distribution of forest leaf types across temperate regions of the Northern Hemisphere that cannot be explained by the environment alone, suggesting signatures of alternative forest states.

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  • Plant-soil biodiversity interactions are crucial for terrestrial ecosystems, yet it's unclear which specific topsoil microbial and small invertebrate organisms consistently associate with land plants.
  • A field survey of 150 land plant species across 124 locations revealed that these plants only shared less than 1% of the soil organisms, mostly generalist decomposers and phagotrophs, with their presence linked to important functional genes.
  • Environmental factors like aridity, soil pH, and carbon content can significantly disrupt the relationships between land plants and soil organisms, potentially impacting soil ecosystem processes in the face of climate change.
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Perennial plants create productive and biodiverse hotspots, known as fertile islands, beneath their canopies. These hotspots largely determine the structure and functioning of drylands worldwide. Despite their ubiquity, the factors controlling fertile islands under conditions of contrasting grazing by livestock, the most prevalent land use in drylands, remain virtually unknown.

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Self-organized spatial patterns are a common feature of complex systems, ranging from microbial communities to mussel beds and drylands. While the theoretical implications of these patterns for ecosystem-level processes, such as functioning and resilience, have been extensively studied, empirical evidence remains scarce. To address this gap, we analyzed global drylands along an aridity gradient using remote sensing, field data, and modeling.

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Article Synopsis
  • Crossing certain aridity thresholds in drylands can lead to significant declines in plant productivity and can contribute to land degradation and desertification.
  • Our research found that adding nitrogen (N) to these ecosystems can boost plant biomass and shift the aridity threshold higher, potentially reducing the negative impacts of increased dryness.
  • We predict that under high-emission scenarios, the impact of nitrogen could help mitigate the adverse effects of climate change on vegetation in drylands compared to scenarios without considering nitrogen.
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Large-scale, abrupt ecosystem change in direct response to climate extremes is a critical but poorly documented phenomenon. Yet, recent increases in climate-induced tree mortality raise concern that some forest ecosystems are on the brink of collapse across wide environmental gradients. Here we assessed climatic and productivity trends across the world's five Mediterranean forest ecosystems from 2000 to 2021 and detected a large-scale, abrupt forest browning and productivity decline in Chile (>90% of the forest in <100 days), responding to a sustained, acute drought.

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Fairy circles (FCs) are regular vegetation patterns found in drylands of Namibia and Western Australia. It is virtually unknown whether they are also present in other regions of the world and which environmental factors determine their distribution. We conducted a global systematic survey and found FC-like vegetation patterns in 263 sites from 15 countries and three continents, including the Sahel, Madagascar, and Middle-West Asia.

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Increasing the number of environmental stressors could decrease ecosystem functioning in soils. Yet this relationship has never been globally assessed outside laboratory experiments. Here, using two independent global standardized field surveys, and a range of natural and human factors, we test the relationship between the number of environmental stressors exceeding different critical thresholds and the maintenance of multiple ecosystem services across biomes.

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Soils support an immense portion of Earth's biodiversity and maintain multiple ecosystem functions which are essential for human well-being. Environmental thresholds are known to govern global vegetation patterns, but it is still unknown whether they can be used to predict the distribution of soil organisms and functions across global biomes. Using a global field survey of 383 sites across contrasting climatic and vegetation conditions, here we showed that soil biodiversity and functions exhibited pervasive nonlinear patterns worldwide and are mainly governed by water availability (precipitation and potential evapotranspiration).

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Soil contamination is one of the main threats to ecosystem health and sustainability. Yet little is known about the extent to which soil contaminants differ between urban greenspaces and natural ecosystems. Here we show that urban greenspaces and adjacent natural areas (i.

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While the contribution of biodiversity to supporting multiple ecosystem functions is well established in natural ecosystems, the relationship of the above- and below-ground diversity with ecosystem multifunctionality remains virtually unknown in urban greenspaces. Here we conducted a standardized survey of urban greenspaces from 56 municipalities across six continents, aiming to investigate the relationships of plant and soil biodiversity (diversity of bacteria, fungi, protists and invertebrates, and metagenomics-based functional diversity) with 18 surrogates of ecosystem functions from nine ecosystem services. We found that soil biodiversity across biomes was significantly and positively correlated with multiple dimensions of ecosystem functions, and contributed to key ecosystem services such as microbially driven carbon pools, organic matter decomposition, plant productivity, nutrient cycling, water regulation, plant-soil mutualism, plant pathogen control and antibiotic resistance regulation.

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Grazing represents the most extensive use of land worldwide. Yet its impacts on ecosystem services remain uncertain because pervasive interactions between grazing pressure, climate, soil properties, and biodiversity may occur but have never been addressed simultaneously. Using a standardized survey at 98 sites across six continents, we show that interactions between grazing pressure, climate, soil, and biodiversity are critical to explain the delivery of fundamental ecosystem services across drylands worldwide.

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Article Synopsis
  • * Analyzing over 1300 soil samples, researchers found that hot, arid regions in developing countries have the lowest levels of essential micronutrients like Cu, Fe, and Zn.
  • * The study indicates that rising temperatures could lead to sudden drops in these micronutrients, especially if the temperature exceeds 12-14°C, affecting ecosystem function and food production in vulnerable areas.
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  • * A 20-year satellite study of dryland vegetation shows that 50% of ecosystems experience abrupt increases or decreases in plant productivity, with such changes occurring more frequently in regions facing recent droughts.
  • * Identifying these abrupt changes helps to pinpoint vulnerable areas in drylands and informs strategies for effective management, especially in ecosystems with low soil organic carbon or high aridity.
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Soils are the foundation of all terrestrial ecosystems. However, unlike for plants and animals, a global assessment of hotspots for soil nature conservation is still lacking. This hampers our ability to establish nature conservation priorities for the multiple dimensions that support the soil system: from soil biodiversity to ecosystem services.

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  • The study investigates how temperature affects the distribution and abundance of soil fungal decomposers, which are key players in the global carbon cycle.
  • Researchers found that small increases in temperature, particularly beyond a 9°C threshold, can lead to significant drops in these decomposers' populations, impacting soil carbon content.
  • The findings suggest that as temperatures rise, especially in dry environments, the decline in fungal decomposers may hinder soil decomposition processes and alter carbon emissions, emphasizing the need to understand temperature thresholds for future climate change impacts.
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