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  • 1
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 366, No. 6464 ( 2019-10-25), p. 480-485
    Abstract: Soil organisms, including earthworms, are a key component of terrestrial ecosystems. However, little is known about their diversity, their distribution, and the threats affecting them. We compiled a global dataset of sampled earthworm communities from 9212 sites in 57 countries as a basis for predicting patterns in earthworm diversity, abundance, and biomass. We found that local species richness and abundance typically peaked at mid-latitudes, displaying patterns opposite to those observed in aboveground organisms. However, high species dissimilarity across tropical locations may cause diversity across the entirety of the tropics to be higher than elsewhere. Climate variables and habitat cover were found to be more important in shaping earthworm communities than soil properties. These findings suggest that climate and habitat change may have serious implications for earthworm communities and for the functions they provide.
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
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    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2019
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  • 2
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 371, No. 6526 ( 2021-01-15), p. 239-241
    Abstract: Nature conservation literature and policy instruments mainly focus on the impacts of human development and the benefits of nature conservation for oceans and aboveground terrestrial organisms (e.g., birds and plants) and processes (e.g., food production), but these efforts almost completely ignore the majority of terrestrial biodiversity that is unseen and living in the soil ( 1 ). Little is known about the conservation status of most soil organisms and the effects of nature conservation policies on soil systems. Yet like “canaries in the coal mine,” when soil organisms begin to disappear, ecosystems will soon start to underperform, potentially hindering their vital functions for humankind. Soil biodiversity and its ecosystem functions thus require explicit consideration when establishing nature protection priorities and policies and when designing new conservation areas. To inform such efforts, we lay out a global soil biodiversity and ecosystem function monitoring framework to be considered in the context of the post-2020 discussions of the Convention on Biological Diversity (CBD). To support this framework, we suggest a suite of soil ecological indicators based on essential biodiversity variables (EBVs) ( 2 ) (see the figure and table S3) that directly link to current global targets such as the ones established under the CBD, the Sustainable Development Goals (SDGs), and the Paris Agreement (table S1).
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
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    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2021
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  • 3
    Online Resource
    Online Resource
    Proceedings of the National Academy of Sciences ; 2015
    In:  Proceedings of the National Academy of Sciences Vol. 112, No. 22 ( 2015-06-02), p. 7033-7038
    In: Proceedings of the National Academy of Sciences, Proceedings of the National Academy of Sciences, Vol. 112, No. 22 ( 2015-06-02), p. 7033-7038
    Abstract: Decomposition of organic material by soil microbes generates an annual global release of 50–75 Pg carbon to the atmosphere, ∼7.5–9 times that of anthropogenic emissions worldwide. This process is sensitive to global change factors, which can drive carbon cycle–climate feedbacks with the potential to enhance atmospheric warming. Although the effects of interacting global change factors on soil microbial activity have been a widespread ecological focus, the regulatory effects of interspecific interactions are rarely considered in climate feedback studies. We explore the potential of soil animals to mediate microbial responses to warming and nitrogen enrichment within a long-term, field-based global change study. The combination of global change factors alleviated the bottom-up limitations on fungal growth, stimulating enzyme production and decomposition rates in the absence of soil animals. However, increased fungal biomass also stimulated consumption rates by soil invertebrates, restoring microbial process rates to levels observed under ambient conditions. Our results support the contemporary theory that top-down control in soil food webs is apparent only in the absence of bottom-up limitation. As such, when global change factors alleviate the bottom-up limitations on microbial activity, top-down control becomes an increasingly important regulatory force with the capacity to dampen the strength of positive carbon cycle–climate feedbacks.
    Type of Medium: Online Resource
    ISSN: 0027-8424 , 1091-6490
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    Language: English
    Publisher: Proceedings of the National Academy of Sciences
    Publication Date: 2015
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  • 4
    Online Resource
    Online Resource
    Proceedings of the National Academy of Sciences ; 2015
    In:  Proceedings of the National Academy of Sciences Vol. 112, No. 37 ( 2015-09-15)
    In: Proceedings of the National Academy of Sciences, Proceedings of the National Academy of Sciences, Vol. 112, No. 37 ( 2015-09-15)
    Type of Medium: Online Resource
    ISSN: 0027-8424 , 1091-6490
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    Language: English
    Publisher: Proceedings of the National Academy of Sciences
    Publication Date: 2015
    detail.hit.zdb_id: 209104-5
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  • 5
    Online Resource
    Online Resource
    American Association for the Advancement of Science (AAAS) ; 2021
    In:  Science Vol. 371, No. 6533 ( 2021-03-05)
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 371, No. 6533 ( 2021-03-05)
    Abstract: Our study showed that increases in seasonal productivity drive earlier autumn senescence of temperate trees. Norby argues that this finding is contradicted by observations from free-air CO 2 enrichment (FACE) experiments, where elevated CO 2 has been found to delay senescence in some cases. We provide a detailed answer showing that the results from FACE studies are in agreement with our conclusions.
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
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    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2021
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  • 6
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 381, No. 6653 ( 2023-07-07)
    Abstract: Ongoing climate change is causing rapid shifts in plant phenology, with far-reaching effects on the terrestrial carbon cycle and biodiversity. While advances in spring leaf-out dates in temperate and boreal forests are well documented, the effects on autumn leaf senescence are less clear. This is because leaf senescence is not only affected by temperature but also by day length and vegetation activity early in the season in ways that are poorly understood. Accurately predicting future growing-season lengths and plant photosynthesis requires a better understanding of these interacting mechanisms at broad spatial scales. RATIONALE Local observations and experiments suggest that early-season warming, causing earlier spring leaf-out and faster plant development, tends to advance autumn senescence dates. Conversely, late-season warming tends to delay autumn senescence. If true more generally, then climate warming has opposing effects at the start and end of the growing season, with a reversal of effects somewhere in between. To test the generality of the opposing effects of climate warming on leaf senescence in Northern Hemisphere forests, we used satellite, ground, and carbon flux data, as well as controlled experiments. RESULTS Our results revealed that warming early and late in the growing season indeed has contrasting effects on leaf senescence, with a reversal occurring after the summer solstice. Across 84% of the northern forest area, we found that warmer temperatures and increased vegetation activity before the solstice advance the onset of senescence by 1.9 ± 0.1 days per °C, whereas warmer post-solstice temperatures slow the progression of senescence by 2.6 ± 0.1 days per °C. Between 1966 and 2015, the earlier onset of senescence has led to advances of 0.20 ± 0.07 days per year of the date at which autumn temperature starts to drive senescence progression. By contrast, mid-senescence continues to occur slightly later by 0.04 ± 0.01 days per year, leading to a lengthening of the autumnal senescence period. In our experiments, warmer pre-solstice temperatures also led to earlier primary growth cessation (bud set), demonstrating that the impact of a warmer pre-solstice period extends beyond leaf development and life span. This highlights the crucial role of overall plant development and sink activity before the summer solstice in determining growing-season length. CONCLUSION We have developed a unified explanatory framework for predicting autumn phenology, showing that leaf senescence now tends to begin earlier, because of increased pre-solstice vegetation activity, but progresses more slowly, such that the end of senescence occurs later. The reversal in trees’ responsiveness to warming after the summer solstice likely is triggered by changes in day length and allows them to initiate the physiological processes of leaf senescence and nutrient resorption in a fine-tuned balance between source and sink dynamics. Our results demonstrate the impact of developmental constraints (from cell and tissue growth) on autumn leaf senescence and forest productivity, affecting trends in growing-season length across the entire Northern Hemisphere. These insights provide a better understanding of the changes in growing seasons and carbon uptake of temperate and boreal forests under climate change. Autumn phenological responses to pre-solstice and post-solstice climate warming. In cold years, slow development before the summer solstice delays the onset of senescence, and cold autumn temperatures accelerate senescence progression. In warm years, fast development before the summer solstice advances senescence onset, and warm autumn temperatures slow senescence progression, delaying the end of senescence.
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
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    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2023
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    detail.hit.zdb_id: 2066996-3
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  • 7
    In: Proceedings of the National Academy of Sciences, Proceedings of the National Academy of Sciences, Vol. 117, No. 22 ( 2020-06-02), p. 12192-12200
    Abstract: Late-spring frosts (LSFs) affect the performance of plants and animals across the world’s temperate and boreal zones, but despite their ecological and economic impact on agriculture and forestry, the geographic distribution and evolutionary impact of these frost events are poorly understood. Here, we analyze LSFs between 1959 and 2017 and the resistance strategies of Northern Hemisphere woody species to infer trees’ adaptations for minimizing frost damage to their leaves and to forecast forest vulnerability under the ongoing changes in frost frequencies. Trait values on leaf-out and leaf-freezing resistance come from up to 1,500 temperate and boreal woody species cultivated in common gardens. We find that areas in which LSFs are common, such as eastern North America, harbor tree species with cautious (late-leafing) leaf-out strategies. Areas in which LSFs used to be unlikely, such as broad-leaved forests and shrublands in Europe and Asia, instead harbor opportunistic tree species (quickly reacting to warming air temperatures). LSFs in the latter regions are currently increasing, and given species’ innate resistance strategies, we estimate that ∼35% of the European and ∼26% of the Asian temperate forest area, but only ∼10% of the North American, will experience increasing late-frost damage in the future. Our findings reveal region-specific changes in the spring-frost risk that can inform decision-making in land management, forestry, agriculture, and insurance policy.
    Type of Medium: Online Resource
    ISSN: 0027-8424 , 1091-6490
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    Language: English
    Publisher: Proceedings of the National Academy of Sciences
    Publication Date: 2020
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  • 8
    Online Resource
    Online Resource
    American Association for the Advancement of Science (AAAS) ; 2019
    In:  Science Vol. 366, No. 6469 ( 2019-11-29)
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 366, No. 6469 ( 2019-11-29)
    Abstract: Our study quantified the global tree restoration potential and its associated carbon storage potential under existing climate conditions. Skidmore et al . dispute our findings, using as reference a yearly estimation of carbon storage that could be reached by 2050. We provide a detailed answer highlighting misunderstandings in their interpretation, notably that we did not consider any time limit for the restoration process.
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
    RVK:
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    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2019
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    detail.hit.zdb_id: 2066996-3
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  • 9
    Online Resource
    Online Resource
    Proceedings of the National Academy of Sciences ; 2017
    In:  Proceedings of the National Academy of Sciences Vol. 114, No. 43 ( 2017-10-24), p. 11464-11469
    In: Proceedings of the National Academy of Sciences, Proceedings of the National Academy of Sciences, Vol. 114, No. 43 ( 2017-10-24), p. 11464-11469
    Abstract: The structure of the competitive network is an important driver of biodiversity and coexistence in natural communities. In addition to determining which species survive, the nature and intensity of competitive interactions within the network also affect the growth, productivity, and abundances of those individuals that persist. As such, the competitive network structure may likewise play an important role in determining community-level functioning by capturing the net costs of competition. Here, using an experimental system comprising 18 wood decay basidiomycete fungi, we test this possibility by quantifying the links among competitive network structure, species diversity, and community function. We show that species diversity alone has negligible impacts on community functioning, but that diversity interacts with two key properties of the competitive network—competitive intransitivity and average competitive ability—to ultimately shape biomass production, respiration, and carbon use efficiency. Most notably, highly intransitive communities comprising weak competitors exhibited a positive diversity–function relationship, whereas weakly intransitive communities comprising strong competitors exhibited a negative relationship. These findings demonstrate that competitive network structure can be an important determinant of community-level functioning, capturing a gradient from weakly to strongly competitive communities. Our research suggests that the competitive network may therefore act as a unifying link between diversity and function, providing key insight as to how and when losses in biodiversity will impact ecosystem function.
    Type of Medium: Online Resource
    ISSN: 0027-8424 , 1091-6490
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    Language: English
    Publisher: Proceedings of the National Academy of Sciences
    Publication Date: 2017
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  • 10
    Online Resource
    Online Resource
    Proceedings of the National Academy of Sciences ; 2020
    In:  Proceedings of the National Academy of Sciences Vol. 117, No. 21 ( 2020-05-26), p. 11551-11558
    In: Proceedings of the National Academy of Sciences, Proceedings of the National Academy of Sciences, Vol. 117, No. 21 ( 2020-05-26), p. 11551-11558
    Abstract: As the primary decomposers of organic material in terrestrial ecosystems, fungi are critical agents of the global carbon cycle. Yet our ability to link fungal community composition to ecosystem functioning is constrained by a limited understanding of the factors accounting for different wood decomposition rates among fungi. Here we examine which traits best explain fungal decomposition ability by combining detailed trait-based assays on 34 saprotrophic fungi from across North America in the laboratory with a 5-y field study comprising 1,582 fungi isolated from 74 decomposing logs. Fungal growth rate (hyphal extension rate) was the strongest single predictor of fungal-mediated wood decomposition rate under laboratory conditions, and accounted for up to 27% of the in situ variation in decomposition in the field. At the individual level, decomposition rate was negatively correlated with moisture niche width (an indicator of drought stress tolerance) and with the production of nutrient-mineralizing extracellular enzymes. Together, these results suggest that decomposition rates strongly align with a dominance-tolerance life-history trade-off that was previously identified in these isolates, forming a spectrum from slow-growing, stress-tolerant fungi that are poor decomposers to fast-growing, highly competitive fungi with fast decomposition rates. Our study illustrates how an understanding of fungal trait variation could improve our predictive ability of the early and midstages of wood decay, to which our findings are most applicable. By mapping our results onto the biogeographic distribution of the dominance-tolerance trade-off across North America, we approximate broad-scale patterns in intrinsic fungal-mediated wood decomposition rates.
    Type of Medium: Online Resource
    ISSN: 0027-8424 , 1091-6490
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    Language: English
    Publisher: Proceedings of the National Academy of Sciences
    Publication Date: 2020
    detail.hit.zdb_id: 209104-5
    detail.hit.zdb_id: 1461794-8
    SSG: 11
    SSG: 12
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