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Habitat Affinity of Riverine Dissolved Organic Matter Linked to Molecular Traits 与分子特征相关的河流溶解有机质生境亲和性
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-05 DOI: 10.1111/gcb.70736
Yifan Cui, Ang Hu, James C. Stegen, Jianjun Wang

Fluxes of organic matter across Earth habitats shape ecosystem function and carbon storage. Yet, it is challenging to predict how the molecules are preferentially accumulated in specific habitats, that is, the habitat affinities, due to their diverse characteristics. Here, we develop an indicator of compositional-level habitat affinity for dissolved organic matter (DOM) by quantifying the aggregated affinities of individual molecules that are over- or under-represented relative to a reference habitat. Applying this indicator to 93 paired riverine water-sediment sites, we find that 65.1% of molecules show non-significant habitat affinities for water or sediment and are thermodynamically favorable and susceptible to microbial degradation. Consistently, the habitat affinities of DOM assemblages decrease with lower molecular weights and recalcitrance for waters, and with higher thermodynamic favorability for sediments. These affinities are both reduced by elevated temperatures and anthropogenic pressures, such as nitrogen loading and land-use change. Our projection of habitat affinities of global riverine DOM shows that regions with intense anthropogenic disturbances or warm climates, such as East Asia, Western Europe, and the Amazon, tend to exhibit lower affinities. These findings suggest enhanced molecular homogenization between water and sediment habitats is associated with environmental changes and underscore the importance of habitat affinities for predicting the potential trajectories of organic carbon across ecosystems.

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引用次数: 0
Correction to “Soil Protist Diversity and Biotic Interactions Shape Ecosystem Functions Under Climate Change” 修正“气候变化下土壤原生生物多样性和生物相互作用塑造生态系统功能”。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-05 DOI: 10.1111/gcb.70744

Liu, H., C. S. C. Martins, G. Zhou, et al. 2026. “Soil Protist Diversity and Biotic Interactions Shape Ecosystem Functions Under Climate Change.” Global Change Biology 32, no. 1: e70692. https://doi.org/10.1111/gcb.70692.

We wish to correct the following aspects Liu et al. (2026) concerning data availability. These changes are made to improve accuracy and transparency in acknowledging the original experiment and dataset on which this study builds. The corrections do not affect the results, interpretations, or overall conclusions of the article.

1. Data Availability section

Original text:

“All sequence data generated in this study are publicly available in the European Nucleotide Archive under project accession PRJEB53575. The complete raw datasets underlying the analyses presented here, together with associated supporting files, are archived on Figshare via the DOI https://doi.org/10.6084/m9.figshare.30968560.”

Corrected text:

“Original datasets from the microcosm study are available on Figshare (https://doi.org/10.6084/m9.figshare.20077217). All datasets used in the present study are archived on Figshare (https://doi.org/10.6084/m9.figshare.30968560). All sequence data generated in this study are publicly available in the European Nucleotide Archive under project accession PRJEB53575.”

This correction ensures that both the original experimental data and the processed datasets used in the study are properly referenced.

2. Material and Methods attribution:

Sections 2.2–2.6 and 2.8 of the Methods are adapted from the previously published article: Martins et al. (2024) Aboveground and belowground biodiversity have complementary effects on ecosystem functions across global grasslands. PLOS Biology 22(8): e3002736. https://doi.org/10.1371/journal.pbio.3002736.

This ensures proper attribution to the original source. These changes do not affect the results, interpretations, or overall conclusions of the article.

We apologize for these errors.

Liu, H., C. S. C. Martins, G. Zhou, et al. 2026. “Soil Protist Diversity and Biotic Interactions Shape Ecosystem Functions Under Climate Change.” Global Change Biology 32, no. 1: e70692. https://doi.org/10.1111/gcb.70692.

Martins, C. S., M. Delgado-Baquerizo, R. H. Jayaramaiah, et al. 2024. “Aboveground and Belowground Biodiversity Have Complementary Effects on Ecosystem Functions Across Global Grasslands.” PLoS Biology 22, no. 8: e3002736.

{"title":"Correction to “Soil Protist Diversity and Biotic Interactions Shape Ecosystem Functions Under Climate Change”","authors":"","doi":"10.1111/gcb.70744","DOIUrl":"10.1111/gcb.70744","url":null,"abstract":"<p>Liu, H., C. S. C. Martins, G. Zhou, et al. 2026. “Soil Protist Diversity and Biotic Interactions Shape Ecosystem Functions Under Climate Change.” <i>Global Change Biology</i> 32, no. 1: e70692. https://doi.org/10.1111/gcb.70692.</p><p>We wish to correct the following aspects Liu et al. (2026) concerning data availability. These changes are made to improve accuracy and transparency in acknowledging the original experiment and dataset on which this study builds. The corrections do not affect the results, interpretations, or overall conclusions of the article.</p><p>1. Data Availability section</p><p>Original text:</p><p>“All sequence data generated in this study are publicly available in the European Nucleotide Archive under project accession PRJEB53575. The complete raw datasets underlying the analyses presented here, together with associated supporting files, are archived on Figshare via the DOI https://doi.org/10.6084/m9.figshare.30968560.”</p><p>Corrected text:</p><p>“Original datasets from the microcosm study are available on Figshare (https://doi.org/10.6084/m9.figshare.20077217). All datasets used in the present study are archived on Figshare (https://doi.org/10.6084/m9.figshare.30968560). All sequence data generated in this study are publicly available in the European Nucleotide Archive under project accession PRJEB53575.”</p><p>This correction ensures that both the original experimental data and the processed datasets used in the study are properly referenced.</p><p>2. Material and Methods attribution:</p><p>Sections 2.2–2.6 and 2.8 of the Methods are adapted from the previously published article: Martins et al. (2024) Aboveground and belowground biodiversity have complementary effects on ecosystem functions across global grasslands. PLOS Biology 22(8): e3002736. https://doi.org/10.1371/journal.pbio.3002736.</p><p>This ensures proper attribution to the original source. These changes do not affect the results, interpretations, or overall conclusions of the article.</p><p>We apologize for these errors.</p><p>Liu, H., C. S. C. Martins, G. Zhou, et al. 2026. “Soil Protist Diversity and Biotic Interactions Shape Ecosystem Functions Under Climate Change.” <i>Global Change Biology</i> 32, no. 1: e70692. https://doi.org/10.1111/gcb.70692.</p><p>Martins, C. S., M. Delgado-Baquerizo, R. H. Jayaramaiah, et al. 2024. “Aboveground and Belowground Biodiversity Have Complementary Effects on Ecosystem Functions Across Global Grasslands.” <i>PLoS Biology</i> 22, no. 8: e3002736.</p>","PeriodicalId":175,"journal":{"name":"Global Change Biology","volume":"32 2","pages":""},"PeriodicalIF":12.0,"publicationDate":"2026-02-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/gcb.70744","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146117069","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Detected Shifts Towards Drought-Adaptive Strategies in the Amazon Forest Over the Last Four Decades 在过去的四十年里,亚马逊森林向干旱适应策略的转变。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-04 DOI: 10.1111/gcb.70727
Milton Barbosa, Renata A. Maia, Imma Oliveras Menor, Ben Hur Marimon Junior, Beatriz Schwantes Marimon, G. Wilson Fernandes, Yadvinder Malhi, Jesús Aguirre-Gutiérrez

The Amazon Forest is undergoing rapid ecological shifts driven by intensifying drought, rising temperatures, and widespread anthropogenic disturbance. Yet the reorganization of vegetation functional strategies under climate stress remains poorly quantified at the biome scale. Here, we show that the temporal stability of canopy reflectance offers a sensitive remote proxy for sclerophylly—leaf toughness, a key indicator of conservative, drought-adaptive plant strategies. By integrating ground-based trait data (specific leaf area, SLA) from over 3000 trees across 448 plots in the Amazon-Cerrado savanna transition zone with high-resolution remote sensing imagery, we demonstrate that lower SLA—a well-established proxy for conservative leaf strategies—is associated with reduced dry-season variability in the blue band spectral reflectance of vegetation. Extending the analysis across 130 plots in nine Amazonian countries using 40 years of harmonised remote sensing data, we find that dry-season reflectance variability has declined by ~34% (a drop of ~10 percentage points) since 1984, indicating a biome-wide shift toward greater drought tolerance. This trend is most pronounced in the southern and eastern Amazon and closely tracks rising climate stress, particularly increased temperature, evaporative demand, and water deficit. If these patterns persist, much of the southern and eastern Amazon could reach reflectance-stability levels comparable to transitional zones with the Cerrado savanna biome within the next three to four decades. Our results show signals of an early-stage forest functional transformation that could reduce forest productivity and carbon uptake, increase vulnerability to fire, and diminish biodiversity. These findings highlight regions where early signs of reduced forest resilience are emerging, underscoring the need for spatially targeted conservation.

由于干旱加剧、气温上升和广泛的人为干扰,亚马逊森林正在经历快速的生态变化。然而,在生物群系尺度上,气候胁迫下植被功能策略的重组仍然缺乏量化。本研究表明,冠层反射率的时间稳定性为植物的硬叶韧性提供了一个敏感的远程代理,而硬叶韧性是保守的干旱适应性植物策略的关键指标。通过将亚马逊-塞拉多热带草原过渡区448个样地的3000多棵树的地面特征数据(比叶面积,SLA)与高分辨率遥感图像相结合,我们证明了较低的SLA(保守叶片策略的成熟代表)与植被蓝波段光谱反射率的干季变异性减少有关。利用40年的统一遥感数据,将分析扩展到9个亚马逊国家的130个样地,我们发现自1984年以来,旱季反射率变率下降了约34%(下降了约10个百分点),表明整个生物群落向更强的耐旱性转变。这一趋势在亚马逊南部和东部最为明显,并与不断上升的气候压力密切相关,特别是温度升高、蒸发需求和水短缺。如果这种模式持续下去,亚马逊南部和东部的大部分地区将在未来三到四十年内达到与塞拉多热带稀树草原生物群落过渡区相当的反射稳定性水平。我们的研究结果表明,早期森林功能转变可能会降低森林生产力和碳吸收,增加对火灾的脆弱性,并减少生物多样性。这些发现突出表明,一些地区正在出现森林恢复力下降的早期迹象,强调有必要开展有针对性的空间保护。
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引用次数: 0
Large-Scale Forest Restoration Accompanied by Biodiversity Recovery in Costa Rica's Redistributive Payment for Ecosystem Service Program 哥斯达黎加生态系统服务再分配支付方案中伴随生物多样性恢复的大规模森林恢复。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-04 DOI: 10.1111/gcb.70730
Giacomo L. Delgado, Johan van den Hoogen, Daisy H. Dent, Tom Bradfer-Lawrence, Leland K. Werden, Rebecca Cole, Cristian Diaz Quesada, Jose-Angel Jimenez Fajarado, Alberto Méndez Rodríguez, Eduardo Mesén Solorzano, Gilmar Navarrete Chacón, Mario Coto, Irene Suarez Perez, Lucas Vahlas, Yuting Liang, Thomas Ward Crowther

Ecosystem restoration is widely recognized as among the most important means to combat both climate change and biodiversity loss. A vast range of studies have illustrated the potential for local ecological recovery, but its efficacy at large spatial scales remains highly uncertain. Until now, the lack of standardized biodiversity monitoring systems has restricted our capacity to evaluate the potential for ecological recovery at large spatial scales. Here, we use an ecoacoustic dataset from 119 locations to evaluate the biodiversity implications of large-scale forest restoration within Costa Rica's redistributive Payment for Ecosystem Service (PES) program. Soundscapes recorded in degraded pastures were marked by significant changes in the timing and frequencies typical of mature reference forests. In contrast, we show that the acoustic patterns of restored PES sites have recovered and now resemble reference forests more closely. The age and ecological composition of naturally regenerating forests within the PES have led to more dramatic patterns of acoustic recovery (soundscapes 1.4 times more similar to reference forests than pastures) than in their monoculture plantation counterparts (1.24 times). The scale and consistency of these findings provide strong evidence of effective restoration at scale, highlighting the ecological merits of natural restoration approaches over monoculture plantations.

生态系统恢复被广泛认为是应对气候变化和生物多样性丧失的最重要手段之一。大量的研究表明了局部生态恢复的潜力,但其在大空间尺度上的有效性仍然高度不确定。到目前为止,缺乏标准化的生物多样性监测系统限制了我们在大空间尺度上评估生态恢复潜力的能力。在此,我们使用来自119个地点的生态声学数据集来评估哥斯达黎加生态系统服务再分配支付(PES)计划中大规模森林恢复对生物多样性的影响。在退化牧场中记录的声景在时间和频率上的显著变化是成熟参考森林的典型特征。相比之下,我们发现恢复的PES站点的声学模式已经恢复,并且现在更接近参考森林。PES内自然再生森林的年龄和生态组成导致了更显著的声恢复模式(声景观与参考森林的相似度是参考森林的1.4倍,而不是与单一栽培人工林的相似度(1.24倍))。这些发现的规模和一致性为大规模的有效恢复提供了强有力的证据,突出了自然恢复方法相对于单一种植人工林的生态优势。
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引用次数: 0
Losing a Hidden Ally: The Shrinking Capacity of Upland Soils to Remove Atmospheric Methane 失去一个隐藏的盟友:陆地土壤去除大气甲烷的能力不断缩小。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-02 DOI: 10.1111/gcb.70741
Jingrui Yang, Xiaoyuan Yan, Longlong Xia
<p>Methane (CH<sub>4</sub>) is a powerful greenhouse gas and a central target for near-term climate mitigation. Despite its shorter atmospheric lifetime compared with carbon dioxide (CO<sub>2</sub>), CH<sub>4</sub> exerts a strong warming effect, contributing ~0.5°C of the observed 1.15°C global surface warming since preindustrial periods (IPCC <span>2023</span>). Consequently, rapid reductions in CH<sub>4</sub> emissions are widely recognized as one of the most effective ways to slow warming in the coming decades. This urgency is reflected in global initiatives like the Global Methane Pledge, which aims for substantial emission cuts by 2030. The atmospheric CH<sub>4</sub> budget is controlled by a balance between sources and sinks. While oxidation by hydroxyl radicals dominates global CH<sub>4</sub> removal, aerobic upland soils constitute the second-largest CH<sub>4</sub> sink, accounting for approximately 4% of global CH<sub>4</sub> uptake (Kirschke et al. <span>2013</span>). This sink is unique. Unlike atmospheric chemical sinks, soil CH<sub>4</sub> uptake is embedded within terrestrial ecosystems. This means it can, in principle, respond to land management and stewardship (Song et al. <span>2024</span>). For decades, upland soils have therefore been regarded as an important and manageable ally in mitigating climate change.</p><p>However, the upland soil methane sink is dynamic, especially in a rapidly changing climate. This is because methanotrophic microbes are highly sensitive to multiple factors: temperature, soil moisture, substrate availability, and land-use disturbance. Shifts in temperature and precipitation regimes, together with intensifying human land use, are altering the spatial and temporal patterns of CH<sub>4</sub> uptake in upland ecosystems (Guo et al. <span>2023</span>; Wang et al. <span>2025</span>). Yet the size and direction of these changes remain poorly understood. Observational soil–atmosphere CH<sub>4</sub> exchange remains spatially uneven, and existing models differ substantially in their capacity to represent the nonlinear and interacting controls on CH<sub>4</sub> fluxes.</p><p>To address these knowledge gaps, Li et al. (<span>2025</span>) make a major step forward. It provides the first observation-driven, three-decade (1993–2022) assessment of the changing role and spatiotemporal dynamics of global upland soils as CH<sub>4</sub> sinks and sources. Their study is built on an extensive compilation of in situ CH<sub>4</sub> flux measurements from upland ecosystems worldwide, including croplands, forests, grasslands and tundra. This dataset constitutes the most systematic and comprehensive collection of upland soil CH<sub>4</sub> observations currently available. Based on this rich data foundation, Li et al. (<span>2025</span>) upscaled site-level measurements to global gridded estimates with advanced machine-learning approaches, most notably the XGBoost algorithm. By integrating climatic variables, soil properties
{"title":"Losing a Hidden Ally: The Shrinking Capacity of Upland Soils to Remove Atmospheric Methane","authors":"Jingrui Yang,&nbsp;Xiaoyuan Yan,&nbsp;Longlong Xia","doi":"10.1111/gcb.70741","DOIUrl":"10.1111/gcb.70741","url":null,"abstract":"&lt;p&gt;Methane (CH&lt;sub&gt;4&lt;/sub&gt;) is a powerful greenhouse gas and a central target for near-term climate mitigation. Despite its shorter atmospheric lifetime compared with carbon dioxide (CO&lt;sub&gt;2&lt;/sub&gt;), CH&lt;sub&gt;4&lt;/sub&gt; exerts a strong warming effect, contributing ~0.5°C of the observed 1.15°C global surface warming since preindustrial periods (IPCC &lt;span&gt;2023&lt;/span&gt;). Consequently, rapid reductions in CH&lt;sub&gt;4&lt;/sub&gt; emissions are widely recognized as one of the most effective ways to slow warming in the coming decades. This urgency is reflected in global initiatives like the Global Methane Pledge, which aims for substantial emission cuts by 2030. The atmospheric CH&lt;sub&gt;4&lt;/sub&gt; budget is controlled by a balance between sources and sinks. While oxidation by hydroxyl radicals dominates global CH&lt;sub&gt;4&lt;/sub&gt; removal, aerobic upland soils constitute the second-largest CH&lt;sub&gt;4&lt;/sub&gt; sink, accounting for approximately 4% of global CH&lt;sub&gt;4&lt;/sub&gt; uptake (Kirschke et al. &lt;span&gt;2013&lt;/span&gt;). This sink is unique. Unlike atmospheric chemical sinks, soil CH&lt;sub&gt;4&lt;/sub&gt; uptake is embedded within terrestrial ecosystems. This means it can, in principle, respond to land management and stewardship (Song et al. &lt;span&gt;2024&lt;/span&gt;). For decades, upland soils have therefore been regarded as an important and manageable ally in mitigating climate change.&lt;/p&gt;&lt;p&gt;However, the upland soil methane sink is dynamic, especially in a rapidly changing climate. This is because methanotrophic microbes are highly sensitive to multiple factors: temperature, soil moisture, substrate availability, and land-use disturbance. Shifts in temperature and precipitation regimes, together with intensifying human land use, are altering the spatial and temporal patterns of CH&lt;sub&gt;4&lt;/sub&gt; uptake in upland ecosystems (Guo et al. &lt;span&gt;2023&lt;/span&gt;; Wang et al. &lt;span&gt;2025&lt;/span&gt;). Yet the size and direction of these changes remain poorly understood. Observational soil–atmosphere CH&lt;sub&gt;4&lt;/sub&gt; exchange remains spatially uneven, and existing models differ substantially in their capacity to represent the nonlinear and interacting controls on CH&lt;sub&gt;4&lt;/sub&gt; fluxes.&lt;/p&gt;&lt;p&gt;To address these knowledge gaps, Li et al. (&lt;span&gt;2025&lt;/span&gt;) make a major step forward. It provides the first observation-driven, three-decade (1993–2022) assessment of the changing role and spatiotemporal dynamics of global upland soils as CH&lt;sub&gt;4&lt;/sub&gt; sinks and sources. Their study is built on an extensive compilation of in situ CH&lt;sub&gt;4&lt;/sub&gt; flux measurements from upland ecosystems worldwide, including croplands, forests, grasslands and tundra. This dataset constitutes the most systematic and comprehensive collection of upland soil CH&lt;sub&gt;4&lt;/sub&gt; observations currently available. Based on this rich data foundation, Li et al. (&lt;span&gt;2025&lt;/span&gt;) upscaled site-level measurements to global gridded estimates with advanced machine-learning approaches, most notably the XGBoost algorithm. By integrating climatic variables, soil properties","PeriodicalId":175,"journal":{"name":"Global Change Biology","volume":"32 2","pages":""},"PeriodicalIF":12.0,"publicationDate":"2026-02-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/gcb.70741","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146099578","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
When Clearing Out an Old House Advances Science: The Hump-Shaped Diversity Distribution in Central European Grasslands Better Explained 当清理老房子推进科学:更好地解释中欧草原的驼峰形多样性分布。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-02 DOI: 10.1111/gcb.70731
Pascal Vittoz
<p>The proportion of natural grasslands in Central European landscapes prior to the Neolithic period, which were maintained through grazing by large herbivores or frequent disturbances, remains a subject of debate (Svenning <span>2002</span>). However, most of the grasslands in the current landscape were created by deforestation following the Late Bronze Age (Hejcman et al. <span>2013</span>). Centuries of stable management involving low-intensity mowing or grazing without fertilisation have since created species-rich ecosystems that are considered semi-natural in Central Europe. Wilson et al. (<span>2012</span>) concluded that European temperate grasslands are the richest ecosystems in the world up to 50 m<sup>2</sup>, with a maximum of 43 vascular plant species on 0.1 m<sup>2</sup> (in Romania) and 116 species on 25 m<sup>2</sup> (in the Czech Republic).</p><p>As with many taxonomic groups, the species richness of vascular plants in Central European grasslands, when inventoried in plots, exhibits a hump-shaped pattern in relation to elevation (e.g., Descombes et al. <span>2017</span>). However, the reason for the lower species richness in lowland areas compared to mid-elevations remains unclear. Until now, the hypothesis that grassland diversity decreased in low-lying areas following agricultural intensification after the Second World War has largely been accepted (Descombes et al. <span>2017</span>), despite a lack of available historical data to verify it. This intensification became possible following the production of mineral fertilisers after 1950, which allowed for a higher mowing frequency. Indeed, it is common to apply over 100 kg of nitrogen per hectare per year to meadows, with over three annual cuts (Zechmeister et al. <span>2003</span>).</p><p>As Widmer et al. (<span>2025</span>) explained, there are numerous assessments of species richness evolution in temperate grasslands, with contrasting results. However, they are all based on quite recent baseline data, mostly from after 1970 that is, after the peak of agricultural intensification. Therefore, although a decrease in species richness at the plot level in these grasslands was strongly suspected, it has not yet been possible to quantify it.</p><p>In 2003, during a building renovation, some of the authors discovered boxes containing 580 exhaustive plant inventories of Swiss grasslands, recorded between 1884 and 1931 (Riedel et al. <span>2023</span>). This impressive dataset was completely forgotten. The 0.3 × 0.3-m plots were widely distributed across Switzerland, at elevations ranging from 212 to 2547 m.</p><p>Resurveying such small plots, with only rough location information (mostly the name of the village and the elevation), scattered in landscapes that have completely changed within a century, was challenging. The authors followed a convincing procedure to produce a comparable data set (Widmer et al. <span>2025</span>): definition of a potential area based on available data and
{"title":"When Clearing Out an Old House Advances Science: The Hump-Shaped Diversity Distribution in Central European Grasslands Better Explained","authors":"Pascal Vittoz","doi":"10.1111/gcb.70731","DOIUrl":"10.1111/gcb.70731","url":null,"abstract":"&lt;p&gt;The proportion of natural grasslands in Central European landscapes prior to the Neolithic period, which were maintained through grazing by large herbivores or frequent disturbances, remains a subject of debate (Svenning &lt;span&gt;2002&lt;/span&gt;). However, most of the grasslands in the current landscape were created by deforestation following the Late Bronze Age (Hejcman et al. &lt;span&gt;2013&lt;/span&gt;). Centuries of stable management involving low-intensity mowing or grazing without fertilisation have since created species-rich ecosystems that are considered semi-natural in Central Europe. Wilson et al. (&lt;span&gt;2012&lt;/span&gt;) concluded that European temperate grasslands are the richest ecosystems in the world up to 50 m&lt;sup&gt;2&lt;/sup&gt;, with a maximum of 43 vascular plant species on 0.1 m&lt;sup&gt;2&lt;/sup&gt; (in Romania) and 116 species on 25 m&lt;sup&gt;2&lt;/sup&gt; (in the Czech Republic).&lt;/p&gt;&lt;p&gt;As with many taxonomic groups, the species richness of vascular plants in Central European grasslands, when inventoried in plots, exhibits a hump-shaped pattern in relation to elevation (e.g., Descombes et al. &lt;span&gt;2017&lt;/span&gt;). However, the reason for the lower species richness in lowland areas compared to mid-elevations remains unclear. Until now, the hypothesis that grassland diversity decreased in low-lying areas following agricultural intensification after the Second World War has largely been accepted (Descombes et al. &lt;span&gt;2017&lt;/span&gt;), despite a lack of available historical data to verify it. This intensification became possible following the production of mineral fertilisers after 1950, which allowed for a higher mowing frequency. Indeed, it is common to apply over 100 kg of nitrogen per hectare per year to meadows, with over three annual cuts (Zechmeister et al. &lt;span&gt;2003&lt;/span&gt;).&lt;/p&gt;&lt;p&gt;As Widmer et al. (&lt;span&gt;2025&lt;/span&gt;) explained, there are numerous assessments of species richness evolution in temperate grasslands, with contrasting results. However, they are all based on quite recent baseline data, mostly from after 1970 that is, after the peak of agricultural intensification. Therefore, although a decrease in species richness at the plot level in these grasslands was strongly suspected, it has not yet been possible to quantify it.&lt;/p&gt;&lt;p&gt;In 2003, during a building renovation, some of the authors discovered boxes containing 580 exhaustive plant inventories of Swiss grasslands, recorded between 1884 and 1931 (Riedel et al. &lt;span&gt;2023&lt;/span&gt;). This impressive dataset was completely forgotten. The 0.3 × 0.3-m plots were widely distributed across Switzerland, at elevations ranging from 212 to 2547 m.&lt;/p&gt;&lt;p&gt;Resurveying such small plots, with only rough location information (mostly the name of the village and the elevation), scattered in landscapes that have completely changed within a century, was challenging. The authors followed a convincing procedure to produce a comparable data set (Widmer et al. &lt;span&gt;2025&lt;/span&gt;): definition of a potential area based on available data and ","PeriodicalId":175,"journal":{"name":"Global Change Biology","volume":"32 2","pages":""},"PeriodicalIF":12.0,"publicationDate":"2026-02-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC12862448/pdf/","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146099633","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Spatiotemporal Trade-Offs and Synergies Among Environmental Footprints of Grain Crop Production in China. 中国粮食作物生产环境足迹的时空权衡与协同效应
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-01 DOI: 10.1111/gcb.70739
Fubin Sun, Wenfeng Liu, Han Su, Mesfin M Mekonnen, Zenghui Xu, Wei Wang, Minhui Qiang, Xiangxiang Ji, Pute Wu, La Zhuo

Human agricultural activities have exacerbated multiple types of natural resource depletion and environmental impacts through complex interactions with land, water, carbon, and nutrient cycles, which can be measured as corresponding environmental footprints (EFs). However, the spatiotemporal trade-offs and synergies among multiple EFs in agricultural systems remain under-quantified, hindering effective mitigation strategies. Here, we propose an assessment framework of spatiotemporal trade-offs and synergies among multiple EFs of crop production, with a case study on blue water, green water, land, carbon, nitrogen, and phosphorus footprints for wheat, maize, rice, and soybean production across 31 Chinese provinces over 2000-2018. In total, 3630 pairwise EFs were analyzed. Results show that, although the EFs of unit mass crop production generally declined across provinces, national total EFs increased, with land, carbon, and phosphorus footprints rising by 16%, 17%, and 23%, respectively, during the study period. Synergistic interactions among EFs prevailed, comprising 50% positive and 32% negative synergies. The spatial distribution of trade-offs and synergies varies by crop and region. Land use intensity is the main factor limiting the positive EF synergies.

{"title":"Spatiotemporal Trade-Offs and Synergies Among Environmental Footprints of Grain Crop Production in China.","authors":"Fubin Sun, Wenfeng Liu, Han Su, Mesfin M Mekonnen, Zenghui Xu, Wei Wang, Minhui Qiang, Xiangxiang Ji, Pute Wu, La Zhuo","doi":"10.1111/gcb.70739","DOIUrl":"https://doi.org/10.1111/gcb.70739","url":null,"abstract":"<p><p>Human agricultural activities have exacerbated multiple types of natural resource depletion and environmental impacts through complex interactions with land, water, carbon, and nutrient cycles, which can be measured as corresponding environmental footprints (EFs). However, the spatiotemporal trade-offs and synergies among multiple EFs in agricultural systems remain under-quantified, hindering effective mitigation strategies. Here, we propose an assessment framework of spatiotemporal trade-offs and synergies among multiple EFs of crop production, with a case study on blue water, green water, land, carbon, nitrogen, and phosphorus footprints for wheat, maize, rice, and soybean production across 31 Chinese provinces over 2000-2018. In total, 3630 pairwise EFs were analyzed. Results show that, although the EFs of unit mass crop production generally declined across provinces, national total EFs increased, with land, carbon, and phosphorus footprints rising by 16%, 17%, and 23%, respectively, during the study period. Synergistic interactions among EFs prevailed, comprising 50% positive and 32% negative synergies. The spatial distribution of trade-offs and synergies varies by crop and region. Land use intensity is the main factor limiting the positive EF synergies.</p>","PeriodicalId":175,"journal":{"name":"Global Change Biology","volume":"32 2","pages":"e70739"},"PeriodicalIF":12.0,"publicationDate":"2026-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146130535","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Patterns and Drivers of Pest and Disease Occurrence in UK Treescapes. 英国树木病虫害发生的模式和驱动因素。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-01 DOI: 10.1111/gcb.70706
Peter S Stewart, Louise J Barwell, Katharine Turvey, Jane Barbrook, Sarah Green, Ana Pérez-Sierra, Bethan V Purse, Daniel Chapman

Tree pests and diseases are a key threat to woodland biodiversity and commercial forestry worldwide. In the UK, the ongoing spread of pests and diseases is severely affecting a range of nationally important tree species, resulting in substantial ecological and economic impacts. As the risk posed by pests and diseases varies across the UK's treescapes, understanding the patterns of risk and the factors underlying these patterns is crucial for designing and implementing effective mitigation strategies. To address this challenge, we modelled the distribution of pests and diseases across mainland Great Britain, focusing on the total pest and disease burdens for nine host tree species of particular ecological, economic and cultural importance. Using integrated species distribution models, we combined two datasets-totalling 18,871 pest and disease records across 22 years-to model the spatial patterns of risk. To examine the factors underlying these distributions, we used graph-based causal inference approaches to inform our model design and to explore the robustness of our conclusions to variations in our modelling assumptions. We found that pest and disease burdens for broadleaved host trees exhibited hotspots in England, while burdens for conifer hosts tended to be high in Scotland. We identified urban area, human population density and local recreation as important drivers for several species, mainly native broadleaves. By contrast, woodland connectivity, afforestation and the level of conifer coverage were the most important drivers of pest and disease burdens for conifer hosts. Deforestation was also an important driver, with effects on pest and disease burdens for both conifers and broadleaves. Our findings have implications for the management of the UK's treescapes in the face of continuing threats from tree pests and diseases, including supporting targeted surveillance and the prioritisation of tree species for future planting.

{"title":"Patterns and Drivers of Pest and Disease Occurrence in UK Treescapes.","authors":"Peter S Stewart, Louise J Barwell, Katharine Turvey, Jane Barbrook, Sarah Green, Ana Pérez-Sierra, Bethan V Purse, Daniel Chapman","doi":"10.1111/gcb.70706","DOIUrl":"10.1111/gcb.70706","url":null,"abstract":"<p><p>Tree pests and diseases are a key threat to woodland biodiversity and commercial forestry worldwide. In the UK, the ongoing spread of pests and diseases is severely affecting a range of nationally important tree species, resulting in substantial ecological and economic impacts. As the risk posed by pests and diseases varies across the UK's treescapes, understanding the patterns of risk and the factors underlying these patterns is crucial for designing and implementing effective mitigation strategies. To address this challenge, we modelled the distribution of pests and diseases across mainland Great Britain, focusing on the total pest and disease burdens for nine host tree species of particular ecological, economic and cultural importance. Using integrated species distribution models, we combined two datasets-totalling 18,871 pest and disease records across 22 years-to model the spatial patterns of risk. To examine the factors underlying these distributions, we used graph-based causal inference approaches to inform our model design and to explore the robustness of our conclusions to variations in our modelling assumptions. We found that pest and disease burdens for broadleaved host trees exhibited hotspots in England, while burdens for conifer hosts tended to be high in Scotland. We identified urban area, human population density and local recreation as important drivers for several species, mainly native broadleaves. By contrast, woodland connectivity, afforestation and the level of conifer coverage were the most important drivers of pest and disease burdens for conifer hosts. Deforestation was also an important driver, with effects on pest and disease burdens for both conifers and broadleaves. Our findings have implications for the management of the UK's treescapes in the face of continuing threats from tree pests and diseases, including supporting targeted surveillance and the prioritisation of tree species for future planting.</p>","PeriodicalId":175,"journal":{"name":"Global Change Biology","volume":"32 2","pages":"e70706"},"PeriodicalIF":12.0,"publicationDate":"2026-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC12881709/pdf/","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146130580","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Tree Regeneration After Unprecedented Forest Disturbances in Central Europe Is Robust but Maladapted to Future Climate Change. 中欧史无前例的森林扰动后的树木再生强劲,但不适应未来的气候变化。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-01 DOI: 10.1111/gcb.70734
Mária Potterf, Christian Schattenberg, Kirsten Krüger, Kilian Hochholzer, Werner Rammer, Marc Grünig, Kristin H Braziunas, Christina Dollinger, Aikio Erhardt, Jean-Claude Gégout, Lisa Geres, Sina Greiner, Tomáš Hlásny, Anne Huber, Jonas Kerber, Judit Lecina-Diaz, Lisa Mandl, Roman Modlinger, Johannes S Mohr, Jörg Müller, Miguel Muñoz Mazón, Paulina E Pinto, Tobias Richter, Sebastian Seibold, Cornelius Senf, Josep M Serra-Diaz, Ana Stritih, Dominik Thom, Alba Viana-Soto, Jiayun Zou, Rupert Seidl

Central Europe has been a hotspot of forest disturbance during 2018-2020, with large pulses of tree mortality from drought and bark beetles. Post-disturbance recovery is crucial for forest resilience and the continued provision of ecosystem services. We surveyed 849 plots in disturbance hotspots across 10 Central European countries to assess the state of early (3-5 years) post-disturbance tree regeneration. Our specific objectives were to quantify post-disturbance tree recovery, identify key drivers, and assess future trajectories using model-based analyses. We found robust tree recovery throughout Central Europe, with median stem densities of 4750 n ha-1. Only 7% of plots had no regeneration. Regeneration density increased with precipitation, particularly at warm sites, and decreased with disturbance severity and size. The most frequently regenerating tree species was Picea abies (present on 48% of plots), a species that is poorly adapted to future heat and drought. Overall, we found that 75% of the currently established trees are projected to be outside of their climatic niche by the end of the century under moderate climate change (RCP4.5). We conclude that while Central European forests recover well from recent disturbances, they lack sufficient post-disturbance reorganization to enable sufficient adaptation to future climate.

{"title":"Tree Regeneration After Unprecedented Forest Disturbances in Central Europe Is Robust but Maladapted to Future Climate Change.","authors":"Mária Potterf, Christian Schattenberg, Kirsten Krüger, Kilian Hochholzer, Werner Rammer, Marc Grünig, Kristin H Braziunas, Christina Dollinger, Aikio Erhardt, Jean-Claude Gégout, Lisa Geres, Sina Greiner, Tomáš Hlásny, Anne Huber, Jonas Kerber, Judit Lecina-Diaz, Lisa Mandl, Roman Modlinger, Johannes S Mohr, Jörg Müller, Miguel Muñoz Mazón, Paulina E Pinto, Tobias Richter, Sebastian Seibold, Cornelius Senf, Josep M Serra-Diaz, Ana Stritih, Dominik Thom, Alba Viana-Soto, Jiayun Zou, Rupert Seidl","doi":"10.1111/gcb.70734","DOIUrl":"10.1111/gcb.70734","url":null,"abstract":"<p><p>Central Europe has been a hotspot of forest disturbance during 2018-2020, with large pulses of tree mortality from drought and bark beetles. Post-disturbance recovery is crucial for forest resilience and the continued provision of ecosystem services. We surveyed 849 plots in disturbance hotspots across 10 Central European countries to assess the state of early (3-5 years) post-disturbance tree regeneration. Our specific objectives were to quantify post-disturbance tree recovery, identify key drivers, and assess future trajectories using model-based analyses. We found robust tree recovery throughout Central Europe, with median stem densities of 4750 n ha<sup>-1</sup>. Only 7% of plots had no regeneration. Regeneration density increased with precipitation, particularly at warm sites, and decreased with disturbance severity and size. The most frequently regenerating tree species was Picea abies (present on 48% of plots), a species that is poorly adapted to future heat and drought. Overall, we found that 75% of the currently established trees are projected to be outside of their climatic niche by the end of the century under moderate climate change (RCP4.5). We conclude that while Central European forests recover well from recent disturbances, they lack sufficient post-disturbance reorganization to enable sufficient adaptation to future climate.</p>","PeriodicalId":175,"journal":{"name":"Global Change Biology","volume":"32 2","pages":"e70734"},"PeriodicalIF":12.0,"publicationDate":"2026-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC12881712/pdf/","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146130597","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Soil Food Webs Regulate Carbon Persistence Across Succession 土壤食物网调节演替过程中的碳持久性。
IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Pub Date : 2026-02-01 DOI: 10.1111/gcb.70726
Wenjia Wu, Zhanfeng Liu
<p>Understanding why soil organic carbon (SOC) persists—or is lost—under global change ultimately depends on which biological processes constrain pathways of carbon stabilization. In this issue of <i>Global Change Biology</i>, Du et al. (<span>2025</span>) show that soil food webs, long treated as secondary to decomposition, play an active and context-dependent role in regulating microbial carbon cycling along successional gradients. Predicting SOC persistence has long been central to ecosystem–climate feedback research. Over the past decade, microbial residues have emerged as major precursors of long-lived SOC, particularly mineral-associated organic matter, as formalized in the Microbial Efficiency–Matrix Stabilization (MEMS) framework (Cotrufo et al. <span>2013</span>). Subsequent work has reinforced the importance of microbial anabolism and physicochemical protection in shaping SOC persistence (Liang et al. <span>2017</span>). However, most SOC theory remains largely microbe-centered. Soil fauna are typically subsumed within microbial biomass dynamics rather than treated as regulators in their own right. At the global scale, soil fauna—particularly nematodes—mediate substantial carbon fluxes through grazing and trophic interactions. This influence underscores their potential to shape soil carbon cycling in ways not captured by microbial-centric frameworks (van den Hoogen et al. <span>2019</span>; Neher <span>2010</span>).</p><p>It is against this background that Du et al. (<span>2025</span>) integrated replicated field sampling across two long-term successional chronosequences on the eastern Qinghai–Tibet Plateau. These included a glacier-retreat primary succession and a post-disturbance secondary succession, both examined via complementary molecular, biochemical and food-web approaches. Soils (0–10 cm) from six stages in each sequence (<i>n</i> = 60 composite samples) were analysed for SOC and microbial necromass using amino-sugar biomarkers. Nematode trophic structure was quantified using 18S rDNA metabarcoding, while microbial functional potential was assessed by shotgun metagenomics targeting growth pathways, carbon-degrading CAZymes and carbon-fixation genes. Finally, these data were integrated using partial least-squares path modelling (PLS-PM), redundancy analysis and mixed-effects models. This analytical framework explicitly partitioned trophic versus edaphic controls on microbial carbon processing. Rather than emphasizing variation in decomposition rates, their analysis shifts attention from carbon loss to carbon retention. In doing so, it brings food-web structure into closer alignment with microbial metabolic allocation and necromass formation.</p><p>A central outcome of Du et al. (<span>2025</span>) is that trophic regulation of microbial carbon metabolism depends strongly on successional stage and associated nutrient constraints. In primary successional soils, microbial growth is constrained. These soils are typically characteriz
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Global Change Biology
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