IF: 4.5
CiteScore: 6.3
Editors-in-Chief
Yuanhe Yang
Bernhard Schmid
CN 10-1172/Q
ISSN 1752-9921(print)
ISSN 1752-993X(online)
  • Volume 19,Issue 4
    01 August 2026
      Reviews
      He Lyu, Xue-Qian Zhang, Jian Su, Ming-Kai Jiang
      2026, 19 (4): rtag033.
      Abstract ( 93 )   PDF(pc) (2089KB) ( 30 )   Save
      Anthropogenic global change profoundly affects terrestrial ecosystem structure and function, creating an urgent and persistent need to accurately predict future ecosystem states. Field-based manipulative experiments provide critical mechanistic insights into these impacts but are inherently limited in spatio-temporal scope. Conversely, process-based models can extrapolate to broader scales but often contain simplified or unrealistic mechanisms that lead to uncertain projections. Data-model integration has emerged as an essential approach to bridging this gap, testing model assumptions against empirical evidence and guiding experimental design via model-based hypotheses. This review synthesized progress in integrating manipulative experiments with process-based models across three key global change drivers: elevated CO2, climate change (warming and altered rainfall) and nutrient manipulation. We demonstrated how this integration reduced key uncertainties in processes such as photosynthesis, carbon-nutrient coupling and soil biogeochemistry, whilst exposing persistent gaps in plant hydraulics, microbial dynamics and multifactorial stresses. These advances were most pronounced in representing CO2 fertilization effects, including improved stomatal optimization theory, dynamic carbon allocation schemes and coupled carbon-nitrogen-phosphorus cycling. By contrast, its application to warming, rainfall change and multi-nutrient interactions remained underdeveloped. To catalyze future progress, we propose specific strategies to foster a more synergistic cycle of knowledge co-production. These include prioritizing the quantification of mechanism-specific data to develop dynamic model formulations, systematically using multi-site experimental networks to benchmark and refine model processes across scales, and strategically employing models to design targeted experiments. Ultimately, these strategies are indispensable for developing more realistic models and achieving predictive understanding of ecosystem responses to global change.
      Hao Liu, Lijuan Cui, Wei Li, Guangxuan Han, Jihua Wu, Bo Li, Ming Nie
      2026, 19 (4): rtag125.
      Abstract ( 35 )   PDF(pc) (1455KB) ( 17 )   Save
      Plant functional traits offer a mechanistic framework for understanding how plant communities respond to environmental change and shape ecosystem functioning. However, despite rapid advances over the past decades, the role of functional traits in driving wetland ecosystem functioning remains less well understood than in terrestrial systems, thereby limiting effective wetland conservation and restoration. In this review, we synthesize existing evidence on how plant functional traits and functional diversity influence key wetland ecosystem functioning, such as productivity, carbon cycling and nutrient cycling. We find that functional traits are key regulators of ecosystem functioning; therefore, targeted restoration should prioritize species with specific traits. We also call for coordinated actions across local and landscape scales to manage potential trade-offs among restoration objectives and enhance ecosystem multifunctionality. Clarifying the roles of functional diversity and wetland-specific flooding-adaptive traits in driving ecosystem functioning is identified as an important focus for future work. Moreover, a deeper understanding of how functional traits and diversity regulate wetland ecosystem functioning requires more manipulative experiments. This review highlights the role of plant traits in mechanistically linking vegetation dynamics to ecosystem functioning in wetlands.
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    Moderate grazing optimizes the allocation and microbial fate of recently assimilated carbon in an alpine grassland
    Mingxue Xiang, Junxi Wu, Lha Duo, Ben Niu, Ying Pan, Xianzhou Zhang, Zhaoqi Wang, Xinquan Zhao, Yakov Kuzyakov
    doi: 10.1093/jpe/rtag165
    Abstract ( 2 )    PDF    Save
    Alpine grasslands are crucial carbon (C) reservoirs, facing strong disruptions from intensified grazing. However, how grazing intensity regulates the allocation of recently assimilated C belowground and its utilization by soil microorganisms remains uncertain. Using in-situ 13CO2 pulse labeling in an alpine steppe, we compared the effects of non-grazing (NG), moderate grazing (MG), and heavy grazing (HG) on the allocation and cycling of recently assimilated C in shoots, roots, soil, and soil microorganisms. The initially assimilated 13C in shoots were highest under MG (245 mg C m-2). Root δ13C peaks were also highest under MG (28.5 mg C m-2), yet their mean residence time (MRT) was shortest (3.1 days), indicating rapid uptake and downward transport of newly fixed C through roots under MG. In contrast, HG delayed shoot δ13C peaks (to day 14) and produced the only pronounced soil δ13C peak (4‰), followed by a rapid decline, suggesting accelerated but short-lived belowground C allocation after severe defoliation. Despite phospholipid fatty acid (PLFA) profiles remaining stable, the share of 13C-PLFA held by Gram- positive bacteria increased from 30% to 40% under HG, indicating they became the dominant consumers of rhizodeposits. Besides, increasing grazing intensity exponentially shortened MRT across plant, soil, and microbial C pools. These results demonstrate that MG optimizes C allocation belowground and the microbial fate of plant-derived C, but HG accelerates plant-soil C fluxes and alters microbial consumer of rhizodeposits. Our study emphasizes the need to track where C flows and how long it resides in grazing grasslands.
    Widespread leaf phenology change detected by the leaf-age-dependent leaf area index (Lad-LAI) in pantropical evergreen broadleaf forests
    Hao-Ran Xu, Xue-Qin Yang, Mei Wang, Xin-Yue Fu, Jie Tian, Xiu-Zhi Chen
    doi: 10.1093/jpe/rtag164
    Abstract ( 4 )    PDF    Save
    Leaf phenology in tropical evergreen broadleaf forests (EBFs) often exhibits weak seasonality, making it challenging to detect the start of season (SOS) and end of season (EOS) from satellite-based vegetation indices particularly challenging. Leaf age structure describes the seasonal variability in canopy leaves of different age cohorts (young, mature, old) and for characterizing leaf phenology in tropical EBFs. Here, we built a methodological framework to produce a 0.25° leaf phenology dataset for tropical EBFs across 30°S–30°N using a leaf-age-dependent leaf area index product (Lad-LAI) for 2001–2023. SOS and EOS from the new dataset showed strong agreement with PhenoCam-derived metrics and good correlations with EVI-, NIRv-, and kNDVI-derived metrics. Across continents, the Amazon exhibited relatively later SOS dates, mainly during DOY 210–330, and earlier EOS dates, mainly during DOY 60–210. Conversely, the Congo and tropical Asia were characterized by relatively smaller SOS and larger EOS. Notably, SOS increases while EOS decreases progressively from northern to southern latitudes, showing contrasting latitudinal patterns. From 2001 to 2023, tropical EBFs experienced a widespread advance in SOS, which was most pronounced in the Congo region, with an average rate of -1.39 days yr-1. In contrast, EBFs mostly experienced a delay in EOS, which was strongest in tropical Asia, with a mean delay rate of 2.12 days yr-1. Consequently, the growing season (EOS minus SOS) increased significantly across all three continents. Overall, our leaf-age-dependent phenology dataset provides fundamental data for leaf phenology monitoring, carbon-cycle modeling, and climate-change impact predictions in tropical EBFs.
    Decoupling of whole-plant economic strategy from population performance in the invasive Solidago canadensis along geographic gradients in China
    Li-Jia Dong, Huan Mei, Hong-Wei Yu, Mark van Kleunen, Wei-Ming He
    doi: 10.1093/jpe/rtag166
    Abstract ( 8 )    PDF    Save
    The whole-plant economic spectrum captures resource-use strategies along three key gradients: a conservation–acquisition gradient reflecting trade-offs in resource investment, a belowground collaboration gradient representing the continuum from 'do-it-yourself' to 'outsourcing' via mycorrhizal fungi, and a plant size gradient capturing variation in stature. However, how these axes apply to intraspecific trait variation and mediate invasion success along geographic gradients remains unclear. We measured traits, population performance, and environmental variables in the invasive forb Solidago canadensis across latitudinal and longitudinal gradients in eastern subtropical China. Populations shifted along the conservation–acquisition axis from conservative to acquisitive strategies with increasing longitude; this shift was marginally significant along latitude. Contrary to the expectation that plant size and collaboration gradients are independent, these two dimensions were coupled and showed no clear geographic trends. Environmental factors significantly influenced intraspecific trait variation, economic strategy positioning, and invasion performance. Native diversity explained the largest proportion of variation in economic strategy and performance. Crucially, we found no significant relationship between the major axes of the whole-plant economic spectrum and population performance. This suggests that diverse trait combinations may yield similar fitness outcomes, indicating fitness homeostasis across heterogeneous environments. We conclude that while geographic gradients shape whole-plant economic strategies in S. canadensis, its invasion success is likely driven by adaptive trait combinations that maintain high fitness, rather than a single optimal strategy directly mediating performance.
    Mid-decay Quercus liaotungensis logs drive soil carbon and nitrogen heterogeneity in association with microbial reorganization
    Junning Li, Yulian Wei, Wen Zhao, Reyila Mumin, Shun Liu, Yifei Sun, Baokai Cui
    doi: 10.1093/jpe/rtag162
    Abstract ( 13 )    PDF    Save
    Fallen logs are key components of forest biogeochemical processes, regulating carbon and nitrogen dynamics in forest soils. By altering resource availability and environmental conditions, they also influence soil microbial community structure, yet these responses remain poorly understood. To address this gap, we investigated soil microbial communities adjacent to Quercus liaotungensis fallen logs at the mid-decay stage, which is characterized by distinctive decomposition conditions. Soil samples were collected beneath fallen logs (FL) and from paired control sites (CT). Based on whether soil organic carbon (SOC) and total nitrogen (TN) increased (Pos) or decreased (Neg) in log-affected soils relative to controls, the samples were categorized into four microsites to compare microbial communities. Amplicon sequencing of 16S rRNA and ITS regions revealed differences in microbial communities across microsites. Co- occurrence network analysis revealed stronger bacterial–fungal coupling in soils affected by fallen logs, particularly in the log-affected Neg group, which showed increased bacterial– bacterial connections and the most complex network structure. Community assembly analysis showed that bacterial communities in FL-Pos soils were dominated by homogeneous selection and homogenizing dispersal, which indicates stronger environmental filtering, whereas FL-Neg soils showed greater dispersal limitation and drift. Predicted functional profiles indicated enrichment of saprotrophic taxa in soils beneath fallen logs and alterations of bacteria in nitrogen-cycling pathways, with FL-Neg microsite showing lower predicted abundances of nitrification- and denitrification-related functions and higher predicted abundance of nitrogen- fixing taxa. Overall, this study highlights the overlooked ecological importance of mid-decay fallen logs and shows that microbial community reorganization is associated with decomposition-driven forest-floor heterogeneity.
    Multiple environmental drivers yield predictable growth responses in a marine diatom
    Peixuan Liu, Bin Huang, Junyan Li, Enqi Zhang, Shuming Lin, Zihong Li, Jing Tian, Zijie Wei, Zihan Liu, Mengyao Liang, Runqian Jiang, Jianrong Xia, Peng Jin
    doi: 10.1093/jpe/rtag157
    Abstract ( 8 )    PDF    Save
    Environmental change is characterized by the simultaneous action of multiple drivers, yet predicting biological responses under high environmental complexity remains challenging. Most experiments examine only a few stressors, leaving uncertainty about how population performance scales as the number of drivers increases. Here, we experimentally tested how increasing environmental dimensionality affects population growth in the marine diatom Thalassiosira weissflogii. Populations were exposed to a combinatorial set of environmental conditions created by manipulating seven drivers, including warming, elevated CO2, light intensity, nutrient limitation, and metal stress, resulting in 127 unique environmental conditions representing all possible combinations of one to seven drivers. These 127 unique environmental conditions were independently cultured in 96-well microplates within plant growth chambers, where temperature, light intensity, and nutrient conditions were rigorously controlled. Population growth declined systematically as driver number increased, independent of specific driver identity, while extinction risk rose sharply with environmental complexity. Across the full driver space, growth responses were best explained by the presence of a single dominant stressor rather than additive or multiplicative accumulation of effects. However, consistent deviations from dominant- driver predictions revealed that additional drivers further intensified physiological stress. Global change drivers such as temperature and CO2 modulated these patterns, sometimes buffering and sometimes amplifying stress, resulting in context-dependent predictability. Together, these findings demonstrate that environmental dimensionality itself constrains population persistence, while dominant stressors set physiological limits, highlighting both the utility and the limits of scalable frameworks for predicting phytoplankton responses to complex environmental change.
  • 2026, Vol. 19 No.3 No.2 No.1
    2025, Vol. 18 No.6 No.5 No.4 No.3 No.2 No.1
    2024, Vol. 17 No.6 No.5 No.4 No.3 No.2 No.1
    2023, Vol. 16 No.6 No.5 No.4 No.3 No.2 No.1
    2022, Vol. 15 No.6 No.5 No.4 No.3 No.2 No.1
    2021, Vol. 14 No.6 No.5 No.4 No.3 No.2 No.1
    2020, Vol. 13 No.6 No.5 No.4 No.3 No.2 No.1
    2019, Vol. 12 No.6 No.5 No.4 No.3 No.2 No.1
    2018, Vol. 11 No.6 No.5 No.4 No.3 No.2 No.1
    2017, Vol. 10 No.6 No.5 No.4 No.3 No.2 No.1
    2016, Vol. 9 No.6 No.5 No.4 No.3 No.2 No.1
    2015, Vol. 8 No.6 No.5 No.4 No.3 No.2 No.1
    2014, Vol. 7 No.6 No.5 No.4 No.3 No.2 No.1
    2013, Vol. 6 No.6 No.5 No.4 No.3 No.2 No.1
    2012, Vol. 5 No.4 No.3 No.2 No.1
    2011, Vol. 4 No.4 No.3 No.1-2
    2010, Vol. 3 No.4 No.3 No.2 No.1
    2009, Vol. 2 No.4 No.3 No.2 No.1
    2008, Vol. 1 No.4 No.3 No.2 No.1
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Special Issue

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