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ORIGINAL RESEARCH article

Front. Plant Sci., 06 November 2025

Sec. Functional Plant Ecology

Volume 16 - 2025 | https://doi.org/10.3389/fpls.2025.1707246

Variation in leaf functional traits of Pinus armandii and their drivers along an altitudinal gradient in Karst mountains

Bin He,Bin He1,2Wangjun Li,Wangjun Li1,2Xiaolong Bai,Xiaolong Bai1,2Shun Zou,*Shun Zou1,2*Qing Li,*Qing Li1,2*
  • 1College of Ecological Engineering, Guizhou University of Engineering Science, Bijie, Guizhou, China
  • 2Guizhou Province Key Laboratory of Ecological Protection and Restoration of Typical Plateau Wetlands, Bijie, Guizhou, China

Introduction: Leaf functional traits are pivotal indicators of plant ecological strategies, reflecting adaptations to environmental conditions. However, the patterns of intraspecific trait variation along environmental gradients and their underlying drivers remain inadequately explored, particularly in fragile ecosystems like karst landscapes.

Methods: We investigated 12 leaf functional traits (encompassing morphological and chemical characteristics) of Pinus armandii along an elevational transect (2128 to 2509 m) in the Karst mountainous region of southwestern China. Using correlation and redundancy analyses, we examined altitudinal trends in trait variation and their relationships with key soil factors.

Results: Our results revealed substantial intraspecific variability in all leaf traits, with coefficients of variation ranging from 3.24% to 28.15%. Specific leaf area, leaf length, thickness, area, carbon content, potassium content, and the ratios of C:N, C:P, and N:P decreased significantly with increasing elevation. Conversely, leaf dry matter content, nitrogen content, and phosphorus content increased significantly. We found notable coordination and trade-offs among traits, forming an integrated network centered on the C:N ratio. Soil factors—specifically soil organic carbon, pH, and available potassium—were identified as the primary drivers of this trait variation.

Discussion: P. armandii in karst mountainous regions adapts to elevational changes through coordinated adjustments in leaf functional traits, thereby optimizing resource acquisition and use strategies. These findings advance our understanding of plant adaptation mechanisms in such fragile environments.

1 Introduction

Global change is rapidly and extensively altering species distributions, biodiversity, and ecosystem functioning (Batllori et al., 2020; Chapin et al., 2000), with profound implications for human well-being (Wang et al., 2021). These changes reshape biodiversity through extinctions, range shifts, and population fluctuations, thereby profoundly altering ecosystem functions (Cardinale et al., 2012; De Laender et al., 2016). Predicting these changes is crucial for conservation and restoration, yet remains challenging due to species diversity and ecosystem complexity. Plant persistence under rapid climate change hinges on adaptive capacity through phenotypic plasticity or genetic change (Nicotra et al., 2015). Consequently, understanding how plant traits respond plastically or genetically along existing environmental gradients is essential for predicting in situ persistence under climate change (Chevin and Lande, 2010; Anderson and Gezon, 2015).

Plant functional traits-morphological, physiological, or phenological characteristics-directly reflect plant survival and resource-use strategies across environmental gradients, revealing evolutionary trade-offs and ecological strategies from physiology to ecosystem function (Wright, 2010; Kumari et al., 2021). As primary sensors of global change, plants dynamically adjust traits (e.g., leaf morphology, nutrient allocation) in response to climatic stressors, serving as indicators of ecosystem resilience (Wang et al., 2020; Zhang et al., 2020). Among plant functional traits, leaf functional traits (LFTs), the direct plant-atmosphere interface, are particularly sensitive diagnostic tools. Traits like specific leaf area (SLA), leaf nitrogen content (LNC), leaf dry matter content (LDMC), and photosynthetic capacity are highly sensitive to temperature, moisture, soil nutrients, and altitude (Klich, 2000; Wright et al., 2004; Ordoñez et al., 2009; Ni et al., 2022), elucidating resource acquisition strategies (e.g., leaf economics spectrum) and evolutionary responses to pressures like drought or nutrient limitation (Wright et al., 2004; Reich et al., 2003; Akram et al., 2023). While phylogeny influences LFTs, environmental filters dominate regional trait variation, especially in dynamic habitats (Akram et al., 2023; Liu et al., 2013), underscoring the need to resolve trait responses at the species and population level to scale ecological insights (Navas et al., 2010). Thus, studying PFTs, particularly LFTs, provides a powerful framework for deciphering plant-environment interactions and predicting ecosystem responses to global change (Webb et al., 2010; Díaz et al., 2016; Wang et al., 2023).

Plant functional traits variation underpins species coexistence, community assembly, and ecosystem processes. Intraspecific trait variation (ITV), driven by phenotypic plasticity and local adaptation, constitutes a significant component (up to 30-40%) of total trait variation (Albert et al., 2010; Kattge et al., 2011). ITV critically influences species’ niche breadth, adaptive capacity (Ackerly and Cornwell, 2007), community stability, and ecosystem functioning (Violle et al., 2012; Westerband et al., 2021). However, methodological constraints often lead researchers to rely on species mean traits, potentially obscuring individual-level responses (Westerband et al., 2021). ITV is heterogeneous along environmental gradients like elevation, arising from divergent life forms (Frey et al., 2016; Körner, 2007), ontogenetic plasticity (Siefert et al., 2015), variable precipitation-elevation relationships (Körner, 2007; Martin and Asner, 2009), and evolutionary divergences (Wellstein et al., 2017). Traits also exhibit differential plasticity: structural traits (e.g., SLA, LT) often show high ITV tracking environmental filters, while others (e.g., wood density) display constrained variation due to genetic limitations or counter-gradient responses (Siefert et al., 2015; Umaña et al., 2018). This context-dependency explains inconsistent ITV patterns across studies. A key unresolved question is the link between ITV and individual performance along gradients: whether ITV reflects local adaptation towards an optimum or serves as phenotypic buffering to maintain performance across conditions (Körner, 1991). Therefore, analyzing multi-trait ITV within species across gradients is vital for scaling eco-physiological processes, elucidating assembly mechanisms, and forecasting biodiversity responses.

Mountain ecosystems, characterized by steep environmental gradients, provide unparalleled natural laboratories for studying plant functional responses (Körner, 2007; Graae et al., 2012). Elevational gradients induce systematic shifts in temperature, radiation, moisture, and soil conditions, imposing strong selective pressures that drive intraspecific variation in LFTs linked to resource strategies (Violle et al., 2007; Sides et al., 2014). Typically, lower elevations favor resource-acquisitive traits (e.g., higher SLA), while higher elevations typically select for conservative strategies (e.g., reduced SLA, increased LDMC) (Callaway et al., 2002; Poorter et al., 2009; Pfennigwerth et al., 2017). However, trait responses exhibit significant complexity, showing species specificity, phylogenetic constraints, and functional group divergence (He et al., 2023). Empirical findings for core traits (e.g., SLA, LNC) are often inconsistent across studies, showing increases, decreases, or no trend with elevation (Melis et al., 2023; Xu et al., 2023; Zhao et al., 2016). This uncertainty reflects the context-dependency of trait-environment relationships, modulated by local heterogeneity (topography, soil), biotic interactions (Rasmann et al., 2014), stand factors, and soil properties (e.g., N/P availability, pH) (Liu et al., 2021b; Yang et al., 2023). Furthermore, the mechanisms driving individual LFT responses and trait-trait covariation remain poorly resolved (Onoda et al., 2017). Disentangling these interactions is essential for predicting plant responses to global change and impacts on ecosystem functions (De Deyn et al., 2008; Rixen et al., 2022).

Karst mountains present unique “rock-water-soil-biota” continua with slow soil formation, shallow lithic soils, and high heterogeneity (Wang and Li, 2007). Plants here face dual stressors: seasonal drought and nutrient limitation (Liu et al., 2021a), potentially driving divergent trait strategies compared to other ecosystems. Bedrock exposure may override temperature-driven patterns (He et al., 2020), while calcareous soils (high Ca, low P) exacerbate nutrient constraints (Zhang et al., 2021). Although studies have compared traits between life forms (e.g., evergreen vs. deciduous) or karst/non-karst regions (Jiang et al., 2016; Fu and Sun, 2022), and assessed soil influences (Pan et al., 2011), the relative contributions of plant characteristics versus environmental factors to trait variation in these heterogeneous systems remain unclear. Furthermore, existing studies often focus on single-trait variation, neglecting multi-trait coordination and stoichiometric interactions (Han et al., 2023). Pinus armandii, a pioneer species in ecological restoration across southwestern China’s karst regions, is vital for ecosystem stability. Despite research on its population dynamics (Yao et al., 2020), ecophysiology (Li et al., 2025), distribution (Liu et al., 2021a), and nutrient limitations (Dong et al., 2022), the elevational patterns of leaf functional trait covariation and their driving mechanisms in karst habitats remain poorly understood. Here, we investigate P. armandii along a 2128–2509 m elevational gradient in Guizhou’s karst mountains. By systematically measuring leaf morphological and chemical traits, coupled with soil-climate monitoring, we address: (1) How do LFTs of P. armandii vary along elevational gradients in karst habitats? (2) How are morphological traits coordinated with stoichiometric and chemical traits? (3) What are the relative roles of soil properties in driving trait covariation? Our findings will advance understanding of karst plant adaptation, guide restoration species selection, and refine models of leaf trait responses to climate change.

2 Materials and methods

2.1 Study area

The study was conducted in Bijie City(103°36′–106°43′ E, 26°21′–27°46′ N), located in Guizhou Province, China (Figure 1). The region lies within the core area of the contiguous karst zone of Yunnan-Guizhou-Guangxi, which belongs to the East Asian karst region-one of the three major global karst concentration areas. It is characterized by a subtropical humid monsoon climate with synchronous heat and moisture availability. Due to significant altitudinal variation, vertical climatic zonation is pronounced. The mean annual temperature ranges from 10 to 15°C, annual sunshine duration ranges from 1096 to 1769 hours, and the frost-free period lasts from 245 to 290 days. The dominant soil types include yellow soil and yellow-brown soil, with sporadic distributions of calcareous soil, purple soil, and paddy soil, exhibiting clear vertical zonation. All experimental sites in this study were situated on yellow-brown soil. The original vegetation was mid-subtropical evergreen broad-leaved forest. However, due to long-term human disturbance, primary forests are poorly preserved. The current vegetation is predominantly dominated by secondary and artificial forests. Common tree species include P. armandii, Pinus yunnanensis, Pinus massoniana, as well as species from the Fagaceae family (e.g., Castanopsis and Cyclobalanopsis) and the Lauraceae family (e.g., Cinnamomum and Machilus).

Figure 1
Map showing the elevation of Weining County in Bijie, Guizhou Province, China. The elevation ranges from 1,170 to 2,836 meters, with sampling sites marked by red triangles. Two inset maps locate Weining within Bijie and Guizhou.

Figure 1. Distribution of sampling point of P. armandii in Bijie City, Guizhou Province, China.

2.2 Sampling design

From September to October 2024, a transect was established along an elevational gradient within the main distribution area of P. armandii in Bijie City. This sampling period was strategically chosen to coincide with the late growing season, when leaf functional traits are relatively stable and plants undergo nutrient resorption for dormancy preparation. This timing was ideal for investigating altitudinal variations in leaf traits during a key phenological stage, thereby ensuring reliable comparisons across elevations. Five elevation levels were selected at 100 m intervals between 2100 and 2600 m (specifically: 2128 m, 2204 m, 2310 m, 2426 m, and 2509 m) (Figure 1). At each elevation, three 20 m×20 m quadrats were randomly established, resulting in a total of 15 quadrats. Within each quadrat, stand characteristics were recorded, including latitude, longitude, elevation, aspect, and slope.

In each quadrat, five healthy P. armandii individuals were selected as standard trees. From the middle outer part of the canopy, current-year branches were collected from the east, south, west, and north directions. From each branch, 50 bundles of healthy, undamaged needles were selected, wrapped in moist filter paper, and stored in a cooling box. Within each quadrat, three sampling points were randomly set up. At each sampling point, soil was collected from a depth of 0–20 cm using the five-point sampling method (centered on the point within a 1 m × 1 m area). After removing the surface litter, soil augers were used for sampling. The five soil subsamples from the same sampling point were mixed to form one composite sample. Thus, each quadrat yielded three independent composite samples, giving a total of 45 independent soil samples (15 quadrats × 3 samples per quadrat). All samples were sealed and stored for subsequent analysis.

2.3 Measurement of leaf functional traits and soil properties

LFTs were measured following the protocols described in the”Leaf traits”section of the Handbook for Standardized Measurement of Plant Functional Traits Worldwide (Pérez-Harguindeguy et al., 2013). A total of 12 LFTs, associated with plant growth and metabolic strategies, were assessed: Leaf Length (LL, cm), Leaf Thickness (LT, mm), Leaf Area (LA, cm2), Specific Leaf Area (SLA, cm2·g−1), Leaf Dry Matter Content (LDMC, mg·g−1), Leaf Carbon Content (LCC, g·kg−1), Leaf Nitrogen Content (LNC, g·kg−1), Leaf Phosphorus Content (LPC, g·kg−1), Leaf Potassium Content (LKC, g·kg−1), Leaf Carbon to Nitrogen Ratio (LC:N), Leaf Carbon to Phosphorus Ratio (LC:P), and Leaf Nitrogen to Phosphorus Ratio (LN:P).

Prior to measurement, needles were stored in darkness at 5°C for 12 hours, then surface-dried and weighed to determine leaf fresh weight (LFW) using an electronic balance with a precision of 0.001 g. Leaf images were acquired with a flatbed scanner, and LA was quantified using ImageJ software. LT was measured at three locations (base, middle, and apex) with a vernier caliper (precision: 0.02 mm), and the mean value was recorded. Subsequently, leaves were oven-dried at 105°C to deactivate enzymes, followed by drying at 80°C to constant weight to determine leaf dry weight (LDW). Dried leaf samples were ground and sieved for subsequent elemental analyses.

LNC and LPC was determined using a SEAL AA3 Continuous Flow Analyzer (Germany). LKC was measured with a Puxi A3 AFG-12 Flame Atomic Absorption Spectrophotometer (Wang et al., 2024). Similarly, soil N and P contents were analyzed with the continuous flow analyzer, and soil K was assessed via flame atomic absorption spectrometry. Soil pH was measured using the glass electrode method (Wang et al., 2024).

SLA and LDMC were calculated as follows:

SLA=LALDW
LDMC=LDWLFW

2.4 Data analysis

All statistical analyses were performed in R 3.5.1. Spatial autocorrelation in trait data was assessed using Moran’s I test in the spdep package. A spatial weight matrix was constructed based on the inverse distance between the geographic coordinates of the 15 plots. The Moran’s I test revealed no significant spatial autocorrelation in any of the measured leaf functional traits (all |Moran’s I|< 0.1, p>0.05). On this basis, linear regression was considered appropriate for subsequent analysis. Linear regression models were employed to evaluate the relationships between elevation and leaf functional traits. Differences in leaf traits across elevation gradients were compared using one-way analysis of variance (ANOVA) followed by Tukey’s honestly significant difference (HSD) test for post-hoc comparisons. Pearson correlation and functional trait network were used to analyze trait correlations. Forward selection with double-stopping criteria identified key environmental factors, and redundancy analysis (RDA) explored trait-environment relationships. Additionally, path analysis was performed to partition the direct and indirect effects of environmental factors on traits, thereby elucidating the underlying mechanisms. All analyses were carried out using the vegan, car, agricolae, and spdep packages in R.

2.4.1 Plant trait network construction

To investigate the co-variation relationships among plant traits, we constructed a plant trait network following these specific steps:

Data Preprocessing: All plant trait data were tested for normality using the Shapiro-Wilk test. The results indicated that most traits did not follow a normal distribution (p < 0.05). Therefore, we used the non-parametric Spearman’s rank correlation to calculate correlations between all trait pairs, as this method is insensitive to outliers and produces more robust results.

Correlation Matrix and Significance Testing: A matrix of Spearman’s correlation coefficients (rs) and their corresponding p-values was computed for all pairwise trait combinations.

Control of Spurious Correlations and Edge Filtering: To mitigate spurious correlations arising from multiple comparisons, we employed the False Discovery Rate (FDR) control method to correct the p-values (Benjamini, 2010). Specifically, the Benjamini-Hochberg procedure was used to calculate the FDR-adjusted q-value (which represents the minimum FDR at which a test may be called significant) for each correlation. Only correlations with q-value< 0.05 were considered statistically significant and retained as edges in the final network. This step is crucial for controlling the false positive rate and ensuring that network edges represent reliable ecological relationships.

Network Visualization and Analysis: The filtered matrix of significant correlations was imported into the igraph package for network visualization and analysis. In the resulting network, nodes represent plant traits, and edges represent Spearman correlations that remained significant after FDR correction. Edge thickness is proportional to the absolute value of the correlation coefficient, providing visual representation of association strength.

2.4.2 Path analysis and variable selection

Path analysis was conducted to disentangle the direct and indirect effects of environmental factors on plant functional traits. The variable selection procedure was implemented as follows:

Initial Full Model Construction: For each plant trait, a full path model was constructed incorporating all eight soil factors.

Stepwise Variable Selection:

To mitigate multicollinearity, we computed the variance inflation factor (VIF) for each soil factor. Predictors with VIF values exceeding 10 - indicating severe multicollinearity - were sequentially excluded to ensure model stability and interpretability (James et al., 2013).

After addressing multicollinearity, a backward stepwise selection procedure was applied based on the Akaike information criterion (AIC). Predictors with the highest p-values were iteratively removed until all remaining path coefficients were statistically significant (p < 0.05).

Final Model Validation: The final path model for each trait retained only those variables that were both statistically significant and ecologically interpretable, ensuring a parsimonious and meaningful representation of the underlying processes.

3 Results

3.1 LFTs variation characteristics

Variance analysis revealed significant differences (p<0.05) in most LFTs across the elevational gradient, with the exception of LN:P (Table 1). Specifically, LL, LT, SLA, and LDMC did not show significant differences among middle elevation gradients, but exhibited significant variation across other elevation ranges (p<0.05). In contrast, LA showed significant differences (p<0.05) across all five distinct elevation gradients. Significant differences (p<0.05) in LCC, LNC, LPC, LKC, as well as LC:N and LC:P were primarily observed between the highest elevation (2509 m) and the other gradients, indicating that these functional traits exhibit the greatest divergence between the highest elevation and other gradients.

Table 1
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Table 1. Leaf functional trait parameters and their coefficients of variation for P. armandii at different altitudinal gradients.

The coefficients of variation (CV) for the LFTs of P. armandii ranged from 3.24% to 28.15%. Among these traits, LCC displayed the lowest variability (CV = 3.24%), suggesting minimal influence of elevational change on carbon allocation and relatively stable carbon metabolism. In contrast, LPC exhibited the highest variability (CV = 28.15%), reflecting a high sensitivity of phosphorus metabolism to the environmental gradients associated with elevation.

3.2 Altitudinal divergence in LFTs

Linear regression analysis revealed significant altitudinal divergence patterns in LFTs (Figure 2). SLA, LL, LT, and LA exhibited significant decreasing trends with increasing elevation (p<0.01). Conversely, LDMC showed a significant increasing trend (p<0.01). These morphological traits demonstrated strong correlations with elevation, which were either positive (R>0.80) or negative (R<-0.80).

Figure 2
Twelve scatter plots show various leaf traits against elevation from 2100 to 2500 meters. Each plot includes a blue regression line with a shaded confidence interval. Correlation coefficients and p-values are displayed, indicating significant relationships between traits such as leaf area, leaf length, leaf thickness, and element concentrations, with elevation. Most plots show negative correlations, except for E and H, which demonstrate positive correlations. Plots are labeled from A to L.

Figure 2. Trends in leaf functional trait parameters of P. armandii along the elevation gradient. In the figure, the regression line fitted by the solid line indicates a significant linear relationship (p<0.05), while the regression line fitted by the dashed line indicates a non-significant linear relationship (p> 0.05). The gray shaded area represents the 95% confidence interval.

LCC, LKC, LC:N, LC:P, and LN:P decreased significantly with increasing elevation (p<0.05). In contrast, LNC and LPC increased significantly (p<0.05). These nutrient-related traits showed substantial correlations with elevation, which were either positive (R>0.50) or negative (R<-0.50). Notably, the strength of correlation between elevation and morphological traits (LL, LT, LA, SLA, LDMC) was substantially greater than those observed for nutrient traits (LCC, LKC, LNC, LPC, LC:N, LC:P, LN:P).

3.3 Analysis of correlations among LFTs

Correlation analysis revealed widespread but variable significant relationships among LFTs of P. armandii (Figure 3). Notably, LDMC exhibited significant correlations with all traits except LN:P. LT, LA, SLA, and LKC were significantly associated with most traits, excluding LCC and LN:P. LL and LPC also showed strong connectivity, lacking significant correlations only with LCC, LPC, LN:P and with LL, LCC, LNC, respectively. LNC correlated significantly with the majority of traits, showing non-significance only with LCC, LPC, LC:P, and LN:P. Conversely, LCC displayed the weakest connectivity, correlating significantly only with LDMC, while LN:P exhibited limited connectivity, correlating significantly only with LPC and LC:P.

Figure 3
A heatmap graph visually represents a correlation matrix with values ranging from minus one to one, shown in a diverging color scheme from blue (negative correlation) to red (positive correlation). Ellipses within the squares indicate the strength and direction of correlations. Bold asterisks signify statistical significance. Correlation coefficients are displayed numerically in each cell. Labels on the axes refer to various variables compared in the analysis.

Figure 3. The correlation between leaf functional traits of P. armandii. Different numbers and color blocks represent Pearson correlation coefficients between different functional traits, with asterisks indicating the level of correlation significance (*p<0.05; **p<0.01).

The functional trait network constructed based on these correlations (Figure 4) further demonstrated that the LFTs of P. armandii form a tightly interconnected and highly coordinated complex network. Topological analysis of the network (Table 2) identified LC:N as the most central hub trait, exhibiting the highest degree centrality (Degree=7), closeness centrality (Closeness=0.818), and betweenness centrality (Betweenness=0.222). This centrality highlighted the pivotal regulatory role of LC:N in the environmental adaptation strategies of P. armandii.

Figure 4
Network diagram with nodes labeled LT, C:P, P, C:N, LDMC, SLA, N:P, N, LA, and LL. Nodes are connected by variously weighted lines, indicating relationships or interactions among them. Each node is a different color.

Figure 4. The correlation network among the functional traits of P. armandii. Each different node represents a distinct trait of the plant, and the edges represent the relationships between the traits.

Table 2
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Table 2. Node parameters of correlation network among leaf functional traits of P. armandii.

3.4 Response of LFTs to environmental factors

Given the limited spatial scale of the study area and the minimal variation in climatic factors within the region, we hypothesized that soil properties would exert a greater influence on the variation in LFTs of P. armandii. Redundancy analysis (RDA) identified eight key soil variables: SOC, TP, TCa, TK, AN, pH, AK, and AP (Figure 5). Collectively, these factors explained 84.65% of the total variation observed in the LFTs. Among them, SOC, pH, and AK exhibited statistically significant correlations with the leaf functional traits (p<0.05), indicating their predominant role in driving the variation of leaf functional characteristics in P. armandii.

Figure 5
A scatter plot with two axes, RDA1 (75.54%) and RDA2 (9.11%), showing data points categorized by elevation levels from 2128 meters to 2509 meters, indicated by different colors. Vectors represent variables: SOC, pH, TC, AP, AN, TK, TP, and AK.

Figure 5. Redundancy analysis between the leaf functional traits of P. armandii. and soil factors.

Path analysis of LFTs and environmental factors (Table 3) revealed significant divergence in the dominant environmental drivers among different leaf traits of P. armandii. Specifically, LL was primarily regulated by SOC, AP, and AK, with SOC and AP exerting positive effects, while AK exerted a negative effect. LT was mainly influenced by AP and AK; AK exerted a direct negative effect, while AP contributed a positive effect primarily through a significant indirect pathway. LA was predominantly regulated by SOC, pH, and AK, with SOC and pH exerting positive effects and AK exerting a negative effect. SLA was primarily governed by SOC, TCa, and TK, where SOC and TCa exerted positive effects and TK a negative effect. LDMC was mainly regulated by SOC, pH, AK, and AP; AK exerted a positive direct effect, SOC and pH exerted negative direct effects, and AP exerted a negative effect via a significant indirect pathway. LNC was predominantly influenced by TP, TCa, and pH; TP exerted a positive direct effect, whereas TCa and pH exerted negative direct effects. LKC was primarily driven by pH, AK, and AP, with pH exerting a positive direct effect and both AK and AP exerting negative direct effects. LN:P was mainly controlled by TCa, pH, AK, and AP; pH exerted a positive direct effect, while TCa, AK, and AP exerted negative direct effects. LC:P was predominantly influenced by pH and AK, with pH exerting a positive direct effect and AK exerting a negative direct effect. Additionally, pH exerted a direct positive effect on LC:N.

Table 3
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Table 3. Path coefficients of main influencing factors of leaf functional traits of P. armandii.

4 Discussion

As a primary organ for material accumulation and energy exchange, the leaf plays a fundamental role in ecosystem primary productivity. Leaf traits reflect key aspects of plant adaptation strategies developed through long-term evolution (Wright et al., 2005). Investigating how these traits vary along environmental gradients provides critical insights into the mechanisms underlying plant environmental adaptation.

4.1 Altitudinal effects on LFTs of P. armandii

Variation in altitude drives gradient changes in environmental factors such as temperature, precipitation, light availability, and soil properties, leading to pronounced redistribution of heat and moisture within relatively confined spatial scales. In response to these complex environmental shifts, plants exhibit adaptive adjustments in functional traits. This study revealed significant altitudinal variation (p<0.05) in LFTs of P. armandii, with coefficients of variation ranging from 3.24% to 28.15%, indicating considerable trait plasticity. These results suggest that P. armandii employs coordinated changes in multiple leaf functional traits to adapt to varying altitudinal habitats. While interspecific variation has traditionally been emphasized in plant functional trait studies, growing evidence indicates that intraspecific variation is also substantial, accounting for 28%-52% of total trait variation (Albert et al., 2010; Auger and Shipley, 2013; Jiang et al., 2016). In this study, the average intraspecific variation in LFTs of P. armandii was 16.80%, which is relatively low compared to other vegetation types. We propose several non-exclusive explanations for this constrained variation. First, it may indeed reflect limited morphological plasticity in response to the strong filtering effect of the harsh, high-elevation environmental conditions (Auger and Shipley, 2013), which selects for a narrow range of trait values. Second, the studied elevational gradient, while capturing the species’ primary distribution, might not encompass the full environmental spectrum necessary to elicit broader trait variation. Finally, as a long-lived conifer, P. armandii may possess an inherently conservative growth strategy, leading to lower intraspecific variability compared to more opportunistic herbaceous species commonly reported in other studies.

Plants adapt to environmental heterogeneity through functional traits such as LA, SLA, LDMC, LL, and LT. These traits collectively reflect strategies of resource acquisition and conservation (Yao et al., 2023). SLA, in particular, is a key structural trait related to light interception efficiency and environmental acclimation (Xu et al., 2023). In this study, SLA decreased significantly with increasing altitude, consistent with observations across multiple mountain ecosystems (Pensa et al., 2009; Rixen et al., 2022). This pattern can be explained by divergent resource-use strategies: at lower altitudes, where conditions are warmer and resources more abundant, plants prioritize light capture and photosynthetic rates by producing larger, thinner leaves with high SLA. At higher altitudes, plants invest in denser mesophyll tissues, reduce LA, and decrease SLA to limit respiration and transpiration, thereby enhancing photoprotection and adaptation to resource-limited environments (Gao and Liu, 2018; Liu et al., 2023a). This shift toward a conservative strategy aligns with observations that plants in arid or cold environments often prioritize structural durability over rapid growth (Melis et al., 2023; Poggiato et al., 2023).

Conversely, LDMC showed a significant positive correlation with altitude (p<0.01). LDMC reflects nutrient retention capacity and is largely independent of other leaf traits. Higher LDMC at elevated altitudes suggests greater investment in carbon-rich structural tissues, which reduces water loss by increasing diffusion resistance and enhances mechanical support under environmental stress. These findings align with reports that plants in high-altitude environments-characterized by low temperatures, high radiation, and nutrient-poor soils-allocate more biomass to supportive tissues, resulting in elevated LDMC (Saura-Mas and Lloret, 2007). A negative correlation between SLA and LDMC further supports a trade-off between resource acquisition and conservation strategies along the altitudinal gradient. However, the ecological implications of this relationship may vary between species due to divergent adaptive responses to altitude.

Carbon (C), nitrogen (N), and phosphorus (P) are major constituents of leaf dry mass and play vital roles in photosynthesis, cell growth, and differentiation (He et al., 2006). Their stoichiometric ratios provide valuable insights into plant metabolic strategies and environmental adaptability (Pulido et al., 2023). In this study, both LN and LP increased with elevation, consistent with results from a 3000-m elevation gradient on Gongga Mountain (Xu et al., 2021). This trend supports the Temperature-Plant Physiology Hypothesis (TPPH), which posits that low temperatures at high altitudes reduce metabolic and phosphate cycling rates, prompting plants to accumulate N and P to maintain photosynthetic and enzyme activity (e.g., Rubisco synthesis). These adjustments help compensate for reduced physiological efficiency under cold conditions and facilitate adaptation to short growing seasons and high light intensity.

LC:N and LC:P decreased with increasing elevation, indicating lower nitrogen and phosphorus use efficiency in high-altitude populations. This likely results from constrained leaf development and reduced photosynthetic rates under cooler and drier conditions, limiting nutrient accumulation and utilization. These findings align with the observed reduction in SLA, suggesting greater resource allocation to structural defense at the expense of growth-related functions at higher elevations (Rauf et al., 2023). The N:P ratio serves as an indicator of nutrient limitation. Across all five elevations, LN:P was below 14, suggesting that nitrogen is the primary limiting nutrient for P. armandii growth in the study area (Koerselman and Meuleman, 1996). Leaf stoichiometric traits exhibited varying degrees of altitudinal sensitivity: phosphorus content showed the highest coefficient of variation, indicating stronger phenotypic plasticity and faster response to elevation changes compared to nitrogen, carbon, and C:N ratios (Zhang et al., 2023). This highlights the role of P in mediating plant adaptation to altitudinal gradients.

4.2 Coupling and trade-offs among LFTs

In the process of plant environmental adaptation, leaf functional traits do not operate in isolation but form integrated suites through trade-offs and synergies, as captured by the leaf economics spectrum framework (Fajardo and Siefert, 2018; Monge-González et al., 2021; Wright et al., 2007). These trait combinations reflect fundamental ecological strategies in resource allocation. However, the strength and direction of these trait relationships can vary across study scales. A key uncertainty lies in understanding how the response of a given trait along elevational gradients is constrained by its correlations with other traits (Midolo et al., 2019). This study demonstrates widespread significant correlations among LFTs in P. armandii, indicating that leaf traits respond to environmental stress in a modular and coordinated manner. This reflects a strategy optimizing carbon investment and return, consistent with the “fast-slow”trade-off framework of the plant economics spectrum. SLA and LDMC, key indicators of ecological strategies, represent opposing ends of the resource acquisition-conservation spectrum (van Bodegom et al., 2014). Here, they exhibited a highly significant negative correlation, consistent with previous studies (Reich et al., 1991; Wilson et al., 1999; Wright and Cannon, 2001; Wei et al., 2011). In high-elevation environments characterized by low temperatures, low SLA and high LDMC help reduce water loss by increasing resistance to water diffusion and prolonging the diffusion pathway, thereby extending carbon payback time and allocating more resources to defense and structural support, which enhances survival under resource-limited conditions (Cornelissen et al., 2003). Additionally, a significant negative correlation was observed between LDMC and LT, suggesting that at high altitudes, P. armandii adopts a “slow investment-return” strategy characterized by high LDMC and low LT, improving tolerance to adverse conditions through increased dry matter content. In contrast, at low elevations, a”fast investment-return”strategy with low LDMC and high LT is favored. Meanwhile, the positive correlation between SLA and LT may be related to leaf size effects on boundary layer dynamics and thermal regulation (Wright et al., 2017). Larger leaves with thicker boundary layers can reduce sensible heat exchange, influencing leaf temperature and transpiration rates, thereby aiding water conservation and reducing transpiration (Leigh et al., 2017).

Significant trade-offs were also observed between structural and chemical traits. LDMC was positively correlated with LNC and negatively with LC:N, indicating that higher nitrogen investment may support denser structural tissue synthesis and improve nitrogen use efficiency. Conversely, SLA was positively correlated with LC:N and negatively with LNC, aligning with the leaf economics spectrum: high-SLA leaves favor rapid resource acquisition, whereas low-SLA leaves reflect a conservative strategy (Wright et al., 2004). This coordinated variation between structural and chemical traits reflects an adaptive mechanism through which plants optimize resource use efficiency by balancing photosynthetic gain, structural investment, and metabolic cost in nutrient-poor habitats, consistent with the role of trait coordination in ecosystem functional recovery emphasized by Gao et al. (2025). Furthermore, LCC was significantly correlated only with LDMC, suggesting that carbon accumulation is primarily driven by structural demands rather than metabolic requirements. LN:P was correlated only with LPC and LC:P, indicating that nitrogen and phosphorus allocation may be independently regulated by genetic constraints or soil phosphorus availability. The lack of a significant correlation between LNC and LPC along the elevational gradient further suggests that nutrient limitations (e.g., low temperature or soil nutrient availability) may decouple stoichiometric relationships, reflecting adaptive divergence of P. armandii across heterogeneous habitats.

In the trait network, traits with high node degree centrality often play core roles in functional integration (Flores-Moreno et al., 2019). In this study, LC:N emerged as a central node (with the highest degree, closeness, and betweenness centrality), indicating that carbon-nitrogen balance plays a pivotal regulatory role in trait coordination. This finding supports the ecological stoichiometry theory, which posits that carbon-to-nitrogen ratios mediate growth-defense trade-offs. A high LC:N typically signifies resource allocation to structural defense, whereas a low ratio promotes nitrogen metabolism and growth, suggesting that P. armandii dynamically adjusts carbon and nitrogen allocation to balance photosynthetic, structural, and defensive investments, thereby enhancing environmental adaptability.

4.3 Environmental drivers of LFTs

It is well-established that plant leaf functional traits are influenced by a range of abiotic and biotic factors, including climate (Sardans and Penuelas, 2014; Yuan and Chen, 2009), soil properties (Chen et al., 2013; Zhang et al., 2019), and plant life forms (He et al., 2006; Zhao et al., 2018). At broad spatial scales, climatic variables are often the dominant drivers of trait variation (Craine and Lee, 2003), whereas at finer regional scales, soil factors become particularly influential (Luo et al., 2019). Soil conditions affect plant growth through both direct and indirect pathways, serving as a primary source of nutrients and mediating resource availability (Peguero et al., 2023; Chen et al., 2024). Variations in nutrient supply can significantly impact plant functional traits, thereby influencing plant performance (Zhang et al., 2023). In line with these observations, our study demonstrated that multiple soil nutrients collectively influence the LFTs of P. armandii, though distinct traits being influenced by different key factors.

First, soil organic carbon (SOC) exerted significant positive direct effects on multiple leaf traits, particularly LL, LA, and SLA. This indicates that SOC promotes rapid leaf expansion and enhances light capture capacity by improving soil structure and nutrient availability, aligning with a “resource-acquisitive” ecological strategy. Conversely, SOC showed a significant negative correlation with LDMC, further supporting the idea that plants in high-SOC environments may prioritize resource allocation toward growth rather than structural defense. These findings align with previous studies by Huang et al. (2018) and Duan et al. (2017), which identified SOC as a key driver of divergence in plant functional traits. Similarly, Fan et al. (2022) reported SOC as a critical soil factor influencing LFTs in Pinus tabulaeformis. SOC, derived mainly from the decomposition of plant, animal, and microbial residues, as well as litter input, significantly modulates plant functional trait variation. Furthermore, by improving soil structure and enhancing water and nutrient retention, SOC provides plants with more sufficient moisture and nutrients, thereby facilitating transpiration and photosynthesis and promoting plant growth and development (Kühn et al., 2021).

Second, soil pH also significantly influenced multiple traits, particularly stoichiometric traits such as LC:N and LC:P, indicating that soil acidity or alkalinity plays a crucial role in regulating internal carbon, nitrogen, and phosphorus balance in plants. The underlying mechanism may involve pH-induced changes in microbial activity and nutrient availability, which indirectly modulate elemental stoichiometry in plants (Liu et al., 2023b). In high-pH environments, plants tended to accumulate more carbon, reflecting a conservative resource-use strategy likely driven by nutrient limitations (e.g., reduced phosphorus availability) under alkaline conditions (Lin et al., 2022).

Notably, available potassium (AK) was negatively correlated with most leaf traits, particularly LL, LT, LA, and LDMC. For instance, the direct path coefficients of AK on LA and SLA were -0.5309 and -0.3179, respectively, suggesting that potassium availability may inhibit leaf expansion and specific leaf area, thereby promoting a more conservative leaf construction strategy. Although potassium is essential for plant growth, excess levels may inhibit leaf development via ionic toxicity or antagonism with other elements (e.g., calcium, magnesium), while also increasing LDMC- indicating a potential shift toward higher tissue density to maintain water and ionic balance under potassium stress.

Moreover, available phosphorus (AP) exhibited a complex relationship with LT: although their correlation coefficient was positive (0.3205), the direct path coefficient was negative (-0.2215), while the indirect effect was positive (0.5421). This implies that AP may indirectly promote leaf thickening through interactions with other factors (e.g., SOC or AK), rather than exerting a direct positive effect. This indirect influence highlights the complex synergistic and antagonistic interactions among soil factors, underscoring the need for multi-path analysis rather than relying solely on simple correlations when interpreting the effects of phosphorus on plant morphogenesis. Consistent with our findings, Chen et al. (2024) also identified soil phosphorus as a key factor influencing leaf functional traits.

5 Conclusion

This study examined LFTs of P. armandii along a small-scale elevational gradient, revealing significant altitudinal variation and coordinated trait relationships indicative of ecological adaptation to local environmental conditions. Key leaf traits exhibited synergistic or trade-off relationships in response to shifts in hydrothermal factors and soil properties along the gradient. Multiple soil drivers influenced these traits, with SOC, pH, and AK identified as primary factors, although different traits were influenced by distinct environmental factors. These results illuminate how P. armandii in karst mountainous areas adjusts to elevation-dependent environmental conditions, highlighting mechanisms underlying plant adaptation to changing habitats. The findings further imply that through trait integration, plants achieve a balance between growth and survival, offering insights for ecological restoration in rocky desertification zones. Future research should incorporate broader environmental dimensions-such as climate and topography-and extend trait analysis across multiple plant organs and functional groups to improve multi-scale understanding of trait-environment-ecosystem linkages. Particularly critical is exploring how global change alters soil nutrient availability and subsequently affects plant traits and ecosystem functioning.

Data availability statement

The original contributions presented in the study are included in the article/supplementary material. Further inquiries can be directed to the corresponding authors.

Author contributions

BH: Conceptualization, Data curation, Funding acquisition, Investigation, Methodology, Project administration, Resources, Writing – original draft, Writing – review & editing. WL: Conceptualization, Formal Analysis, Investigation, Methodology, Writing – original draft. XB: Data curation, Investigation, Software, Supervision, Validation, Writing – original draft. SZ: Conceptualization, Investigation, Project administration, Software, Validation, Writing – original draft. QL: Data curation, Formal Analysis, Project administration, Writing – original draft.

Funding

The author(s) declare financial support was received for the research and/or publication of this article. This work was supported by the following funding sources: • the Project of Guizhou Science and Technology Fund (No. Qiankehe Jichu-ZK [2024] Key 077) • the Technology Top Talent Project in Department of Education of Guizhou Province (No. [2022]096) • the Project of Bijie Science and Technology Fund (No. Bikelianhe [2023]10, 22, and 24).

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

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Keywords: Pinus armandii, leaf functional trait, elevational gradient, soil factors, Karst mountains

Citation: He B, Li W, Bai X, Zou S and Li Q (2025) Variation in leaf functional traits of Pinus armandii and their drivers along an altitudinal gradient in Karst mountains. Front. Plant Sci. 16:1707246. doi: 10.3389/fpls.2025.1707246

Received: 17 September 2025; Accepted: 21 October 2025;
Published: 06 November 2025.

Edited by:

César Marín, Santo Tomás University, Chile

Reviewed by:

Xiao-Dong Yang, Ningbo University, China
Yaseen Khan, Hainan University, China

Copyright © 2025 He, Li, Bai, Zou and Li. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Qing Li, bGlxaW5nZHJlYW1AMTYzLmNvbQ==; Shun Zou, em91c2h1bkBndWVzLmVkdS5jbg==

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