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Article

Ecological Factors Driving Tree Diversity across Spatial Scales in Temperate Forests, Northeast China

1
School of Life Sciences, Qufu Normal University, Shandong 273165, China
2
Erguna Forest–Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
3
CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
4
Changbai Mountain Academy of Sciences, Erdaobaihe, Yanji 133613, China
*
Author to whom correspondence should be addressed.
Forests 2023, 14(6), 1241; https://doi.org/10.3390/f14061241
Submission received: 13 May 2023 / Revised: 7 June 2023 / Accepted: 9 June 2023 / Published: 15 June 2023
(This article belongs to the Section Forest Biodiversity)

Abstract

:
Species diversity has been shown to be influenced by environmental factors, but the mechanism underlying their relationship remains unclear across spatial scales. Based on field investigation data collected from 3077 sample plots in temperate forest ecosystems, we compared tree species richness, evenness and dominance at 10 km × 10 km, 30 km × 30 km and 90 km × 90 km spatial scales. Then, we detected the scale dependence of changes in tree species composition on climate, topography and forest structure using variation partitioning and quantified their contribution to tree diversity with gradient–boosted models (GBMs) and fitted their relationships. The magnitude of tree richness, evenness and dominance significantly increased with spatial scale. Ecological factors jointly accounted for 24.3%, 26.5% and 38.5% of the variation in tree species composition at the three spatial scales, respectively. The annual mean temperature had a strong impact on tree richness, evenness and dominance and peaked at an intermediate scale. Tree evenness and dominance increased with the variation of temperature but had upper and lower limits. Tree richness obviously increased with annual precipitation on multiple scales and decreased with annual sunshine duration at large spatial scales. Tree richness, evenness and dominance obviously increased with the variation in elevation and diameter at breast height at large scales and small scales, respectively. Tree dominance decreased with tree height at a small scale. The dependence of tree diversity on ecological factors increased with spatial scales. Furthermore, different factors exert various controls on tree diversity at different spatial scales, representing a comprehensive mechanism regulating tree diversity.

1. Introduction

The dependence of biodiversity on spatial scale has long been a hot topic in ecology research [1,2,3,4]. Studying plant diversity at different spatial scales has great significance for understanding the spatial pattern of species diversity and its ecological drivers [5]. Given that the assembly mechanisms of communities vary across different spatial scales [1,6], diversity patterns at smaller spatial scales are usually different from those at larger scales [7,8,9,10,11]. However, there is still a lack of consensus regarding how ecological factors impact species diversity and drive its changes across different spatial scales.
Species diversity and environmental factors can be strongly scale—dependent, which presents a major obstacle to answering the above questions [4,12,13,14,15]. Climate, as one of the most important abiotic factors, has a stronger impact on biodiversity across large spatiotemporal scales than small scales [3,6,16], and topographic factors, especially altitude, are thought to be more associated with diversity in regional scales than local scale [17]. Niche theory indicates that both biotic and abiotic interactions for living space and natural resources can promote the evolution rate and niche specialization, which tends to change with climatic gradient, especially temperature, through the kinetics of metabolism [18,19,20]. Species with broader niches can adapt to more abiotic conditions and tolerate a wider range of abiotic habitat changes and thus can disperse across larger geographic ranges [21]. In addition, latitude has a strong impact on plant richness mainly by influencing the climate, such as temperature and precipitation [22,23,24]. Studies have shown that communities in warm, humid regions support more species than communities in cold, dry regions [25,26,27,28]. The intermediate stress hypothesis (ISH) demonstrates that species diversity would likely peak at medium levels of environmental gradients [29]; for example, plant species richness varying with altitude in a hump—type has been found in numerous taxa [7,26,30]. However, the variation in species—environment relationships across spatial scales is still unclear.
In contrast to the regional scale, the horizontal and vertical structure of forests, including the number and size of coexisting tree individuals in the community, closely influences species diversity at the local scale by changing the energy distribution in the community [31]. The species—energy theory supposes that climate can strongly affect the primary productivity of plants, which mainly increases with temperature along latitudinal gradients, or the available energy partitioned into ecological systems [19,32,33]. On the one hand, more individuals can generally indicate higher species richness in statistics because (1) rare species may be more absent in smaller samples and (2) larger population sizes represent a lower risk of extinction [32,33,34]. On the other hand, more tree abundance may not translate to higher species diversity [32,33] because available energy may also be distributed to maintain fewer higher/larger individuals rather than more. Disproportional species competition between larger/higher trees and smaller/shorter trees for limiting resources, such as sunshine, moisture or nutrients, can suppress plant diversity [35,36,37,38]. However, the effect of forest structure vs. climate and topography on species diversity varying with spatial scales remains unclear in temperate forests.
The mechanisms mentioned above are not mutually exclusive, but they may work together in explaining different aspects of biodiversity [31], such as species composition, richness, evenness (Shannon–Wiener index) and dominance (Simpson index). The community represents the different species assembling in a space; species richness is the actual number of species in the community; species evenness (weighting individual abundance of each specie in the community) and species dominance (representing the relative percentage of species in the community) can reflect the development of the community. Furthermore, comparing tree diversity among sites on a single spatial scale may yield unmatched results and hinder synthetic analyses [4,5], while multiple spatial scales are suitable for exploring complex ecological variations [39]. However, comprehensive tests on the relative contribution of ecological factors to various aspects of tree diversity across multiple spatial scales are infrequent.
The forest in northeast China is one of the most species—rich areas in temperate ecosystems. We quantified the contributions of climatic, topographic and forest structure conditions to tree diversity at three spatial scales, 10 km × 10 km, 30 km × 30 km and 90 km × 90 km. The primary aims of our study were to examine the variations in the ecological mechanisms driving tree diversity on different spatial scales. We investigated the following specific hypotheses about plant diversity in temperate forests: (I) the effect of ecological factors driving tree diversity increase with spatial scale; (II) various factors affecting tree diversity on different spatial scales. We used species richness, the Shannon index and the Simpson index as primary measures of species diversity. Our study provides insights into the driving mechanisms of tree diversity patterns at multiple spatial scales.

2. Materials and Methods

2.1. Study Region and Sample Sites

This study concentrates on the natural mountain forests in northeast China, mainly including 9 montane areas: Greater and Lesser Khingan, Zhangguangcailing, Wanda, Hadaling, Laoyeling, Longgang, Changbai, the western Liaoning mountains (Figure 1). The survey area extended from 39° N to 53° N and 116° E to 135° E, and this area has a temperate continental climate zone, with warm—rainy summers and cold—dry winters. The annual mean temperature varies from −6 °C in the north to 11 °C in the south. Most precipitation mainly occurs from June to September every year. The annual precipitation increases from 380 mm in the northwest to 1130 mm in the southeast. The altitude ranges from 31 to 2115 m, and the slope varies from 0 to 46°. The forest types include mixed broad—leaved forest, mixed broadleaf—conifer forest, and coniferous forest [26].
In the summers of 2008 to 2016, we totally collected 3077 sample plots, which had an area of 900 m2 (30 m × 30 m). All the sample plots we investigated were natural forests far from roads and other human infrastructure. For the subsequent analysis, these plots served as the basic unit of the various grid scales. We recorded the geographic coordinates of the sampling centre and measured the elevation (m) and slope (°) of each plot. Then, we conducted the surveys on the trees with a diameter at breast height (DBH) of ≥5 cm in each plot and standardized the tree species names based on the Flora of China (http://www.iplant.cn/foc, accessed on 10 March 2018). Finally, a total of 289,124 tree individuals including 155 tree species were collected. The number of tree species in the 3077 sample plots ranged from 1 to 21 (Figure S1).

2.2. Tree Diversity Scaling

Spatial representation and a consistent approach for sampling plots at the local scale are crucial to the effective results about species diversity patterns and the dominant drivers at regional scales [11]. In this study, a sampling method executing contiguously arrayed grids such as Scheiner’s Type II approach was used [40]. Compared to Scheiner’s Type II approach, the main difference was that our examining grids were composed of the investigated 3077 sampling plots. First, we transformed the longitude and latitude (°) of the plots into geographic distance coordinates (km) on the plane with R package ‘geosphere’. Then, we divided the plane into 10 km × 10 km, 30 km × 30 km and 90 km × 90 km spatial scales of sampling grids, level by level (Figure S2), and then extracted the grid containing sample plots for subsequent statistical analysis. Finally, we obtained 615, 420 and 117 grids, which were the number of grids containing sample plots, at the three spatial scales, respectively.
In this study, the distribution of 3077 sampling plots was uneven covering the study area as shown in Figure 1. The tree diversity analysis could be potentially biased by the uneven sampling coverage. For example, we sampled more plots in the Changbai Mountains due to its higher species pool, and we sampled fewer plots in the Greater Khingan Mountains due to its lower species pool. To minimize this problem, we used a rarefaction and extrapolation approach to generate estimates of the tree diversity in each grid with the R package iNEXT [41]. Then, the 95% confidence intervals were calculated by the 0.025 and 0.975 quantiles with 1000 simulations of bootstrap samples. The simulated species richness, Shannon index and Simpson index values were the expected diversity.

2.3. Explanatory Variable Selection

We chose 9 variables to explain the variability in tree diversity, including climate, topography and forest structure (Table 1). We obtained standardized climate data, including the annual mean temperature (AMT, °C), annual precipitation (AP, mm) and annual sunshine duration (ASD, hour), with 500 m × 500 m resolution from the website of China Meteorological Administration (http://www.cma.gov.cn/, accessed on 30 November 2018). The climate data we used were averaged from 2008 to 2016, corresponding to the time of the plot survey. We selected three topographic factors, such as elevation (EL, m), slope (SL, °) and soil moisture index (SMI). As a function of topographic position and soil physicochemical properties, the SMI represents the capacity of soil holding water. In each grid, three easily measured and ecologically important forest structure variables were detected, including tree density (TD, the abundance of tree individuals per hectare), the diameter at breast height (DBH, cm) and tree height (TH, m). We calculated both the mean value and the coefficient of variation for the 9 variables in each grid, as the mean value may weaken the effect of the local conditions with increasing scale. Finally, we obtained 14 variables after excluding 4 collinear variables (r > 0.7), including APcv, SMIcv, DBHmean and THcv.

2.4. Data Analysis

These 14 variables, classified as climatic, topographic and forest structure conditions, were used for partitioning the total variation in tree diversity across northeast China. We partitioned the explanatory variables into independent and shared components to analyse the three groups of predictors explaining the variation in tree species diversity. The ‘varpart’ function in the vegan package based on linear regression was used to compute the adjusted R2 [42].
We fitted the gradient—boosted models (GBMs) to detect the relative importance of predictors to tree diversity. The GBMs can provide accurate coefficients and reliable results, especially partitioning the correlation among predictive factors [43,44]. To minimize the influence of extreme outliers, the regression trees were gradually added, and data were reweighted to compensate for the improper fitting of previous regression trees [24]. Therefore, the GBM can fit complex nonlinear relationships and realize higher accuracy and less bias without overfitting [45]. When fitting GBMs, we should specify two main parameters, including learning rate and tree complexity, which regulate the number and the interaction depth of regression trees, respectively [46]. We set 0.001 as the learning rate value and 2 as the tree complexity value. A Poisson distribution of errors was operated to match the response of tree richness to variables, as richness is the number of species [24]. The R package dismo and “gbm” scripts were used to examine the contribution of predictors. We detected the residuals of the GBMs for spatial independence with Moran’s I test and detected no statistically significant spatial autocorrelation; thus, we did not explore further. All descriptive statistical analyses were performed with R version 3.4.3 (http://www.r-project.org, accessed on 2 December 2022).

3. Results

3.1. Tree Diversity at Different Spatial Scales

The tree richness, Shannon index and Simpson index showed the same spatial patterns, and all increased with the incremental spatial scale (Figure 2). Analysis of variance indicated that the tree richness, Shannon index and Simpson index on different spatial scales were significantly different (p ≤ 0.01).

3.2. Ecological Drivers of Tree Diversity

The measured ecological variables explaining the variation in tree species composition at the three spatial scales were 24.3%, 26.5% and 38.5%, respectively (Figure 3). Climatic factors explained the most independent fraction of tree diversity at the three grid scales (9.6%, 11.1% and 12.5%), but a small independent fraction was explained by topography (2.9%, 2.7% and 4.3%) and forest structure (4.2%, 3.9% and 5.0%). The combined explanations of the three components were 2.6%, 3.2% and 8.1%, respectively, with spatial scale.
The DBHcv statistically influenced most tree richness, followed by the APmean and AMTmean at the 10 km × 10 km spatial scale (Table 1). APmean was the strongest impact, followed by AMTmean and DBHcv at the 30 km × 30 km spatial scale. APmean contributed most, followed by ASDmean and ELcv at the 90 km × 90 km spatial scale.
The DBHcv had the greatest statistical impact on the Shannon index, followed by the AMTmean and AMTcv at the 10 km × 10 km spatial scale (Table 1). AMTmean had the strongest influence, followed by DBHcv and AMTcv at the 30 km × 30 km spatial scale. AMTcv contributed the most, followed by AMTmean and ELcv at the 90 km × 90 km spatial scale.
For the Simpson index (Table 1), DBHcv had the greatest statistical influence, followed by AMTmean and THmean at the 10 km × 10 km spatial scale. AMTmean was the strongest impact, followed by AMTcv and DBHcv at the 30 km × 30 km spatial scale. AMTcv contributed the most, followed by AMTmean and ELcv at the 90 km × 90 km spatial scale.
In Figure 4, the three indexes of tree diversity responding to AMTmean and AMTcv had similar variation trends on different scales, but the extent of each was diverse. Tree richness increased with the AMTmean and then decreased slightly at the 10 km × 10 km, 30 km × 30 km and 90 km × 90 km scale. Tree richness increased with APmean, ELcv and DBHcv in an ascending ladder type. The changes in the Shannon index and Simpson index with AMTmean, ELcv and DBHcv at the three scales were analogous to that of tree richness. The Shannon index increased with AMTcv and then smoothed, and the same with the Simpson index. The Simpson index decreased with the THmean in an ascending ladder type.

4. Discussion

To explore the underlying mechanism of biodiversity, we evaluated the contributions of climatic, topographic and forest structure factors to tree diversity at three spatial scales. We aimed to verify that the effect of these factors driving tree diversity was scale—dependent. Our results showed that tree diversity of temperate forests in northeast China was strongly affected by ecological factors across spatial scales (Figure 3) and various factors driving tree diversity at multiple spatial scales (Table 1).
The results showed that the strong dependence of tree species diversity on ecological factors increased with spatial scale (Figure 2). Many studies have indicated that the patterns of species diversity had complex cross—scale effects on the environment [12,15,47]. One explanation is that large regions with a high number of species could contain historically accumulated species which segregated by climate refuges [48] or survived in complex physiographical heterogeneity in small spaces [49]. This phenomenon would produce a strong regional effect at a large spatial scale, rather than at a small scale [4]. In addition, plant diversity patterns indicate overlapping differences in the dispersal range of species [26,34], as species in different spaces have various demands for spatial resources and adaptabilities to the environment [50]. Thus, larger regions with more plant species have higher scale dependence on the environment. Our results indicated that climate has a stronger influence on tree diversity than topography and forest structure (Figure 3). Most studies have found that climate significantly impacts tree diversity across large regions, and the impact far exceeds the effects of other environmental factors [3,6,16,17,24,51], which is consistent with our study.
A positive relationship between tree diversity and annual mean temperature was found in our results (Figure 4). A study has shown that temperature drive species diversity across different spatial scales [52]. Chu et al. [31] suggested that regions with a less variable annual climate contain more tree species, which is consistent with our results. Appropriate temperature variation can increase the temperature niche for tree species and maintain higher tree diversity. Niche theory demonstrates that the life history strategy of plant species is determined by their ecological and biological characteristics, and different approaches to utilizing natural resources are used by species via occupying their respective ecological niches [46,53]. This analysis supports niche theory and is consistent with our findings that temperature variation within the upper and lower limits has a positive effect on the evenness (Shannon index) and dominance (Simpson index) of tree species (Figure 4). We found that tree diversity responded to temperature in a slight hump—type manner at the medium scale, which consists of the intermediate stress hypothesis (ISH). As temperature represents energy, we analysed whether warmer regions may have stronger competition among canopy species and reduced tree diversity. Although this situation in warmer regions can lead to energy redundancy [26,54,55], it creates conditions for trees with higher energy utilization formed via evolution or niche specialization promoted by the kinetics of metabolism [18,19,20].
Tree richness exhibited significant positive relationships with increasing precipitation at different spatial scales (Figure 4), suggesting that wetter sites have higher richness than drier sites [26]. Studies have revealed that climate warming inclines to restrict species diversity in regions containing relatively scarce water resources [56], but increased precipitation can offset the negative effect [25]. The biophysical interaction between temperature and precipitation is not easily disentangled in studies of plant diversity at a regional scale [57,58]. Furthermore, complex topography can affect the local water and energy budgets at small spatial scales and then indirectly drive the distribution of plant species and the diversity patterns in a region [17,32,59]. However, precipitation contributes more to tree richness, while temperature contributes more to tree evenness and tree species dominance. This result reveals that community composition is greatly affected by precipitation, which is consistent with Zhang et al. [47], while the spatial distribution and development of communities are mainly regulated by temperature. This analysis simultaneously supports the species—energy theory and niche theory.
The sunshine duration had a pronounced negative effect on tree richness at large spatial scales (Figure 4). This may be because sites with high sunshine duration are located on ridges or at high elevations, where harsh environments, especially low temperatures, limit the survival of species [26]. Valleys and sites at low elevations tend to provide suitable microclimates and thus contain higher species diversity. We detected an obvious effect of elevation on tree diversity at large spatial scales (Table 1), which is consistent with other studies [2,60]. Our results showed that tree diversity increased with elevation variation but had an upper limit (Figure 4). This result indicated that greater topographic heterogeneity provides more habitat types and living spaces and improves tree diversification by promoting species to occupy different niches [61,62,63,64]. Furthermore, complex topography can create refuges for species that persist in adverse environmental conditions [5] and thus have more species.
A large DBHcv had a positive effect on diversity at small spatial scales (Table 1 and Figure 4). Trees occupying different spaces (horizontal and vertical) can improve community richness, evenness, and dominance because DBHcv represents the difference in the size of tree individuals [26], which is consistent with niche theory. We did not find a significant contribution of tree density to tree diversity, but there was a negative relationship between tree height and the Simpson index. The results showed that excessive tree height of the larger tree can reduce the dominance of the community by increasing disproportional species competition with small trees as the shading effect [31], although a diversified tree height could increase vertical space and promote diversity. This analysis clearly supports the species—energy theory which states that available energy is distributed to support higher individuals, rather than more individuals, because of the suppression of tree diversity through asymmetric competition between taller trees and shorter trees for natural resources [35,36,37,38].

5. Conclusions

In conclusion, we detected the contribution of ecological factors on tree diversity and found that the effect of ecological factors driving tree diversity was scale—dependent. Different factors exerted various controls on tree diversity at different spatial scales. Changes in tree diversity were strongly impacted by ecological factors, especially climate, which had the greatest contribution, and the effect increased with spatial scale. Temperature and precipitation could significantly promote tree diversity at multiple spatial scales. Temperature mainly regulated the species evenness and dominance, while precipitation greatly affected species richness. Tree richness decreased with sunshine duration at large spatial scales. Tree diversity increased with large altitudinal heterogeneity, providing more survival habitat. Various individual sizes can improve tree diversity by occupying different niches, while excessive tree height in the community can suppress tree dominance due to intense canopy competition. However, our findings illustrate that a comprehensive mechanism regulates tree diversity across multiple spatial scales in temperate forests. This study can provide insights into the conservation and management of natural tree diversity at different spatial scales. In future research, we should systematically compare and analyse biodiversity from multiple aspects and spatiotemporal scales, especially in the context of climate change.

Supplementary Materials

The following supporting information can be downloaded at: https://www.mdpi.com/article/10.3390/f14061241/s1, Figure S1: Frequency occurrences of top 50 of 155 species abundance distribution in the 3077 forest plots. The inset histogram is the species-richness distribution of the 3077 plots. Figure S2 Sampling diagram across the study area. X is the distance of the sample point along the latitude. Y is the distance of the sample point along the longitude. The gray grids were the spatial scale for analysis.

Author Contributions

Y.G. (Yue Gu): Methodology, Software, Writing—Original Draft, Writing—Review and Editing, Visualization; J.Z.: Software, Data Curation, Funding Acquisition; W.M.: Formal Analysis, Writing—Review and Editing; Y.F.: Formal Analysis, Visualization; L.Y.: Formal Analysis; Z.L.: Investigation; Y.G. (Yanshuang Guo): Investigation; G.S.: Investigation; S.H.: Conceptualization, Validation, Data Curation, Supervision, Project Administration, Funding Acquisition. All authors have read and agreed to the published version of the manuscript.

Funding

This work was supported by the National Key Research and Development Program of China (No. 2016YFA0600804); the Natural Science Foundation of Liaoning Province (No. 2019—BS—262); and the Academy of Changbai Mountain Science (No. 2017—03).

Data Availability Statement

The data presented in this study are available on request from the corresponding author. The data are not publicly available due to survey respondents being assured raw data would remain confidential.

Acknowledgments

We would like to thank Shihong Jia for providing language help and writing assistance.

Conflicts of Interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

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Figure 1. Distribution of the 3077 sampling plots in northeast China.
Figure 1. Distribution of the 3077 sampling plots in northeast China.
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Figure 2. Box plots showing the variation in tree diversity at different grid scales. (1) Tree richness, (2) Shannon index, and (3) Simpson index. The letters a, b and c indicate significant differences in the diversity among different spatial scales.
Figure 2. Box plots showing the variation in tree diversity at different grid scales. (1) Tree richness, (2) Shannon index, and (3) Simpson index. The letters a, b and c indicate significant differences in the diversity among different spatial scales.
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Figure 3. Venn diagrams indicating the variation partitioning of tree species diversity explained by climate (X1), topography (X2) and forest structure (X3). The numbers in the diagrams represent the R2 values explained by ecological variables. The histograms are the total explained proportion of the diversity variation. (1) 10 km × 10 km grid scale, (2) 30 km × 30 km grid scale, and (3) 90 km × 90 km grid scale.
Figure 3. Venn diagrams indicating the variation partitioning of tree species diversity explained by climate (X1), topography (X2) and forest structure (X3). The numbers in the diagrams represent the R2 values explained by ecological variables. The histograms are the total explained proportion of the diversity variation. (1) 10 km × 10 km grid scale, (2) 30 km × 30 km grid scale, and (3) 90 km × 90 km grid scale.
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Figure 4. The relationships between tree species diversity and predictors at three spatial scales. (1) Tree richness; (2) Shannon index; and (3) Simpson index. AMT, annual mean temperature; AP, annual precipitation; ASD, annual sunshine duration; EL, elevation; DBH, diameter at breast height; TH, tree height.
Figure 4. The relationships between tree species diversity and predictors at three spatial scales. (1) Tree richness; (2) Shannon index; and (3) Simpson index. AMT, annual mean temperature; AP, annual precipitation; ASD, annual sunshine duration; EL, elevation; DBH, diameter at breast height; TH, tree height.
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Table 1. The contribution of ecological variables (%) to tree diversity fitted in GBM.
Table 1. The contribution of ecological variables (%) to tree diversity fitted in GBM.
VariablesRichnessShannonSimpson
10 × 1030 × 3090 × 9010 × 1030 × 3090 × 9010 × 1030 × 3090 × 90
ClimateAMTmean14.020.011.723.730.228.120.922.219.7
AMTcv13.310.110.69.314.328.78.116.946.7
APmean24.521.623.68.27.44.36.45.13.3
ASDmean4.84.418.72.62.23.32.62.21.0
ASDcv0.97.92.00.32.92.50.21.21.1
TopographyELmean2.52.92.53.82.40.72.63.80.1
ELcv2.42.613.43.12.116.44.84.415.2
SLmean0.52.90.31.61.80.52.73.91.5
SLcv3.31.23.01.41.61.93.51.40.6
SMImean0.51.30.41.32.50.42.44.40.8
Forest structureTDmean2.83.02.92.55.53.33.46.53.1
TDcv2.73.10.95.64.30.98.86.62.9
DBHcv26.618.39.631.620.37.823.613.12.4
THmean1.20.70.64.92.51.310.18.31.6
Model parametersDistributionPoissonPoissonPoissonGaussianGaussianGaussianGaussianGaussianGaussian
TC222222222
LR0.0010.0010.0010.0010.0010.0010.0010.0010.001
R20.650.770.850.690.800.860.620.730.69
Note: AMT, annual mean temperature; AP, annual precipitation; ASD, annual sunshine duration; EL, elevation; SL, slope; SMI, soil moisture index; TD, tree density; DBH, diameter at breast height; TH, tree height; TC, tree complexity; LR, learning rate. Bold numbers indicate the top three impacts of environmental factors on tree diversity.
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MDPI and ACS Style

Gu, Y.; Zhang, J.; Ma, W.; Feng, Y.; Yang, L.; Li, Z.; Guo, Y.; Shi, G.; Han, S. Ecological Factors Driving Tree Diversity across Spatial Scales in Temperate Forests, Northeast China. Forests 2023, 14, 1241. https://doi.org/10.3390/f14061241

AMA Style

Gu Y, Zhang J, Ma W, Feng Y, Yang L, Li Z, Guo Y, Shi G, Han S. Ecological Factors Driving Tree Diversity across Spatial Scales in Temperate Forests, Northeast China. Forests. 2023; 14(6):1241. https://doi.org/10.3390/f14061241

Chicago/Turabian Style

Gu, Yue, Junhui Zhang, Wang Ma, Yue Feng, Leilei Yang, Zhuo Li, Yanshuang Guo, Guoqiang Shi, and Shijie Han. 2023. "Ecological Factors Driving Tree Diversity across Spatial Scales in Temperate Forests, Northeast China" Forests 14, no. 6: 1241. https://doi.org/10.3390/f14061241

APA Style

Gu, Y., Zhang, J., Ma, W., Feng, Y., Yang, L., Li, Z., Guo, Y., Shi, G., & Han, S. (2023). Ecological Factors Driving Tree Diversity across Spatial Scales in Temperate Forests, Northeast China. Forests, 14(6), 1241. https://doi.org/10.3390/f14061241

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