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Article

Beta Diversity Patterns and Drivers of Macroinvertebrate Communities in Major Rivers of Ningxia, China

1
School of Civil and Hydraulic Engineering, Ningxia University, Yinchuan 750021, China
2
School of Life Sciences, Ningxia University, Yinchuan 750021, China
*
Author to whom correspondence should be addressed.
Animals 2025, 15(14), 2034; https://doi.org/10.3390/ani15142034
Submission received: 25 April 2025 / Revised: 5 July 2025 / Accepted: 9 July 2025 / Published: 10 July 2025
(This article belongs to the Section Ecology and Conservation)

Simple Summary

Elucidating the community assembly mechanisms of macroinvertebrates and their relative contributions to the formation of beta diversity is a central issue in aquatic ecology. In this study, we employed Generalized Dissimilarity Modelling to quantify the relative importance of explanatory variables in shaping community beta diversity. We further identified the dominant assembly processes by integrating Generalized Dissimilarity Modelling with the Normalized Stochasticity Ratio and determined the most appropriate beta diversity metric for the study region. The findings provide a scientific basis for optimizing land use configurations and guiding aquatic biodiversity assessment and conservation.

Abstract

The clarification of community assembly mechanisms in benthic macroinvertebrates and their respective contributions to the development of beta diversity is a fundamental concern in aquatic ecology. Nonetheless, the intrinsic complexity of community alterations and their non-linear reactions to gradients of explanatory variables present considerable obstacles to measuring the determinants of beta diversity. Fifty sampling points were set up along the major rivers of the Yellow River Irrigation Area (YRIA), the Central Arid Zone (CAZ), and the Southern Mountainous Area (SMA) in Ningxia in April, July, and October 2023. The findings demonstrate that the optimal parameter-based geographical detector (OPGD) model identified a 3000 m circular buffer as the spatial scale at which landscape structure most significantly influences water quality. A degradation in water quality presumably results in diminished differences in species composition among communities. The Sørensen index was determined to be more appropriate for this investigation, and the total beta diversity of the communities was relatively high (βSOR ≥ 0.82), with no identifiable nested spatial patterns detected. Except in the YRIA, environmental variability contributed more significantly to the variance in beta diversity than spatial factors, and deterministic mechanisms dominated the community assembly of benthic macroinvertebrates across all three months. To improve biodiversity and aquatic ecosystem health, the study region should optimize its landscape structure by reducing the amount of bare land and increasing the percentage of forest land within buffer zones. Additionally, a multi-site conservation strategy should be put into place.

1. Introduction

Water, which has many different uses and functions that are vital to the sustainable provision of human well-being, is universally acknowledged as the most critical natural resource [1]. However, readily accessible freshwater sources—such as wetlands, rivers, and lakes—constitute less than 1% of the Earth’s total water volume [2]. Among the most frequently used freshwater resources, rivers are unique and irreplaceable ecosystems whose openness, dynamism, and longitudinal connection make them crucial for ecological integrity and societal advancement [3,4,5]. Urbanization, agriculture, and dam construction are examples of human activities that change the spatial arrangement of vegetation and habitats in watersheds, causing habitat fragmentation and deterioration of water quality [6]. These changes exacerbate biotic homogenization and decrease aquatic biodiversity [7,8].
Beta diversity can be viewed as being based on the equilibrium between alpha diversity and gamma diversity [9], offering a robust framework for evaluating biotic homogeneity [10]. Deterministic processes (e.g., environmental filtering, whereby species are sorted along environmental gradients and occupy their optimal habitats) and stochastic processes (e.g., dispersal limitation) jointly govern beta diversity during community assembly [11,12], with their relative contributions varying across spatial and temporal scales [13]. Community assembly mechanisms establish the ecological foundation for the emergence of beta diversity, which subsequently reflects the spatiotemporal results of these mechanisms [14]. Environmental filtering, which favours the preservation of adapted species, and allopatric speciation, resulting from geographic isolation, can improve beta diversity [15]. Collinearity, however, affects the measurement of the independent effects of these two ecological processes [16]. Prior research has primarily utilized techniques including the Mantel test (or partial Mantel test), linear matrix regression, and multiple regression on dissimilarity matrices to investigate the relationship between beta diversity and environmental gradients [17,18,19]. Nonetheless, the non-linear correlation among these variables diminishes the precision of the outcomes obtained from these techniques [20]. Variance partitioning analysis (VPA) has been employed to investigate the distinct impacts of several variables (or groups of variables) on the development of beta diversity [21]. Nevertheless, the quantity of groups is frequently restricted, failing to address the common effect problem resulting from factor collinearity [22]. Effectively quantifying the relative contributions of ecological processes to forming beta diversity is a key issue in maintaining biodiversity [23].
Macroinvertebrates are characterized by wide geographic distributions, high species richness, and limited dispersal capabilities [24]. Owing to their sensitivity to environmental fluctuations, they are regarded as sentinels [25]. They provide several ecological functions, including enhancing organic detritus decomposition, facilitating nutrient flows, and regulating food webs [26,27]. Consequently, they are regarded as optimal species for examining the mechanisms that govern the development of beta diversity [28].
The Ningxia Hui Autonomous Region (Ningxia) has advanced irrigation-based agriculture to foster regional economic development, but this has also intensified non-point source pollution, such as nitrogen pollution, and heightened ecological risks to aquatic organisms [29,30]. This study centres on macroinvertebrates, aiming to (1) ascertain the patterns of beta diversity within macroinvertebrate communities, (2) elucidate the applicability of two types of beta diversity calculation schemes within the study area, and (3) uncover the predominant roles of stochastic and deterministic processes in community assembly.

2. Materials and Methods

2.1. Study Area

Ningxia (35°14′~39°23′ N, 104°17′~107°39′ E) encompasses an area of 66,400 km2 and is the sole provincial-level territory in China that is situated entirely inside the Yellow River Basin. The area has a moderate continental arid and semi-arid climate, with an average annual temperature of 5 °C to 9 °C and annual precipitation of 150 mm to 600 mm [31]. The region can be categorized into three zones from north to south, based on multi-year average precipitation lines (200 mm and 400 mm) and other environmental attributes, including agricultural and pastoral distributions: the Yellow River Irrigation Area (YRIA), the Central Arid Zone (CAZ), and the Southern Mountainous Area (SMA) [32,33]. Our study monitored macroinvertebrates and physicochemical factors across these three zones in April, July, and October 2023. The quantity of monitoring sites in YRIA, CAZ, and SMA was 16 (S1–S16), 14 (S17–S30), and 20 (S31–S50), respectively (Figure 1).

2.2. Collection of Datasets

2.2.1. Benthic Macroinvertebrates

Beginning at the upstream segment of the monitoring transect, macroinvertebrate collection was performed over a 100 m river reach using a D-net (mesh size: 0.5 mm; frame dimensions: 30 cm × 30 cm), with six replicate samples collected at each point from different habitats and pooled into a single composite sample [34]. Samples were filtered using a 40-mesh screen, packaged in polyethylene zip-lock bags, and transferred to the laboratory under refrigeration. Upon arrival, they were arranged on white porcelain trays for sorting, fixed in 75% ethanol, and stored in 50 mL specimen vials. Identification and enumeration were primarily conducted using a dissecting microscope (LIOO SMZ61, Beijing, China), and biological abundance was calculated as the number of individuals per square metre (ind./m2). Identification of macroinvertebrates relied predominantly on the aquatic invertebrate reference literature [35,36], with specimens classified according to the most specific taxonomic unit achievable.

2.2.2. Environmental Factors

At each sampling site, the latitude, longitude, and altitude (ALT) were recorded in the field. Simultaneously, physicochemical parameters—including river width (RW), pH, water temperature (WT), dissolved oxygen (DO), electrical conductivity (EC), flow velocity (VEL), turbidity (TUR), chlorophyll a (Chl a), salinity (SAL), total dissolved solids (TDS), and fluoride (F)—were measured. Water was collected using a 1 L sampler at 0.5 m below the surface, with three parallel samples combined into a single composite. In reaches shallower than 0.5 m, sampling was performed at mid-depth. The composite sample was used to rinse 500 mL polyethylene bottles prior to filling; the bottles were then sealed, stored at 0~4 °C in a refrigerator, and transported to the laboratory for analysis at the earliest opportunity. The levels of pollutants, including ammonia nitrogen (NH3-N), total nitrogen (TN), total phosphorus (TP), nitrate (NO3-N), nitrite (NO2-N), and the permanganate index (CODMn), were assessed in accordance with the national water quality standards HJ 535-2009 (Water quality—Determination of ammonia nitrogen—Nessler’s reagent spectrophotometry), HJ 636-2012 (Water quality—Determination of total nitrogen—Alkaline potassium persulfate digestion UV spectrophotometric method), GB/T 11893-1989 (Water quality—Determination of total phosphorus—Ammonium molybdate spectrophotometric method), GB 7480-87 (Water quality—Determination of nitrate-Spectrophotometric method with phenol disulfonic acid), GB 7493-87 (Water quality—Determination of nitrogen (nitrite)—Spectrophotometric method), and GB 11892-89 (Water quality—Determination of benzene and its analogies—Gas chromatographic method).

2.2.3. Land Use

Liu et al. [37] created a 10 m resolution land-cover map for China in 2020, utilizing a deep classification network and Sentinel-2 imagery as data sources. The projected overall accuracy was 84.35% ± 0.92%. This dataset exhibits enhanced classification accuracy and spatial detail compared to other land-cover products (e.g., GlobeLand30, ESA WorldCover, Esri Land Cover, and FROM-GLC-10), rendering it particularly suitable for the requirements of this study. According to the current land use classification (GB/T 21010-2017) and the specific conditions of the study region, the land was classified into seven categories: cultivated land, forest land, grass/shrubland, construction land, water area, wetland, and bare land.

2.3. Methods

2.3.1. Environmental Heterogeneity

The geographical distance between sampling points was computed using the distm function from the “geosphere” package [38] in R (v.4.3.3), utilizing their latitude and longitude coordinates. The vertical distance between two points was calculated using the Euclidean distance approach through the dist function. Environmental dissimilarity (Ed) between sampling locations was determined based on environmental variables (Equation (1)) [39], and environmental heterogeneity was assessed based on environmental dissimilarity.
Ed = Euc / Euc max + 0.001
where Euc signifies the Euclidean distance between two sample points, while Eucmax indicates the maximum Euclidean distance within the distance matrix. The inclusion of 0.001 is mainly designed to address the null similarity between sampling points.

2.3.2. Beta Diversity Measurement

The pairwise Sørensen dissimilarity index was employed to compute the beta diversity (βsor) between sample points, utilizing binary species presence/absence data. According to the additive partitioning approach introduced by Baselga [40], βsor can be divided into species turnover (βsim) and species nestedness (βnes). The multiple-site Sørensen index was utilized to compute the overall beta diversity (βSOR), which was subsequently divided into turnover (βSIM) and nestedness (βSNE) to evaluate the contributions of various components. Simultaneously, utilizing species abundance data, the beta.pair.abund function was employed to assess the Bray–Curtis dissimilarity index (dBC) between locations, which was subsequently partitioned into the balanced variation component (dBC-bal) and the abundance gradient component (dBC-gra), with dBC-bal and dBC-gra corresponding to βsim and βnes, respectively [40]. The beta.multi.abund function was employed to calculate the Bray–Curtis index (βBC) for measuring overall dissimilarity, which was then divided into the balanced variation component (βBC.BAL) and the abundance gradient component (βBC.GRA) [41]. Beta diversity was calculated primarily using the R package “betapart”.

2.3.3. Buffer Zone Screening

Considering the retention and bi-directionality of the rivers, as well as the multidirectional water sources, circular buffer zones (100 m, 500 m, 1000 m, 2000 m, 3000 m, and 4000 m) centred around sampling points were established using ArcGIS 10.8, following approaches from previous studies [42]. Concurrently, the “GD” package was utilized to determine the optimal parameter-based geographical detector (OPGD) model, particularly in the parameter optimization segment, to ascertain the critical spatial scales affecting water quality [43]. The q value (q ∈ [0, 1]) signifies the explanatory capacity of independent variables, with elevated values indicating more explanatory strength. The ideal scale is established when the 90th percentile of all independent variables attains its peak value. The influencing factors were classified into three categories: (1) the distribution of various land use types within the buffer zones; (2) landscape metrics at the landscape level, comprising the Largest Patch Index (LPI), Contagion Index (CONTAG), and Shannon’s Diversity Index (SHDI), with their ecological significance detailed in Table S1; (3) the human activity intensity of land surface (HAILS) (Equations (S1) and (S2)) [44].
The water quality index (WQI; Equation (S3)) integrates multiple physicochemical parameters into a single weighted value that reflects the overall status of the aquatic environment [45,46,47,48,49]. Thirteen indicators—pH, WT, EC, TUR, DO, TDS, TN, NH3-N, NO2-N, NO3-N, TP, CODMn, and Chl a—were included in the WQI calculation. Details of the parameter settings, calculation procedure, and water quality classification scheme are provided in the Supplementary Material. The mean WQI for April, July, and October was used as the response variable.

2.4. Statistical Analysis

Shapiro–Wilk’s test and Levene’s test demonstrated that the WQI values for different months and different zones within the same month both followed a normal distribution (p > 0.05) and exhibited homogeneity of variance (p > 0.05). Therefore, independent-sample t-tests were employed to compare water quality among sections within the same month, while linear mixed-effects models (LMMs) were used to assess differences across months. p-values were adjusted using the Bonferroni correction. LMM analyses were conducted primarily with the R packages “lme4”, “lmerTest”, and “emmeans”.
Generalized Dissimilarity Modelling (GDM) analysis was conducted utilizing the “gdm” package, employing the gdm function and formatsitepair function to investigate the underlying mechanisms of beta diversity [18]. This analysis utilized the beta diversity matrix across sampling sites as the response variable, with geographic distance, altitude distance, and environmental heterogeneity as predictor variables. The number of I-splines and the positions of the “knots” were established at their default values. The partial response plots of the fitted predictor factors demonstrate that the peak value on the y-axis signifies the extent of the variable’s contribution to community variation, whereas the curve’s slope represents the rate of change in the response variable along the predictor variable’s gradient [50].
The significance of stochastic and deterministic processes in macroinvertebrate community assembly was evaluated using the Normalized Stochasticity Ratio (NST) [51]. The NST was predominantly computed utilizing the tNST function from the “NST” package, employing the “bray” distance matrix and the “PF” null model [52].

3. Results

3.1. Composition of Species

Sixty-nine taxonomic units of macroinvertebrates were found, classified into 4 phyla, 7 classes, 20 orders, and 58 families (Figure S1). Arthropoda constituted the majority, with 72.5% of the total taxonomic units, followed by Mollusca at 18.8%. In contrast, Nematomorpha was the least represented, with only one species, Gordius aquaticus, collected (Figure 2a). A novel record in Ningxia, Himalopsyche sp. (Figure 2b), was identified. This species was obtained from a rapidly moving stream in the Liupan Mountains (sampling location S50, Figure 1c, Figure 1e S50). The pronotum is completely sclerotized, whereas the mesonotum and metanotum are wholly membranous. The mesothorax, metathorax, and abdominal segments one to eight possess prominent lateral gills. This species is classed as a predator under the family Rhyacophilidae of the order Trichoptera [53].

3.2. Beta Diversity and Its Components

Analysis utilizing the multiple-site Sørensen index and Bray–Curtis index of dissimilarity indicated that overall beta diversity was notably high across various months or spatial scales (βSOR ≥ 0.82, βBC ≥ 0.9), with βSIMSOR and βBC.BALBC both above 0.5 (Figure 3a). This suggests that species turnover is a primary factor influencing alterations in beta diversity, with no notable nested pattern detected.
Consistent with the overall beta diversity, the pairwise Sørensen dissimilarity index analysis revealed that the mean species composition similarity (1 − βsor) was below 0.5, with βsimsor above 59%, signifying a greater influence of turnover components (Figure 3b–e, Figures S2a–d and S3a–d). For example, in April, the average beta diversity across 1225 pairs of sampling sites in all sampling points was 0.67, with turnover and nested components accounting for 74.63% and 25.37%, respectively. Compared to the Sørensen index, the mean species composition similarity (1 − dBC) derived from the Bray–Curtis index was diminished (Figure 3f–i, Figures S2e–h and S3e–h). Moreover, in the CAZ between April and July, dBC-gra exceeded dBC-bal (Figure 3h and Figure S2g), signifying the predominance of the nested component.

3.3. Determinants of Beta Diversity Patterns

3.3.1. Water Quality Evaluation and Optimal Buffer Zone Selection

The average WQI readings for April, July, and October varied from 53.3 to 84.4, classifying water quality into two tiers. Of the sampling sites, 44% were designated as having “Good” water quality, while 56% were categorized as “Medium” (Figure 4a). In October, water quality was optimum, with no significant variations noted between April and July (p > 0.05) (Figure 4b). Furthermore, the water quality across the three months exhibited the hierarchy of SMA > YRIA > CAZ (p < 0.05), signifying that the SMA had the highest water quality, while the CAZ had the lowest (Figure 4b).
The examination of the OPGD model indicated that the 90th percentile of q-values for the 11 driving factors had an early increase, followed by a decline, peaking at 0.406 within the 3000 m buffer zone (Figure 4c). Consequently, the 3000 m buffer zone was chosen for further research. At this spatial scale, forest land (q = 0.520) and bare land (q = 0.406) were recognized as the principal environmental factors influencing spatial variance in water quality. As the percentage of forest area rose, the WQI initially ascended and subsequently declined (p < 0.001). In contrast, as the percentage of bare land rose, the WQI correspondingly diminished (p = 0.04) (Figure 4d).

3.3.2. Analysis of the Factors Influencing Beta Diversity

The GDM fitted six predictor variables to βsor and dBC: geographical distance, altitude difference, dissimilarity of physicochemical property, dissimilarity of the proportion of land use types, dissimilarity of HAILS, and dissimilarity of landscape pattern (Figure 5). Overall, in the same month and region, the total explained variance of the predictor variables for βsor exceeded that for dBC. For example, in April, the total explained variance of the predictor variables for βsor in the YRIA, the SMA, all sampling points, and the CAZ was 38.81%, 33.53%, 17.33%, and 5.13%, respectively; only for the CAZ was βsor lower than dBC (21.82%). The relative contributions of the predictor factors to βsor and dBC exhibited significant variance. Except for the YRIA, the cumulative explained variance of geographical distance and altitude difference for βsor was inferior to that for the other four predictor variables. However, no such trend was noted for dBC.

3.4. Community Assembly Mechanisms of Macroinvertebrates

The NST analysis indicated that the NST values were outside the 0~1 range (Figure 6a–c), necessitating the application of the modified stochasticity ratio (MST) to assess the relative significance of two ecological processes in community assembly. The distribution of MST values is illustrated in Figure 6d–f. At all sampling points, deterministic processes accounted for 57.71% in April, 62.69% in July, and 67.27% in October, whereas the share of stochastic processes was comparatively minor and exhibited a progressive decline. Regionally, the percentage of MST values below 0.5 surpassed the 50% criterion in both the CAZ and the SMA, signifying a more pronounced effect of deterministic selection in both areas, with the CAZ exhibiting a stronger deterministic influence than the SMA. In the YRIA, the percentages of MST values over 0.5 in April and October were 71.67% and 51.67%, respectively, signifying a more pronounced impact of stochastic processes, although the severity of this impact waned over time.

4. Discussion

4.1. Optimal Selection of Buffer Zones

Scale effects are prevalent in geographical spatial analysis [54]. Landscape composition also exhibits scale dependence in relation to water quality [55]. Establishing appropriate management buffer widths holds regional and temporal importance [56]. Techniques such as redundancy analysis (RDA), stepwise multiple linear regression (SMLR), partial least squares structural equation modelling (PLS-SEM), and VPA are frequently employed to determine the optimal spatial scale of landscape structure’s influence on water quality [57,58,59,60]. Wang et al. [61] emphasized the viability of such methodologies (e.g., RDA) in their analysis. It is worth noting that the response of water quality to environmental gradients is frequently non-linear [62,63], even though these methodologies often presume linear correlations to examine variable linkages [64,65]. This presents constraints in tackling intricate non-linear correlations or collinearity challenges in ecological data [22,66]. Consequently, this paper presents the OPGD model. The Geographical Detector (GD) model operates without assumptions regarding the variables, and can quantify both linear and non-linear connections [67,68]. Moreover, in contrast to the GD model, the OPGD model addresses challenges such as inadequate discretization effects and subjectivity, thereby enhancing the model’s resilience and enabling it to more precisely reveal the magnitude of individual factors’ effects on the dependent variable [69].
The analysis indicated that 3000 m is a breakpoint affecting water quality in the study area, denoting the ideal buffer zone. Huang et al. [70] revealed that landscape configuration within a 5.5 km radius buffer exerted the most substantial influence on water quality. The primary cause of this mismatch may stem from the varied determination methods utilized. Furthermore, the argument persists over which geographical sizes (e.g., circular, riparian, or watershed) have the most substantial impact on water quality [71]. Mello et al. [72] posited that watershed scales have greater influence than riparian zones; however, Zhou et al. [73] asserted that riparian zones have a more pronounced effect than both watershed and circular buffers. The regional heterogeneity of geographical phenomena, the diversity of data sources, and the complex interplay of human and environmental forces result in a lack of consensus on the optimal spatial scale [74,75,76]. Consequently, evaluating local conditions and using context-specific strategies is essential when establishing the ideal spatial scale for river management.

4.2. Analysis of Beta Diversity and Its Influencing Mechanisms

Various methodologies exist for quantifying beta diversity; however, a consensus on which method most correctly addresses particular ecological concerns has yet to be established [77]. The Sørensen index, based exclusively on incidence data, is straightforward to comprehend and compute, and has been extensively utilized in beta diversity assessments [78]. Integrating abundance data, the Bray–Curtis index is more resilient to undersampling—a failure to document all species present at a sampling site—than earlier indices [79,80]. This study calculated the beta diversity of macroinvertebrate communities using the Sørensen and Bray–Curtis indices. The outcomes from multiple-site and pairwise dissimilarity analyses reveal substantial discrepancies between the beta diversity estimates derived from the two indices. For instance, the frequency distribution of βsor within the value range of sample pairs in the ternary plot typically has a parabolic shape, with a peak occurring within a specific central range. Conversely, dBC demonstrates the greatest proportion inside the (0.9, 1] range, exhibiting a declining tendency as the interval values diminish (Figures S4–S6). Errors are prevalent in empirical research, rendering the selection of relatively precise methods for evaluating beta diversity more crucial [81].
GDM is a matrix-regression-based approach that is insensitive to multicollinearity among predictor variables and is capable of automatically selecting predictors during model fitting [82]. Furthermore, by incorporating generalized linear modelling with I-spline basis functions, GDM effectively uncovers non-linear relationships in ecological datasets [83]. The GDM method was employed to assess the significance of individual predictors in relation to beta diversity (Figure 5). At the same time, the partial response plots validated the non-linear associations among environmental gradients, geographical factors, and alterations in community composition (Figures S7–S12), aligning with prior research [84,85,86]. Furthermore, these findings suggest that linear models (e.g., Mantel test) are inadequate in capturing and characterizing the dynamic responses of beta diversity to various environmental gradients. Concerning the relevance of the two beta diversity calculation methods in the research area, the pairwise Sørensen dissimilarity index yielded results more compatible with total beta diversity. Secondly, in general, the total explained variance of the predictors for βsor changes exceeded that for dBC. Ultimately, the MST analysis indicated that except for the YRIA in April and October, the composition of macroinvertebrate communities was primarily influenced by deterministic processes, suggesting that environmental variables were more significant than spatial factors [87]. A comparison of the analysis results between GDM and the MST revealed that the spatial factors (geographical distance and altitude difference) explained the cumulative variation in βsor with a discrepancy only in July for the YRIA, where the GDM analysis suggested that stochastic processes primarily drove the variation in community composition, whereas the MST indicated that deterministic processes were the dominant driver of community assembly. Both methods showed high consistency for the remaining months and regions. However, the analysis of dBC using GDM exhibited a greater divergence from the MST results. The community assembly mechanism dictates the species composition of various communities [88,89], and variations in species composition represent beta diversity. Accordingly, studying beta diversity using the Sørensen index is more pertinent in this domain.
At the scale of all sampling points, the similarity among communities (1 − βsor) was seen to be minimal (Figure 3b, Figures S2a and S3a), signifying a rising trend in beta diversity with the enlargement of the spatial scale. This result aligns with the research conducted by He et al. [90] regarding macroinvertebrates. It is noteworthy that, according to GDM fitting, the predicted variables accounted for 17.33%, 11.1%, and 16.71% of the variance in βsor for April, July, and October, respectively (Figure 5). The considerable amount of unexplained variance indicates the existence of other factors influencing the disparities in species composition across communities. Factors such as precipitation, substrate type, river morphology, and hydrological connectivity [91,92] require further investigation. For the YRIA, the relative contribution of altitude difference to βsor exceeded 62%, and its partial response plot demonstrated that the pace of change in beta diversity escalated with more significant altitude differences (Figures S7–S9). Two possible reasons may elucidate the observed occurrence. Firstly, the study area includes various aquatic habitat types, such as drainage ditches (e.g., S3 and S4), the primary channel of the Yellow River (e.g., S14 and S16), and its tributaries (e.g., S12 and S13). Secondly, prolonged irrigation impacts have resulted in diverse alterations in hydrodynamic conditions at various elevations, with the consequent local microhabitats contributing to ecological filtration [93,94]. Compared to other places, the CAZ demonstrated the most remarkable community resemblance (Figure 3d, Figures S2c and S3c), mainly attributable to the inferior water quality in this area (Figure 4b), which diminished the beta diversity [27].

4.3. Limitations and Prospects

This study preliminarily explores the applicability of beta diversity and two indices from a species perspective, offering valuable insights for developing conservation strategies for macroinvertebrates. However, the formation of and variation in beta diversity in macroinvertebrates in rivers is an exceedingly complex process. Focusing solely on the species dimension, while neglecting interspecies functional trait variation (functional diversity) and evolutionary differences (phylogenetic diversity), may impose certain limitations on the analysis of community dynamics and associated ecological processes [95,96,97]. An extensive investigation of benthic macroinvertebrate beta diversity over all three dimensions would enhance comprehension of the mechanisms driving alterations in species composition within communities [98].
In addition to the two aspects of spatial beta diversity and its temporal variation explored in this study, beta diversity also encompasses temporal beta diversity and its spatial variation. Research on temporal beta diversity and its spatial dynamics helps to elucidate the stability of communities in different habitats, highlighting environmental characteristics that influence species fluctuations, thereby enabling the effective conservation of specific sites [99]. Future researchers may investigate beta diversity characteristics from a temporal perspective.

5. Conclusions

The OPGD model determines the optimal riparian buffer width for explaining water-quality variability and lays the foundation for identifying the drivers of macroinvertebrate beta diversity. GDM captures non-linear community responses to environmental gradients and spatial factors, quantifying the relative contribution of each predictor. Combined with the MST, it selected the appropriate beta diversity metric for the Ningxia reach and elucidated the underlying assembly mechanisms. By integrating OPGD, GDM, and the MST into a unified framework and incorporating multidimensional beta diversity analyses across spatial and temporal scales, the approach provides local conservation managers with a scientific foundation for delineating spatial priorities and guiding ecological restoration, thereby enhancing the health of riverine ecosystems. Although developed using the Ningxia reach as its study area, the framework is inherently region-neutral in its data requirements (land use layers, routine water quality indicators, and macroinvertebrate survey data), scale settings (modifiable according to data resolution and management objectives), and model assumptions, demonstrating strong potential for application across diverse river systems. Future inter-basin comparative studies will be instrumental in assessing the applicability of this framework under varying climatic and habitat conditions, thereby further enriching and refining riverine ecosystem management strategies.

Supplementary Materials

The following supporting information can be downloaded at https://www.mdpi.com/article/10.3390/ani15142034/s1. Figure S1: Composition of macroinvertebrates in Ningxia; Figure S2: Beta diversity of macroinvertebrates and characteristics of its two components at different sampling scales in July; Figure S3: Beta diversity of macroinvertebrates and characteristics of its two components at different sampling scales in October; Figure S4: Beta diversity and its component decomposition characteristics between paired sampling sites in April; Figure S5: Beta diversity and its component decomposition characteristics between paired sampling sites in July; Figure S6: Beta diversity and its component decomposition characteristics between paired sampling sites in October; Figure S7: Partial response graph of GDM for analyzing βsor in April; Figure S8: Partial response graph of GDM for analyzing βsor in July; Figure S9: Partial response graph of GDM for analyzing βsor in October; Figure S10: Partial response graph of GDM for analyzing dBC in April; Figure S11: Partial response graph of GDM for analyzing dBC in July; Figure S12: Partial response graph of GDM for analyzing dBC in October; Table S1: The landscape pattern index and its significance at the landscape level; Table S2: Conversion coefficients of different land use types for construction land equivalent; Table S3: The relative weights (Pi) and normalized values (Ci) of water quality parameters.

Author Contributions

Q.Y.: conceptualization, investigation, methodology, writing—original draft, writing—review and editing. Z.W.: investigation, methodology. X.Q.: funding acquisition, supervision, writing—review and editing. Z.Z.: investigation, software. All authors have read and agreed to the published version of the manuscript.

Funding

This study was supported by the Ningxia Natural Science Foundation (2023AAC02026) and the Ningxia University First-class Discipline (Water Conservancy Engineering) Construction Subsidy Project (NXYLXK2021A03).

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

Data will be made available on request.

Conflicts of Interest

The authors declare no conflicts of interest.

References

  1. Vörösmarty, C.J.; McIntyre, P.B.; Gessner, M.O.; Dudgeon, D.; Prusevich, A.; Green, P.; Glidden, S.; Bunn, S.E.; Sullivan, C.A.; Liermann, C.R.; et al. Global threats to human water security and river biodiversity. Nature. 2010, 467, 555–561. [Google Scholar] [CrossRef] [PubMed]
  2. Shi, X.Y.; Mao, D.H.; Song, K.S.; Xiang, H.X.; Li, S.J.; Wang, Z.M. Effects of landscape changes on water quality: A global meta-analysis. Water Res. 2024, 260, 121946. [Google Scholar] [CrossRef]
  3. Roccatello, S.; Lagrotteria, A.; Andrà, C.; Doretto, A. Bridging science and society: Developing a citizen science biomonitoring approach for river ecosystems in Italy. Ecol. Indic. 2025, 171, 113199. [Google Scholar] [CrossRef]
  4. Tiyasha; Tung, T.M.; Yaseen, Z.M. A survey on river water quality modelling using artificial intelligence models: 2000–2020. J. Hydrol. 2020, 585, 124670. [Google Scholar] [CrossRef]
  5. Wang, H.; Xiong, X.; Wang, K.H.; Li, X.; Hu, H.J.; Li, Q.L.; Yin, H.Q.; Wu, C.X. The effects of land use on water quality of alpine rivers: A case study in Qilian Mountain, China. Sci. Total Environ. 2023, 875, 162696. [Google Scholar] [CrossRef]
  6. Emi Fergus, C.; Renée Brooks, J.; Kaufmann, P.R.; Herlihy, A.T.; Hill, R.A.; Mitchell, R.M.; Ringold, P. Disentangling natural and anthropogenic effects on benthic macroinvertebrate assemblages in western US streams. Ecosphere 2023, 14, e4688. [Google Scholar] [CrossRef]
  7. Liu, Z.Y.; Zhou, T.T.; Heino, J.; Castro, D.M.P.; Cui, Y.D.; Li, Z.F.; Wang, W.M.; Chen, Y.S.; Xie, Z.C. Land conversion induced by urbanization leads to taxonomic and functional homogenization of a river macroinvertebrate metacommunity. Sci. Total Environ. 2022, 825, 153940. [Google Scholar] [CrossRef] [PubMed]
  8. Dalu, T.; Mwedzi, T.; Wasserman, R.J.; Madzivanzira, T.C.; Nhiwatiwa, T.; Cuthbert, R.N. Land use effects on water quality, habitat, and macroinvertebrate and diatom communities in African highland streams. Sci. Total Environ. 2022, 846, 157346. [Google Scholar] [CrossRef] [PubMed]
  9. Piló, D.; Carvalho, A.N.; Pereira, F.; Coelho, H.E.; Gaspar, M.B. Evaluation of macrobenthic community responses to dredging through a multimetric approach: Effective or apparent recovery? Ecol. Indic. 2019, 96, 656–668. [Google Scholar] [CrossRef]
  10. Liu, Y.; Jiang, X.F.; Li, D.P.; Shen, J.C.; An, S.Q.; Leng, X. Intensive human land uses cause the biotic homogenization of algae and change their assembly process in a major watershed of China. Sci. Total Environ. 2023, 871, 162115. [Google Scholar] [CrossRef]
  11. Zhang, X.; Liu, S.R.; Wang, J.X.; Huang, Y.T.; Freedman, Z.; Fu, S.L.; Liu, K.; Wang, H.; Li, X.Z.; Yao, M.J.; et al. Local community assembly mechanisms shape soil bacterial β diversity patterns along a latitudinal gradient. Nat. Commun. 2020, 11, 5428. [Google Scholar] [CrossRef] [PubMed]
  12. He, S.W.; Wang, B.X.; Chen, K.; Li, N.; Soininen, J. Species–environment sorting explains latitudinal patterns in spatiotemporal β-diversity for freshwater macroinvertebrates. Ecography 2024, 2024, e07111. [Google Scholar] [CrossRef]
  13. Zhang, Y.L.; Liu, J.W.; Song, D.R.; Yao, P.; Zhu, S.D.; Zhou, Y.; Jin, J.; Zhang, X.H. Stochasticity-driven weekly fluctuations distinguished the temporal pattern of particle-associated microorganisms from its free-living counterparts in temperate coastal seawater. Water Res. 2024, 248, 120849. [Google Scholar] [CrossRef]
  14. Mori, A.S.; Isbell, F.; Seidl, R. β-Diversity, Community Assembly, and Ecosystem Functioning. Trends Ecol. Evol. 2018, 33, 549–564. [Google Scholar] [CrossRef] [PubMed]
  15. Leprieur, F.; Tedesco, P.A.; Hugueny, B.; Beauchard, O.; Dürr, H.H.; Brosse, S.; Oberdorff, T. Partitioning global patterns of freshwater fish beta diversity reveals contrasting signatures of past climate changes. Ecol. Lett. 2011, 14, 325–334. [Google Scholar] [CrossRef]
  16. Wang, J.; Ding, C.Z.; Tao, J.; Jiang, X.M.; Heino, J.; Ding, L.Y.; Su, W.; Chen, M.L.; Zhang, K.; He, D.M. Damming affects riverine macroinvertebrate metacommunity dynamics: Insights from taxonomic and functional beta diversity. Sci. Total Environ. 2021, 763, 142945. [Google Scholar] [CrossRef]
  17. Legendre, P. Comparison of permutation methods for the partial correlation and partial mantel tests. J. Stat. Comput. Sim. 2000, 67, 37–73. [Google Scholar] [CrossRef]
  18. Mokany, K.; Ware, C.; Woolley, S.N.C.; Ferrier, S.; Fitzpatrick, M.C. A working guide to harnessing generalized dissimilarity modelling for biodiversity analysis and conservation assessment. Global Ecol. Biogeogr. 2022, 31, 802–821. [Google Scholar] [CrossRef]
  19. Wan, X.H.; Fang, Y.; Jiang, Y.M.; Lu, X.Q.; Zhu, L.; Feng, J.F. Temperature and nutrients alter the relative importance of stochastic and deterministic processes in the coastal macroinvertebrates biodiversity assembly on long-time scales. Ecol. Evol. 2024, 14, e11062. [Google Scholar] [CrossRef]
  20. Ferrier, S.; Manion, G.; Elith, J.; Richardson, K. Using generalized dissimilarity modelling to analyse and predict patterns of beta diversity in regional biodiversity assessment. Divers. Distrib. 2007, 13, 252–264. [Google Scholar] [CrossRef]
  21. Lv, Y.Y.; Liu, G.H.; Wang, Y.C.; Wang, Y.X.; Jin, X.W.; Chen, H.; Wu, N.C. Near-natural streams: Spatial factors are key in shaping multiple facets of zooplankton alpha and beta diversity. Environ. Res. 2024, 255, 119174. [Google Scholar] [CrossRef] [PubMed]
  22. Lai, J.S.; Zou, Y.; Zhang, J.L.; Peres-Neto, P.R. Generalizing hierarchical and variation partitioning in multiple regression and canonical analyses using the rdacca.hp R package. Methods Ecol. Evol. 2022, 13, 782–788. [Google Scholar] [CrossRef]
  23. Wu, Y.H.; Yang, Z.Y.; Chen, S.R.; Chen, L.Y.; Sui, M.Z.; Zhang, G.Q.; Liu, Q.F.; Chen, D.M.; He, Y.J.; Zang, L.P. Drivers of β-diversity and its component-dependence along the natural restoration in an extremely heterogeneous forest ecosystem. Catena 2024, 243, 108224. [Google Scholar] [CrossRef]
  24. Nie, R.; Xu, X.M.; Xu, P.J.; Zhuge, Y.S.; Zheng, T.; Yu, X.; Yao, R.; Tan, H.W.; Li, G.Q.; Zhao, X.H.; et al. Taxonomic and functional responses of benthic macroinvertebrates to wastewater effluents in the receiving river of ecologically vulnerable karst areas in Southwest China. Environ. Res. 2025, 278, 121666. [Google Scholar] [CrossRef] [PubMed]
  25. Fahy, J.C.; Demierre, E.; Oertli, B. Long-term monitoring of water temperature and macroinvertebrates highlights climate change threat to alpine ponds in protected areas. Biol. Conserv. 2024, 290, 110461. [Google Scholar] [CrossRef]
  26. Liu, Z.Y.; Heino, J.; Soininen, J.; Zhou, T.T.; Wang, W.M.; Cui, Y.D.; Chen, Y.S.; Li, Z.F.; Zhang, J.Q.; Xie, Z.C. Different responses of incidence-weighted and abundance-weighted multiple facets of macroinvertebrate beta diversity to urbanization in a subtropical river system. Ecol. Indic. 2022, 143, 109357. [Google Scholar] [CrossRef]
  27. Zhao, X.; Ma, Y.; Xie, H.Y.; Du, C.; Zhan, A.B.; Xu, J.; Giesy, J.P.; Wu, F.C.; Jin, X.W. Spatial distribution of benthic taxonomic and functional diversity in the Yellow River Basin: From ecological processes to associated determinant factors. Environ. Int. 2024, 188, 108745. [Google Scholar] [CrossRef]
  28. Li, Z.F.; Chen, X.; Jiang, X.M.; Tonkin, J.D.; Xie, Z.C.; Heino, J. Distance decay of benthic macroinvertebrate communities in a mountain river network: Do dispersal routes and dispersal ability matter? Sci. Total Environ. 2021, 758, 143630. [Google Scholar] [CrossRef]
  29. Zhang, T.P.; Lei, Q.L.; Liang, X.; Lindsey, S.; Luo, J.F.; Pei, W.; Du, X.Z.; Wu, S.X.; An, M.Y.; Qiu, W.W.; et al. Optimization of the N footprint model and analysis of nitrogen pollution in irrigation areas: A case study of Ningxia Hui Autonomous Region, China. J. Environ. Manag. 2023, 340, 118002. [Google Scholar] [CrossRef]
  30. Zhao, Y.; Chen, Y.P. Coming ecological risks of organochlorine pesticides and novel brominated flame retardants in the Yellow River Basin. Sci. Total Environ. 2023, 857, 159296. [Google Scholar] [CrossRef]
  31. Li, R.; Shi, Y.; Feng, C.C.; Guo, L. The spatial relationship between ecosystem service scarcity value and urbanization from the perspective of heterogeneity in typical arid and semiarid regions of China. Ecol. Indic. 2021, 132, 108299. [Google Scholar] [CrossRef]
  32. Wang, D.; Hao, H.G.; Liu, H.; Sun, L.H.; Li, Y.Y. Spatial-temporal changes of landscape and habitat quality in typical ecologically fragile areas of western China over the past 40 years: A case study of the Ningxia Hui Autonomous Region. Ecol. Evol. 2024, 14, e10847. [Google Scholar] [CrossRef]
  33. Tan, C.P.; Yang, J.P.; Li, M. Temporal-Spatial Variation of Drought Indicated by SPI and SPEI in Ningxia Hui Autonomous Region, China. Atmosphere 2015, 6, 1399–1421. [Google Scholar] [CrossRef]
  34. Barbour, M.T.; Gerritsen, J.; Snyder, B.D.; Stribling, J.B. Rapid Bioassessment Protocols for Use in Streams and Wadable Rivers: Periphyton, Benthic Macroinvertebrates and Fish, 2nd ed.; EPA 841-B-99-002; US Environmental Protection Agency: Washington, DC, USA, 1999. [Google Scholar]
  35. Hamada, N.; Thorp, J.H.; Christopher Rogers, D. Thorp and Covich’s Freshwater Invertebrates, 4th ed.; Volume III: Keys to Neotropical Hexapoda; Academic Press: Cambridge, MA, USA, 2018. [Google Scholar]
  36. Qiu, W.G.; Wang, J.C.; Zhang, Z. Map of Benthic Fauna Monitoring in Liaohe River Basin; China Environmental Science Press: Beijing, China, 2014. (In Chinese) [Google Scholar]
  37. Liu, Y.H.; Zhong, Y.F.; Ma, A.L.; Zhao, J.; Zhang, L.P. Cross-resolution national-scale land-cover mapping based on noisy label learning: A case study of China. Int. J. Appl. Earth Obs. 2023, 118, 103265. [Google Scholar] [CrossRef]
  38. Hijmans, R. Geosphere: Spherical Trigonometry. R Package Version 1.5-20. 2024. Available online: https://CRAN.R-project.org/package=geosphere (accessed on 2 July 2024).
  39. Ranjard, L.; Dequiedt, S.; Chemidlin Prévost-Bouré, N.; Thioulouse, J.; Saby, N.P.A.; Lelievre, M.; Maron, P.A.; Morin, F.E.R.; Bispo, A.; Jolivet, C.; et al. Turnover of soil bacterial diversity driven by wide-scale environmental heterogeneity. Nat. Commun. 2013, 4, 1434. [Google Scholar] [CrossRef]
  40. Baselga, A. Separating the two components of abundance-based dissimilarity: Balanced changes in abundance vs. abundance gradients. Methods Ecol. Evol. 2013, 4, 552–557. [Google Scholar] [CrossRef]
  41. Baselga, A. Partitioning abundance-based multiple-site dissimilarity into components: Balanced variation in abundance and abundance gradients. Methods Ecol. Evol. 2017, 8, 799–808. [Google Scholar] [CrossRef]
  42. Wang, W.W.; Liu, C.J.; Zhang, F.; Tan, M.L.; Shi, J.C.; Zhang, Z.M.; Duan, P.; Kung, H.-T.; Xin, H.Y. Evaluation of impacts of environmental factors and land use on seasonal surface water quality in arid and humid regions using structural equation models. Ecol. Indic. 2022, 144, 109546. [Google Scholar] [CrossRef]
  43. Song, Y.Z.; Wang, J.F.; Ge, Y.; Xu, C.D. An optimal parameters-based geographical detector model enhances geographic characteristics of explanatory variables for spatial heterogeneity analysis: Cases with different types of spatial data. GISci Remote Sens. 2020, 57, 593–610. [Google Scholar] [CrossRef]
  44. Xu, Y.; Xu, X.R.; Tang, Q. Human activity intensity of land surface: Concept, methods and application in China. J. Geogr. Sci. 2016, 26, 1349–1361. [Google Scholar] [CrossRef]
  45. Pesce, S.F.; Wunderlin, D.A. Use of water quality indices to verify the impact of Cordoba City (Argentina) on Suquia River. Water Res. 2000, 34, 2915–2926. [Google Scholar] [CrossRef]
  46. Sun, W.; Xia, C.Y.; Xu, M.Y.; Guo, J.; Sun, G.P. Application of modified water quality indices as indicators to assess the spatial and temporal trends of water quality in the Dongjiang River. Ecol. Indic. 2016, 66, 306–312. [Google Scholar] [CrossRef]
  47. Wang, J.L.; Fu, Z.S.; Qiao, H.X.; Liu, F.X. Assessment of eutrophication and water quality in the estuarine area of Lake Wuli, Lake Taihu, China. Sci. Total Environ. 2019, 650, 1392–1402. [Google Scholar] [CrossRef]
  48. Wu, Z.S.; Wang, X.L.; Chen, Y.W.; Cai, Y.J.; Deng, J.C. Assessing river water quality using water quality index in Lake Taihu Basin, China. Sci. Total Environ. 2018, 612, 914–922. [Google Scholar] [CrossRef] [PubMed]
  49. Tian, Y.L.; Jiang, Y.; Liu, Q.; Dong, M.; Xu, D.; Liu, Y.; Xu, X. Using a water quality index to assess the water quality of the upper and middle streams of the Luanhe River, northern China. Sci. Total Environ. 2019, 667, 142–151. [Google Scholar] [CrossRef] [PubMed]
  50. Chen, X.T.; Wang, Z.T. Distribution pattern and composition difference of urban spontaneous plants of multi-mountainous city. Glob. Ecol. Conserv. 2025, 59, e03564. [Google Scholar] [CrossRef]
  51. Ning, D.L.; Deng, Y.; Tiedje, J.M.; Zhou, J.Z. A general framework for quantitatively assessing ecological stochasticity. Proc. Natl. Acad. Sci. USA 2019, 116, 16892–16898. [Google Scholar] [CrossRef] [PubMed]
  52. Li, C.; Chen, H.Q.; Gao, P.; Huang, X.H.; Zhu, Y.X.; Xu, M.; Yuan, Q.; Gao, Y.; Shen, X.X. Distribution and drivers of antibiotic resistance genes in brackish water aquaculture sediment. Sci. Total Environ. 2023, 860, 160475. [Google Scholar] [CrossRef]
  53. Hjalmarsson, A.E.; Graf, W.; Jähnig, S.C.; Vitecek, S.; Pauls, S.U. Molecular association and morphological characterisation of Himalopsyche larval types (Trichoptera, Rhyacophilidae). ZooKeys 2018, 773, 79–108. [Google Scholar] [CrossRef]
  54. Ju, H.R.; Zhang, Z.X.; Zuo, L.J.; Wang, J.F.; Zhang, S.R.; Wang, X.; Zhao, X.L. Driving forces and their interactions of built-up land expansion based on the geographical detector—A case study of Beijing, China. Int. J. Geogr. Infor. Sci. 2016, 30, 2188–2207. [Google Scholar] [CrossRef]
  55. Gao, J.; Deng, G.Y.; Jiang, H.B.; Ma, Q.Y.; Wen, Y.; He, C.G.; Guo, Y.; Cao, Y.Y. Water quality management of micro swamp wetland based on the “source-transfer-sink” theory: A case study of Momoge Swamp Wetland in Songnen Plain, China. J. Clean Prod. 2024, 446, 141450. [Google Scholar] [CrossRef]
  56. Zhang, J.Y.; Wang, M.; Ren, K.; Yan, K.; Liang, Y.G.; Yuan, H.L.; Yang, L.; Ren, Y.X. The relationship between mountain wetland health and water quality: A case study of the upper Hanjiang River Basin, China. J. Environ. Manag. 2023, 346, 118998. [Google Scholar] [CrossRef]
  57. Yao, X.C.; Zeng, C.F.; Duan, X.J.; Wang, Y.Z. Effects of land use patterns on seasonal water quality in Chinese basins at multiple temporal and spatial scales. Ecol. Indic. 2024, 166, 112423. [Google Scholar] [CrossRef]
  58. Zhu, J.Y.; Peng, S.Y.; Shen, X.J.; Lin, Z.Q.; Gong, L.P.; Zhang, R.; Huang, B.M. Multiple scale impacts of land use intensity on water quality in the Chishui river source area. Ecol. Indic. 2024, 166, 112396. [Google Scholar] [CrossRef]
  59. Wang, W.W.; Zhang, F.; Zhao, Q.; Liu, C.J.; Jim, C.Y.; Johnson, V.C.; Tan, M.L. Determining the main contributing factors to nutrient concentration in rivers in arid northwest China using partial least squares structural equation modeling. J. Environ. Manag. 2023, 343, 118249. [Google Scholar] [CrossRef] [PubMed]
  60. Xu, Q.Y.; Wang, P.; Shu, W.; Ding, M.J.; Zhang, H. Influence of landscape structures on river water quality at multiple spatial scales: A case study of the Yuan river watershed, China. Ecol. Indic. 2021, 121, 107226. [Google Scholar] [CrossRef]
  61. Wang, W.Y.; Yang, P.; Xia, J.; Huang, H.Q.; Li, J. Impact of land use on water quality in buffer zones at different scales in the Poyang Lake, middle reaches of the Yangtze River basin. Sci. Total Environ. 2023, 896, 165161. [Google Scholar] [CrossRef]
  62. Qian, S.S.; King, R.S.; Richardson, C.J. Two statistical methods for the detection of environmental thresholds. Ecol. Model 2003, 166, 87–97. [Google Scholar] [CrossRef]
  63. Wang, H.; Xiong, Q.Q.; Feng, Q.Y.; Xiao, S.Z.; Mu, D.J.; Sun, X.X.; Wang, S.J. Prediction and impact of Location-Weighted landscape Index on water quality in a typical karst region in southwest China: A case study of the Huanghou basin. Ecol. Indic. 2024, 165, 112186. [Google Scholar] [CrossRef]
  64. Xiao, H.B.; Su, R.L.; Luo, Y.; Jiang, Y.B.; Wang, Y.; Hu, R.G.; Lin, S. Effects of land cover patterns on pond water nitrogen and phosphorus concentrations in a small agricultural watershed in Central China. Catena 2024, 237, 107800. [Google Scholar] [CrossRef]
  65. Wu, H.W.; Wu, F.; Li, Z.H.; Gao, X.; Wu, X.H.; Bao, G.J. Considering scale effects in water quality analysis to enhance the precision of influencing factor response analysis. Ecol. Indic. 2024, 163, 112091. [Google Scholar] [CrossRef]
  66. Xu, Y.T.; Li, P.; Ma, F.M.; Liu, X.H.; Zhang, N.C.; Pan, J.J.; Meng, Y.X. Watershed landscape characteristics and connectivity drive river water quality under seasonal dynamics. J. Clean Prod. 2024, 473, 143533. [Google Scholar] [CrossRef]
  67. Wang, J.F.; Hu, Y. Environmental health risk detection with GeogDetector. Environ. Modell Softw. 2012, 33, 114–115. [Google Scholar] [CrossRef]
  68. Wang, J.F.; Li, X.H.; Christakos, G.; Liao, Y.L.; Zhang, T.; Gu, X.; Zheng, X.Y. Geographical Detectors-Based Health Risk Assessment and its Application in the Neural Tube Defects Study of the Heshun Region, China. Int. J. Geogr. Inf. Sci. 2010, 24, 107–127. [Google Scholar] [CrossRef]
  69. Wang, G.J.; Peng, W.F.; Zhang, L.D.; Zhang, J. Quantifying the impacts of natural and human factors on changes in NPP using an optimal parameters-based geographical detector. Ecol. Indic. 2023, 155, 111018. [Google Scholar] [CrossRef]
  70. Huang, L.; Chen, X.H.; Yuan, Z.; Ye, C.X.; Liang, Y.S. Impact of Landscape Patterns on Water Quality in Urbanized Rivers at Characteristic Scale: A Case of Pearl River Delta, China. Environ. Manag. 2024, 74, 715–728. [Google Scholar] [CrossRef] [PubMed]
  71. Shi, P.; Zhang, Y.; Li, Z.B.; Li, P.; Xu, G.C. Influence of land use and land cover patterns on seasonal water quality at multi-spatial scales. Catena 2017, 151, 182–190. [Google Scholar] [CrossRef]
  72. Mello, K.d.; Valente, R.A.; Randhir, T.O.; Santos, A.C.A.d.; Vettorazzi, C.A. Effects of land use and land cover on water quality of low-order streams in Southeastern Brazil: Watershed versus riparian zone. Catena 2018, 167, 130–138. [Google Scholar] [CrossRef]
  73. Zhou, H.Y.; Rao, K.; Yao, M.J.; Xiong, Y.; Wang, Y.; Yin, Y.H. Effects of land use, meteorology, and hydrology on nutrients, biochemical indexes, and heavy metals in Qingjiang River Basin, China. J. Clean Prod. 2022, 370, 133416. [Google Scholar] [CrossRef]
  74. Wang, J.F.; Zhang, T.L.; Fu, B.J. A measure of spatial stratified heterogeneity. Ecol. Indic. 2016, 67, 250–256. [Google Scholar] [CrossRef]
  75. Locke, K.A. Modelling relationships between land use and water quality using statistical methods: A critical and applied review. J. Environ. Manag. 2024, 362, 121290. [Google Scholar] [CrossRef]
  76. Wang, Y.B.; Junaid, M.; Deng, J.Y.; Tang, Q.P.; Luo, L.; Xie, Z.Y.; Pei, D.S. Effects of land-use patterns on seasonal water quality at multiple spatial scales in the Jialing River, Chongqing, China. Catena 2024, 234, 107646. [Google Scholar] [CrossRef]
  77. Anderson, M.J.; Crist, T.O.; Chase, J.M.; Vellend, M.; Inouye, B.D.; Freestone, A.L.; Sanders, N.J.; Cornell, H.V.; Comita, L.S.; Davies, K.F.; et al. Navigating the multiple meanings of beta diversity: A roadmap for the practicing ecologist. Ecol. Lett. 2011, 14, 19–28. [Google Scholar] [CrossRef]
  78. Chen, J.; Shiyomi, M.; Huang, D.M.; Yu, H.L. Quantitative evaluation of species composition dissimilarity within a community and among communities. Ecol. Res. 2021, 36, 152–160. [Google Scholar] [CrossRef]
  79. Barwell, L.J.; Isaac, N.J.B.; Kunin, W.E. Measuring β-diversity with species abundance data. J. Anim. Ecol. 2015, 84, 1112–1122. [Google Scholar] [CrossRef] [PubMed]
  80. Beck, J.; Holloway, J.D.; Schwanghart, W. Undersampling and the measurement of beta diversity. Methods Ecol. Evol. 2013, 4, 370–382. [Google Scholar] [CrossRef]
  81. Schroeder, P.J.; Jenkins, D.G. How robust are popular beta diversity indices to sampling error? Ecosphere 2018, 9, e02100. [Google Scholar] [CrossRef]
  82. Wang, H.X.; He, X.L.; Yao, Z.L.; Wang, B.; Jiang, Y.T.; Lin, L.X. Acoustic beta indices exhibited a weak correlation with both vocal species composition dissimilarity and environmental factors dissimilarity in a subtropical forest. Ecol. Indic. 2025, 172, 113266. [Google Scholar] [CrossRef]
  83. Delciellos, A.C.; Borges-Júnior, V.N.T.; Cerqueira, R.; Vieira, M.V.; Prevedello, J.A. Non-linear homogenization of small mammal communities following habitat loss in a biodiversity hotspot. Biol. Conserv. 2025, 306, 111144. [Google Scholar] [CrossRef]
  84. Xu, Y.P.; Xiang, Z.L.; Rizo, E.Z.; Naselli-Flores, L.; Han, B.P. Combination of linear and nonlinear multivariate approaches effectively uncover responses of phytoplankton communities to environmental changes at regional scale. J. Environ. Manag. 2022, 305, 114399. [Google Scholar] [CrossRef]
  85. Woolley, S.N.C.; Foster, S.D.; O’Hara, T.D.; Wintle, B.A.; Dunstan, P.K. Characterising uncertainty in generalised dissimilarity models. Methods Ecol. Evol. 2017, 8, 985–995. [Google Scholar] [CrossRef]
  86. Chen, Y.T.; Liu, Z.X.; Régnière, J.; Vasseur, L.; Lin, J.; Huang, S.G.; Ke, F.S.; Chen, S.P.; Li, J.Y.; Huang, J.L.; et al. Large-scale genome-wide study reveals climate adaptive variability in a cosmopolitan pest. Nat. Commun. 2021, 12, 7206. [Google Scholar] [CrossRef] [PubMed]
  87. Li, Z.F.; Wang, J.; Liu, Z.Y.; Meng, X.L.; Heino, J.; Jiang, X.K.; Xiong, X.; Jiang, X.M.; Xie, Z.C. Different responses of taxonomic and functional structures of stream macroinvertebrate communities to local stressors and regional factors in a subtropical biodiversity hotspot. Sci. Total Environ. 2019, 655, 1288–1300. [Google Scholar] [CrossRef] [PubMed]
  88. Chase, J.M. Stochastic community assembly causes higher biodiversity in more productive environments. Science 2010, 328, 1388–1391. [Google Scholar] [CrossRef] [PubMed]
  89. Chase, J.M.; Myers, J.A. Disentangling the importance of ecological niches from stochastic processes across scales. Phil. Trans. R Soc. B 2011, 366, 2351–2363. [Google Scholar] [CrossRef] [PubMed]
  90. He, S.W.; Qin, C.Y.; Soininen, J. A flexible framework to assess patterns and drivers of beta diversity across spatial scales. Ecography 2024, 2024, e06901. [Google Scholar] [CrossRef]
  91. Growns, I. Differences in bioregional classifications among four aquatic biotic groups: Implications for conservation reserve design and monitoring programs. J. Environ. Manag. 2009, 90, 2652–2658. [Google Scholar] [CrossRef]
  92. Dong, R.; Wang, Y.Y.; Lu, C.; Lei, G.C.; Wen, L. The seasonality of macroinvertebrate β diversity along the gradient of hydrological connectivity in a dynamic river-floodplain system. Ecol. Indic. 2021, 121, 107112. [Google Scholar] [CrossRef]
  93. Chen, J.; Gao, Y.Y.; Qian, H.; Jia, H.; Zhang, Q.Y. Insights into water sustainability from a grey water footprint perspective in an irrigated region of the Yellow River Basin. J. Clean Prod. 2021, 316, 128329. [Google Scholar] [CrossRef]
  94. López-Rodríguez, M.J.; Muñoz, C.M.; Ripoll-Martín, E.; Figueroa, J.M.T.d. Effect of shifts in habitats and flow regime associated to water diversion for agriculture on the macroinvertebrate community of a small watershed. Aquat. Ecol. 2019, 53, 483–495. [Google Scholar] [CrossRef]
  95. Li, J.X.; Ma, M.D.; Wang, L.Y.; Jin, Y.J.; Liu, Y.M.; Yin, X.W.; Liu, G.; Song, J.X. Ecological drivers of taxonomic, functional, and phylogenetic beta diversity of macroinvertebrates in Wei River Basin of northwest China. Front. Ecol. Evol. 2024, 12, 1410915. [Google Scholar] [CrossRef]
  96. Pavoine, S.; Marcon, E.; Ricotta, C. ‘Equivalent numbers’ for species, phylogenetic or functional diversity in a nested hierarchy of multiple scales. Methods Ecol. Evol. 2016, 7, 1152–1163. [Google Scholar] [CrossRef]
  97. Martins, A.; Collart, F.; Sim-Sim, M.; Patiño, J. Ecological drivers of taxonomic, functional, and phylogenetic diversity of bryophytes in an oceanic island. Ecol. Evol. 2024, 14, e70023. [Google Scholar] [CrossRef] [PubMed]
  98. Farooq, M.; Liu, S.; Tan, L.; Cai, Q.H.; Chiu, M.-C.; Resh, V.H. Multidimensional aspects of riverine biodiversity can vary in response to nutrient pollution and environmental dynamics across climatic watersheds. Environ. Pollut. 2024, 361, 124775. [Google Scholar] [CrossRef]
  99. Heino, J.; Bini, L.M.; García-Girón, J.; Lansac-Tôha, F.M.; Lindholm, M.; Rolls, R.J. Navigating the spatial and temporal aspects of beta diversity to clarify understanding biodiversity change. Glob. Ecol. Conserv. 2024, 56, e03343. [Google Scholar] [CrossRef]
Figure 1. (a) Geographic position of Ningxia in Northwest China; (b) land use classifications in 2020; (c) spatial distribution of sub-regions and sampling points in Ningxia; Regions (I–III) correspond to YRIA, CAZ, and SMA, respectively; (d) six categories of circular buffer zones; (e) representative photos of some sampling points.
Figure 1. (a) Geographic position of Ningxia in Northwest China; (b) land use classifications in 2020; (c) spatial distribution of sub-regions and sampling points in Ningxia; Regions (I–III) correspond to YRIA, CAZ, and SMA, respectively; (d) six categories of circular buffer zones; (e) representative photos of some sampling points.
Animals 15 02034 g001
Figure 2. (a) Gordius aquaticus; (b) Himalopsyche sp.
Figure 2. (a) Gordius aquaticus; (b) Himalopsyche sp.
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Figure 3. Analysis of macroinvertebrate beta diversity. (a) Overall beta diversity and characterization of its components; (be) ternary plots of beta diversity computed with the incidence-based Sørensen index in April; (fi) ternary plots of beta diversity computed with the incidence-based Bray–Curtis index in April. Note: Each filled circle represents a pair of sampling sites; the grey triangle denotes the overall mean across all site pairs; and the small triangles along each side illustrate how that mean is decomposed into the respective components.
Figure 3. Analysis of macroinvertebrate beta diversity. (a) Overall beta diversity and characterization of its components; (be) ternary plots of beta diversity computed with the incidence-based Sørensen index in April; (fi) ternary plots of beta diversity computed with the incidence-based Bray–Curtis index in April. Note: Each filled circle represents a pair of sampling sites; the grey triangle denotes the overall mean across all site pairs; and the small triangles along each side illustrate how that mean is decomposed into the respective components.
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Figure 4. (a) Average WQI values for April, July, and October; (b) analysis of WQI variations between months and across distinct zones within the same month; (c) results of optimal buffer zone selection derived from the OPGD model; (d) correlation of the ratio of forested land to bare land with the WQI. Note: *, p ≤ 0.05; **, p ≤ 0.01; ***, p ≤ 0.001; ****, p ≤ 0.0001.
Figure 4. (a) Average WQI values for April, July, and October; (b) analysis of WQI variations between months and across distinct zones within the same month; (c) results of optimal buffer zone selection derived from the OPGD model; (d) correlation of the ratio of forested land to bare land with the WQI. Note: *, p ≤ 0.05; **, p ≤ 0.01; ***, p ≤ 0.001; ****, p ≤ 0.0001.
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Figure 5. Total explained variance and relative contribution of predictors to beta diversity of macroinvertebrate community.
Figure 5. Total explained variance and relative contribution of predictors to beta diversity of macroinvertebrate community.
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Figure 6. The ecological assembly mechanisms of macroinvertebrate communities. (ac) NST values; (df) MST values; (gi) the ratio of stochastic to deterministic processes derived from the MST values. MST > 0.5 and MST < 0.5, respectively, indicate the predominance of stochastic and deterministic processes in community assembly.
Figure 6. The ecological assembly mechanisms of macroinvertebrate communities. (ac) NST values; (df) MST values; (gi) the ratio of stochastic to deterministic processes derived from the MST values. MST > 0.5 and MST < 0.5, respectively, indicate the predominance of stochastic and deterministic processes in community assembly.
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MDPI and ACS Style

Yang, Q.; Wei, Z.; Qiu, X.; Zhao, Z. Beta Diversity Patterns and Drivers of Macroinvertebrate Communities in Major Rivers of Ningxia, China. Animals 2025, 15, 2034. https://doi.org/10.3390/ani15142034

AMA Style

Yang Q, Wei Z, Qiu X, Zhao Z. Beta Diversity Patterns and Drivers of Macroinvertebrate Communities in Major Rivers of Ningxia, China. Animals. 2025; 15(14):2034. https://doi.org/10.3390/ani15142034

Chicago/Turabian Style

Yang, Qiangqiang, Zeyu Wei, Xiaocong Qiu, and Zengfeng Zhao. 2025. "Beta Diversity Patterns and Drivers of Macroinvertebrate Communities in Major Rivers of Ningxia, China" Animals 15, no. 14: 2034. https://doi.org/10.3390/ani15142034

APA Style

Yang, Q., Wei, Z., Qiu, X., & Zhao, Z. (2025). Beta Diversity Patterns and Drivers of Macroinvertebrate Communities in Major Rivers of Ningxia, China. Animals, 15(14), 2034. https://doi.org/10.3390/ani15142034

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