Benthic diatom assemblages can sensitively respond to aquatic environmental changes. However, it is still ambiguous whether benthic diatom assemblages can well indicate the environmental status in an urban river with highly heterogeneous habitats. This study investigated the environmental heterogeneity of an urban river and explored the response of benthic diatom assemblages to environmental changes. First, the urban river showed significant spatio-temporal heterogeneity in both physical and chemical characteristics. Higher concentrations of total nitrogen and CODMn indicated eutrophic and organic pollution conditions in the river. In addition, benthic diatom assemblages also implied the habitat heterogeneity of the urban river. Dominant diatoms, including Nitzschia palea, Melosira varians, Cyclotella meneghiniana, and Achnanthidium minutissimum, are pollution-tolerant species, further confirming the eutrophic and organic status. Then, the interaction between environmental heterogeneity and benthic diatom assemblages was analyzed by redundancy analysis and Mantel tests. Results suggested that environmental variables, such as conductivity, total nitrogen, total phosphorus, and chlorophyll a, significantly affected the composition of benthic diatom assemblages in the urban river. These findings demonstrated that environmental heterogeneity shapes the benthic diatom assemblages of the urban river, and benthic diatoms can be good indicators of environmental status for urban river monitoring and assessment.

  • The CaoE River is an urban river with highly heterogeneous habitats.

  • Benthic diatom assemblages indicate environmental heterogeneity.

  • Benthic diatom assemblages can be good indicators of the urban river environment.

River systems play a crucial role in supporting human activities, including urban water supply, flood mitigation, and disposal of wastewater (Findlay & Taylor 2006). The health and stability of river ecosystems are essential for the sustainable development of urban areas. However, rapid economic development and continuous growth of urbanization are profoundly impacting the ecological status of rivers, especially in plain river network regions (Ren et al. 2022).

Benthic diatoms play a fundamental ecological role, significantly supporting primary productivity and nutrient cycles in river ecosystems (Masouras et al. 2021). Their rapid reproduction makes them more sensitive to environmental changes than other biotic groups (Seckbach & Kociolek 2011). Due to their distinctive morphological and ecological characteristics, benthic diatoms are considered one of the best bioindicators of environmental changes. Moreover, changes in benthic diatom assemblages can impact entire river ecosystems (Stubbington et al. 2017). Consequently, there is increasing attention on exploring the interaction between benthic diatom assemblages and environmental factors.

Environmental filtering is considered a major mechanism for structuring benthic diatom assemblages (Wu et al. 2021). Environmental factors determine community composition directly by affecting survival and indirectly by shaping competition (Cadotte & Tucker 2017). The interaction between benthic diatom assemblages and environmental factors has been extensively studied in various aquatic ecosystems, including lakes (Rivera et al. 2018), rivers (Jakovljević et al. 2016), reservoirs (Yang et al. 2023), and estuaries (Nunes et al. 2022). In rivers, benthic diatoms are particularly valuable as biological indicators for water monitoring (Masouras et al. 2021). Numerous studies have focused on understanding how benthic diatom assemblages respond to environmental variables, such as nutrients (Schneider et al. 2013), acidity (Andrén & Jarlman 2008), and hydrological alterations (Falasco et al. 2021). Despite extensive research on benthic diatoms in different river types, it remains unclear how environmental heterogeneity shapes the distribution of benthic diatom assemblages in urban rivers with highly heterogeneous habitats.

In this study, the succession of benthic diatoms during the flood and dry seasons was evaluated along the CaoE River in the urban plain river network of East China. Environmental factors were simultaneously measured within the benthic diatom habitats. The relationship between benthic diatom assemblages and environmental heterogeneity was further analyzed using redundancy analysis (RDA) and the Mantel test. Overall, the results enhance the understanding of the indicative role of benthic diatoms in the environmental assessment of urban rivers.

Study area

The CaoE River is located in Shaoxing County, Zhejiang Province, China. It is a main tributary of the Qiantang River, with a total length of 197.2 km. Since 2008, a dam has been constructed at the estuary of the CaoE River. In this study, 12 sampling sites have been distributed along the mainstream and tributaries (Figure 1(a)). Sampling sites S1–S6 are located along the mainstream, while S7–S12 are positioned along four tributaries. Various habitats can be observed along the CaoE River. Upstream sites (S7–S12) exhibit riffle characteristics with high velocity and low depth (Figure 1(b)). Middle stream sites (S4–S6) are characterized by a pool-riffle configuration with medium velocity and depth (Figure 1(c)). Downstream sites (S1–S3) are predominantly pool habitats with low velocity and high depth (Figure 1(d)) (Rosenfeld et al. 2011). All samples were collected during the flood season (May 2021) and the dry season (November 2020).
Figure 1

Profiling of sampling area. (a) Distribution of sampling sites in the CaoE River. (b)–(d) Habitat pictures of upstream, midstream, and downstream. (e) Map of Zhejiang Province. The red dashed line indicates the riverway and the black arrow indicates the flow direction.

Figure 1

Profiling of sampling area. (a) Distribution of sampling sites in the CaoE River. (b)–(d) Habitat pictures of upstream, midstream, and downstream. (e) Map of Zhejiang Province. The red dashed line indicates the riverway and the black arrow indicates the flow direction.

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Measurements of physicochemical variables

Physical parameters, including water temperature, pH, conductivity, and dissolved oxygen, were measured in situ using a portable multi-parameter water analyzer (Leici DZB-712, China). Surface water samples were collected for the analysis of chemical variables. The concentration of total nitrogen was determined by employing alkaline potassium persulfate digestion-UV spectrophotometry (Shimadzu UV-2600, Japan) (Ren et al. 2015). The concentration of total phosphorus was measured using a colorimetric molybdenum blue assay (Cao et al. 2016). The potassium permanganate index (CODMn) was quantified using a titration method by acid digestion with potassium permanganate and oxalic acid (Liu et al. 2021). To measure the chlorophyll a content, 500 mL of water was filtered through Whatman GF/C glass fiber filters, followed by extraction using 90% acetone. Four wavelengths (630, 645, 663, 750 nm) of acetone solution were recorded by a spectrophotometer (Shimadzu UV-2600, Japan). Chlorophyll a content was calculated according to Zhou et al. (2016).

Diatom collection and identification

Benthic diatoms on cobbles were collected for identification and enumeration following the methods of Kelly et al. (1998) and Wang et al. (2022). In brief, five submerged cobbles were picked randomly along the bank (50 m) to minimize random errors in diatom collection. Biofilms on cobbles were carefully scrapped using a sterile toothbrush. The cobbles were further rinsed with distilled water. All samples were thoroughly mixed in a stainless steel basin and preserved using 4% formaldehyde. Diatom collection at all sample sites followed the same procedure. Organic matter was digested using 35% hydrochloric acid and 30% hydrogen peroxide at 95°C for 4 h. The digestion solution was centrifuged to remove the supernatant, and the sediment was rinsed several times with distilled water. Cleaned diatoms were stored in absolute ethyl alcohol (Yang et al. 2023). For the identification of benthic diatoms, a light microscope with 1,000× magnification (Olympus BX-53, Japan) was used. A minimum of 350 frustules per sample was identified as the lowest possible taxonomic level following Lange-Bertalot et al. (2017), Krammer (1986, 1988, 1991), and Krammer & Lange-Bertalot (1991). Taxonomic names were verified using AlgaeBase (Guiry & Guiry 2020). The top 10 genera were selected for statistical analyses.

Statistical analysis

Alpha diversity of benthic diatom communities was calculated at the species level using PC-ORD 5 software. The multi-response permutation procedure (MRPP), analysis of similarities (ANOSIM), and Mantel test were conducted using R 4.0.2 (R Core Team). MRPP is a class of multivariate permutation tests of group difference (Cai 2006). Observed delta is the weighted mean within-group distance from actual data; expected delta is the weighted mean distance from permutations; A value is the chance corrected within-group agreement; p values are the significance of delta (Bakker 2023a). ANOSIM is a non-parametric technique based on ranks (Bakker 2023b), which was conducted to evaluate the temporal differences in benthic diatom communities. A Mantel test was performed to investigate the relationships between benthic diatom communities, environmental variables, and productivity. The Euclidean distance method was used for the calculation of environmental variables and productivity distances, and the Bray–Curtis distance method was used for the calculation of dominant genera and biodiversity distances. RDA was performed to analyze the relationship between diatom communities and environmental variables by using Canoco 4.5 software.

Spatio-temporal heterogeneity of environmental variables

The CaoE River is a distinctive water body located within the plain river network of East China. Its estuary connects to the Qiantang River near the East China Sea. Hence, tides significantly influence the aquatic ecosystem of the CaoE River, particularly in its middle and lower reaches. However, since the operation of a dam at the river's estuary in 2008, the river's characteristics have been substantially altered, resulting in a blend of river and reservoir features (Wu et al. 2022). Typically, the upstream section exhibited river characteristics with high water velocity and strong exchange capacity, while the downstream resembled a reservoir with low water velocity and weak exchange capacity (Zhang et al. 2006). Furthermore, water levels fluctuate seasonally to accommodate the river's functions (Li et al. 2013), such as drainage, irrigation, and shipping. These hydrodynamic alterations result in significant spatio-temporal heterogeneity in the environmental characteristics of the CaoE River. The hypothesis was confirmed by cluster analysis of environmental variables (Figure 2), which indicated the existence of spatio-temporal heterogeneity in the CaoE River.
Figure 2

Cluster analysis of environmental variables during the flood and dry seasons.

Figure 2

Cluster analysis of environmental variables during the flood and dry seasons.

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Regarding temporal heterogeneity (Figure 3(a)), statistical analyses revealed significant differences in water temperature, dissolved oxygen, total nitrogen, and CODMn between the flood and dry seasons (p < 0.001). Specifically, the average total nitrogen was significantly higher in the dry season at 3.6 mg/L, compared to 0.9 mg/L during the flood season. According to the environmental quality standards for surface water (GB3838-2002, China), this suggested that the water quality of the CaoE River was below Class V during the flood season and reached Class III in the dry season. Similar phenomena have been observed in other studies, where nutrient concentrations are higher in the dry season compared to the flood season (Woldeab et al. 2018). This is attributed to the increased concentration effect resulting from reduced water volume during the dry season. Conversely, the average CODMn exhibited an inverse trend, with levels of 5.5 mg/L in the flood season (water quality Class III) and 3.2 mg/L in the dry season (water quality Class II). The higher CODMn during the flood season indicated a greater degree of organic pollution. This finding is consistent with observations from the Dagujia River, where high CODMn concentrations are primarily associated with increased flow during the flood season (Yi et al. 2022).
Figure 3

Temporal and spatial changes in environmental variables. (a) Comparison of environmental variables between flood and dry seasons. (b) Comparison of environmental variables between different habitats in the flood season. (c) Comparison of environmental variables between different habitats in the dry season. Significant levels are indicated by asterisks (*p < 0.05, **p < 0.01, ***p < 0.001).

Figure 3

Temporal and spatial changes in environmental variables. (a) Comparison of environmental variables between flood and dry seasons. (b) Comparison of environmental variables between different habitats in the flood season. (c) Comparison of environmental variables between different habitats in the dry season. Significant levels are indicated by asterisks (*p < 0.05, **p < 0.01, ***p < 0.001).

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In terms of spatial heterogeneity (Figure 3(b) and 3(c)), significant differences were observed in conductivity in both the flood and dry seasons. A decreasing gradient was observed from downstream (pool habitat) to upstream (riffle habitat). This gradient is typical in coastal freshwater ecosystems with semi-tidal movements. According to Aslan et al. (2018), the flux and reflux of tides can affect water levels of coastal freshwater ecosystems, leading to conductivity increases of up to 4.6 times during flood tides. However, the construction of a dam in the CaoE River has blocked tidal effects, resulting in reduced estuarine conductivity and stabilizing the spatial gradient of conductivity.

In addition, chlorophyll a content showed a decreasing gradient from downstream (pool habitat) to upstream (riffle habitat). Given the uniformity of nutrient levels along the CaoE River (Figure 3(b) and 3(c)), it was suggested that nutrients were not the primary factor driving the high chlorophyll a content. Instead, the limited exchange capacity of the downstream water body, which promotes phytoplankton growth (Wu et al. 2022), appears to play the predominant role in the formation of higher chlorophyll a contents.

Benthic diatom assemblages and its role in environmental indicator

Benthic diatom assemblages can serve as good indicators of habitat environments. Especially, the dominant species can reflect the ecological condition of a water body due to their rapid adaption to environmental changes. In this study, a total of 189 diatom taxa, belonging to 53 genera (Supplement 1), were identified in the CaoE River during the flood and dry seasons. The analyses of diatom community structure and biodiversity are presented in Figures 4 and 5, and Table 1.
Table 1

MRPP and ANOSIM analyses of benthic diatom assemblages during the flood and dry seasons

MRPP
ANOSIM
GroupObserved deltaExpected deltaA valuePRP
Flood vs. Dry 0.703 0.831 0.154 0.001 0.981 0.001 
MRPP
ANOSIM
GroupObserved deltaExpected deltaA valuePRP
Flood vs. Dry 0.703 0.831 0.154 0.001 0.981 0.001 
Figure 4

Temporal differences of benthic diatom assemblages during the flood and dry seasons. (a) and (b) Histogram visualization of the top 10 diatom genera during the flood and dry seasons. (c)–(f) Alpha diversity indices for benthic diatom assemblages during the flood and dry seasons. Significant levels are indicated by asterisks (*p < 0.05, **p < 0.01, ***p < 0.001).

Figure 4

Temporal differences of benthic diatom assemblages during the flood and dry seasons. (a) and (b) Histogram visualization of the top 10 diatom genera during the flood and dry seasons. (c)–(f) Alpha diversity indices for benthic diatom assemblages during the flood and dry seasons. Significant levels are indicated by asterisks (*p < 0.05, **p < 0.01, ***p < 0.001).

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Figure 5

Spatial differences of benthic diatom assemblages during the flood and dry seasons. (a) Histogram visualization of the top 10 diatom genera during the flood season. (b) Histogram visualization of the top 10 diatom genera during the dry season. (c)–(f) Alpha diversity indices for benthic diatom assemblages during the flood season. (g)–(j) Alpha diversity indices for benthic diatom assemblages during the dry season. Significant levels are indicated by asterisks (*p < 0.05, **p < 0.01, ***p < 0.001).

Figure 5

Spatial differences of benthic diatom assemblages during the flood and dry seasons. (a) Histogram visualization of the top 10 diatom genera during the flood season. (b) Histogram visualization of the top 10 diatom genera during the dry season. (c)–(f) Alpha diversity indices for benthic diatom assemblages during the flood season. (g)–(j) Alpha diversity indices for benthic diatom assemblages during the dry season. Significant levels are indicated by asterisks (*p < 0.05, **p < 0.01, ***p < 0.001).

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To assess the temporal similarity of diatom composition, MRPP and ANOSIM analyses were performed. The results showed a significant dissimilarity between the flood and dry seasons (MRPP: A value = 0.154, P = 0.001; ANOSIM: R = 0.981, P = 0.001) (Table 1). Significant differences were observed in species richness and Pielou's index rather than Shannon Wiener's index and Simpson's index (Figure 4(c)–4(f)). In the flood season (Figure 4(a)), dominant genera (defined as those with a relative abundance ≥10%) were Nitzschia (28.7%), Navicula (21.0%), and Melosira (14.0%). Dominant species (defined as those with a relative abundance ≥5%) included Nitzschia palea (24.1%), Melosira varians (14.0%), Cyclotella meneghiniana (8.9%), and Navicula rostellata (5.6%). Among these, N. palea, M. varians, and C. meneghiniana belong to pollution-tolerant species. Nitzschia palea is commonly found in α-meso to polysaprobic water (Beauger et al. 2020), while M. varians and C. meneghiniana exhibit high resistance to organic pollution (Szczepocka & Szulc 2009; Fontana et al. 2014). These findings are consistent with the evaluated CODMn levels observed during the flood season (Figure 3(a)).

In the dry season, changes in the composition of benthic diatom assemblages reflected changes in the habitat environment (Figure 4(b)). Dominant genera were Melosira (16.5%), Nitzschia (15.5%), and Achnanthidium (13.5%). Dominant species were M. varians (16.5%), Achnanthidium minutissimum (10.1%), N. palea (9.7%), C. meneghiniana (8.1%), and Cymbella turgidula (5.6%). Among these, A. minutissimum is considered an indicator of anthropogenic pressure, particularly associated with high nutrient levels (Zelnik & Sušin 2020). This change may be attributed to the increased total nitrogen during the dry season.

The spatial heterogeneity of benthic diatom assemblages is further shown in Figure 5. According to habitat classification (Figure 1(b)–1(c)), distinct differences were observed among benthic diatom assemblages in pool, pool-riffle, and riffle habitats (Figure 5(a) and 5(b)). In the flood season, Pielou's index, Shannon Wiener index, and Simpson's index were significantly lower in pool-riffle habitat compared to other habitats (Figure 5(c)–5(f)). However, no significant differences were observed among different habitats during the dry season (Figure 5(g)–5(j)). To further explore the relationships between habitats and benthic diatom assemblages, cluster analyses of sampling sites were performed (Figure 6). Three distinct clusters were identified in both the flood and dry seasons. The first group included the sampling sites in the lower reaches (S1–S2), characterized as pool habitat. Dominant genera in this group were Cyclotella, Nitzschia, and Navicula during the flood season, and Cyclotella, Cymbella, and Aulacoseira during the dry season. The second group represented the pool-riffle habitat, consisting of sites S3 and S5 during the flood season and sites S3 and S4 during the dry season. Dominant genera included Navicula, Nitzschia, and Cyclotella in the flood season, and Nitzschia, Bacillaria, and Navicula in the dry season. The third group was riffle habitat, mainly comprising the sites located in the tributaries. Dominant genera were Navicula, Nitzschia, and Melosira in the flood season, and Melosira, Achnanthidium, and Nitzschia in the dry season. As demonstrated in studies of streams (Bere et al. 2016), the composition of benthic diatom assemblages results from a comprehensive interplay of environmental factors. Different diatom species respond differently to nutrient enrichment and organic pollution due to varying tolerances, as well as interactions with factors such as conductivity and velocity (Bere et al. 2016). Therefore, the spatial dissimilarity in the benthic diatom assemblages implied habitat heterogeneity in the CaoE River. Vice versa, benthic diatom assemblages serve as effective indicators of habitat heterogeneity.
Figure 6

Cluster analyses of the top 10 diatom genera during the flood (a) and dry (b) seasons.

Figure 6

Cluster analyses of the top 10 diatom genera during the flood (a) and dry (b) seasons.

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Correlations between environmental variables and benthic diatoms

Environmental heterogeneity plays a key role in shaping benthic diatom assemblages (Yang et al. 2023). Both physical and chemical factors affect the succession of benthic diatom assemblages. To elucidate the relationship between benthic diatom assemblages and environmental variables, Mantel's test was performed (Figure 7).
Figure 7

Relationships between environmental factors and benthic diatom assemblages. (a) Flood season. (b) Dry season. Pairwise comparisons of environmental variables are shown with a color gradient denoting Spearman's correlation coefficients. The relationship between benthic diatom assemblages and environmental variables was analyzed by Mantel's test. Edge width corresponds to Mantel's r values and edge color denotes the statistical significance.

Figure 7

Relationships between environmental factors and benthic diatom assemblages. (a) Flood season. (b) Dry season. Pairwise comparisons of environmental variables are shown with a color gradient denoting Spearman's correlation coefficients. The relationship between benthic diatom assemblages and environmental variables was analyzed by Mantel's test. Edge width corresponds to Mantel's r values and edge color denotes the statistical significance.

Close modal
During the flood season, significant correlations (p < 0.05) were found between conductivity and total nitrogen with dominant genera of benthic diatoms. The RDA in Figure 8(a) indicated that conductivity explained 16.6% of the total variance, while total nitrogen explained 1.4% of the total variance. Conductivity exhibited a positive correlation with total nitrogen, and both parameters showed positive correlations with genera such as Navicula, Cyclotella, and Nitzschia. Spearman's correlation analysis further indicated the statistical significance of these relationships (Figure 8(c)). Conductivity showed a significant positive relationship with genera such as Navicula, Cyclotella, Craticula, and Luticola, while total nitrogen displayed a significant positive relationship with Nitzschia and Navicula.
Figure 8

Relationship between environmental variables and dominant diatoms in the genus level. (a) and (b) RDA analyses for the flood and dry seasons. (c) and (d) Spearman's correlation for the flood and dry seasons. The gradient color denotes the Spearman's correlation coefficients.

Figure 8

Relationship between environmental variables and dominant diatoms in the genus level. (a) and (b) RDA analyses for the flood and dry seasons. (c) and (d) Spearman's correlation for the flood and dry seasons. The gradient color denotes the Spearman's correlation coefficients.

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In general, conductivity emerged as one of the most important factors in shaping benthic diatom assemblages, consistent with findings from other studies (Stenger-Kovács et al. 2023). It has been reported that conductivity not only affects species composition but also the trait and guild of diatom communities. Elevated conductivity leads to the selection of conductivity-tolerant taxa, such as N. palea and C. meneghiniana (Stenger-Kovács et al. 2020; Tapolczai et al. 2021). Simultaneously, species richness and diversity of benthic diatoms tend to decrease at elevated conductivity in freshwater ecosystems (Perrett et al. 2021). In terms of changes in trait and guild composition, high conductivity tends to push assemblages toward a higher proportion of trait extremes, such as small or large-size categories (Stenger-Kovács et al. 2023). In addition, an increase in conductivity also elevates the proportion of motile diatoms (Stenger-Kovács et al. 2020). On the other hand, total nitrogen significantly explained the variance of benthic diatom assemblages during the flood season. This phenomenon aligns with observations from a study of a tropical river in Brazil (Bere & Tundisi 2011). It was proposed that the succession of benthic diatom assemblages along the gradient of conductivity was driven in part by nutrients.

During the dry season, the combined effects of total nitrogen, total phosphorus, and chlorophyll a provided a good explanation for the total variance. Mantel's test revealed significant correlations between total nitrogen and chlorophyll a with dominant genera of benthic diatoms (p < 0.01), and biodiversity was significantly related to total phosphorus (p < 0.05). RDA analysis (Figure 8(b)) showed that total nitrogen, chlorophyll a, and total phosphorus explained 24.6, 18.7, and 8.1% of the total variance, respectively. Consistent with the flood season, total nitrogen remained a primary factor influencing diatom composition during the dry season. Evaluated nitrogen concentrations may stimulate the growth of benthic diatoms while potentially leading to the extinction of certain taxa (Boulêtreau et al. 2006). In this study, total nitrogen was positively correlated with Nitzschia but negatively correlated with Gomphonema and Cocconeis (Figure 8(d)).

Recent research has highlighted the impact of productivity parameters, such as total phosphorus and chlorophyll a, on benthic diatom assemblages (Yang et al. 2023). Virta et al. (2019) reported a strong relationship between productivity and diatom diversity. Yang et al. (2023) also found that productivity indicators such as total phosphorus and chlorophyll a had a significant positive effect on diatom dissimilarity. In this study, chlorophyll a was positively associated with genera such as Cyclotella, Cymbella, and Aulacoseira, whereas Nitzschia and Navicula showed positive correlations with total phosphorus. Total phosphorus, as a productivity indicator, also showed a significant relationship with the diversity of benthic diatoms (Figure 7(b)). Therefore, benthic diatom assemblages are highly related to environmental variables, making them a reliable and effective tool for monitoring and assessing environmental conditions.

Benthic diatom assemblages can be good indicators of environmental conditions. This study aimed to assess how benthic diatom assemblages respond to environmental variations along the CaoE River in the plain river network of East China. The results revealed temporal heterogeneity in water temperature, dissolved oxygen, total nitrogen, and CODMn, and spatial heterogeneity in conductivity and chlorophyll a. In addition, the structure of benthic diatom assemblages also exhibited significant spatio-temporal variations. The dominant diatoms indicated that the water body of the CaoE River was under the condition of eutrophic and organic pollution. Statistical analyses highlighted the importance of environmental variables (such as conductivity, total nitrogen, total phosphorus, and chlorophyll a) in shaping benthic diatom assemblages in the CaoE River. Hence, this study explored how environmental heterogeneity influences the distribution and diversity of benthic diatoms in an urban river within the plain river network of East China. Furthermore, it provides an applicable way for the development and improvement of river monitoring and assessment with highly heterogeneous habitats.

This work was supported by the Shaoxing Natural Science Foundation (Grant No. 2022A13008) and the Shanxi Province Science Foundation for Youths (Grant No. 202203021222006).

All relevant data are included in the paper or its Supplementary Information.

The authors declare there is no conflict.

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