The Liaohe Estuary (lat. 40o20’-41oN and Lon. 121o20’-122oE) is located in the Liaodong Bay, a part of the Bohai Sea, Northeastern China (Fig. 1). With the rapid industrialization and urbanization of upstream cities, the Liaohe Estuary is exposed to considerable anthropogenic pressures including industrial and agricultural effluent, domestic sewage discharge, oil mining, and physical disturbance by trawling and dredging. The surrounding sea-going rivers (i.e., Liaohe River, Shuangtaizi River, Daling River, and Xiaoling River) carry large amounts of terrigenous pollutants, which significantly deteriorate the habitat quality of Liaohe Estuary20. With the massive expansion of high-density aquaculture practice in the Liaohe delta wetland, crab aquaculture pollution has also become a severe environmental problem21. Liaohe Oilfield, the third-largest oilfield in China, also poses high pollution pressures on the surrounding environment. Furthermore, Liaohe Estuary is serving as a vital fishery ground, and commercial bottom trawling may alter the structure and function of ecosystems. According to the “Bulletin of Marine Ecology and Environment Status of China in 2018” (Ministry of Ecology and Environment of the People’s Republic of China), Liaohe Estuary is one of the most contaminated area in China, with the primary dominant pollutants being inorganic nitrogen and active phosphate. In present study, a total of 25 sublittoral sampling stations were set up in the Liaohe Estuary, which were divided into six categories based on the distance from the station to the river inlet (A, No. 1–2; B, No. 3–6; C, No. 7–10; D, No. 11–15; E, No. 16–20; and F, No. 21–25; A to F meant closest to farthest from the river inlet). After data collection in spring, summer, and autumn seasons, the spatial-temporal variations of environmental conditions and benthic indices were investigated.
Environmental variables
The spatial-temporal variability of abiotic parameters in the studied estuary is presented in Fig. 2. Significantly higher Chl-a, NO2-N, and COD concentrations were recorded in summer compared to spring and autumn (ANOVA, p < 0.05). In contrast, the water salinity increased in spring and decreased in summer compared to autumn (ANOVA, p < 0.05). The NO3-N and NH4 contents in the water were higher in summer and lower in autumn compared to spring (ANOVA, p < 0.05). Moreover, the TOC concentrations in summer and autumn were significantly higher than those in spring. however, the PO4-P in spring and summer were significantly lower than autumn (ANOVA, p < 0.05). In addition, no significant differences were observed in the sediment compositions and PHc content among the different seasons (ANOVA, p > 0.05).
Changes in environmental quality indicators at different distances within the same season were also analyzed. Salinity rose in all three seasons as the distance from the inlet increased. In summer, Chl-a concentrations in water samples from the A, D, E, and F regions were significantly higher than in the other samples. In summer and spring, the NO2-N, NO3-N, NH4-N, PO4-P, and COD concentrations significantly decreased as the distance from the inlet increased. In contrast, the values of these indicators showed no significant spatial variance in autumn. As the distance from the estuary increased, the proportion of sand and clay in sediments decreased at first, and then increased. No obvious change in the pattern of PHc content was found in the sediments at different distances within the same season.
Macrobenthic community structure and seasonal variation
We sampled 15,680 individuals from 105 species during three seasons, representing 87 Genera, 70 Families, and 27 Orders. Polychaete was the dominant taxa, with the largest number of species. Mollusca, Crustacea, and Echinodermata were also common, in contrast, Bryozoa, Nemertinea, Sipuncula, and Plathyelminthes were far less common. Mollusca (56.7%) was the dominant taxa in terms of abundance, followed by Polychaeta (23.7%), Crustacea (13.8%), Echinodermata (3.3%), and others (2.5%). The number of each taxonomic unit and the dominant species in each season with aggregation ratio (ɸ) (Bevilacqua et al. 2012) (higher rank taxon count to species count) are shown in Table 1. Species richness slightly decreased from summer to autumn and spring, with 59, 57, and 57 taxa, respectively. Only 20 species (19%) were common among all three seasons, while 57 species (54%) were season specific. Moreover, 31 species were common in both summer and autumn, whereas 28 were common in spring and autumn (Fig. 3).
Table 1
Summary of orders, families, genus and species counts, aggregation ratio (ɸ) for higher taxonomic resolutions and dominant species in three seasons. Ecological groups assigned to dominant species are provided in parenthesis. NA indicates “not assigned”.
Season | Orders | Families | Genera | Species | Dominant Species (≥ 2%) |
Spring | 18 | 37 | 47 | 59 | Potamocorbula ustulata (NA) |
Aggregation ratio (ɸ) | 0.42 | 0.83 | 0.87 | | Ampelisca sp. (I) |
Summer | 19 | 39 | 58 | 57 | Potamocorbula laevis (V) |
Aggregation ratio (ɸ) | 0.37 | 0.80 | 0.98 | | Aonides oxycephala (III) |
| | | | | Capitella capitata (V) |
Autumn | 20 | 36 | 50 | 57 | Corophium acherusicum (III) |
Aggregation ratio (ɸ) | 0.47 | 0.85 | 0.93 | | Grandidierella sp. (I) |
| | | | | Amphioplus sp. (I) |
| | | | | Capitella capitata (V) |
| | | | | Potamocorbula laevis (V) |
| | | | | Glossaulax didyma (I) |
All the identified taxa were assigned to 5 EGs based on the AZTI’s classification (Table S1 in Appendix. A), 33 taxa (31.4%) were classified as EG I, 36 taxa (34.3%) assigned to EG II, 16 taxa (15.2%) were assigned to EG III, 7 taxa (6.7%) assigned to EG IV, 2 taxa (1.9%) assigned to EG V, and 11 species (10.5%) were unassigned. In terms of abundance, EG VI and EG I were dominant, which were due to the higher densities of Potamocorbula laevis and Amphioplus sp., respectively. Aggregating the species data to genus and family taxonomic levels produced 93 and 74 taxa, respectively (Table S1).
Calculation and inter-calibration of M-AMBI across taxonomic levels
Among all 70 M-AMBI values for sampling stations in all three seasons, the ecological status derived from species-level data indicated that the majority of the stations were categorized as Good, Moderate, and Poor status (40%, 18.6%, and 20%, respectively). A minority of 8.6% stations were classified as High, and 12.8% were ranked as Bad. In terms of seasonal variability, 20 of 25 (75%) showed variations in their ecological status over the sampling periods (Fig. 4). Most of the variations occurred among the adjacent categories (e.g., High to Good, Good to Moderate), however, S6 and S14 fluctuated from High to Bad. The stations with consistent ecological classification belonged to the Good (S12, S16, S21 and S22) and Moderate (S3) categories. Overall, the summer showed the highest M-AMBI values among the three seasons, which indicated a decreased ecological status. Moreover, M-AMBI values showed consistent spatial distribution during all three seasons, with a clear distribution pattern related to the distance from the estuary and coast (Fig. 4). The inshore sites were more disturbed than the offshore sites. It is noted that the inshore sites (e.g., S1 to S6) generally had the highest temporal variations in the ecological status. Conversely, offshore sites showed a relatively consistent increased ecological status.
Kappa analysis indicated “Almost perfect” agreement existing between species- and genus-level M-AMBI EcoQ classifications using the standard class boundaries (Table 2) (Kappa value = 96.2%, Asymp. Std. Error = 2.7%). However, similar analysis for species- and family-level outputs resulted in “Substantial” agreement (Kappa value = 68.8%, Asymp. Std. Error = 6.6%) between EcoQ classifications. Inter-calibrating the class boundaries (High/Good 0.78, Good/Moderate 0.56, Moderate/Poor 0.44 and Poor/Bad 0.24) for family-level EcoQ outputs produced a positive effect on the agreement between species- and family-level EcoQ classifications, which resulted in an “Almost perfect” agreement (Kappa value = 82.7%, Asymp. Std. Error = 5.4%).
Table 2
Number of stations for each ecological quality (EcoR) classification using the M-AMBI calculated with aggregated datasets.
EcoR Classification | Aggregation level |
Speciesa | Genusa | Familyb |
High | 6 | 6 | 6 |
Good | 28 | 26 | 28 |
Moderate | 13 | 15 | 12 |
Poor | 14 | 14 | 15 |
Bad | 9 | 9 | 9 |
Total | 70 | 70 | 70 |
a Standard EcoQ classification aboundaries used; High/Good 0.77, Good/Moderate 0.53, Moderate/Poor 0.39 and Poor/Bad 0.2. |
b Inter-calibrated EcoQ classification boundaries used: High/Good 0.78, Good/Moderate 0.56, Moderate/Poor 0.44 and Poor/Bad 0.24. |
Relationships between M-AMBI, ecological group distribution, and abiotic factors
The assemblage-environment relationships were explored by DistLM analysis (Table S2). The sequential tests using forward procedure revealed that seven environmental variables collectively contributing power of explanatory model for macrofauna assemblage composition in three taxonomic levels. The increased prediction power (adjusted R2) was observed as taxonomic levels increased, with the family level showing the best predictive power, followed by the genus and species levels. The db-RDA routine also showed that environmental variables of importance differed among three seasons within the three taxonomic levels (Fig. 5). M-AMBI scores obtained from three taxonomic-level datasets (i.e., species, genus, and family) indicated a significant relationship with abiotic factors. M-AMBI scores showed strong correlation with salinity, EI, and TOC (Fig. 6). The highest correlations with salinity, EI, and TOC were all obtained from the family-level data.