3.1 Sediment Properties
The physicochemical properties, including organic carbon, nitrogen, pH, and phosphorus, have been demonstrated to affect the fate of ARGs in sediments (Zhang et al., 2020b). Therefore, the physicochemical properties of the marine sediments were characterized, which include pH and contents of total carbon (TC), organic carbon (OrgC), ammonium (NH4+-N), nitrate (NO3−-N), total inorganic nitrogen (TIN), and total nitrogen (TN) (Table 1). All the sediments were alkaline, with a pH value ranging from 8.00 to 8.80. The pH of the sediments from the South China Sea was slightly higher than that of the sediments from the other three seas. The TC contents of these sediments were in the range of 8.60 g/kg to 80.43 g/kg. Sediments from the South China Sea had the highest TC content, whereas sediments from the Yellow Sea showed the lowest. The OrgC contents in the sediments ranged from 1.26 g/kg to 32.73 g/kg and presented a similar pattern to the TC. The NH4+-N contents in sediments from the Bohai Sea (38.43 ~ 67.79 mg/kg) and the Yellow Sea (26.10 ~ 45.65 mg/kg) were much higher than that of the East China Sea (4.84 ~ 26.36 mg/kg) and the South China Sea (7.59 ~ 14.07 mg/kg). On the other hand, there is no apparent difference in the NO3−-N content in the sediments from different seas, which ranged from 2.37 mg/kg to 7.94 mg/kg. The content of TN in different sediments varied significantly, ranging from 27.42 mg/kg to 315.92 mg/kg.
Table 1
Physicochemical properties of the sediments collected from the Bohai Sea, the Yellow Sea, the East China Sea, and the South China Sea.
Sea area | Sampling sites | Longitude and latitude | pH | NH4+-N | NO3−-N | OrgC | TIN | TN | TC |
(mg/kg) |
The Bohai Sea | NS-25 | 38.5°N, 119.0°E | 8.37 | 40.34 | 6.65 | 14.60 | 47.00 | 57.75 | 18.69 |
NS-26 | 38.5°N, 119.5°E | 8.43 | 67.79 | 7.94 | 9.69 | 75.83 | 212.44 | 13.43 |
NS-27 | 38.5°N, 120.0°E | 8.26 | 38.43 | 5.45 | 5.21 | 43.89 | 93.08 | 8.60 |
The Yellow Sea | YS-7 | 34.0°N, 123.8°E | 8.13 | 45.65 | 3.05 | 5.25 | 48.86 | 120.82 | 10.13 |
YS-9 | 34.0°N, 123.0°E | 8.00 | 40.39 | 2.37 | 6.48 | 42.93 | 220.40 | 13.12 |
YS-11 | 34.0°N, 122.0°E | 8.42 | 26.10 | 5.00 | 1.26 | 31.20 | 43.47 | 11.45 |
The East China Sea | S01-1 | 30.0°N, 122.7°E | 8.15 | 4.84 | 5.54 | 7.01 | 12.18 | 315.92 | 27.85 |
S01-3 | 30.0°N, 123.5°E | 8.22 | 26.36 | 6.06 | 5.50 | 32.44 | 126.20 | 21.01 |
S01-5 | 30.0°N, 124.3°E | 8.44 | 9.78 | 4.78 | 4.05 | 14.60 | 27.42 | 15.76 |
The South China Sea | DZ1 | 21.8°N, 116.8°E | 8.80 | 9.13 | 4.01 | 9.56 | 13.34 | 49.51 | 35.49 |
Q02 | 21.0°N, 118.0°E | 8.56 | 14.07 | 2.97 | 32.60 | 17.17 | 184.49 | 80.43 |
Q10 | 20.5°N, 115.5°E | 8.70 | 7.59 | 3.42 | 32.73 | 11.21 | 57.10 | 52.14 |
3.2 Abundance of ARGs and intI1 in the marine sediments
Due to the wide application of antibiotics β-lactam, sulfonamide, tetracycline, and vancomycin, the corresponding ARGs have been frequently detected in natural environments. The abundances of five prevalent ARGs (i.e. blaTEM, sul1, tetA, tetC, and vanA) and intI1 in the marine sediments were determined and presented as relative abundances in Fig. 2. blaTEM was the most prevalent and abundant class of ARGs, with a detection frequency of 100% and a relative abundance ranging from 7.6×10− 5-2.7×10− 3 (Fig. 2) that accounts for 71.5% of the total ARGs (Table S1). Higher abundances of blaTEM were found in sediments from the South China Sea, which were in the range of 5.8×10− 4- 2.7×10− 3. The relative abundances of blaTEM in the Bohai Sea sediments were 1–2 orders of magnitude lower than those in the South China Sea sediments, which ranged from 7.6×10− 5 to 1.1×10− 4. The relative abundances of blaTEM in the Yellow sea sediments varied marginally between different sites, ranging from 2.2 ×10− 4 − 3.8×10− 4. The usage of β-lactams (e.g., cephalosporin and penicillin) were the largest among the four target antibiotics in China (Zhang et al., 2015), which possibly explained the dominance of blaTEM in the marine sediments. The usage of sulfonamides in China ranked only second to β-lactams, followed by tetracyclines (Zhang et al., 2015). Consequently, occurrences of sul1 and tetC were also observed in all the sediments, accounting for 19.8% and 7.6% of the total ARGs respectively. The sul1 genes were more abundant in the sediments of the East China Sea, with a relative abundance of 6.4×10− 5-6.8×10− 4. The relative abundances of sul1 genes were at the minimum in the Yellow Sea sediment, ranging from 4.5×10− 6 to 3.9×10− 5. The relatively higher abundances of blaTEM and sul1 over the other ARGs might be attributed to the wide application of antibiotics from aquaculture (Zhang et al., 2020b). Furthermore, tetC genes exhibited higher abundances in the South China Sea and the Yellow Sea, holding relative abundances in the range of 5.8 × 10− 6-2.4 × 10− 4. tetA, another tetracycline resistance gene, was detected with a frequency of 67%. tetA was detected with significantly lower relative abundances compared to those of tetC, which ranged from 5.9 × 10− 7 to 3.8 × 10− 5. The vancomycin resistance gene vanA was only detected in the Bohai Sea sediments with a low detection frequency of 25%. The relative abundance of vanA was 1–4 orders of magnitude lower than that of the blaTEM. Among the five ARGs investigated in this work, blaTEM showed the highest abundance in the sediments of four seas from the north to the south of China, with an average of 6.0×10− 4. The average relative abundance of sul1, tetA, tetC, and vanA in the sediments from four sea sites were 1.6×10− 4, 6.7×10− 6, 5.7×10− 5, and 1.9×10− 6 respectively. β-lactam, tetracycline, and sulfanilamide were widely used in China. Consequently, the widespread occurrence of blaTEM, tetC, and sul1 in various environments has been reported (Fu et al., 2022; Guo et al., 2018; Jia et al., 2018; Leng et al., 2020; Xu et al., 2016).
intI was detected in all sampling sites excluding Q10 from the South China Sea. intI was detected with higher abundances (3.9 × 10− 4 to 1.2 × 10− 3) in the East China sea sediments, while those in the South China Sea sediments were relatively lower (0 to 1.0 × 10− 4). In general, the abundance of intI demonstrated the tendency of the East China sea > The Bohai sea > the Yellow sea > the South China Sea. The presence of intI1 is beneficial to the dissemination of bacterial resistance (Na et al., 2019), which is used to evaluate the horizontal transfer ability of ARGs. Once ARGs were captured by int1, they could be quickly transferred to bacteria (Gillings et al., 2015). ARGs can be further spread via the ocean currents, birds, atmosphere, and animal migration in the environment (Allen et al., 2010).
Taken into all the target ARGs, the relative abundance of total ARGs ranged from 1.0 × 10− 4 to 3.2 × 10− 3 in the marine sediments. Of the 12 sampling sites, Q10 and Q02 from the South China Sea had higher relative abundances of total ARGs with 3.2 × 10− 3 and 1.9 × 10− 3 respectively, whereas sediments from the Bohai Sea had the lowest relative abundance of total ARGs ranging from 1.0 × 10− 4 to 1.3 ×10− 4. ARGs detected in the South China Sea were more abundant than those in other seas, following the trend of the South China Sea > the Yellow Sea > the East China Sea > the Bohai Sea. The higher abundance of ARGs in the South China Sea might be attributed to the intensive anthropogenic activities in the Pearl River Delta, which was the dominant source of the ARG contamination. Compared with the occurrence of ARGs in the rivers with a relative abundance up to 2.43×10− 2 (Wang et al., 2020a), the abundance of ARG in the marine sediments was 1–2 orders of magnitude lower. This was consistent with the ARGs distribution in aquatic environments as rivers receive large volumes of effluents from wastewater treatment plants which were found to contain many ARGs (Zhang et al., 2018a). Although the pollution status in the sea was relatively weaker due to the highly dynamic nature and dilutions of seawater, the ubiquitous presence of ARGs in all sea sediments investigated revealed that seas have suffered from ARGs contamination to some extent.
3.3 Microbial community in the marine sediments
The microbial community of the sediment samples was characterized using 16S rRNA amplicon sequencing. The raw sequencing data of the sediment samples were trimmed and filtered to remove low-quality sequences, generating a total of 1.4 million high-quality reads and an average of 116,834 sequences per sample. The goods coverage of all the sediment samples was greater than 99%, which indicated that the sequencing depth was sufficient to reveal the microbial populations in the sediment samples. The microbial community of the sediment samples was analyzed at the same sequencing depth of 108,782. The relative abundance of phylotypes in the sediments at phylum and genus levels were shown in Fig. 3A and B. At the phylum level, Proteobacteria and Bacteroidetes were the two most abundant phyla in all the sediments (Fig. 3A), with a relative abundance of 21.15%-55.51% and 16.49%-46.89% respectively. Other Phyla such as Firmicutes, Actinobacteria, and Verrucomicrobia were also presented in the sediments with a relatively high abundance of 1.24%~17.98%, 1.89%~5.07%, and 0.27%~13.32% respectively. These five phyla accounted for 73.85 ~ 95.65% of the total population in the sediments. Previous findings have highlighted the abundance of Proteobacteria (comprising > 50% of the microbial biomass) in most surface marine sediments (Dang et al., 2010; Durbin and Teske, 2011; Suzuki et al., 2019). Bacteroidetes were the dominant phylum in sediment samples derived from Cyanobacterial aggregates (Liu et al., 2015b). Proteobacteria and Bacteroidetes, which have been long regarded as dominant microbes in marine sediments and play important roles in the biogeochemical processes (Durbin and Teske, 2011), were predominated in all the sediments samples in this study.
Figure 3B shows the top 10 genera in the sediments, and the genera of Lutibacter, Marinobacter, Amphritea, Sulfitobacter, and Arenibacter were detected with higher relative abundances. These microbes are distributed globally, many of which have flexible adaptations to various environments of marine sediments (Liu et al., 2015b). The dominant genera of bacteria exhibited distinct spatial distribution. For example, Lutibacter were predominant in the Bohai Sea sediments, while Marinobacter were detected with higher relative abundances in the Yellow Sea sediments. The genus of Amphritea was dominant in the East China Sea sediments, and the genus of sulfitobacter was found relatively high in the South China Sea sediments. NMDS analysis of OTUs based on unweighted UniFrac distance matrix was displayed in Fig. 3C. The microbial communities in the sediments from the four seas were clustered into four divergent groups, suggesting obvious differences in the microbial community between the sea areas. Specifically, sediments from the Bohai Sea (NS-25, NS-26, NS-27), the Yellow Sea (YS-7, YS-9, YS-11), the East China Sea (S01-1, S01-3, S01-5), and the South China Sea (Q02, Q10, DZ1) were divided into group1, group 2, group 3, and group 4 respectively (Fig. 3C). The obvious spatial heterogeneity indicates a correlation between the microbial community and the environment (Liu et al., 2015b). The apparent spatial distribution was further confirmed by UPGMA analysis (Fig. 3D), where sediments from the four seas were categorized into four clusters. Bacterial assemblages of the sediments in the South China Sea appeared to be the most distinct cluster, as these samples were separated into three main clusters. This indicated that different environmental parameters might play important roles in shaping the microbial communities of sediments on the coast of China (Liu et al., 2015b). Similar microbial communities especially key microbial groups might present in environments with significant similarities (Dang et al., 2009).
3.4 Correlation among ARGs, environmental factors, and microorganisms
Environmental factors (e.g., nutrients and organics) have been demonstrated to affect the distribution and abundance of ARGs (Lu et al., 2019b) (Zhang et al., 2020a; Zhao et al., 2019). Therefore, correlation analysis and Mantel test were performed to evaluate the correlations among the target genes, the microbial community, and the environmental factors (Fig. 4A). blaTEM, tetC, sul1, and intI1 were found to be significantly positively correlated with the environmental factors. Specifically, both blaTEM and tetC showed strong positive correlations with NO3−-N, OrgC, and TC (p < 0.05). Positive correlations were found between sul1 and NH4+-N (p < 0.05). In addition, both blaTEM and tetC were found to be positively related to latitude (p < 0.05), while intI1 shown positive correlation with longitude (p < 0.05). This study showed that the occurrence of ARGs was positively correlated with the level of nutrients (e.g, nitrate and ammonium) and organics. Therefore, reducing the discharge of conventional pollutants could be an effective way to control the ARG risk in the seas.
Microbial community could be used as a biological indicator of the changes in geochemical and physicochemical characteristics of sediments due to the specificity of microbe habitats (Dang et al., 2010). The correlations between the microbial community and the environmental factors were also demonstrated in Fig. 4A. Proteobacteria were significantly negatively correlated with NO3−-N (p < 0.05), whereas Bacteroidetes showed a significant positive correlation with NO3−-N (p < 0.05). Bacteroidetes prefer to develop in sediments of eutrophic water environments (Liu et al., 2015b).
Complex correlations were shown between the target genes and the microbial community (Fig. 4A). For instance, a significantly positive correlation was found between the relative abundance of blaTEM and Bacteroidetes (p < 0.05). Similarly, there was a significant positive correlation between the relative abundance of sul1 and Acidobacteria (p < 0.05). Network analysis was further conducted to reveal the potential host bacteria of the target genes. Colored Nodes represent int1, blaTEM, tetC sul1, and potential host bacteria in Fig. 4B, and connections indicate significant positive or negative correlations (p < 0.05). int1, blaTEM, tetC, and sul1 exhibited strong and significant correlations with 11 bacterial phyla (e.g., Bacteroidetes, Firmicutes, Tenericutes, and Hadesarchaeaeota) (p < 0.05), which were speculated to serve as the potential host bacteria for these ARGs. Bacteroidetes and Firmicutes with relatively high abundances (Fig. 3A) were the dominant bacteria host of ARGs in the marine sediments. These bacteria potentially hosted multi-drug resistance, which would develop into antibiotic resistance bacteria through horizontal or vertical gene transfer under ongoing selection pressures of antibiotics (Lu et al., 2019a).