Next Article in Journal
Genome-Wide Identification of the U-Box E3 Ubiquitin Ligase Gene Family in Cabbage (Brassica oleracea var. capitata) and Its Expression Analysis in Response to Cold Stress and Pathogen Infection
Next Article in Special Issue
Reduction in the Use of Some Herbicides Favors Nitrogen Fixation Efficiency in Phaseolus vulgaris and Medicago sativa
Previous Article in Journal
Stimulation of PGP Bacteria on the Development of Seeds, Plants and Cuttings of the Obligate Halophyte Arthrocaulon (Arthrocnemum) macrostachyum (Moric.) Piirainen & G. Kadereit
Previous Article in Special Issue
Identification and Characterization of Common Bean (Phaseolus vulgaris) Non-Nodulating Mutants Altered in Rhizobial Infection
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Communication

Studies on the Composition and Diversity of Seagrass Ruppia sinensis Rhizosphere Mmicroorganisms in the Yellow River Delta

1
School of Biological and Environmental Engineering, Binzhou University, Binzhou 256600, China
2
College of Marine Life Sciences, Ocean University of China, Qingdao 266005, China
3
First Institute of Oceanography, Department of Natural Resources, Qingdao 266061, China
*
Authors to whom correspondence should be addressed.
Plants 2023, 12(7), 1435; https://doi.org/10.3390/plants12071435
Submission received: 4 February 2023 / Revised: 19 March 2023 / Accepted: 21 March 2023 / Published: 24 March 2023
(This article belongs to the Special Issue Interactions between Plants and Soil Microorganisms)

Abstract

:
Seagrass is a significant primary producer of coastal ecosystems; however, the continued degradation of seagrass beds is a serious problem that has attracted widespread attention from researchers. Rhizosphere microorganisms affect seagrass and participate in many life activities of seagrass. This study explored the relationship between the composition of microbes in the rhizosphere and the surrounding environment of Ruppia sinensis by using High-throughput sequencing methods. The dominant bacterial groups in the rhizosphere surface sediments of R. sinensis and the surrounding environment are Proteobacteria, Bacteroidota, and Firmicutes. Moreover, the dominant fungal groups are Ascomycota, Basidiomycota, and Chytridiomycota. Significant differences (p < 0.05) were identified in microbial communities among different groups (rhizosphere, bulk sediment, and surrounding seawater). Seventy-four ASVs (For bacteria) and 48 ASVs (For fungal) were shared among seagrass rhizosphere, surrounding sediment, and seawater. The rhizosphere was enriched in sulfate-reducing bacteria and nitrogen-fixing bacteria. In general, we obtained the rhizosphere microbial community of R. sinensis, which provided extensive evidence of the relative contribution of the seagrass rhizosphere and the surrounding environment.

1. Introduction

Seagrass, a secondary entry from land to water, was adapted to the marine environment between 70 and 100 million years ago [1]. Compared to 250,000 species of terrestrial angiosperms, only 60 species of seagrass were adapted to the marine environment [2]. Seagrass meadows are one of the ecosystems with the richest biodiversity and highest productivity and ecological service function value in the earth’s biosphere. It provides habitats for many marine organisms and is essential for maintaining coastal ecosystems’ structural complexity, spatial heterogeneity, and functional stability [3]. Due to the interaction between land and sea, the seagrass meadows’ ecological environment is fragile and vulnerable to biological invasion. It faces worldwide degradation, which has attracted worldwide attention [4].
Complex and dynamic interactions between microorganisms and host plants can improve plant resistance to environmental stress [5]. Rhizosphere microorganisms play an important role in the growth and development of plants, promoting host plants’ growth, nutrient absorption, and stress resistance. Meanwhile, rhizosphere microorganisms can transport organic matter, nitrogen fixation, and denitrification [6]. The rhizosphere microbiome is also known as the plant’s second genome. The rhizosphere microbial assemblages are complicated and influenced by other biological and abiotic factors (soil pH value, soil salinity, soil conductivity, organic carbon, nitrogen, and phosphorus sources). Plants resist environmental changes by recruiting bacteria and fungi that are beneficial to them. These microorganisms influence the growth state of plants by regulating the secretion of plant hormones to improve nutrient absorption and produce volatile organic matter, thus improving the stress resistance of plants [7], and maintaining the dynamic stability of plants and rhizosphere microorganisms. The roots and rhizomes of seagrasses penetrate the sediment to form vast meadows. Seagrass roots can secrete amino acids, sugars, and oxygen to construct a complex relationship between seaweed and rhizosphere microbes [8]. Seagrass meadows form surface sediments and provide a specific environment for a rich and diverse microbial community [9]. Seagrass microorganisms play an essential role in maintaining the stability of the seagrass ecosystem [10]. There are many sulfide-metabolizing bacteria in seagrass, which can oxidize phytotoxic sulfides into non-toxic sulfates and play a vital role in the growth and development of seagrass [11]. The epiphytic microorganism can help seagrass resist pathogens and increase its ecological adaptability. Thus, microbial communities not only affect the growth and health of seagrass, but also control the succession of the seagrass community and even regulate the biochemical cycle of the seagrass bed, which plays an essential role in seagrass resistance to environmental changes [12]. As an essential supporting species of seagrass beds, R. sinensis is a widely distributed seagrass species in China and a vital support species of seagrass beds with crucial ecological functions. Due to the dual effects of global environmental change and human activities, R. sinensis faces population reductions due to anthropogenic impacts [13]. Meanwhile, R. sinensis is also widely distributed in the Yellow River Delta (YRD); the YRD is one of China’s three major estuarine deltas [14]. Furthermore, it is a typical coastal wetland ecosystem with high biodiversity. As an important component of biodiversity in the YRD, seagrasses play an essential role in maintaining the stability of the YRD ecosystem.
Several studies have been carried out on the microbial composition of Zostera japonica in the YRD [15], while the microbial communities of R. sinensis were still unknown. The present study explored the rhizospheric- and surrounding-environment microbial communities of R. sinensis using root, seawater, and sediment samples. Thus, we focused on characterizing each sample’s bacterial and fungal communities using high-throughput sequencing of 16S and ITS genes. We aimed to find the taxonomic composition characteristic of the R. sinensis microbiome.

2. Results

2.1. Characteristics of Environmental Factors in Seagrass Beds

In the present study, the One-way ANOVA method was used to analyze the environmental factors between the surrounding environment and the rhizosphere of seagrass beds. These results showed that the TOC and TS did not significantly differ between the BS and RS groups (p > 0.05). The EC was significantly different among the three groups and the order of the EC value was BS > RS > SW (p < 0.05). The pH in the SW group was significantly higher than that in the BS and RS groups (Table 1) (p < 0.05).

2.2. Alpha Diversity

For bacteria, these results showed that the Shannon index and Simpson index of the SW group were significantly lower than that of the other groups (p < 0.05). According to the Ace index and Chao1 index, it can be seen that the order is RS > BS > SW, and there were significant differences among the three groups (p < 0.05) (Figure 1).
For bacteria, these results showed that the Shannon index and Simpson index of the SW group was significantly lower than that of the other groups (p > 0.05), while the Simpson index of the SW group was significantly lower than that of the BS group (p < 0.05). The Ace index and Chao1 index of the SW group are higher than those of the other two groups (Figure 2).

2.3. Beta Diversity

We examined bacterial and fungal community structure differences between the seagrass rhizosphere and the surrounding environments. For bacteria, the PCoA results showed that the PC1 explained 38.95% of the variation, and the PC2 explained 17.32% of the variation, respectively. In total, 56.27% of the variation was explained by PC1 and PC2 (Figure 3a). For fungi, PC1 explained 48.90% of the variation, and PC2 explained 12.56% of the variation. In total, 61.46% of the variation was explained by PC1 and PC2 (Figure 3b).
The PERMANOVA was used to calculate the bacterial and fungal communities clustering among the three groups (Figure 4). These results showed that the different groups explained about 20% of the differences in bacterial and fungal community structure (R2 = 0.232, p = 0.001; R2 = 0.227, p = 0.001).

2.4. Sequence Variants and Abundant Genera

For bacteria, 74 ASVs were shared among seagrass rhizosphere, surrounding sediment, and seawater. The number of unique ASVs was 13,390, 8102, and 5022 in the RS, BS, and SW groups (Figure 5a). For fungi, the community shared 48 ASVs among the groups. The number of unique ASVs was 801, 455, and 1651 in the RS, BS, and SW groups (Figure 5b).

2.5. Composition of the Rhizosphere Microbial Community

The present study contained 1,935,998 raw reads and 2,063,349 raw reads in the bacteria and fungi, respectively. The generated serial number is PRJNA882191 and PRJNA881797. For bacteria, the dominant phyla were Proteobacteria, Bacteroidota, Actinobacteriota, Chloroflexi, Desulfobacterota, Firmicutes, Cyanobacteria, Gemmatimonadota, and Acidobacteriota in the RS group; the Proteobacteria, Bacteroidota, Actinobacteriota, Chloroflexi, Desulfobacterota, Firmicutes, Acidobacteriota, and Gemmatimonadota were dominant in the BS group; and the Proteobacteria, Bacteroidota, Actinobacteriota, Firmicutes, and Cyanobacteria were dominant in the SW group (Figure 6a). The Proteobacteria was the highest in the three groups. Except for the unclassified genera, Roseibacterium, Candidatus_Aquiluna, and Cyanobium_PCC_6307 were dominant in three groups at the genus level (Figure 6c).
For fungi, the Ascomycota, Basidiomycota, Mortierellomycota, and Chytridiomycota were dominant in the RS group; the Ascomycota, Basidiomycota, Mortierellomycota, and Chytridiomycota were dominant in the BS group; and the Ascomycota, Basidiomycota, and Chytridiomycota were dominant in the SW group (Figure 6b). Except for the unclassified genera, Talaromyces, Fusarium, Stachybotrys, Thanatephorus, and Penicillium were dominant in the BS and RS groups at the genus level (Figure 6d). The Ascomycota was the highest in the BS and RS groups, while the Basidiomycota was the highest in the SW group.

3. Discussion

Plants and their microbiome together form a “holobiont” that interacts and coevolves with each other. Host plants provide a variety of microhabitats for microbial communities, and the microbes participate in various physiological processes of host plants. The surrounding environment is a vibrant microbial resource pool from host microorganisms [16].
Bacterial community diversity in the sediment and rhizosphere of seagrass was higher than in the surrounding seawater. The sediment and rhizosphere contain more nutrients than seawater and can protect microorganisms from sunlight and predation, leading to higher bacterial diversity in the rhizosphere and sediment [17]. Moreover, fungal community diversity in the sediment and rhizosphere of seagrass were similar. The similarity might be due to the proximity of the sediment and rhizosphere [18]. The Proteobacteria, Bacteroidota, Actinobacteriota, Chloroflexi, Desulfobacterota, Firmicutes, Cyanobacteria, Gemmatimonadota, and Acidobacteriota were dominant in the seagrass rhizosphere. Bacteroidota is known to be widely distributed across marine environments, and are decomposers of macromolecules, such as cellulose and chitin [19]. Nitrogen-fixing microorganisms are essential, including Proteobacteria, Firmicutes, and Actinobacteriota. Nitrogen fixation is essential in seagrass photosynthesis and balancing nitrogen loss. The relative stability of nitrogen-fixing flora in seagrass beds is crucial to seagrass beds’ health and ecological functions.
A study of two tropical seagrasses (Thalassia hemprichii and Enhalus acoroides) found that the dominant bacterial communities involved sulfate cycling, nitrogen, and carbon fixing [20]. Several studies believed that Proteobacteria was the most abundant phylum [21] and was consistently enriched in the seagrass rhizosphere compared to bulk sediment [22]. A previous study found that the Proteobacteria were important in the low-molecular-weight substrates [23]. This study also found that the Proteobacteria was dominant in the seagrass rhizosphere, consistent with previous studies. In addition to providing fixed nitrogen to meet the needs of the rapid growth of seagrass, iron-reducing bacteria can also reduce sulfide toxicity by forming pyrite through long-term precipitation [24]. Previous studies found that sulfate-reducing bacteria are the main groups that degrade organic matter anaerobic in coastal oceans, and abundant organic carbon sources are conducive to their reproduction. Hence, they are more abundant in seagrass areas. In addition, the metabolic processes of sulfur and nitrogen are not independent of each other, and sulfate-reducing bacteria are also prominent members of nitrogen fixation in seagrass sediments [25]. Like other coastal marine ecosystems, microorganisms rapidly deplete oxygen in seagrass bed root sediments, resulting in an anoxic environment below the surface. In the present study, the sulfate-reducing bacteria occupy a crucial position in the seagrass rhizosphere ecosystem. Since a large amount of sulfate in the sediments can easily acquire electrons and become terminal electron acceptors, sulfuric acid Salt-reducing bacteria dominate the mineralization of organic matter. Geochemical evidence suggests sulfate reduction is closely related to carbon and nutrient cycling in seagrass bed sediments [26]. For fungi, Ascomycota was the most abundant in the BS and RS groups. It has been reported that fungi from Ascomycota represent the predominant microflora in marine environments. Penicillium, dominant in the rhizosphere and sediment, was demonstrated as common inhabitants of marine environments because these are adapted to peculiar chemical and physical conditions [27].
The study of microbial community organization is the basis for understanding the microbial ecosystem in seagrass beds, and its influencing factors are very complex. For bacteria, the Venn results showed that the 1524 common ASVs were identified between the RS and BS groups, and 779 common ASVs were identified between the SW and RS groups. Compared with the surrounding seawater, the microbiological compositions in the seagrass rhizosphere are more similar to the surrounding sediment. For fungi, 120 common ASVs were identified between the RS and BS groups, and 168 ASVs were identified between the SW and RS groups. Compared with the bacteria, the composition of fungi in the seagrass rhizosphere is more similar to that of the surrounding seawater. We speculated that the rhizosphere microbial community of R. sinensis was endemic and environment-acquired, not only from water bodies but also from sediments. A previous study found that compared with the perennial population, the annual R. sinensis population had a higher TOC [27]. Compared with the TOC of R. sinensis population, this research had a higher TOC.
Moreover, the fungal community structure of the seagrass rhizosphere is mainly related to TOC and PH in the surrounding seawater. The enrichment process of seagrass rhizosphere microbes could provide critical information on the interactions between seagrass and the surrounding environment [28]. A study of the Z. marina microbiome found that the bacterial leaf communities were similar to the seawater. The root bacterial communities were less heterogeneous and more distinct from the surrounding sediment [29].

4. Materials and Methods

4.1. Study Area

The study site was located in the YRD, Shandong, China. This area is located in the wetland at Bohai Sea, which widely distributes Suaeda salsa, Tamarix chinensis [30], Cynanchum chinense, Spartina alterniflora, and R. sinensis. The density of R. sinensis, it is the only seagrass species in the area. The seagrass rhizosphere, sediment, and seawater samples were collected from each site in the present study. The rhizosphere soil of R. sinensis was collected by first removing the associated plants, then excavating the whole solid goldenrod, followed by kneading the stalks of R. sinensis, then shaking the roots gently, and finally shaking off the soil. The rhizosphere soil of R. sinensis was obtained by following a previous study [31]. The seagrass rhizosphere soil samples were marked as the RS group; the sediment samples as the BS group; and the seawater samples as the SW group. All samples were divided into two parts; one part was used to determine soil and water physicochemical properties, and the other was used for DNA extraction.

4.2. Sediment and Seawater Physicochemical Properties Analysis

The present study determined the sediment and seagrass pH using a pH meter (Sartorius PB-10, Goettingen, Germany). Electrical conductivity (EC) was measured using a conductivity meter (Hanna HI98192, Villafranca Padovana, Italy). The Total Organic Carbon (TOC) and total sulfur (TS) were measured by following a previous study [31].

4.3. Molecular Methods

The DNA was extracted from the root, seawater, and sediment samples using the E.Z.N.A.® Soil DNA Kit (D4015, Omega, Inc., Syracuse, NY, USA). For bacteria, the primers of the V3–V4 region of the 16S ribosomal RNA gene was amplified by following a previous study [32]. For fungi, the primers of ITS1 were amplified using a previous study [33]. The Illumina Novaseq 6000 platform was used to obtain the raw data.

4.4. Statistical Analysis

In the present study, the raw data were denoised, and chimeric sequences were removed to get the final compelling data by using the Dada2 method in the QIIME2 2020.6 software [34]. The SILVA was used to classify for taxonomic annotation. The QIIME software generated the species abundance table for different taxonomic groups. The R was used to obtain the beta-diversity bar plots at each taxonomic level [35]. The Alpha diversity indices (AEC, Chao1, Shannon and Simpson indices) and beta diversity were obtained using the QIIME2 software [34]. The shared and unique amplicon sequence variants (ASVs) between the seagrass rhizosphere and the surrounding environment were shown by using the Venn diagrams. Principal coordinate analysis (PCoA) was used to visualize the difference in the microbial community structure between the seagrass rhizosphere, surrounding sediment, and seawater. The One-way ANOVA method and student’s t-test were used to calculate the differences in soil physicochemical properties and soil alpha diversity indices using SPSS 23.0 (IBM SPSS Inc., USA).

5. Conclusions

This study provides extensive evidence of the relative contribution of the seagrass rhizosphere and the surrounding environment. The dominant bacterial groups in the rhizosphere surface sediments of R. sinensis and the surrounding environment are Proteobacteria, Bacteroidota, and Firmicutes. Moreover, the dominant fungal groups are Ascomycota, Basidiomycota, and Chytridiomycota. Significant differences were identified in microbial communities among different groups (rhizosphere, bulk sediment, and surrounding seawater). The rhizosphere was enriched in sulfate-reducing bacteria and nitrogen-fixing bacteria.

Author Contributions

Formal analysis, S.S.; writing—original draft preparation, S.S., L.L., H.X. and J.C.; writing—review and editing, Y.Z., J.W. and X.T.; All authors have read and agreed to the published version of the manuscript.

Funding

This work was supported by the NSFC-Shandong Joint Fund (No. U1806213), the Natural Science Foundation of Shandong Province (ZR2021QD082), and the National Natural Science Foundation of China (No. 42176154).

Data Availability Statement

The data that support the findings of this study are available in NCBI (accession number PRJNA882191 and PRJNA881797).

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. Les, D.H.; Cleland, M.A.; Waycott, M. Phylogenetic studies in alismatidae, II: Evolution of marine angiosperms (seagrasses) and hydrophily. Syst. Bot. 1997, 22, 443–463. [Google Scholar] [CrossRef]
  2. Orth, R.J.; Carruthers, T.J.B.; Dennison, W.C.; Duarte, C.M.; Fourqurean, J.W.; Heck, K.L.; Hughes, A.R.; Kendrick, G.A.; Kenworthy, W.J.; Olyarnik, S.; et al. A global crisis for seagrass ecosystems. Bioscience 2006, 56, 987–996. [Google Scholar] [CrossRef] [Green Version]
  3. Fourqurean, J.W.; Duarte, C.M.; Kennedy, H.; Marba, N.; Holmer, M.; Mateo, M.A.; Apostolaki, E.T.; Kendrick, G.A.; Krause-Jensen, D.; McGlathery, K.J.; et al. Seagrass ecosystems as a globally significant carbon stock. Nat. Geosci. 2012, 5, 505–509. [Google Scholar] [CrossRef]
  4. Yue, S.D.; Zhou, Y.; Zhang, Y.; Xu, S.C.; Gu, R.T.; Xu, S.; Zhang, X.M.; Zhao, P. Effects of salinity and temperature on seed germination and seedling establishment in the endangered seagrass Zostera japonica Asch. & Graebn. in northern China. Mar. Pollut. Bull. 2019, 146, 848–856. [Google Scholar] [CrossRef]
  5. Trivedi, P.; Batista, B.D.; Bazany, K.E.; Singh, B.K. Plant-microbiome interactions under a changing world: Responses, consequences and perspectives. New Phytol. 2022, 234, 1951–1959. [Google Scholar] [CrossRef]
  6. Zhang, P.; Nie, M.; Li, B.; Wu, J.H. The transfer and allocation of newly fixed C by invasive Spartina alterniflora and native Phragmites australis to soil microbiota. Soil Biol. Biochem. 2017, 113, 231–239. [Google Scholar] [CrossRef]
  7. Qin, Y.; Druzhinina, I.S.; Pan, X.Y.; Yuan, Z.L. Microbially Mediated Plant Salt Tolerance and Microbiome-Based Solutions for Saline Agriculture. Biotechnol. Adv. 2016, 34, 1245–1259. [Google Scholar] [CrossRef]
  8. Christiaen, B.; McDonald, A.; Cebrian, J.; Ortmann, A.C. Response of the microbial community to environmental change during seagrass transplantation. Aquat. Bot. 2013, 109, 31–38. [Google Scholar] [CrossRef]
  9. Markovski, M.; Najdek, M.; Herndl, G.J.; Korlevic, M. Compositional stability of sediment microbial communities during a seagrass meadow decline. Front. Mar. Sci. 2022, 9, 966070. [Google Scholar] [CrossRef]
  10. Cole, L.W.; McGlathery, K.J. Nitrogen fixation in restored eelgrass meadows. Mar. Ecol. Prog. Ser. 2012, 448, 235–246. [Google Scholar] [CrossRef] [Green Version]
  11. Martin, B.C.; Bougoure, J.; Ryan, M.H.; Bennett, W.W.; Colmer, T.D.; Joyce, N.K.; Olsen, Y.S.; Kendrick, G.A. Oxygen loss from seagrass roots coincides with colonisation of sulphide-oxidising cable bacteria and reduces sulphide stress. ISME J. 2019, 13, 707–719. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  12. Ugarelli, K.; Chakrabarti, S.; Laas, P.; Stingl, U. The Seagrass Holobiont and Its Microbiome. Microorganisms 2017, 5, 81. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  13. Gu, R.T.; Zhou, Y.; Song, X.Y.; Xu, S.C.; Zhang, X.M.; Lin, H.Y.; Xu, S.; Zhu, S.Y. Effects of temperature and salinity on Ruppia sinensis seed germination, seedling establishment, and seedling growth. Mar. Pollut. Bull. 2018, 134, 177–185. [Google Scholar] [CrossRef]
  14. Bai, J.H.; Xiao, R.; Zhang, K.J.; Gao, H.F. Arsenic and heavy metal pollution in wetland soils from tidal freshwater and salt marshes before and after the flow-sediment regulation regime in the Yellow River Delta, China. J. Hydrol. 2012, 450, 244–253. [Google Scholar] [CrossRef]
  15. Song, Z.L.; Sun, Y.Y.; Liu, P.Y.; Wang, Y.B.; Huang, Y.Y.; Gao, Y.; Hu, X.K. Invasion of Spartina alterniflora on Zostera japonica enhances the abundances of bacteria by absolute quantification sequencing analysis. Ecol. Evol. 2022, 12, e8939. [Google Scholar] [CrossRef]
  16. Xiong, C.; Zhu, Y.G.; Wang, J.T.; Singh, B.; Han, L.L.; Shen, J.P.; Li, P.P.; Wang, G.B.; Wu, C.F.; Ge, A.H.; et al. Host selection shapes crop microbiome assembly and network complexity. New Phytol. 2021, 229, 1091–1104. [Google Scholar] [CrossRef]
  17. Wang, S.P.; Yan, Z.G.; Wang, P.Y.; Zheng, X.; Fan, J.T. Comparative metagenomics reveals the microbial diversity and metabolic potentials in the sediments and surrounding seawaters of Qinhuangdao mariculture area. PLoS ONE 2020, 15, e0234128. [Google Scholar] [CrossRef]
  18. Ugarelli, K.; Laas, P.; Stingl, U. The Microbial Communities of Leaves and Roots Associated with Turtle Grass (Thalassia testudinum) and Manatee Grass (Syringodium filliforme) are Distinct from Seawater and Sediment Communities, but Are Similar between Species and Sampling Sites. Microorganisms 2019, 7, 4. [Google Scholar] [CrossRef] [Green Version]
  19. Sun, Y.Y.; Song, Z.L.; Zhang, H.K.; Liu, P.Y.; Hu, X.K. Seagrass vegetation affect the vertical organization of microbial communities in sediment. Mar. Environ. Res. 2020, 162, 105174. [Google Scholar] [CrossRef]
  20. Zhang, X.; Zhao, C.Y.; Yu, S.; Jiang, Z.J.; Liu, S.L.; Wu, Y.C.; Huang, X.P. Rhizosphere Microbial Community Structure Is Selected by Habitat but Not Plant Species in Two Tropical Seagrass Beds. Front. Microbiol. 2020, 11, 161. [Google Scholar] [CrossRef] [Green Version]
  21. Ettinger, C.L.; Voerman, S.E.; Lang, J.M.; Stachowicz, J.J.; Eisen, J.A. Microbial communities in sediment from Zostera marina patches, but not the Z. marina leaf or root microbiomes, vary in relation to distance from patch edge. PeerJ 2017, 5, e3246. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  22. Behera, P.; Mahapatra, S.; Mohapatra, M.; Kim, J.Y.; Adhya, T.K.; Raina, V.; Suar, M.; Pattnaik, A.K.; Rastogi, G. Salinity and macrophyte drive the biogeography of the sedimentary bacterial communities in a brackish water tropical coastal lagoon. Sci. Total Environ. 2017, 595, 472–485. [Google Scholar] [CrossRef] [PubMed]
  23. Goldfarb, K.C.; Karaoz, U.; Hanson, C.A.; Santee, C.A.; Bradford, M.A.; Treseder, K.K.; Wallenstein, M.D.; Brodie, E.L. Differential growth responses of soil bacterial taxa to carbon substrates of varying chemical recalcitrance. Front. Microbiol. 2011, 2, 94. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  24. Sun, F.F.; Zhang, X.L.; Zhang, Q.Q.; Liu, F.H.; Zhang, J.P.; Gong, J. Seagrass (Zostera marina) Colonization Promotes the Accumulation of Diazotrophic Bacteria and Alters the Relative Abundances of Specific Bacterial Lineages Involved in Benthic Carbon and Sulfur Cycling. Appl. Environ. Microbiol. 2015, 81, 6901–6914. [Google Scholar] [CrossRef] [Green Version]
  25. Holmer, M.; Nielsen, S.L. Sediment sulfur dynamics related to biomass-density patterns in Zostera marina (eelgrass) beds. Mar. Ecol. Prog. Ser. 1997, 146, 163–171. [Google Scholar] [CrossRef]
  26. Holmer, M.; Andersen, F.O.; Nielsen, S.L.; Boschker, H.T.S. The importance of mineralization based on sulfate reduction for nutrient regeneration in tropical seagrass sediments. Aquat. Bot. 2001, 71, 1–17. [Google Scholar] [CrossRef]
  27. Panno, L.; Bruno, M.; Voyron, S.; Anastasi, A.; Gnavi, G.; Miserere, L.; Varese, G.C. Diversity, ecological role and potential biotechnological applications of marine fungi associated to the seagrass Posidonia oceanica. New Biotechnol. 2013, 30, 685–694. [Google Scholar] [CrossRef]
  28. Zhang, Y.Z.; Xu, J.; Riera, N.; Jin, T.; Li, J.Y.; Wang, N. Huanglongbing impairs the rhizosphere-to-rhizoplane enrichment process of the citrus root-associated microbiome. Microbiome 2017, 5, 97. [Google Scholar] [CrossRef]
  29. Fahimipour, A.K.; Kardish, M.R.; Lang, J.M.; Green, J.L.; Eisen, J.A.; Stachowicz, J.J. Global-Scale Structure of the Eelgrass Microbiome. Appl. Environ. Microbiol. 2017, 83, e03391-16. [Google Scholar] [CrossRef] [Green Version]
  30. Liu, F.D.; Mo, X.; Kong, W.J.; Song, Y. Soil bacterial diversity, structure, and function of Suaeda salsa in rhizosphere and non-rhizosphere soils in various habitats in the Yellow River Delta, China. Sci. Total Environ. 2020, 740, 140144. [Google Scholar] [CrossRef]
  31. Shang, S.; Li, L.Y.; Zhang, Z.W.; Zang, Y.; Chen, J.; Wang, J.; Wu, T.; Xia, J.B.; Tang, X.X. The Effects of Secondary Growth of Spartina alterniflora after Treatment on Sediment Microorganisms in the Yellow River Delta. Microorganisms 2022, 10, 1722. [Google Scholar] [CrossRef] [PubMed]
  32. Logue, J.B.; Stedmon, C.A.; Kellerman, A.M.; Nielsen, N.J.; Andersson, A.F.; Laudon, H.; Lindstrom, E.S.; Kritzberg, E.S. Experimental insights into the importance of aquatic bacterial community composition to the degradation of dissolved organic matter. ISME J. 2016, 10, 533–545. [Google Scholar] [CrossRef] [PubMed] [Green Version]
  33. Shang, S.; Hu, S.X.; Liu, X.X.; Zang, Y.; Chen, J.; Gao, N.; Li, L.Y.; Wang, J.; Liu, L.X.; Xu, J.K.; et al. Effects of Spartina alterniflora invasion on the community structure and diversity of wetland soil bacteria in the Yellow River Delta. Ecol. Evol. 2022, 12, e8905. [Google Scholar] [CrossRef] [PubMed]
  34. Bolyen, E.; Rideout, J.R.; Dillon, M.R.; Bokulich, N.A.; Abnet, C.C.; Al-Ghalith, G.A.; Alexander, H.; Alm, E.J.; Arumugam, M.; Asnicar, F.; et al. Reproducible, interactive, scalable and extensible microbiome data science using QIIME 2. Nat. Biotechnol. 2019, 37, 852–857, Erratum in Nat. Biotechnol. 2019, 37, 1091. [Google Scholar] [CrossRef] [PubMed]
  35. McMurdie, P.J.; Holmes, S. phyloseq: An R Package for Reproducible Interactive Analysis and Graphics of Microbiome Census Data. PLoS ONE 2013, 8, e61217. [Google Scholar] [CrossRef] [PubMed] [Green Version]
Figure 1. Alpha diversity of bacterial communities. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. (a): Shannon index; (b): Simpson index; (c): ACE index; (d): Chao1 index. Different colored squares represent different groups. Statistical analysis was performed using the student’s t-test.
Figure 1. Alpha diversity of bacterial communities. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. (a): Shannon index; (b): Simpson index; (c): ACE index; (d): Chao1 index. Different colored squares represent different groups. Statistical analysis was performed using the student’s t-test.
Plants 12 01435 g001
Figure 2. Alpha diversity of fungal community. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. (a): Shannon index; (b): Simpson index; (c): ACE index; (d): Chao1 index. Different colored squares represent different groups. Statistical analysis was performed using the student’s t-test.
Figure 2. Alpha diversity of fungal community. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. (a): Shannon index; (b): Simpson index; (c): ACE index; (d): Chao1 index. Different colored squares represent different groups. Statistical analysis was performed using the student’s t-test.
Plants 12 01435 g002
Figure 3. PCoA showing the bacterial (a) and fungal (b) community structure; RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. Different colored ellipsoids represent different groups.
Figure 3. PCoA showing the bacterial (a) and fungal (b) community structure; RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. Different colored ellipsoids represent different groups.
Plants 12 01435 g003
Figure 4. PERMANOVA analysis among different groups. The R-value is closer to 1, indicating that the difference between groups is more significant than the difference within groups; the smaller R-value indicates no significant difference between and within groups. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples.
Figure 4. PERMANOVA analysis among different groups. The R-value is closer to 1, indicating that the difference between groups is more significant than the difference within groups; the smaller R-value indicates no significant difference between and within groups. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples.
Plants 12 01435 g004
Figure 5. Venn diagrams showing the shared and unique bacterial (a) and fungal (b) ASVs among RS, BS and SW groups. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. Each circle represents sampled compartments. Values within intersections represent shared ASVs, values outside intersections represent unique ASVs.
Figure 5. Venn diagrams showing the shared and unique bacterial (a) and fungal (b) ASVs among RS, BS and SW groups. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples. Each circle represents sampled compartments. Values within intersections represent shared ASVs, values outside intersections represent unique ASVs.
Plants 12 01435 g005
Figure 6. Relative abundance of bacterial (a,c) and fungal (b,d) communities at the phylum (a,b) and genus (c,d) level. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples.
Figure 6. Relative abundance of bacterial (a,c) and fungal (b,d) communities at the phylum (a,b) and genus (c,d) level. RS: the seagrass rhizosphere soil samples; BS: sediment samples; SW: seawater samples.
Plants 12 01435 g006
Table 1. Changes in the environmental factors among the BS, RS, and SW groups.
Table 1. Changes in the environmental factors among the BS, RS, and SW groups.
GroupsTOC (g/kg)TS (g/kg)ECpH
BS3.208 ± 0.297 a0.44 ± 0.19 a66.22 ± 6.40 a7.81 ± 0.48 b
RS3.096 ± 0.735 a1.25 ± 0.40 a37.66 ± 7.03 b7.74 ± 0.16 b
SW--13.46 ± 0.40 c8.60 ± 0.09 a
Values are the means ± standard error (n = 5). Lowercase letters in the same column indicate significant differences between the two groups (p < 0.05).
Disclaimer/Publisher’s Note: The statements, opinions and data contained in all publications are solely those of the individual author(s) and contributor(s) and not of MDPI and/or the editor(s). MDPI and/or the editor(s) disclaim responsibility for any injury to people or property resulting from any ideas, methods, instructions or products referred to in the content.

Share and Cite

MDPI and ACS Style

Shang, S.; Li, L.; Xiao, H.; Chen, J.; Zang, Y.; Wang, J.; Tang, X. Studies on the Composition and Diversity of Seagrass Ruppia sinensis Rhizosphere Mmicroorganisms in the Yellow River Delta. Plants 2023, 12, 1435. https://doi.org/10.3390/plants12071435

AMA Style

Shang S, Li L, Xiao H, Chen J, Zang Y, Wang J, Tang X. Studies on the Composition and Diversity of Seagrass Ruppia sinensis Rhizosphere Mmicroorganisms in the Yellow River Delta. Plants. 2023; 12(7):1435. https://doi.org/10.3390/plants12071435

Chicago/Turabian Style

Shang, Shuai, Liangyu Li, Hui Xiao, Jun Chen, Yu Zang, Jun Wang, and Xuexi Tang. 2023. "Studies on the Composition and Diversity of Seagrass Ruppia sinensis Rhizosphere Mmicroorganisms in the Yellow River Delta" Plants 12, no. 7: 1435. https://doi.org/10.3390/plants12071435

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop