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Dong H, He H, Wang M. Community Structure, Assembly and Interactions of Nitrospira Nitrite-Oxidizing Bacteria in Sediments of the Eastern China Marginal Seas. Microorganisms 2025; 13:1112. [PMID: 40431285 PMCID: PMC12114128 DOI: 10.3390/microorganisms13051112] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/10/2025] [Revised: 05/09/2025] [Accepted: 05/09/2025] [Indexed: 05/29/2025] Open
Abstract
Nitrite oxidation, a pivotal process in the nitrogen cycle driven by microorganisms, is primarily carried out by nitrite-oxidizing bacteria (NOB). While extensive studies on Nitrospira have been conducted in terrestrial habitats, knowledge of Nitrospira in marine sediments remains limited. Therefore, we employed high-throughput sequencing analysis to systematically explore the community structure, assembly processes and potential interactions of Nitrospira in the eastern China marginal seas. Our results exhibit pronounced spatial heterogeneity in Nitrospira communities across seas. Widespread distribution of Nitrospira taxa was observed, with Nitrospira lineage II emerging as the most important group in this study. Based on the neutral community model (NCM), normalized stochasticity ratio (NST) and beta nearest-taxon-index (βNTI) analysis, deterministic processes predominantly shaped the community assembly of Nitrospira. Complex interspecies interactions among Nitrospira were observed with molecular ecological network analysis, and the community in the East China Sea showed the highest complexity, while the community displayed the greatest stability in the South Yellow Sea. In addition, the Nitrospira communities were notably influenced by geographic distances and environmental factors, including salinity, temperature, dissolved oxygen concentration and dissolved inorganic nutrient concentration. These results may expand our understanding of Nitrospira in marine environments and enhance our insights into the marine nitrogen cycle.
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Affiliation(s)
- Hao Dong
- College of Marine Life Sciences, Key Laboratory of Evolution & Marine Biodiversity (Ministry of Education) and Institute of Evolution & Marine Biodiversity, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266003, China; (H.D.); (M.W.)
| | - Hui He
- College of Marine Life Sciences, Key Laboratory of Evolution & Marine Biodiversity (Ministry of Education) and Institute of Evolution & Marine Biodiversity, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266003, China; (H.D.); (M.W.)
| | - Min Wang
- College of Marine Life Sciences, Key Laboratory of Evolution & Marine Biodiversity (Ministry of Education) and Institute of Evolution & Marine Biodiversity, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266003, China; (H.D.); (M.W.)
- Haide College, Ocean University of China, Qingdao 266100, China
- UMT-OUC Joint Academic Centre for Marine Studies, Ocean University of China, Qingdao 266003, China
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Jiang L, Zeng F, Wang G, Deng Z, Zhou H, Chen C, Mu Q, Bu K, Zhou S, Zhang C, Dai Y. Occurrence, source, and microbial-driven fate of aliphatic and polycyclic aromatic hydrocarbons in sediments in the Magellan seamount region. MARINE POLLUTION BULLETIN 2025; 213:117645. [PMID: 39923686 DOI: 10.1016/j.marpolbul.2025.117645] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/25/2024] [Revised: 11/22/2024] [Accepted: 02/03/2025] [Indexed: 02/11/2025]
Abstract
Deep-sea sediments, like those in the Mariana Basin, hold various contaminants, including petroleum hydrocarbons. However, little is known about their distribution, potential risks, sources, and fate. This study analyzed 38 surface sediments and 3 sediment cores, finding ∑n-alkanes and ∑PAHs concentrations at 705.43 ± 22.93 and 37.73 ± 1.62 ng/g dw, respectively. Hydrocarbons posed minimal risks and likely originated from aquatic (n-alkanes) and pyrogenic (PAHs) sources. Microbial activity, especially in deeper layers, influenced hydrocarbon degradation, with the deepest layer showing the highest degradation potential, highlighting microbial roles in hydrocarbon transformation in deep-sea sediments. Overall, this work carries out the sources, hazards, and biological removal of hydrocarbons from deep-sea sediments and facilitates the exploration of the life cycle of organic pollutants in extreme environments.
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Affiliation(s)
- Lingbo Jiang
- Zhoushan Institute for Food and Drug Control, Zhoushan 316021, Zhejiang, China
| | - Feng Zeng
- Ocean College, Zhejiang University, Zhoushan 316021, Zhejiang, China
| | - Guoquan Wang
- Zhejiang Marine Ecology and Environment Monitoring Center, Hangzhou 310012, Zhejiang, China
| | - Zhaochao Deng
- Ocean College, Zhejiang University, Zhoushan 316021, Zhejiang, China; Ocean Research Center of Zhoushan, Zhejiang University, Zhoushan 316021, China
| | - Hanghai Zhou
- Institute of Environment Resource and Soil Fertilizer, Zhejiang Academy of Agricultural Sciences, Hangzhou 310021, Zhejiang, China
| | - Chunlei Chen
- Ocean College, Zhejiang University, Zhoushan 316021, Zhejiang, China
| | - Qinglin Mu
- Zhejiang Marine Ecology and Environment Monitoring Center, Hangzhou 310012, Zhejiang, China
| | - Kuiyong Bu
- Xinjiang Keli New Technology Development Co., Ltd., Karamay 834000, Xinjiang, China
| | - Shaoxiong Zhou
- Xinjiang Keli New Technology Development Co., Ltd., Karamay 834000, Xinjiang, China
| | - Chunfang Zhang
- Ocean College, Zhejiang University, Zhoushan 316021, Zhejiang, China.
| | - Yifei Dai
- Zhoushan Institute for Food and Drug Control, Zhoushan 316021, Zhejiang, China.
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Zhao S, Hu X, Li H, Zhang H, Lu J, Li Y, Chen Z, Bao M. Diversity and structure of pelagic microbial community in Kuroshio Extension. MARINE ENVIRONMENTAL RESEARCH 2024; 201:106697. [PMID: 39205358 DOI: 10.1016/j.marenvres.2024.106697] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/27/2024] [Revised: 07/27/2024] [Accepted: 08/15/2024] [Indexed: 09/04/2024]
Abstract
Kuroshio Extension (KE) is the most active region of oceanic change in the North Pacific Ocean, which provides an essential place for the survival of marine microorganisms. However, Vertical changes in microbial communities in the Kuroshio Extension and the mechanisms by which environmental factors drive vertical changes in community structure remain unclear. In this work, microbial diversity, abundance, and community structure of 12 water layers (from surface to bottom) at five stations were uncovered by 16S rRNA gene high-throughput sequencing. Microbial diversity and richness decreased with increasing seawater depth. Microorganisms in the euphotic zone can be well separated from other zones based on NMDS analysis. Proteobacteria (65.20%), Bacteroidota (8.48%), Actinobacteriota (5.76%), and Crenarchaeota (4.49%) accounted for a relatively large proportion and their distribution is similar in four zones. Most of microorganisms were significantly (Spearman test, p < 0.05) correlated with salinity, density, pressure, and temperature. This work enhances our understanding of vertical microbial diversity and provides insights into the pelagic microbial community structure.
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Affiliation(s)
- Shanshan Zhao
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province, 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province, 266100, China
| | - Xin Hu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province, 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province, 266100, China
| | - Haoshuai Li
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province, 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province, 266100, China
| | - Honghai Zhang
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province, 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province, 266100, China
| | - Jinren Lu
- College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province, 266100, China
| | - Yiming Li
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province, 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province, 266100, China
| | - Zhaohui Chen
- Frontier Science Center for Deep Ocean Multispheres and Earth System (FDOMES) and Physical Oceanography Laboratory, Ocean University of China, Qingdao, China; Laoshan Laboratory, Qingdao, China
| | - Mutai Bao
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province, 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province, 266100, China.
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Hamamoto K, Mizuyama M, Nishijima M, Maeda A, Gibu K, Poliseno A, Iguchi A, Reimer JD. Diversity, composition and potential roles of sedimentary microbial communities in different coastal substrates around subtropical Okinawa Island, Japan. ENVIRONMENTAL MICROBIOME 2024; 19:54. [PMID: 39080706 PMCID: PMC11290285 DOI: 10.1186/s40793-024-00594-1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/25/2024] [Accepted: 07/08/2024] [Indexed: 08/02/2024]
Abstract
BACKGROUND Marine benthic prokaryotic communities play crucial roles in material recycling within coastal environments, including coral reefs. Coastal sedimentary microbiomes are particularly important as potential reservoirs of symbiotic, beneficial, and pathogenic bacteria in coral reef environments, and therefore presumably play a core role in local ecosystem functioning. However, there is a lack of studies comparing different environments with multiple sites on the island scale, particularly studies focusing on prokaryotic communities, as previous investigations have focused mainly on a single site or on specific environmental conditions. In our study, we collected coastal sediments from seven sites around Okinawa Island, Japan, including three different benthic types; sandy bottoms, seagrass meadows, and hard substratum with living scleractinian corals. We then used metabarcoding to identify prokaryotic compositions and estimate enzymes encoded by genes to infer their functions. RESULTS The results showed that the three substrata had significantly different prokaryotic compositions. Seagrass meadow sites exhibited significantly higher prokaryotic alpha-diversity compared to sandy bottom sites. ANCOM analysis revealed that multiple bacterial orders were differentially abundant within each substratum. At coral reef sites, putative disease- and thermal stress-related opportunistic bacteria such as Rhodobacterales, Verrucomicrobiales, and Cytophagales were comparatively abundant, while seagrass meadow sites abundantly harbored Desulfobacterales, Steroidobacterales and Chromatiales, which are common bacterial orders in seagrass meadows. According to our gene-coded enzyme analyses the numbers of differentially abundant enzymes were highest in coral reef sites. Notably, superoxide dismutase, an important enzyme for anti-oxidative stress in coral tissue, was abundant at coral sites. Our results provide a list of prokaryotes to look into in each substrate, and further emphasize the importance of considering the microbiome, especially when focusing on environmental conservation. CONCLUSION Our findings prove that prokaryotic metabarcoding is capable of capturing compositional differences and the diversity of microbial communities in three different environments. Furthermore, several taxa were suggested to be differentially more abundant in specific environments, and gene-coded enzymic compositions also showed possible differences in ecological functions. Further study, in combination with field observations and temporal sampling, is key to achieving a better understanding of the interactions between the local microbiome and the surrounding benthic community.
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Affiliation(s)
- Kohei Hamamoto
- Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki, 305-8567, Japan.
- Molecular Invertebrate Systematics and Ecology (MISE) Laboratory, Graduate School of Engineering and Science, University of the Ryukyus, Nishihara, Okinawa, 903-0213, Japan.
| | - Masaru Mizuyama
- Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki, 305-8567, Japan
- Department of Health Informatics, Faculty of Human Health Sciences, Meio University, Nago, Okinawa, 905-8585, Japan
| | - Miyuki Nishijima
- Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki, 305-8567, Japan
| | - Ayumi Maeda
- Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Chiba, 277-8564, Japan
| | - Kodai Gibu
- Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki, 305-8567, Japan
| | - Angelo Poliseno
- Molecular Invertebrate Systematics and Ecology (MISE) Laboratory, Graduate School of Engineering and Science, University of the Ryukyus, Nishihara, Okinawa, 903-0213, Japan
| | - Akira Iguchi
- Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki, 305-8567, Japan.
- Research Laboratory on Environmentally-Conscious Developments and Technologies [E-code], National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki, 305-8567, Japan.
| | - James Davis Reimer
- Molecular Invertebrate Systematics and Ecology (MISE) Laboratory, Graduate School of Engineering and Science, University of the Ryukyus, Nishihara, Okinawa, 903-0213, Japan
- Tropical Biosphere Research Center, University of the Ryukyus, Nishihara, Okinawa, 903-0213, Japan
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Hu X, Zhao S, Li H, Pan Y, Fan Z, Lu J, Li Y, Song G, Zhang H, Liu Q, Bao M. N-alkane shape distinctive microbial patterns in Kuroshio Extension. ENVIRONMENT INTERNATIONAL 2024; 188:108757. [PMID: 38795659 DOI: 10.1016/j.envint.2024.108757] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/09/2024] [Revised: 05/15/2024] [Accepted: 05/15/2024] [Indexed: 05/28/2024]
Abstract
Marine microorganisms are primary drivers of the elemental cycling. The interaction between heterotrophic prokaryotes and biomarker (n-alkane) in Kuroshio Extension (KE) remains unclear. Here, we categorize KE into three characteristic areas based on ocean temperatures and nutrient conditions: Cold Water Area (CWA), Mixed Area (MA), and Warm Water Area (WWA). A total of 49 samples were collected during two-year voyage to identify the source of n-alkane and associated degrading microorganisms. Total n-alkane concentrations (Σn-Alk) in surface water (SW) spanned from 1,308 ng L-1 to 1,890 ng L-1, it was significantly higher (Tukey-Kramer test, p < 0.05) in MA than CWA and WWA. The Σn-Alk in surface sediments (SS) gradually increased from north to south, ranging from 5,982 ng g-1 to 37,857 ng g-1. Bacteria and algae were the primary sources of n-alkane in both SW and SS. Proteobacteria was the most widely distributed among three areas. The presence of Rhodobacteraceae with alkB was the primary reason affecting n-alkane concentrations in SW. The Gammaproteobacteria with alkB and alkR chiefly affected n-alkane concentrations in SS. In summary, n-alkane s serve as an energy source for particular microorganisms, shaping the unique oceanographic patterns.
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Affiliation(s)
- Xin Hu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Shanshan Zhao
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Haoshuai Li
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Yaping Pan
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Zhongxiang Fan
- Physical Oceanography Laboratory, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Jinren Lu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Yiming Li
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Guodong Song
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Honghai Zhang
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Qian Liu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China
| | - Mutai Bao
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qingdao, Shandong Province 266100, China.
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