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Distribution of Fe-oxidizing bacteria in the coastal wetland of the northern East China Sea and their responses to variations in oxygen penetration depth
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Wenlong QI, Lei SU, Zhonglin MA, Peng WANG, Jiangtao LI*
Acta Microbiologica Sinica | 2024, 64(6) : 1704 - 1720
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Acta Microbiologica Sinica | 2024, 64(6): 1704-1720
Marine Microbiome Involved in Element Cycling
Distribution of Fe-oxidizing bacteria in the coastal wetland of the northern East China Sea and their responses to variations in oxygen penetration depth
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Wenlong QI, Lei SU, Zhonglin MA, Peng WANG, Jiangtao LI*
Affiliations
  • State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
Published: 2024-06-04 doi: 10.13343/j.cnki.wsxb.20240021
Outline
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[Objective] Coastal wetland ecosystems, situated at the interface of freshwater and seawater, are characterized by the seepage of groundwater with high Fe2+ concentrations into the surface layers of sediments, which forms wetland runoff. This runoff, combined with periodic tidal flooding, creates an oxic-anoxic interface conducive to the bio-oxidation of Fe2+ by Fe-oxidizing bacteria. However, there is a lack of comprehensive assessment of Fe-oxidizing bacterial communities in coastal wetland ecosystems. [Methods] We measured the basic environmental parameters such as the oxygen penetration depth in the sediments of five coastal wetland sites in Xisha Wetland Park in Chongming, Shanghai and Dongsha Beach in Zhujiajian Island in Zhoushan, Zhejiang. The community composition and distribution of bacteria and Fe-oxidizing bacteria were comprehensively deciphered by 16S rRNA gene amplicon sequencing. [Results] Dongsha Beach in Zhujiajian Island exhibited deeper oxygen penetration (reaching more than 10 mm) than Xisha Wetland in Chongming. The non-metric multidimensional scaling (NMDS) results indicated that the bacterial community structure was primarily influenced by environmental conditions that varied with geographical location, while the community structure of Fe-oxidizing bacteria was influenced by both the geographical location of the sampling sites and the oxygen penetration depth of the sediments. The dominant bacteria in Xisha Wetland and Dongsha Beach wereCyanobacteria,Gammaproteobacteria,Bacteroidetes,Alphaproteobacteria, andActinobacteria. The dominant genera of Fe-oxidizing bacteria wereGallionella,Rhodobacter,Lepthothrix, andSideroxydans. [Conclusion] We studied the Fe-oxidizing bacteria in the sediments of Xisha Wetland in Chongming and Dongsha Beach in Zhujiajian Island and discovered that the composition of Fe-oxidizing bacterial communities was closely linked to the oxygen penetration depth variations caused by different types of wetland sediments.

Xisha Wetland in Chongming  /  Dongsha Beach in Zhujiajian Island  /  coastal wetlands  /  oxygen penetration depth  /  Fe-oxidizing bacteria
Wenlong QI, Lei SU, Zhonglin MA, Peng WANG, Jiangtao LI. Distribution of Fe-oxidizing bacteria in the coastal wetland of the northern East China Sea and their responses to variations in oxygen penetration depth[J]. Acta Microbiologica Sinica, 2024 , 64 (6) : 1704 -1720 . DOI: 10.13343/j.cnki.wsxb.20240021
  • National Natural Science Foundation of China(42072333)
Year 2024 volume 64 Issue 6
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Article Info
doi: 10.13343/j.cnki.wsxb.20240021
  • Receive Date:2024-01-08
  • Online Date:2026-03-19
  • Published:2024-06-04
Article Data
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History
  • Received:2024-01-08
  • Accepted:2024-03-08
Funding
National Natural Science Foundation of China(42072333)
Affiliations
    State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

Corresponding:

*LI Jiangtao, E-mail:
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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