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Spatial distribution and influencing factors of organic carbon in surface sediments of the Bohai Sea and Yellow Sea
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Xiaohui Zhai1, 2, Huawei Wang2, Tian Xia2, Jianhua Gao3, Tianyi Nie2, Zijun You2, Xiuqing Song4, Xinxin Li2, 4, *
Haiyang Xuebao | 2025, 47(1) : 13 - 24
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Haiyang Xuebao | 2025, 47(1): 13-24
Article
Spatial distribution and influencing factors of organic carbon in surface sediments of the Bohai Sea and Yellow Sea
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Xiaohui Zhai1, 2, Huawei Wang2, Tian Xia2, Jianhua Gao3, Tianyi Nie2, Zijun You2, Xiuqing Song4, Xinxin Li2, 4, *
Affiliations
  • 1. Shenzhen Marine Development Research Promotion Center, Shenzhen 518052, China
  • 2. Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
  • 3. School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, China
  • 4. Shanghai Sheshan National Geophysical Observatory, Shanghai Earthquake Agency, Shanghai 201602, China
Published: 2025-01-31 doi: 10.12284/hyxb2025012
Outline
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Understanding the distribution and relevant controlling factors of organic carbon in the ocean is of great significance to study the global carbon cycle and tackle climate change. Here, surface sediment samples were collected from the Bohai Sea and the Yellow Sea. For illustrating the source composition, distribution pattern, and their constraints, material characterization such as specific surface area, total organic carbon, nitrogen, sulfur contents and their isotopes (TOC, TN, TS, S2‒, δ13C, δ15N, and δ34S), as well as pigment biomarkers and thermos-gravimetric analysis were conducted. The results showed that the TOC and TN contents were lower in the nearshore but higher in the offshore region due to stronger hydrodynamics nearshore. The specific surface area had significant impacts on the distribution of organic carbon. The sediments contain a mixture of organic carbon from land plants, soil, and marine algae. Three-endmember mixing model suggested that sediments near the Huanghe River mouth and the shallower region along the Liaodong Peninsula in the Bohai Sea were dominated by soil-derived organic carbon with a smaller carbon reactivity index, while marine phytoplankton contributed mostly to the southern Yellow Sea with increasing carbon reactivity index. Significant correlation between TOC and TS in the Bohai Sea and northern Yellow Sea indicated significant linkages between organic carbon degradation and sulfate reduction. The negative δ34S indicated the process of sulfate reduction-sulfide oxidation-seawater sulfate diffusion at the sediment-water interface, which hinted the oxidation of organic carbon from oxic to anoxic condition. Pigment degradation potentially resulted in its weak correlation with the TOC content. As the risk of harmful algal bloom and hypoxia is becoming more severe, it is essential to monitor the coupling relationship of water chemistry and elemental cycling in the sediment to comprehensively understand the role of the continental shelf on organic carbon burial.

Bohai Sea and Yellow Sea  /  surface sediments  /  organic carbon  /  sulfur isotope  /  pigment  /  thermo-gravimetric analysis
Xiaohui Zhai, Huawei Wang, Tian Xia, Jianhua Gao, Tianyi Nie, Zijun You, Xiuqing Song, Xinxin Li. Spatial distribution and influencing factors of organic carbon in surface sediments of the Bohai Sea and Yellow Sea[J]. Haiyang Xuebao, 2025 , 47 (1) : 13 -24 . DOI: 10.12284/hyxb2025012
Year 2025 volume 47 Issue 1
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Article Info
doi: 10.12284/hyxb2025012
  • Receive Date:2024-01-05
  • Online Date:2025-11-10
  • Published:2025-01-31
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History
  • Received:2024-01-05
  • Revised:2024-08-12
Funding
Affiliations
    1. Shenzhen Marine Development Research Promotion Center, Shenzhen 518052, China
    2. Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
    3. School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, China
    4. Shanghai Sheshan National Geophysical Observatory, Shanghai Earthquake Agency, Shanghai 201602, China
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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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