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Manganese, iron and sulfur diagenesis and diffusive fluxes of porewater iron and manganese in sediments of Laizhou Bay, Bohai Sea
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Beibei Sun1, Jianhua Ren1, Jiawei Zhang1, Wenxuan Sun1, Tie Li1, Maoxu Zhu1, *
Haiyang Xuebao | 2024, 46(9) : 96 - 108
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Haiyang Xuebao | 2024, 46(9): 96-108
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Manganese, iron and sulfur diagenesis and diffusive fluxes of porewater iron and manganese in sediments of Laizhou Bay, Bohai Sea
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Beibei Sun1, Jianhua Ren1, Jiawei Zhang1, Wenxuan Sun1, Tie Li1, Maoxu Zhu1, *
Affiliations
  • 1. Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China
Published: 2024-09-01 doi: 10.12284/hyxb2024116
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Based on analyses of solid-phase and porewater chemistry of sediment cores at four sites collected from Laizhou Bay of the Bohai Sea, we revealed diagenetic cycles of iron, manganese and sulfur and their responses to terrestrial inputs and anthropogenic perturbations. Results suggest that water eutrophication of the bay has not given rise to organic carbon (OC) enrichment in the sediments. Actually, contents and lability of sediment OC are generally low, largely due to the inputs of terrestrial refractory OC and intense sediment resuspension induced by natural processes and anthropogenic perturbations in the river-dominated area. This feature greatly dampens sulfate reduction, resulting in low accumulation of total reduced inorganic sulfide (0.28−88 μmol/g). Porewater Mn2+ is mainly from reductive dissolution of amorphous and poorly crystalline Mn oxides, while precipitation of MnCO3 is mainly responsible for Mn2+ consumption in sediment below 10 cm depth. Intense sediment resuspension and refractory nature of sediment OC encourage dissimilatory iron reduction, with relative contribution of this pathway to total anaerobic OC mineralization of about 51%, on average. At the site (S6) heavily influenced by the Huanghe River input, dynamic depositional regime facilitates reductive dissolution of manganese oxides, but dampens reduction of iron oxides and sulfate to some extent. Upward diffusive fluxes of porewater Mn2+ and Fe2+ in the sediments are at the lower end for sediments of other areas dominated by major river inputs, which is attributable to overall low lability of sediment OC.

Diagenesis  /  porewater  /  sulfide  /  diffusive flux  /  marine sediment  /  iron  /  manganese  /  Laizhou Bay
Beibei Sun, Jianhua Ren, Jiawei Zhang, Wenxuan Sun, Tie Li, Maoxu Zhu. Manganese, iron and sulfur diagenesis and diffusive fluxes of porewater iron and manganese in sediments of Laizhou Bay, Bohai Sea[J]. Haiyang Xuebao, 2024 , 46 (9) : 96 -108 . DOI: 10.12284/hyxb2024116
Year 2024 volume 46 Issue 9
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doi: 10.12284/hyxb2024116
  • Receive Date:2024-04-20
  • Online Date:2025-11-26
  • Published:2024-09-01
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  • Received:2024-04-20
  • Revised:2024-06-11
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    1. Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, 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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