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Sedimentary geochemical records and their indications for environmental variations in Bohai Bay
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Yimeng Gou1, Dongyan Liu1, 2, Xiaowei Dong3, Yang Tan4, Masqué Pere5, Chengfeng Xue6, Yujue Wang1, 2, *
Haiyang Xuebao | 2024, 46(9) : 14 - 28
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Haiyang Xuebao | 2024, 46(9): 14-28
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Sedimentary geochemical records and their indications for environmental variations in Bohai Bay
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Yimeng Gou1, Dongyan Liu1, 2, Xiaowei Dong3, Yang Tan4, Masqué Pere5, Chengfeng Xue6, Yujue Wang1, 2, *
Affiliations
  • 1. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
  • 2. Institute of Eco-Chongming, Shanghai 200241, China
  • 3. Beijing Osees Technology Co., Ltd, Beijing 100083, China
  • 4. Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, China
  • 5. Edith Cowan University, Joondalup, WA6027, Australia
  • 6. Second Institute of Oceanography, MNR, Hangzhou 310012, China
Published: 2024-09-01 doi: 10.12284/hyxb2024076
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In order to understand the long−term variations in the nutritional environment and the key influencing factors of Bohai Bay, sediment cores from the mouth of the bay (BH15) and the outer area of the bay (BH47) were collected in April and June 2018 separately. The contents of total organic carbon (TOC), total nitrogen (TN), phosphorus (P), biogenic silica (BSi), and stable isotopes of carbon and nitrogen (δ13C, δ15N) were analyzed, and the causes of the changes of the above parameters were discussed in combination with the changes of climate and surrounding human activities. The results showed that the TN content in both sediment cores exhibited an increasing trend since the 1980s, which is consistent with the long-term variations in dissolved inorganic nitrogen (DIN) in the sea water. Sewage discharge, fertilizer application and mariculture are the main sources of nitrogen in the Bohai Bay, among which the input of agricultural fertilizer has decreased since 2007, while the discharge of mariculture and domestic sewage into the sea has shown a continuous upward trend. Inorganic Phosphorus (IP) was the main form of phosphorus in sediments. The IP in BH15 in the bay has shown a decreasing trend since the mid-1990s, while the IP in BH47 from the mouth of the bay has shown a decreasing trend after 1970s and a slow increasing trend since 1990s. All of them show obvious terrigenous input characteristics. The results of TOC/TN ratio、δ13C value and δ13C two-endmember mixing model indicated that the sediment organic matter in the mouth of Bohai Bay and adjacent sea area was influenced by both terrestrial input and marine autochthonous sources, with marine organic matter being the dominant source, the contribution of marine organic matter has decreased Since the 1990s. Compared with the BH47 core from the mouth of the bay, the BH15 core is closer to the coastal area, more significantly affected by terrestrial input, with higher TN content and contribution of terrestrial organic matter. This study shows that in order to effectively manage the water environment of Bohai Bay, it is necessary to strengthen the control of mariculture and domestic sewage discharge into the sea while controlling the use of agricultural fertilizers in the future.

biogenic elements  /  isotope tracer  /  environmental change  /  sedimentary records of Bohai Bay
Yimeng Gou, Dongyan Liu, Xiaowei Dong, Yang Tan, Masqué Pere, Chengfeng Xue, Yujue Wang. Sedimentary geochemical records and their indications for environmental variations in Bohai Bay[J]. Haiyang Xuebao, 2024 , 46 (9) : 14 -28 . DOI: 10.12284/hyxb2024076
Year 2024 volume 46 Issue 9
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Article Info
doi: 10.12284/hyxb2024076
  • Receive Date:2023-12-25
  • Online Date:2025-11-26
  • Published:2024-09-01
Article Data
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History
  • Received:2023-12-25
  • Revised:2024-03-29
Funding
Affiliations
    1. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China
    2. Institute of Eco-Chongming, Shanghai 200241, China
    3. Beijing Osees Technology Co., Ltd, Beijing 100083, China
    4. Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, China
    5. Edith Cowan University, Joondalup, WA6027, Australia
    6. Second Institute of Oceanography, MNR, Hangzhou 310012, 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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