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The sources and burial fluxes of sedimentary organic carbon from the intensive mariculture zone in Haizhou Bay, China

文献类型： 外文期刊

作者： Tan, Liushuyi 1 ; Liu, Yi 1 ; Ren, Jeffrey S. 2 ; Zhang, Jihong 1 ;

作者机构： 1.Chinese Acad Fishery Sci, Yellow Sea Fisheries Res Inst, Qingdao 266071, Shandong, Peoples R China

2.Laoshan Lab, Funct Lab Marine Fisheries Sci & Food Prod Proc, Qingdao 266237, Peoples R China

3.Natl Inst Water & Atmospher Res, 10 Kyle St,POB 8602, Christchurch 8440, New Zealand

关键词： Sediment; Mariculture; Organic carbon; Sources; Burial fluxes; MixSIAR

期刊名称：MARINE POLLUTION BULLETIN （ 影响因子：4.9； 五年影响因子：5.6 ）

ISSN： 0025-326X

年卷期： 2025 年 218 卷

页码：

收录情况： SCI

摘要： The rapid development of mariculture would cause a considerable impact on the coastal carbon cycle. For investigating the source and contribution of mariculture to sedimentary organic matter, the composition of sediment cores in Haizhou Bay were analyzed, including 210Pbex activity, sedimentary total organic carbon (TOC), total nitrogen (TN), the stable carbon (delta 13C) and nitrogen (delta 15N) isotopic composition. The sediment accumulation rate in mariculture area varied between 1.7 and 2.8 cm center dot a-1, which is significantly higher than in control site. The results of the MixSIAR isotope mixing model indicated that shellfish biodeposits and soil organic matter are the primary contributors of sedimentary organic matter (SOM), while marine phytoplankton and seaweeds played a lesser role in the study area. The contribution of shellfish biodeposits to SOM in SF-1, SF-2 and BS were 4.1-36.65 %, 4.7-50.31 % and 5.2-19.0 %, respectively. The terrestrial source were the main contributors in the early years, have been affected by the impact of mariculture activities, and their contribution has gradually declined. The OC burial fluxes from shellfish biodeposits (BFbiodepositis) in SF-1 (6.17-23.82 g center dot m-2 center dot a-1), SF-2 (7.62-79.71 g center dot m-2 center dot a-1) and BS (2.9-15.25 g center dot m-2 center dot a-1) tended to increase with the increasing scale of mariculture. Intensive shellfish mariculture influenced the sediment carbon sources and burial fluxes in coastal organic carbon cycles.

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