地球科学进展 doi: 10.11867/j.issn.1001-8166.2025.095

   

陆源输入驱动下中国陆架海水环境变化与赤潮风险评估和环境管理研究进展
冉祥滨1,2,钟晓松1,王昊3,朱卓毅4   
  1. (1. 自然资源部第一海洋研究所,海洋生物资源与环境研究中心,山东 青岛 266061;2. 青岛海洋科技中心,海洋地质过程与环境功能实验室,山东 青岛 266061;3.Deltares 研究院,代尔夫特 2600 MH,荷兰;4. 上海交通大学 海洋学院,上海 200030)
  • 基金资助:
    国家重点研发计划课题(编号:2024YFF0506903);国家自然科学基金项目(编号:42106048,42506031)资助.

Research Progress on Water Environmental Changes, Red Tide Risk Assessment, and Management in the Chinese Continental Shelf Driven by Terrestrial Input

RAN Xiangbin1, 2, ZHONG Xiaosong1, WANG Hao3, ZHU Zhuoyi4   

  1. (1. Marine Bioresource and Environment Research Centre, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China; 2. Laboratory for Marine Geology, Qingdao Marine Science and Technology Center, Qingdao 266237, China; 3. Deltares, Delft, 2600 MH, Netherlands; 4. Shanghai Jiao Tong University, School of Oceanography, Shanghai 200030, China)
  • About author:RAN Xiangbin, Senior Research, research areas include the land-to-sea transport of nutrients and its ecological effects. E-mail: rxb@fio.org.cn
  • Supported by:
    Project supported by the National Key Research and Development Program of China (Grant No. 2024YFF0506903); National Natural Science Foundation of China (Grant No. 42106048 and 42506031).
中国陆架海作为人类活动深度影响的典型海域,生态环境变化显著,对深化海洋学认知与推动海洋环境保护研究及资源开发具有重要的科学意义和实践价值。近年来,随着人类活动的加剧,该海域营养盐水平和结构发生了显著变化,赤潮(有害藻华,HABs)发生的特征和优势种群呈现出新的演变态势。系统综述了中国陆架海营养盐水平和结构变化与赤潮发生的研究进展,深入剖析了当前生态环境存在的主要问题,并对未来发展方向进行了展望。研究发现,中国陆架海的海洋生态环境演变呈现以下特征:磷的限制性和有机氮磷的作用日益凸显,出现赤潮优势种由硅藻向甲藻转变、在某些海域赤潮与绿潮并发的趋势。这一演变过程既受到陆源输入持续变化的驱动,也受到海洋生态系统自身调节机制的影响,是营养盐水平和结构变化长期累积作用的结果。值得注意的是,陆源营养盐管理与陆架海赤潮发生频率之间存在明显的时滞效应,其增加了治理效果评估的难度,也对生态风险临界点或阈值的科学设定提出了挑战。尽管中国在营养盐水平和结构演变与赤潮风险研究领域已取得显著进展,但仍面临诸多挑战,特别是长期系统的观测数据积累不足、研究领域的广度和深度有待拓展、陆海相互作用机制尚未完全阐明。未来研究应着重深化陆海耦合过程研究,完善海洋环境监测网络,提升数据处理水平和技术创新能力,特别是明确氮磷管理的阈值和“测—溯—算—治”的系统策略,从而推动中国陆架海洋环境研究向更高水平发展。
Abstract:The Chinese continental shelf, as a region heavily influenced by human activities, has experienced significant ecological and environmental changes. Studying this area is of great scientific and practical importance for advancing oceanographic knowledge and promoting research on marine environmental protection and resource utilization. In recent years, intensified human activities have caused notable alterations in the water environment, with Harmful Algal Blooms (HABs) showing new characteristics and shifts in dominant species. This paper provides a systematic review of research on water environmental changes and HABs occurrences in the Chinese continental shelf, offering a comprehensive analysis of major ecological and environmental challenges and outlining prospects for future research. The findings indicate that the marine ecological environment in this region is increasingly influenced by phosphorus limitation and the roles of organic nitrogen and phosphorus, accompanied by a shift in dominant HABs species from diatoms to dinoflagellates, and, in some areas, the simultaneous occurrence of HABs and green tides. These changes are driven by both ongoing alterations in terrestrial inputs and intrinsic self-regulatory mechanisms within the marine ecosystem, reflecting the cumulative effects of long-term environmental changes. Notably, there is a significant time lag between reductions in terrestrial pollution and decreases in HABs frequency, complicating the evaluation of management effectiveness and challenging the scientific determination of ecological risk thresholds or tipping points. Despite considerable progress in understanding water environmental evolution and HABs risks in China, significant challenges remain, including insufficient long-term and systematic observational data, the need to expand research scope, and incomplete knowledge of land-sea interaction mechanisms. Future research should focus on elucidating land-sea coupling processes, enhancing marine environmental monitoring networks, improving data processing and technological innovation, and clarifying nitrogen and phosphorus management thresholds while developing integrated strategies encompassing monitoring, tracing, calculation, and management. These efforts are crucial for advancing marine environmental research in the Chinese continental shelf.

中图分类号: 

[1] 邓文文, 王荣, 刘正文, 郑文秀, 张晨雪. 模型揭示的浅水湖泊稳态转换影响因素分析[J]. 地球科学进展, 2021, 36(1): 83-94.
[2] 黄小平,江志坚. 海草床食物链有机碳传递过程的研究进展[J]. 地球科学进展, 2019, 34(5): 480-487.
[3] 邹银洪, 张润宇, 陈敬安, 王立英, 陆顶盘. 黏土矿物在富营养化水体和底泥磷污染控制中的应用研究进展[J]. 地球科学进展, 2018, 33(6): 578-589.
[4] 林晓娟, 高姗, 仉天宇, 刘桂梅. 海水富营养化评价方法的研究进展与应用现状[J]. 地球科学进展, 2018, 33(4): 373-384.
[5] 杨永琼,陈敬安,王敬富,曾艳. 沉积物磷原位钝化技术研究进展[J]. 地球科学进展, 2013, 28(6): 674-684.
[6] 陈莹,庄国顺,郭志刚. 近海营养盐和微量元素的大气沉降[J]. 地球科学进展, 2010, 25(7): 682-690.
[7] 黄廷林,柴蓓蓓. 水源水库水质污染与富营养化控制技术研究进展[J]. 地球科学进展, 2009, 24(6): 588-596.
[8] 周俊,邓伟,刘伟龙. 沟渠湿地的水文和生态环境效应研究进展[J]. 地球科学进展, 2008, 23(10): 1079-1083.
[9] 秦伯强,王小冬,汤祥明,冯胜,张运林. 太湖富营养化与蓝藻水华引起的饮用水危机——原因与对策[J]. 地球科学进展, 2007, 22(9): 896-906.
[10] 黄海军;李凡. 黄河三角洲海岸带陆海相互作用概念模式[J]. 地球科学进展, 2004, 19(5): 808-816.
[11] 赵生才. 我国湖泊富营养化的发生机制与控制对策[J]. 地球科学进展, 2004, 19(1): 138-140.
[12] 魏皓,赵亮,武建平. 浮游植物动力学模型及其在海域富营养化研究中的应用[J]. 地球科学进展, 2001, 16(2): 220-225.
[13] 陈 尚,朱明远,马 艳,李瑞香,李宝华,吕瑞华. 富营养化对海洋生态系统的影响及其围隔实验研究[J]. 地球科学进展, 1999, 14(6): 571-576.
[14] 李明,施永辉. 欧洲陆一海相互作用研究(ELOISE)科学计划及研究领域[J]. 地球科学进展, 1996, 11(5): 475-480.
[15] 李凡. 海岸带陆海相互作用(LOICZ)研究及我们的策略[J]. 地球科学进展, 1996, 11(1): 19-23.
阅读次数
全文


摘要