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MA Wang,LIU Youcai,ZHANG Qian, et al. Density Zoning and Formation Mechanism of Seagrass Beds in Caofeidian Based on Spatial Heterogeneity Analysis[J]. Haiyang Xuebao,2026, 48(x):1–13
Citation: MA Wang,LIU Youcai,ZHANG Qian, et al. Density Zoning and Formation Mechanism of Seagrass Beds in Caofeidian Based on Spatial Heterogeneity Analysis[J]. Haiyang Xuebao,2026, 48(x):1–13

Density Zoning and Formation Mechanism of Seagrass Beds in Caofeidian Based on Spatial Heterogeneity Analysis

  • Received Date: 2025-12-19
  • Rev Recd Date: 2026-01-26
  • Available Online: 2026-02-13
  • Taking the Caofeidian seagrass bed—the largest existing seagrass bed in China—as the research object, this study adopted a combined method of remote sensing interpretation, field investigation, and model analysis to carry out research on the quantitative zoning of density and the formation mechanism of spatial heterogeneity of the Caofeidian seagrass bed. Through the interpretation of high-resolution satellite remote sensing images and combined with on-site field verification, the quantitative data of three core zoning types under the spatial pattern of “dense in the north and sparse in the south” of the Caofeidian seagrass bed were obtained, namely the dense area (with an area of 7.31 km2, accounting for 18.34%), the moderately dense area (with an area of 10.36 km2, accounting for 26.00%), and the sparse area (with an area of 22.18 km2, accounting for 55.66%). On the whole, it shows the characteristics of patchy mosaic distribution. Based on 10 environmental data items (including illumination, ammonium, and sediment density) obtained from field investigations, an MLP-ANN (Multilayer Perceptron-Artificial Neural Network) model was used for analysis, and it was found that the internal friction angle of sediment (contribution: 18%), water temperature (contribution: 15%), and sediment phosphate (contribution: 15%) were the core driving factors affecting the density zoning of the seagrass bed, with a cumulative influence accounting for 48%. The research results indicated that the density zoning of the Caofeidian seagrass bed is formed by thejoint effect of natural dynamic factors and human activities: in the southern region, strong tidal currents cause sediment scouring, and superimposed on the impacts of engineering activities such as oilfield exploration and channel dredging, as well as land-based pollution, forming the degradation chain of “sediment disturbance - nutrient imbalance”; the northern region is far from these disturbance sources, and through ecological restoration, the sediment conditions have been optimized, thus providing support for the formation of the medium-to-high density seagrass bed areas. This study fills the gaps in the quantitative research on the density zoning of the Caofeidian seagrass bed and the research on its formation mechanism, and provides a scientific basis and technical paradigm for the scientific assessment and effective restoration of seagrass beds in the Bohai Bay.
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