江苏省海门牡蛎礁空间分布特征及碳效应研究

    Spatial distribution characteristics and carbon effects of oyster reefs in Haimen, Jiangsu Province

    • 摘要: 为探究江苏海门牡蛎礁对海洋碳汇能力的影响,本研究建立了牡蛎礁碳储量估算模型,分析了牡蛎礁空间分布特征及其碳储量的时空变化特征,并估算了牡蛎礁的固碳潜力。结果表明,牡蛎礁的碳储量和分布特征受多种因素影响,表现出明显的空间异质性,其中,各层总碳和无机碳含量分布较不均匀,有机碳含量分布较均匀;牡蛎礁基底沉积物有机碳含量分布较均匀,沉积物总体波动较大,钻孔垂向呈减少—增加—减少趋势;基于碳储量变化的方法和现场监测数据,江苏海门牡蛎礁的固碳量估算为1.37 kg/m2。牡蛎礁可以通过钙化、生物同化和生物沉积三大过程显著增强海洋碳汇能力,其中,钙化过程封存的碳量尤为突出,为提升海洋生态系统碳汇能力提供了新的视角和方法。

       

      Abstract: Under the context of the spatial distribution characteristics and carbon effects of oyster reefs in Haimen, this study aims to explore the influence of Jiangsu Haimen oyster reefs on marine carbon sequestration capacity. A carbon storage estimation model for oyster reefs was established to analyze their spatial distribution patterns and the spatiotemporal variations in carbon storage, as well as to estimate their carbon sequestration potential. The results indicate that oyster reef carbon storage and distribution are influenced by multiple factors, exhibiting significant spatial heterogeneity. Specifically, the distributions of total carbon and inorganic carbon content across layers are relatively uneven, while organic carbon content shows a more uniform distribution. The organic carbon content in the substrate sediments of oyster reefs is relatively balanced, though overall sediment composition fluctuates considerably, exhibiting a vertical drilling trend of decrease-increase-decrease. Based on carbon storage variation methods and field monitoring data, the estimated carbon sequestration capacity of oyster reefs in Jiangsu Haimen is 1.37 kg/m2. Oyster reefs significantly enhance marine carbon sequestration through three key processes: calcification, biological assimilation, and biodeposition. Among these, the carbon sequestered via calcification is particularly prominent, offering novel perspectives and methodologies for improving carbon sink capacity in marine ecosystems.

       

    /

    返回文章
    返回