三峡库区四种小型鱼类能量溯源及时空差异

ENERGY SOURCE TRACING OF FOUR SMALL-SIZED FISH AND SPATIOTEMPORAL DIFFERENCES IN THE THREE GORGES RESERVOIR AREA

  • 摘要: 为评估在三峡库区食物利用和食物链的营养转化效率, 本研究运用碳氮稳定同位素方法探究了浮游藻类、沿岸带C3植物、C4植物及着生藻类四种基础碳源对银鮈(Squalidus argentatus)、蛇鮈(Saurogobio dabryi)、似鳊(Pseudobrama simoni)和䱗(Hemiculter leucisculus)四种小型鱼类能量贡献比例的时空差异。结果显示, 各种碳源生物的δ13C值和δ15N均存在显著性差异(P<0.05), 能很好的区分各基础碳源。Bayesian混合模型结果表明, 浮游藻类均对四种小型鱼类的能量贡献比例最高, 外源性碳源对小型鱼类能量的贡献率在不同水文时期无显著性差异(P>0.05), 但是在空间尺度上存在极显著性差异(P<0.01)。研究表明, 内源性碳源是库区小型鱼类的主要能量来源, 但外源性碳源对小型鱼类的贡献率在三峡库区河流纵向梯度上有较为明显的变化规律。越靠近库首, 外源性碳源的贡献率越高, 这可能与不同区域消落带的淹没特征和在库首静水环境下外源性碳源颗粒沉积有关。

     

    Abstract: In order to evaluate food utilization and trophic transfer efficiency of the food chain in the Three Gorges Reservoir, stable carbon and nitrogen isotope methods were employed to investigate the spatiotemporal variations in the energy contribution of four fundamental carbon sources-phytoplankton, C3 plants, C4 plants in the riparian zone, and epiphytic algae-to four dominant small fish species, Squalidus argentatus, Saurogobio dabryi, Pseudobrama simoni, and Hemiculter leucisculus. The results indicated significant differences in the δ13C and δ15N values among different carbon source organisms, effectively distinguishing their fundamental carbon sources. The outcomes of the Bayesian mixed model suggested that phytoplankton contributes the highest proportion of energy to the four small fish species. At the hydrological scale, there is no significant difference in the contribution rates of autochthonous and allochthonous carbon sources to the four small fish (P>0.05). However, at the spatial scale, a highly significant difference was observed (P<0.01). This study indicate that autochthonous carbon is the primary energy source for small fish in the reservoir area, while the contribution of allochthonous carbon sources increases noticeably along the longitudinal gradient of the Three Gorges Reservoir. This may be associated with the characteristics of diverse submerged area and the increased sedimentation of exogenous carbon source particles in the quiescent water environment near the reservoir head.

     

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