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Projected Reorganization of Florida Bay Seagrass Communities in Response to the Increased Freshwater Inflow of Everglades Restoration

机译:计划对佛罗里达湾海草群落进行重组,以应对增加的大沼泽地恢复淡水

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摘要

Historic changes in water-use management in the Florida Everglades have caused the quantity of freshwater inflow to Florida Bay to decline by approximately 60% while altering its timing and spatial distribution. Two consequences have been (1) increased salinity throughout the bay, including occurrences of hypersalinity, coupled with a decrease in salinity variability, and (2) change in benthic habitat structure. Restoration goals have been proposed to return the salinity climates (salinity and its variability) of Florida Bay to more estuarine conditions through changes in upstream water management, thereby returning seagrass species cover to a more historic state. To assess the potential for meeting those goals, we used two modeling approaches and long-term monitoring data. First, we applied the hydrological mass balance model FATHOM to predict salinity climate changes in sub-basins throughout the bay in response to a broad range of freshwater inflow from the Everglades. Second, because seagrass species exhibit different sensitivities to salinity climates, we used the FATHOM-modeled salinity climates as input to a statistical discriminant function model that associates eight seagrass community types with water quality variables including salinity, salinity variability, total organic carbon, total phosphorus, nitrate, and ammonium, as well as sediment depth and light reaching the benthos. Salinity climates in the western sub-basins bordering the Gulf of Mexico were insensitive to even the largest (5-fold) modeled increases in freshwater inflow. However, the north, northeastern, and eastern sub-basins were highly sensitive to freshwater inflow and responded to comparatively small increases with decreased salinity and increased salinity variability. The discriminant function model predicted increased occurrences of Halodule wrightii communities and decreased occurrences of Thalassia testudinum communities in response to the more estuarine salinity climates. The shift in community composition represents a return to the historically observed state and suggests that restoration goals for Florida Bay can be achieved through restoration of freshwater inflow from the Everglades.
机译:佛罗里达大沼泽地的用水管理发生了历史性变化,导致流入佛罗里达湾的淡水量减少了约60%,同时改变了时间和空间分布。有两个后果(1)整个海湾盐度增加,包括高盐度的发生,以及盐度变异性的降低,以及(2)底栖生境结构的变化。提出了恢复目标,通过改变上游水管理,使佛罗里达湾的盐度气候(盐度及其多变性)恢复到更多的河口条件,从而使海草物种的覆盖度恢复到更历史的状态。为了评估实现这些目标的潜力,我们使用了两种建模方法和长期监测数据。首先,我们应用水文质量平衡模型FATHOM来预测整个海湾响应来自大沼泽地的大量淡水流入而发生变化的盐碱化气候变化。其次,由于海草物种对盐度气候表现出不同的敏感性,因此我们使用FATHOM模型的盐度气候作为统计判别函数模型的输入,该模型将八种海草群落类型与水质变量相关联,包括盐度,盐度变异性,总有机碳,总磷,硝酸盐和铵盐,以及到达底栖生物的沉积物深度和光线。与墨西哥湾接壤的西部次流域的盐度气候对最大的(5倍)模型的淡水流入量都不敏感。但是,北部,东北和东部子流域对淡水流入高度敏感,并且对盐度降低和盐度变异性增加的相对较小的增加做出了响应。判别函数模型预测,随着河口盐碱化气候的增加,Whalodule wrightii群落的发生率增加,而Thalassia testudinum群落的发生率下降。群落组成的转变代表着向历史观察状态的回归,表明佛罗里达湾的恢复目标可以通过恢复大沼泽地的淡水来实现。

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