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Freshwater Detention by Oyster Reefs: Quantifying a Keystone Ecosystem Service

机译:牡蛎礁的淡水滞留:量化基石生态系统服务

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摘要

Oyster reefs provide myriad ecosystem services, including water quality improvement, fisheries and other faunal support, shoreline protection from erosion and storm surge, and economic productivity. However, their role in directing flow during non-storm conditions has been largely neglected. In regions where oyster reefs form near the mouth of estuarine rivers, they likely alter ocean-estuary exchange by acting as fresh water “dams”. We hypothesize that these reefs have the potential to detain fresh water and influence salinity over extensive areas, thus providing a “keystone” ecosystem service by supporting estuarine functions that rely on the maintenance of estuarine (i.e., brackish) conditions in the near-shore environment. In this work, we investigated the effects of shore-parallel reefs on estuarine salinity using field data and hydrodynamic modeling in a degraded reef complex in the northeastern Gulf of Mexico. Results suggested that freshwater detention by long linear chains of oyster reefs plays an important role in modulating salinities, not only in the oysters’ local environment, but over extensive estuarine areas (tens of square kilometers). Field data confirmed the presence of salinity differences between landward and seaward sides of the reef, with long-term mean salinity differences of >30% between sides. Modeled results expanded experimental findings by illustrating how oyster reefs affect the lateral and offshore extent of freshwater influence. In general, the effects of simulated reefs were most pronounced when they were highest in elevation, without gaps, and when riverine discharge was low. Taken together, these results describe a poorly documented ecosystem service provided by oyster reefs; provide an estimate of the magnitude and spatial extent of this service; and offer quantitative information to help guide future oyster reef restoration.
机译:牡蛎礁提供了无数的生态系统服务,包括水质改善,渔业和其他动物保护,保护海岸线免受侵蚀和风暴潮以及经济生产力。然而,在非风暴条件下它们在引导水流中的作用已被大大忽略。在河口附近形成牡蛎礁的地区,它们可能通过充当淡水“水坝”而改变海洋-河口的交换。我们假设这些珊瑚礁有潜力保留淡水并影响广泛地区的盐度,从而通过支持依赖近海环境中河口(咸淡)条件的河口功能来提供“基石”生态系统服务。在这项工作中,我们使用现场数据和流体动力学模型研究了墨西哥湾东北部退化珊瑚礁群中海岸平行礁对河口盐度的影响。结果表明,牡蛎礁的线性长链滞留淡水不仅在牡蛎的当地环境中,而且在广阔的河口地区(数十平方公里),在调节盐度中都起着重要作用。现场数据证实了礁石的陆侧和海侧之间存在盐度差异,两侧之间的长期平均盐度差异大于30%。建模结果通过说明牡蛎礁如何影响淡水影响的横向和近海程度,扩展了实验结果。通常,模拟礁石的海拔高度最高,没有缝隙,河道流量低时,其影响最为明显。综上所述,这些结果说明了牡蛎礁提供的文献资料很少。提供这项服务的规模和空间范围的估计;并提供定量信息,以帮助指导未来的牡蛎礁恢复。

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