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Coral skeletal geochemistry as a monitor of inshore water quality

机译:珊瑚骨骼地球化学作为近岸水质的监测器

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Coral reefs maintain extraordinary biodiversity and provide protection from tsunamis and storm surge, but inshore coral reef health is degrading in many regions due to deteriorating water quality. Deconvolving natural and anthropogenic changes to water quality is hampered by the lack of long term, dated water quality data but such records are required for forward modelling of reef health to aid their management. Reef corals provide an excellent archive of high resolution geochemical (trace element) proxies that can span hundreds of years and potentially provide records used through the Holocene. Hence, geochemical proxies in corals hold great promise for understanding changes in ancient water quality that can inform broader oceanographic and climatic changes in a given region. This article reviews and highlights the use of coral-based trace metal archives, including metal transported from rivers to the ocean, incorporation of trace metals into coral skeletons and the current 'state of the art' in utilizing coral trace metal proxies as tools for monitoring various types of local and regional source-specific pollution (river discharge, land use changes, dredging and dumping, mining, oil spills, antifouling paints, atmospheric sources, sewage). The three most commonly used coral trace element proxies (i.e., Ba/Ca, Mn/Ca, and Y/Ca) are closely associated with river runoff in the Great Barrier Reef, but considerable uncertainty remains regarding their complex biogeochemical cycling and controlling mechanisms. However, coral-based water quality reconstructions have suffered from a lack of understanding of so-called vital effects and early marine diagenesis. The main challenge is to identify and eliminate the influence of extraneous local factors in order to allow accurate water quality reconstructions and to develop alternate proxies to monitor water pollution. Rare earth elements have great potential as they are self-referencing and reflect basic terrestrial input.
机译:珊瑚礁保持着非凡的生物多样性,并提供了抵御海啸和风暴潮的保护,但是由于水质恶化,许多地区的沿海珊瑚礁健康状况正在下降。缺乏长期的,过时的水质数据阻碍了自然和人为改变水质的变化,但是对珊瑚礁健康进行正向建模以帮助其管理需要这些记录。珊瑚礁提供了一个高分辨率的地球化学(痕量元素)代理的优良档案,其历史可以跨越数百年,并有可能提供通过全新世使用的记录。因此,珊瑚中的地球化学替代物对于理解古代水质的变化具有广阔的前景,这些变化可以为特定地区的海洋和气候变化提供信息。本文回顾并重点介绍了基于珊瑚的痕量金属档案的使用,包括从河流到海洋的金属运输,将痕量金属纳入珊瑚骨架以及利用珊瑚痕量金属代理作为监测工具的当前“最新技术”各种类型的本地和区域源特定污染(河流排放,土地用途变化,疏dr和倾倒,采矿,漏油,防污涂料,大气源,污水)。三种最常用的珊瑚微量元素代理(即Ba / Ca,Mn / Ca和Y / Ca)与大堡礁的河流径流密切相关,但其复杂的生物地球化学循环和控制机制仍存在很大不确定性。然而,基于珊瑚的水质重建缺乏对所谓的重要影响和早期海洋成岩作用的了解。主要挑战是识别并消除外部因素的影响,以实现准确的水质重建并开发替代代理来监控水污染。稀土元素具有自参考功能,可以反映地面的基本输入,因此具有巨大的潜力。

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