首页> 外文期刊>Coral reefs: journal of the International Society for Reef Studies >Incorporating benthic community changes into hydrochemical-based projections of coral reef calcium carbonate production under ocean acidification
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Incorporating benthic community changes into hydrochemical-based projections of coral reef calcium carbonate production under ocean acidification

机译:在海洋酸化作用下,将底栖生物群落的变化纳入基于水化学的珊瑚礁碳酸钙产量预测中

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摘要

The existence of coral reefs is dependent on the production and maintenance of calcium carbonate (CaCO3) framework that is produced through calcification. The net production of CaCO3 will likely decline in the future, from both declining net calcification rates (decreasing calcification and increasing dissolution) and shifts in benthic community composition from calcifying organisms to non-calcifying organisms. Here, we present a framework for hydrochemical studies that allows both declining net calcification rates and changes in benthic community composition to be incorporated into projections of coral reef CaCO3 production. The framework involves upscaling net calcification rates for each benthic community type using mapped proportional cover of the benthic communities. This upscaling process was applied to the reef flats at One Tree and Lady Elliot reefs (Great Barrier Reef) and Shiraho Reef (Okinawa), and compared to existing data. Future CaCO3 budgets were projected for Lady Elliot Reef, predicting a decline of 53 % from the present value by end-century (800 ppm CO2) without any changes to benthic community composition. A further 5.7 % decline in net CaCO3 production is expected for each 10 % decline in calcifier cover, and net dissolution is predicted by end-century if calcifier cover drops below 18 % of the present extent. These results show the combined negative effect of both declining net calcification rates and changing benthic community composition on reefs and the importance of considering both processes for determining future reef CaCO3 production.
机译:珊瑚礁的存在取决于钙化产生的碳酸钙(CaCO3)骨架的产生和维持。 CaCO3的净产量将来可能会下降,既有净钙化率下降(钙化减少和溶出度增加),也有底栖生物的组成从钙化生物向非钙化生物转变。在这里,我们为水化学研究提供了一个框架,该框架允许将下降的净钙化速率和底栖生物群落组成的变化纳入珊瑚礁CaCO3产量的预测中。该框架涉及使用底栖生物群落的比例覆盖图来提高每种底栖生物群落类型的净钙化率。此升级过程已应用于One Tree和Elliot夫人礁(大堡礁)和Shiraho礁(冲绳)的礁滩,并与现有数据进行了比较。预计Lady Elliot Reef的未来CaCO3预算将预测到本世纪末(800 ppm CO2)比现值下降53%,而底栖动物群落组成没有任何变化。钙化器覆盖率每下降10%,预计净CaCO3产量将进一步下降5.7%,如果钙化器覆盖率下降至当前水平的18%以下,则净水溶出率将由世纪末预测。这些结果表明,净钙化率下降和底栖生物群落组成的变化对珊瑚礁的综合负面影响,以及考虑两种确定未来珊瑚礁CaCO3产量的方法的重要性。

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