海洋酸化与水体净碳酸钙形成/溶解的关系以黄海冷水团为例

Exploring the Relationship Between Net Community Calcification Rate and Ocean Acidification: the Yellow Sea Cold Water Mass as a Case

  • 摘要: 综述了黄海冷水团海洋酸化研究的进展。利用2011年、2013年和2017年在北黄海月际调查获取的碳酸盐体系数据,研究得出,北黄海冷水团的净钙化作用速率与底层水体的文石型碳酸钙饱和度正相关,而北黄海冷水团净碳酸钙生产与净碳酸钙溶解之间的临界阈值是文石型碳酸钙饱和度降至1.5~1.6。这是在中国近海首次建立起水体碳化学参数与碳酸钙过程之间的半定量关系,所确定的动物群落净钙化与净的碳酸钙溶解之间的水化学阈值对我国后续的海洋酸化监测与生态效应评估工作有一定借鉴意义。采用这一阈值,结合国家海洋局北海环境监测中心于1977年至2016年期间在北黄海西侧季节性调查断面获取的实测数据,发现北黄海冷水团的季节性酸化现象已于20世纪末开始威胁底栖贝类的净钙化作用(以秋季的平均文石型碳酸钙饱和度频繁低于1.5为标志),在2010年以后更是发生夏秋两季的海水酸化都严重威胁底栖贝类的情况(即文石型碳酸钙饱和度都低于1.5)。这说明,在我国一些近海海域部署海洋酸化相关的防灾减灾措施的需求已经十分迫切。

     

    Abstract: Some progresses of researches on ocean acidification in the Yellow Sea cold water mass were reviewed. Using the data of carbonate system obtained from monthly surveys in the North Yellow Sea in 2011, 2013 and 2017, it has been revealed that the net community calcification rate of the North Yellow Sea cold water mass is positively correlated to aragonite saturation state in the bottom water. A critical threshold between the net calcium carbonate precipitation and the net calcium carbonate dissolution in the North Yellow Sea cold water mass is the low aragonite saturation state value of 1.5–1.6. This is the first attempt to establish a semi-quantitative relationship between seawater carbonate chemistry parameters and the calcium carbonate process in China seas. The hydrochemical threshold between the net community calcium carbonate precipitation and the net community calcium carbonate dissolution determined in the North Yellow Sea is highly relevant to the upcoming China's ocean-acidification monitoring general project and the ecological effect assessment in the nearest future. Using this threshold value, and based on field measured data (including water temperature, salinity, dissolved oxygen and pH values at different depths) obtained by the North Sea Environmental Monitoring Center of the State Oceanic Administration (China) from 1977 to 2016 along a long-term seasonal surveying section on the west side of the North Yellow Sea, it has been convinced that seasonal acidification in the North Yellow Sea becomes serious since the end of the 20th century, as indicated by the autumnal mean aragonite saturation state of frequently below 1.5. The serious acidification status that threatens benthic shellfish (with an aragonite saturation state of lower than 1.5) and prolongs in both of summer and autumn only occurs after 2010. This change in aquatic chemistry is suggested to be partially responsible for scallop-culturing failures in the northwestern North Yellow Sea in the 2010s. Finally, this review paper highlights the urgent need to lay out disaster prevention and reduction measures in response to ocean acidification in some China seas.

     

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