Carbonate mineral saturation states in the East China Sea: present conditions and future scenarios

被引:42
作者
Chou, W. -C. [1 ]
Gong, G. -C. [1 ,2 ,3 ]
Hung, C. -C. [4 ]
Wu, Y. -H. [1 ]
机构
[1] Natl Taiwan Ocean Univ, Inst Marine Environm Chem & Ecol, Keelung 202, Taiwan
[2] Natl Taiwan Ocean Univ, Ctr Excellence Oceans, Keelung 202, Taiwan
[3] Taiwan Ocean Res Inst, Natl Appl Res Labs, Kaohsiung 852, Taiwan
[4] Natl Sun Yat Sen Univ, Inst Marine Geol & Chem, Kaohsiung 804, Taiwan
关键词
CHANGJIANG YANGTZE-RIVER; OCEAN ACIDIFICATION; CONTINENTAL-SHELF; COASTAL; SEAWATER; DIOXIDE; CO2; IMPACT; WATERS; EUTROPHICATION;
D O I
10.5194/bg-10-6453-2013
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
To assess the impact of rising atmospheric CO2 and eutrophication on the carbonate chemistry of the East China Sea shelf waters, saturation states (Omega) for two important biologically relevant carbonate minerals - calcite (Omega(c)) and aragonite (Omega(a)) - were calculated throughout the water column from dissolved inorganic carbon (DIC) and total alkalinity (TA) data collected in spring and summer of 2009. Results show that the highest Omega(c) (similar to 9.0) and Omega(a) (similar to 5.8) values were found in surface water of the Changjiang plume area in summer, whereas the lowest values (Omega(c) =similar to 2.7 and Omega(a) =similar to 1.7) were concurrently observed in the bottom water of the same area. This divergent behavior of saturation states in surface and bottom waters was driven by intensive biological production and strong stratification of the water column. The high rate of phytoplankton production, stimulated by the enormous nutrient discharge from the Changjiang, acts to decrease the ratio of DIC to TA, and thereby increases Omega values. In contrast, remineralization of organic matter in the bottom water acts to increase the DIC to TA ratio, and thus decreases Omega values. The projected result shows that continued increases of atmospheric CO2 under the IS92a emission scenario will decrease Omega values by 40-50% by the end of this century, but both the surface and bottom waters will remain supersaturated with respect to calcite and aragonite. Nevertheless, superimposed on such Omega decrease is the increasing eutrophication, which would mitigate or enhance the Omega decline caused by anthropogenic CO2 uptake in surface and bottom waters, respectively. Our simulation reveals that, under the combined impact of eutrophication and augmentation of atmospheric CO2, the bottom water of the Changjiang plume area will become undersaturated with respect to aragonite (Omega(a) =similar to 0.8) by the end of this century, which would threaten the health of the benthic ecosystem.
引用
收藏
页码:6453 / 6467
页数:15
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