Coral calcification under environmental change: a direct comparison of the alkalinity anomaly and buoyant weight techniques

被引:13
|
作者
Schoepf, Verena [1 ,2 ,3 ]
Hu, Xinping [4 ]
Holcomb, Michael [2 ,3 ,5 ]
Cai, Wei-Jun [6 ,7 ]
Li, Qian [7 ,8 ]
Wang, Yongchen [7 ]
Xu, Hui [7 ,9 ]
Warner, Mark E. [10 ]
Melman, Todd F. [11 ]
Hoadley, Kenneth D. [10 ]
Pettay, D. Tye [10 ]
Matsui, Yohei [1 ]
Baumann, Justin H. [1 ,12 ]
Grottoli, Andrea G. [1 ]
机构
[1] Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA
[2] Univ Western Australia, UWA Oceans Inst, ARC Ctr Excellence Coral Reef Studies, Crawley, WA, Australia
[3] Univ Western Australia, Sch Earth & Environm, Crawley, WA, Australia
[4] Texas A&M Univ Corpus Christi, Dept Phys & Environm Sci, Corpus Christi, TX 78412 USA
[5] Woods Hole Oceanog Inst, Dept Marine Geol & Geophys, Woods Hole, MA 02543 USA
[6] Univ Delaware, Sch Marine Sci & Policy, Newark, DE USA
[7] Univ Georgia, Dept Marine Sci, Athens, GA 30602 USA
[8] Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen, Peoples R China
[9] Zhejiang Univ, Dept Marine Sci, Hangzhou, Zhejiang, Peoples R China
[10] Univ Delaware, Sch Marine Sci & Policy, Lewes, DE 19958 USA
[11] Reef Syst Coral Farm, New Albany, OH USA
[12] Univ North Carolina Chapel Hill, Dept Marine Sci, Chapel Hill, NC USA
基金
美国国家科学基金会;
关键词
Calcification; Buoyant weight; Alkalinity anomaly; Method comparison; Ocean acidification; Incubation; CARBONATE-ION CONCENTRATION; ASTRANGIA POCULATA; REEF COMMUNITIES; WATER MOTION; PHOTOSYNTHESIS; GROWTH; TEMPERATURE; DIOXIDE; PCO(2); LIGHT;
D O I
10.1007/s00338-016-1507-z
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
Two primary methods-the buoyant weight (BW) and alkalinity anomaly (AA) techniques-are currently used to quantify net calcification rates (G) in scleractinian corals. However, it remains unclear whether they are directly comparable since the few method comparisons conducted to date have produced inconsistent results. Further, such a comparison has not been made for tropical corals. We directly compared G (BW) and G (AA) in four tropical and one temperate coral species cultured under various pCO(2), temperature, and nutrient conditions. A range of protocols for conducting alkalinity depletion incubations was assessed. For the tropical corals, open-top incubations with manual stirring produced G (AA) that were highly correlated with and not significantly different from G (BW). Similarly, G (AA) of the temperate coral was not significantly different from G (BW) when incubations provided water motion using a pump, but were significantly lower than G (BW) by 16% when water motion was primarily created by aeration. This shows that the two techniques can produce comparable calcification rates in corals but only when alkalinity depletion incubations are conducted under specific conditions. General recommendations for incubation protocols are made, especially regarding adequate water motion and incubation times. Further, the re-analysis of published data highlights the importance of using appropriate regression statistics when both variables are random and measured with error. Overall, we recommend the AA technique for investigations of community and short-term day versus night calcification, and the BW technique to measure organism calcification rates integrated over longer timescales due to practical limitations of both methods. Our findings will facilitate the direct comparison of studies measuring coral calcification using either method and thus have important implications for the fields of ocean acidification research and coral biology in general.
引用
收藏
页码:13 / 25
页数:13
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