School of Environment, the University of Auckland, Auckland, 1010, New Zealand.
Department of Earth Sciences, Simon Fraser University, Burnaby, BC, Canada.
Sci Rep. 2019 Apr 24;9(1):6515. doi: 10.1038/s41598-019-42985-2.
Coral reefs experienced the third global bleaching event in 2015-2016 due to high sea-surface temperature (SST) anomalies. Declines in net carbonate production associated with coral bleaching are implicated in reef structural collapse and cascading impacts for adjacent coral reef islands. We present the first carbonate budget study of a reef platform surface (reef crest and reef flat) in the southern Maldives and the first record of upper reef flat condition in the central Indian Ocean post the 2015-2016 coral bleaching event. Scleractinian corals were the primary carbonate producers, with live coral cover averaging between 11.1 ± 6.5 and 31.2 ± 21.8% and dominated by massive corals. Gross carbonate production rates averaged 5.9 ± 2.5 G (kg CaCO m yr). Bioerosion was estimated at 3.4 ± 0.4 G, resulting in an average net carbonate production rate of 2.5 ± 2.4 G. Comparison of results with a study of the fore-reef slope highlights major differences in post-bleaching carbonate budget state between the fore-reef slope and the reef platform surface. The positive reef flat carbonate budget is attributed to the persistence of massive corals (Porites spp. and Heliopora spp.) through the bleaching event.
珊瑚礁在 2015-2016 年经历了第三次全球白化事件,这是由于海面温度(SST)异常升高所致。与珊瑚白化相关的净碳酸盐产量下降,导致珊瑚礁结构崩溃,并对相邻珊瑚礁岛屿产生级联影响。我们首次对马尔代夫南部的珊瑚礁平台表面(珊瑚礁顶和礁坪)进行了碳酸盐收支研究,并首次记录了 2015-2016 年珊瑚白化事件后印度洋中部上层礁坪的状况。石珊瑚是主要的碳酸盐生产者,活珊瑚覆盖率平均在 11.1±6.5%至 31.2±21.8%之间,以块状珊瑚为主。总碳酸盐生产速率平均为 5.9±2.5 G(kg CaCO m yr)。生物侵蚀估计为 3.4±0.4 G,导致平均净碳酸盐生产速率为 2.5±2.4 G。将结果与前礁坡的研究进行比较,突出了前礁坡和珊瑚礁平台表面之间白化后碳酸盐预算状态的主要差异。珊瑚礁坪的碳酸盐收支呈正值,这归因于块状珊瑚(Porites spp. 和 Heliopora spp.)在白化事件中的持续存在。