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漂白作用导致马尔代夫南部珊瑚礁的礁碳酸盐预算和礁生长潜力崩溃。

Bleaching drives collapse in reef carbonate budgets and reef growth potential on southern Maldives reefs.

机构信息

Department of Geography, College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, United Kingdom.

出版信息

Sci Rep. 2017 Jan 13;7:40581. doi: 10.1038/srep40581.

DOI:10.1038/srep40581
PMID:28084450
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5233991/
Abstract

Sea-surface temperature (SST) warming events, which are projected to increase in frequency and intensity with climate change, represent major threats to coral reefs. How these events impact reef carbonate budgets, and thus the capacity of reefs to sustain vertical growth under rising sea levels, remains poorly quantified. Here we quantify the magnitude of changes that followed the ENSO-induced SST warming that affected the Indian Ocean region in mid-2016. Resultant coral bleaching caused an average 75% reduction in coral cover (present mean 6.2%). Most critically we report major declines in shallow fore-reef carbonate budgets, these shifting from strongly net positive (mean 5.92 G, where G = kg CaCO m yr) to strongly net negative (mean -2.96 G). These changes have driven major reductions in reef growth potential, which have declined from an average 4.2 to -0.4 mm yr. Thus these shallow fore-reef habitats are now in a phase of net erosion. Based on past bleaching recovery trajectories, and predicted increases in bleaching frequency, we predict a prolonged period of suppressed budget and reef growth states. This will limit reef capacity to track IPCC projections of sea-level rise, thus limiting the natural breakwater capacity of these reefs and threatening reef island stability.

摘要

与气候变化相伴而来的海表温度(SST)变暖事件预计会越来越频繁且剧烈,对珊瑚礁构成重大威胁。这些事件如何影响珊瑚礁的碳酸盐收支平衡,从而影响珊瑚礁在海平面上升情况下维持垂直生长的能力,目前仍难以量化。本文中,我们量化了 2016 年年中海域厄尔尼诺-南方涛动(ENSO)引发的 SST 变暖事件对印度洋地区的影响。由此产生的珊瑚白化导致珊瑚覆盖率平均减少了 75%(目前的平均值为 6.2%)。最关键的是,我们报告了浅海礁前碳酸盐预算的大幅下降,从强烈的净正(平均 5.92 G,其中 G=kg CaCO m yr)转变为强烈的净负(平均-2.96 G)。这些变化极大地降低了珊瑚礁的生长潜力,从平均 4.2 毫米/年降至-0.4 毫米/年。因此,这些浅海礁前生境现在正处于净侵蚀阶段。基于过去的白化恢复轨迹和预计的白化频率增加,我们预测珊瑚礁的预算和生长状态将长期受到抑制。这将限制珊瑚礁适应海平面上升的能力,从而限制这些珊瑚礁的天然防波堤能力,并威胁到珊瑚礁岛的稳定性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/ad0405edce97/srep40581-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/6e7f327722e1/srep40581-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/e2747a177491/srep40581-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/48d79b76be5d/srep40581-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/ad0405edce97/srep40581-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/6e7f327722e1/srep40581-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/e2747a177491/srep40581-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/48d79b76be5d/srep40581-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a437/5233991/ad0405edce97/srep40581-f4.jpg

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