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Spatial and temporal variations in sediment accumulation and their impacts on coral communities in the Sanya Coral Reef Reserve, Hainan, China

机译:中国海南三亚珊瑚礁保护区泥沙淤积的时空变化及其对珊瑚群落的影响

摘要

This study investigated the spatial and temporal variations of sediment accumulation and their impacts on coral communities in four sites at two or three depths (3 m, 6 m and 9 m) at the Sanya Coral Reef Reserve by deploying sediment traps on the sea floor during 2007-2009. Rainfall and typhoon events, which appeared to control sediment accumulation in the sea floor of the coral reef, were positively correlated with total sediment and sand-sized (i.e. 63-2000 mu m) sediment accumulation. Sediment accumulation rate significantly decreased with the distance far away from the coast in Sanya. The mean sediment accumulation rates in Ximaozhou, Luhuitou and Xiaodonghai during 2007 to 2009 were close to 20 mg cm(-2) d(-1), and they were significantly higher than that in Yalongwan, probably as a result of terrestrial soil erosion caused by strong coast human activities (e.g. coastal construction, dredging and hillside clearing). Correlation analysis revealed that silt-clay-sized sediment accumulation rate was highly negatively correlated with total live coral cover and coral cover in some taxa, such as Montipora and branching Porites. whereas, Diploastrea heliopora was positively correlated with silt-clay-sized sediment accumulation. Correlation analysis also suggested that silt-clay-sized sediment accumulation had a higher efficiency in predicting the spatial variation of total live coral cover in Sanya than did the total sediment accumulation. Based on this investigation, we conclude that high rates of sediment accumulation pose a severe threat to the Sanya Coral Reef Reserve, highlighting the importance of integrated watershed management practices in the Sanya Coral Reef Reserve. (C) 2013 Elsevier Ltd. All rights reserved.
机译:这项研究通过在三亚珊瑚礁保护区在海底部署捕集器,调查了三亚珊瑚礁保护区两个或三个深度(3 m,6 m和9 m)的四个地点的沉积物积聚的时空变化及其对珊瑚群落的影响。 2007-2009。降雨和台风事件似乎控制着珊瑚礁海床中的沉积物积累,与总沉积物和沙粒大小(即63-2000微米)的沉积物积累呈正相关。距三亚海岸的距离越远,泥沙的沉积率就明显降低。 2007年至2009年,西芒州,鹿回头和小东海的平均泥沙堆积率接近20 mg cm(-2)d(-1),并且明显高于亚龙湾,这可能是由于陆地水土流失引起的。通过强烈的海岸人类活动(例如,海岸建设,疏ging和清理山坡)。相关分析表明,淤泥粘土大小的沉积物积累率与某些生物分类中的总活珊瑚覆盖率和珊瑚覆盖率呈负相关,如Montipora和分支的Porites。而Diploastrea heliopora与淤泥粘土大小的沉积物正相关。相关分析还表明,淤泥粘土大小的沉积物比三亚沉积物具有更高的预测三亚总活珊瑚覆盖率空间变化的效率。根据这项调查,我们得出的结论是,高沉积物积累对三亚珊瑚礁保护区构成了严重威胁,突出了在三亚珊瑚礁保护区进行集水区综合管理做法的重要性。 (C)2013 Elsevier Ltd.保留所有权利。

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