首页> 外文期刊>Coral reefs: journal of the International Society for Reef Studies >Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia
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Spatial and temporal variations in turbidity on two inshore turbid reefs on the Great Barrier Reef, Australia

机译:澳大利亚大堡礁的两个近岸混浊礁石浊度的时空变化

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This study describes the natural turbidity regimes at two inshore turbid reefs on the central Great Barrier Reef where wind-driven waves are the main agent of sediment resuspension. Many corals on inshore turbid reefs have adapted to high and fluctuating turbidity, however, anthropogenic activities such as dredging are speculated to produce larger and more prolonged turbidity events that may exceed the environmental tolerance and adaptive capacity of corals on these reefs. Natural turbidity regimes must be described and understood to determine whether and when coral communities on inshore turbid reefs are at risk from anthropogenically elevated turbidity, but at present few baseline studies exist. Here, we present turbidity data from (a) Middle Reef, a semi-protected reef located between Magnetic Island and Townsville and (b) Paluma Shoals, a reef exposed to higher energy wind and waves located in Halifax Bay. Instruments were deployed on both reefs for 16 days to measure spatial and temporal variations in turbidity and its driving forces (waves, currents, tides). Locally driven wind waves were the key driver of turbidity, but the strength of the relationship was dependent on wave exposure. Turbidity regimes thus vary markedly over individual reefs and this is reflected in community assemblage distributions, with a high abundance of heterotrophic corals (e. g. Goniopora) in reef habitats subjected to large fluctuations in turbidity (>100 NTU). A turbidity model developed using local wind speed data explained up to 75 % and up to 46 % of the variance in turbidity at Paluma Shoals and Middle Reef, respectively. Although the model was based on a brief two-week observational period, it reliably predicted variations in 24-h averaged turbidity and identified periods when turbidity rose above ambient baseline levels, offering reef managers insights into turbidity responses to modified climate and coastal sediment delivery regimes.
机译:这项研究描述了大堡礁中部两个近海混浊礁的自然浊度状态,其中风驱波是沉积物重悬浮的主要推动力。近海混浊珊瑚礁上的许多珊瑚已经适应了高而波动的浊度,但是,诸如挖泥等人为活动被推测会产生更大,更长时间的浊度事件,这些事件可能超出这些珊瑚对珊瑚的环境耐受性和适应能力。必须描述和理解自然浊度制度,以确定人为浊度升高对近岸混浊礁石上珊瑚群落是否构成威胁,以及何时使之处于危险之中,但目前尚缺乏基线研究。在这里,我们提供以下数据的浊度数据:(a)中层礁石,位于磁岛和汤斯维尔之间的半保护礁石;以及(b)Paluma浅滩,礁石暴露于位于哈利法克斯湾的高能风和海浪中。仪器在两个礁石上部署了16天,以测量浊度及其驱动力(波浪,水流,潮汐)的时空变化。局部驱动的风波是浊度的主要驱动因素,但这种关系的强度取决于波的暴露程度。因此,各个珊瑚礁的混浊度显着不同,这反映在群落的分布上,在混浊度波动较大(> 100 NTU)的珊瑚礁栖息地中,异养珊瑚(如Goniopora)的数量很多。使用当地风速数据开发的浊度模型分别解释了帕卢马浅滩和中礁的浊度变化分别达到75%和46%。尽管该模型基于短暂的两周观测期,但它可以可靠地预测24小时平均浊度的变化并确定浊度升至高于环境基线水平的时间段,从而为礁石管理者提供洞察力,以了解浊度对修改后的气候和沿海沉积物输送制度的响应。

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