Australian Institute of Marine Science, Oceans Institute, University of Western Australia, Crawley, Australia.
PLoS One. 2011;6(10):e25536. doi: 10.1371/journal.pone.0025536. Epub 2011 Oct 31.
The Symbiodinium community associated with scleractinian corals is widely considered to be shaped by seawater temperature, as the coral's upper temperature tolerance is largely contingent on the Symbiodinium types harboured. Few studies have challenged this paradigm as knowledge of other environmental drivers on the distribution of Symbiodinium is limited. Here, we examine the influence of a range of environmental variables on the distribution of Symbiodinium associated with Acropora millepora collected from 47 coral reefs spanning 1,400 km on the Great Barrier Reef (GBR), Australia.
METHODOLOGY/PRINCIPAL FINDINGS: The environmental data included Moderate Resolution Imaging Spectroradiometer (MODIS) satellite data at 1 km spatial resolution from which a number of sea surface temperature (SST) and water quality metrics were derived. In addition, the carbonate and mud composition of sediments were incorporated into the analysis along with in situ water quality samples for a subset of locations. Analyses were conducted at three spatio-temporal scales [GBR (regional-scale), Whitsunday Islands (local-scale) and Keppel Islands/Trunk Reef (temporal)] to examine the effects of scale on the distribution patterns. While SST metrics were important drivers of the distribution of Symbiodinium types at regional and temporal scales, our results demonstrate that spatial variability in water quality correlates significantly with Symbiodinium distribution at local scales. Background levels of Symbiodinium types were greatest at turbid inshore locations of the Whitsunday Islands where SST predictors were not as important. This was not the case at regional scales where combinations of mud and carbonate sediment content coupled with SST anomalies and mean summer SST explained 51.3% of the variation in dominant Symbiodinium communities.
CONCLUSIONS/SIGNIFICANCE: Reef corals may respond to global-scale stressors such as climate change through changes in their resident symbiont communities, however, management of local-scale stressors such as altered water quality is also necessary for maintenance of coral-Symbiodinium associations.
与石珊瑚相关的共生藻群落被广泛认为是由海水温度塑造的,因为珊瑚的温度耐受上限在很大程度上取决于其所含的共生藻类型。由于关于影响共生藻分布的其他环境驱动因素的知识有限,很少有研究对这一范式提出挑战。在此,我们研究了一系列环境变量对从澳大利亚大堡礁(GBR)1400公里范围内47个珊瑚礁采集的多孔鹿角珊瑚相关共生藻分布的影响。
方法/主要发现:环境数据包括空间分辨率为1公里的中分辨率成像光谱仪(MODIS)卫星数据,从中得出了一些海表温度(SST)和水质指标。此外,沉积物的碳酸盐和泥质成分以及部分地点的现场水质样本也被纳入分析。分析在三个时空尺度上进行[大堡礁(区域尺度)、圣灵群岛(局部尺度)和凯珀尔群岛/树干礁(时间尺度)],以研究尺度对分布模式的影响。虽然SST指标在区域和时间尺度上是共生藻类型分布的重要驱动因素,但我们的结果表明,水质的空间变异性与局部尺度上的共生藻分布显著相关。在圣灵群岛浑浊的近岸地点,共生藻类型的背景水平最高,而在这些地点SST预测指标并不那么重要。在区域尺度上情况并非如此,泥质和碳酸盐沉积物含量的组合,加上SST异常和夏季平均SST,解释了优势共生藻群落51.3%的变化。
结论/意义:珊瑚礁珊瑚可能通过其共生生物群落的变化来应对气候变化等全球尺度的压力源,然而,管理局部尺度的压力源,如水质变化,对于维持珊瑚 - 共生藻的共生关系也是必要的。