School of Ocean Sciences, Bangor University, UK.
School of Ocean Sciences, Bangor University, UK.
Mar Environ Res. 2022 Jan;173:105520. doi: 10.1016/j.marenvres.2021.105520. Epub 2021 Nov 6.
The distribution and organisation of benthic organisms on tropical reefs are typically heterogenous yet display distinct zonation patterns across depth gradients. However, there are few datasets which inform our understanding of how depth zonation in benthic community composition varies spatially among and within different reef systems. Here, we assess the depth zonation in benthic forereef slope communities in the Central Indian Ocean, prior to the back-to-back bleaching events in 2014-2017. We compare benthic communities between shallow (5-10 m) and deep (20-25 m) sites, at two spatial scales: among and within 4 atolls. Our analyses showed the variation in both major functional groups and hard coral assemblages between depth varied among atolls, and within-atoll comparisons revealed distinct differences between shallow and deep forereef slope communities. Indicator taxa analyses characterising the hard coral community between depths revealed a higher number of coral genera characteristic of the deep forereef slopes (10) than the shallow forereef slopes (6). Only two coral genera consistently associated with both depths across all atolls, and these were Acropora and Porites. Our results reveal spatial variation in depth zonation of benthic communities, potentially driven by biophysical processes varying across depths and atolls, and provide a baseline to understand and measure the impacts of future global climate change on benthic communities across depths.
热带珊瑚礁上底栖生物的分布和组织通常是异质的,但在深度梯度上表现出明显的分带模式。然而,很少有数据集可以让我们了解底栖生物群落组成在不同珊瑚系统之间和内部的深度分带如何在空间上变化。在这里,我们评估了 2014-2017 年背靠背白化事件之前印度洋中部的前礁坡底栖生物的深度分带情况。我们在两个空间尺度上比较了浅水区(5-10 米)和深水区(20-25 米)的底栖群落:在四个环礁之间。我们的分析表明,主要功能组和硬珊瑚组合在不同环礁之间以及环礁内的深度变化存在差异,浅水区和深水区前礁坡群落之间存在明显差异。在深度之间表征硬珊瑚群落的指示分类群分析显示,深前礁坡(10 个)的珊瑚属数量高于浅前礁坡(6 个)。只有两个珊瑚属在所有环礁中都与两个深度一致相关,它们是 Acropora 和 Porites。我们的结果揭示了底栖生物群落深度分带的空间变化,这可能是由不同深度和环礁的生物物理过程驱动的,并为了解和衡量未来全球气候变化对不同深度底栖生物群落的影响提供了基线。