Marine Spatial Ecology Lab, School of Biological Sciences, The University of Queensland, St. Lucia, Queensland, Australia
Australian Research Council Centre of Excellence for Coral Reef Studies, St. Lucia, Queensland, Australia.
Proc Biol Sci. 2018 Nov 7;285(1890):20182063. doi: 10.1098/rspb.2018.2063.
Understanding the dynamics of habitat-forming organisms is fundamental to managing natural ecosystems. Most studies of coral reef dynamics have focused on clear-water systems though corals inhabit many turbid regions. Here, we illustrate the key drivers of an inshore coral reef ecosystem using 10 years of biological, environmental, and disturbance data. Tropical cyclones, crown-of-thorns starfish, and coral bleaching are recognized as the major drivers of coral loss at mid- and offshore reefs along the Great Barrier Reef (GBR). In comparison, little is known about what drives temporal trends at inshore reefs closer to major anthropogenic stress. We assessed coral cover dynamics using state-space models within six major inshore GBR catchments. An overall decline was detected in nearly half (46%) of the 15 reefs at two depths (30 sites), while the rest exhibited fluctuating (23%), static (17%), or positive (13%) trends. Inshore reefs responded similarly to their offshore counterparts, where contemporary trends were predominantly influenced by acute disturbance events. Storms emerged as the major driver affecting the inshore GBR, with the effects of other drivers such as disease, juvenile coral density, and macroalgal and turf per cent cover varying from one catchment to another. Flooding was also associated with negative trends in live coral cover in two southern catchments, but the mechanism remains unclear as it is not reflected in available metrics of water quality and may act through indirect pathways.
理解造礁生物的动态是管理自然生态系统的基础。尽管珊瑚栖息在许多浑浊的区域,但大多数关于珊瑚礁动态的研究都集中在清水系统上。在这里,我们利用 10 年的生物、环境和干扰数据来说明近岸珊瑚礁生态系统的关键驱动因素。热带气旋、棘冠海星和珊瑚白化被认为是大堡礁(GBR)中近海和中珊瑚礁大量减少的主要驱动因素。相比之下,对于近岸珊瑚礁(离主要人为压力更近)的时间趋势是什么驱动的,人们知之甚少。我们在大堡礁的六个主要近海集水区内使用状态空间模型评估了珊瑚覆盖的动态。在两个深度(30 个地点)的 15 个珊瑚礁中,近一半(46%)检测到了总体下降,而其余的则呈现波动(23%)、静态(17%)或正(13%)的趋势。近岸珊瑚礁与近海珊瑚礁的反应相似,当代趋势主要受急性干扰事件的影响。风暴成为影响近岸大堡礁的主要驱动因素,而其他驱动因素(如疾病、幼年珊瑚密度以及大型藻类和草皮的百分比覆盖)的影响因集水区而异。在两个南部集水区,洪水也与活珊瑚覆盖率的负趋势有关,但由于它未反映在可用的水质指标中,因此其机制尚不清楚,并且可能通过间接途径发挥作用。