Wilson Shaun K, Depcyznski Martial, Fisher Rebecca, Holmes Thomas H, Noble Mae M, Radford Ben T, Rule Michael, Shedrawi George, Tinkler Paul, Fulton Christopher J
Marine Science Program Department of Biodiversity, Conservation and Attractions Kensington WA Australia.
Oceans Institute University of Western Australia Crawley WA Australia.
Ecol Evol. 2018 Jan 15;8(3):1918-1928. doi: 10.1002/ece3.3779. eCollection 2018 Feb.
Fluctuations in marine populations often relate to the supply of recruits by oceanic currents. Variation in these currents is typically driven by large-scale changes in climate, in particular ENSO (El Nino Southern Oscillation). The dependence on large-scale climatic changes may, however, be modified by early life history traits of marine taxa. Based on eight years of annual surveys, along 150 km of coastline, we examined how ENSO influenced abundance of juvenile fish, coral spat, and canopy-forming macroalgae. We then investigated what traits make populations of some fish families more reliant on the ENSO relationship than others. Abundance of juvenile fish and coral recruits was generally positively correlated with the Southern Oscillation Index (SOI), higher densities recorded during La Niña years, when the ENSO-influenced Leeuwin Current is stronger and sea surface temperature higher. The relationship is typically positive and stronger among fish families with shorter pelagic larval durations and stronger swimming abilities. The relationship is also stronger at sites on the coral back reef, although the strongest of all relationships were among the lethrinids ( = .9), siganids ( = .9), and mullids ( = .8), which recruit to macroalgal meadows in the lagoon. ENSO effects on habitat seem to moderate SOI-juvenile abundance relationship. Macroalgal canopies are higher during La Niña years, providing more favorable habitat for juvenile fish and strengthening the SOI effect on juvenile abundance. Conversely, loss of coral following a La Niña-related heat wave may have compromised postsettlement survival of coral dependent species, weakening the influence of SOI on their abundance. This assessment of ENSO effects on tropical fish and habitat-forming biota and how it is mediated by functional ecology improves our ability to predict and manage changes in the replenishment of marine populations.
海洋生物种群的波动通常与洋流带来的新成员数量有关。这些洋流的变化通常由气候的大规模变化驱动,特别是厄尔尼诺-南方涛动(ENSO)。然而,海洋生物分类群的早期生活史特征可能会改变对大规模气候变化的依赖。基于在150公里海岸线上进行的为期八年的年度调查,我们研究了ENSO如何影响幼鱼、珊瑚幼体和形成冠层的大型藻类的数量。然后,我们调查了哪些特征使得某些鱼类家族的种群比其他家族更依赖于ENSO关系。幼鱼和珊瑚幼体的数量通常与南方涛动指数(SOI)呈正相关,在拉尼娜年期间记录到更高的密度,此时受ENSO影响的李尤温洋流更强,海面温度更高。在浮游幼体持续时间较短且游泳能力较强的鱼类家族中,这种关系通常更积极且更强。在珊瑚礁后礁的地点,这种关系也更强,尽管所有关系中最强的是在裸颊鲷科(r = 0.9)、蓝子鱼科(r = 0.9)和羊鱼科(r = 0.8)之间,它们在泻湖中的大型海藻草甸中繁殖。ENSO对栖息地的影响似乎缓和了SOI与幼体数量之间的关系。在拉尼娜年期间,大型藻冠层更高,为幼鱼提供了更有利的栖息地,并加强了SOI对幼体数量的影响。相反,与拉尼娜相关的热浪过后珊瑚的损失可能会危及依赖珊瑚的物种在定居后的生存,削弱SOI对其数量的影响。这种对ENSO对热带鱼类和形成栖息地的生物群的影响以及它如何由功能生态学介导的评估,提高了我们预测和管理海洋种群补充变化的能力。