UWA Oceans Institute and School of Biological Sciences, University of Western Australia, Crawley, Western Australia, Australia.
Institute of Marine Research, Flødevigen Research Station, His, Norway.
Glob Chang Biol. 2024 Aug;30(8):e17469. doi: 10.1111/gcb.17469.
Marine heatwaves (MHWs), increasing in duration and intensity because of climate change, are now a major threat to marine life and can have lasting effects on the structure and function of ecosystems. However, the responses of marine taxa and ecosystems to MHWs can be highly variable, making predicting and interpreting biological outcomes a challenge. Here, we review how biological responses to MHWs, from individuals to ecosystems, are mediated by fine-scale spatial variability in the coastal marine environment (hereafter, local gradients). Viewing observed responses through a lens of ecological theory, we present a simple framework of three 'resilience processes' (RPs) by which local gradients can influence the responses of marine taxa to MHWs. Local gradients (1) influence the amount of stress directly experienced by individuals, (2) facilitate local adaptation and acclimatization of individuals and populations, and (3) shape community composition which then influences responses to MHWs. We then synthesize known examples of fine-scale gradients that have affected responses of benthic foundation species to MHWs, including kelp forests, coral reefs, and seagrass meadows and link these varying responses to the RPs. We present a series of case studies from various marine ecosystems to illustrate the differential impacts of MHWs mediated by gradients in both temperature and other co-occurring drivers. In many cases, these gradients had large effect sizes with several examples of local gradients causing a 10-fold difference in impacts or more (e.g., survival, coverage). This review highlights the need for high-resolution environmental data to accurately predict and manage the consequences of MHWs in the context of ongoing climate change. While current tools may capture some of these gradients already, we advocate for enhanced monitoring and finer scale integration of local environmental heterogeneity into climate models. This will be essential for developing effective conservation strategies and mitigating future marine biodiversity loss.
海洋热浪(MHWs)由于气候变化而持续时间和强度增加,现在对海洋生物构成了重大威胁,并可能对生态系统的结构和功能产生持久影响。然而,海洋分类群和生态系统对 MHWs 的反应可能变化很大,这使得预测和解释生物结果具有挑战性。在这里,我们回顾了从个体到生态系统的海洋生物对 MHWs 的反应是如何受到沿海海洋环境中细尺度空间变异性(以下简称局部梯度)的调节的。通过生态理论的视角来看待观察到的反应,我们提出了一个简单的“恢复力过程”(RP)框架,通过该框架,局部梯度可以影响海洋分类群对 MHWs 的反应。局部梯度(1)直接影响个体所经历的压力量,(2)促进个体和种群的局部适应和驯化,以及(3)塑造群落组成,从而影响对 MHWs 的反应。然后,我们综合了已知的细尺度梯度影响底栖基础物种对 MHWs 反应的例子,包括海带林、珊瑚礁和海草草地,并将这些不同的反应与 RPs 联系起来。我们提出了一系列来自不同海洋生态系统的案例研究,说明了由温度和其他共存驱动因素的梯度介导的 MHWs 的差异影响。在许多情况下,这些梯度的影响幅度很大,有几个例子表明局部梯度导致影响相差 10 倍或更多(例如,存活率、覆盖率)。本综述强调了需要高分辨率环境数据来准确预测和管理在持续气候变化背景下 MHWs 的后果。虽然当前的工具可能已经捕获了其中的一些梯度,但我们主张加强监测并将局部环境异质性更精细地纳入气候模型中。这对于制定有效的保护策略和减轻未来海洋生物多样性的丧失至关重要。