Williamson Joseph, Lu Muyang, Camus M Florencia, Gregory Richard D, Maclean Ilya M D, Rocha Juan C, Saastamoinen Marjo, Wilson Robert J, Bridle Jon, Pigot Alex L
Department of Genetics, Evolution and Environment, University College London, London WC1E 6BT, UK.
College of Life Science, Sichuan University, Chengdu 610065, China.
Philos Trans R Soc Lond B Biol Sci. 2025 Jan 9;380(1917):20230321. doi: 10.1098/rstb.2023.0321.
Anthropogenic climate change is projected to become a major driver of biodiversity loss, destabilizing the ecosystems on which human society depends. As the planet rapidly warms, the disruption of ecological interactions among populations, species and their environment, will likely drive positive feedback loops, accelerating the pace and magnitude of biodiversity losses. We propose that, even without invoking such amplifying feedback, biodiversity loss should increase nonlinearly with warming because of the non-uniform distribution of biodiversity. Whether these non-uniformities are the uneven distribution of populations across a species' thermal niche, or the uneven distribution of thermal niche limits among species within an ecological community, we show that in both cases, the resulting clustering in population warming tolerances drives nonlinear increases in the risk to biodiversity. We discuss how fundamental constraints on species' physiologies and geographical distributions give rise to clustered warming tolerances, and how population responses to changing climates could variously temper, delay or intensify nonlinear dynamics. We argue that nonlinear increases in risks to biodiversity should be the null expectation under warming, and highlight the empirical research needed to understand the causes, commonness and consequences of clustered warming tolerances to better predict where, when and why nonlinear biodiversity losses will occur.This article is part of the discussion meeting issue 'Bending the curve towards nature recovery: building on Georgina Mace's legacy for a biodiverse future'.
预计人为气候变化将成为生物多样性丧失的主要驱动因素,破坏人类社会所依赖的生态系统。随着地球迅速变暖,种群、物种及其环境之间生态相互作用的破坏可能会引发正反馈循环,加速生物多样性丧失的速度和规模。我们认为,即使不考虑这种放大反馈,由于生物多样性分布不均,生物多样性丧失也应随着气候变暖而非线性增加。无论这些不均一性是指物种热生态位内种群分布的不均匀,还是生态群落内物种间热生态位限制分布的不均匀,我们都表明,在这两种情况下,种群变暖耐受性的聚类都会导致生物多样性风险的非线性增加。我们讨论了物种生理和地理分布的基本限制如何导致聚类的变暖耐受性,以及种群对气候变化的反应如何以不同方式缓和、延迟或加剧非线性动态。我们认为,生物多样性风险的非线性增加应该是气候变暖下的默认预期,并强调需要开展实证研究,以了解聚类变暖耐受性的成因、普遍性和后果,从而更好地预测非线性生物多样性丧失将在何时、何地以及为何发生。本文是讨论会特刊“扭转自然衰退趋势:以乔治娜·梅斯的遗产为基础,实现生物多样的未来”的一部分。