Plant–plant interactions can mitigate (or exacerbate) hot drought impacts
Plant–plant interactions can mitigate (or exacerbate) hot drought impacts
复制标题
植物与植物之间的相互作用可以减轻(或加剧)炎热干旱的影响
DOI:
10.1111/nph.19473
复制
发表时间:
2024
期刊:
影响因子:
9.4
通讯作者:
Wright, Alexandra J.
中科院分区:
文献类型:
--
作者:
Wright, Alexandra J.
Climate change will increase global surface temperatures by at least another 1.5 C in the next 50 years (IPCC, 2021). This increase in temperature is already accelerating the water cycle and shifting precipitation regimes globally, with some places receiving less precipitation while others are receiving more (IPCC, 2021). Increased global temperatures are also increasing the drying capacity of the atmosphere, measured as vapor pressure deficit (VPD; Yuan et al., 2019). Elevated VPD increases the rate of water loss from soils and plants, thus exacerbating the already negative effects of reduced precipitation. Hotter droughts with elevated VPD can double productivity losses (over just precipitation reductions; Dannenberg et al., 2022) and increase the risk and volatility of fires (Abatzoglou & Williams, 2016). Given the damages already seen during hotter droughts with higher VPD, it is essential that we identify how individual species and ecosystems will respond to hotter droughts in the future. In an article published in this issue of New Phytologist, Mas et al.(2024; 1021–1034) deepen our understanding of how species interactions might mitigate future hot drought effects. Mas et al. demonstrate how hot drought effects can be mitigated by interspecific neighbors for Quercus pubescens but exacerbated by interspecific neighbors for Fagus sylvatica. This work builds upon 30 years of biodiversity research demonstrating that higher diversity ecosystems may be better able to tolerate environmental change. This work also offers an opportunity to explore habitat-specific mechanisms that could drive how different types of ecosystems will respond to drought in the future.‘… microclimate measurements, feedbacks on constituent species, and inclusion of microclimate facilitation in process models (or Earth Systems Models), is still understudied in drought research.’