Erguna Forest-Steppe Ecotone Research Station, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang, China.
Department of Animal Health and Production, Oyo State College of Agriculture and Technology, Igbo-Ora, Nigeria.
Ecology. 2023 Feb;104(2):e3920. doi: 10.1002/ecy.3920. Epub 2023 Jan 3.
Recurrent droughts are an inevitable consequence of climate change, yet how grasslands respond to such events is unclear. We conducted a 6-year rainfall manipulation experiment in a semiarid grassland that consisted of an initial 2-year drought (2015-2016), followed by a recovery period (2017-2018) and, finally, a second 2-year drought (2019-2020). In each year, we estimated aboveground net primary productivity (ANPP), species richness, community-weighted mean (CWM) plant traits, and several indices of functional diversity. The initial drought led to reduced ANPP, which was primarily driven by limited growth of forbs in the first year and grasses in the second year. Total ANPP completely recovered as the rapid recovery of grass productivity compensated for the slow recovery of forb productivity. The subsequent drought led to a greater reduction in total ANPP than the initial drought due to the greater decline of both grass and forb productivity. The structural equation models revealed that soil moisture influenced ANPP responses directly during the initial drought, and indirectly during the subsequent drought by lowering functional diversity, which resulted in reduced total ANPP. Additionally, ANPP was positively influenced by CWM plant height and leaf nitrogen during the recovery period and recurrent drought, respectively. Overall, the greater impact of the second drought on ecosystem function than the initial drought, as well as the underlying differential mechanism, underscores the need for an understanding of how increased drought frequency may alter semiarid grassland functioning.
反复发生的干旱是气候变化的必然结果,但草原对这些事件的响应尚不清楚。我们在半干旱草原上进行了一项为期 6 年的降雨控制实验,该实验包括最初的 2 年干旱期(2015-2016 年),随后是恢复期(2017-2018 年),最后是第二次 2 年干旱期(2019-2020 年)。在每年,我们估计地上净初级生产力(ANPP)、物种丰富度、群落加权均值(CWM)植物特征以及几种功能多样性指数。最初的干旱导致 ANPP 减少,这主要是由于第一年的杂类草生长受限和第二年的草生长受限。由于草生产力的快速恢复弥补了杂类草生产力的缓慢恢复,总 ANPP 完全恢复。随后的干旱导致总 ANPP 减少幅度大于初始干旱,这是由于草和杂类草生产力下降更大所致。结构方程模型显示,在初始干旱期间,土壤水分直接影响 ANPP 响应,而在随后的干旱期间,通过降低功能多样性间接影响 ANPP 响应,从而导致总 ANPP 减少。此外,在恢复期间和反复干旱期间,CWM 植物高度和叶片氮分别对 ANPP 有积极影响。总的来说,第二次干旱对生态系统功能的影响大于初始干旱,以及潜在的差异机制,突显了需要了解增加的干旱频率如何改变半干旱草原的功能。