Graduate School of Environment and Information Sciences, Yokohama National University, 79-7 Tokiwadai, Hodogaya, Yokohama, 240-8501, Japan.
Department of Ecological Science, Faculty of Science, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands.
Nat Commun. 2020 Sep 11;11(1):4547. doi: 10.1038/s41467-020-18296-w.
Biodiversity loss can alter ecosystem functioning; however, it remains unclear how it alters decomposition-a critical component of biogeochemical cycles in the biosphere. Here, we provide a global-scale meta-analysis to quantify how changes in the diversity of organic matter derived from plants (i.e. litter) affect rates of decomposition. We find that the after-life effects of diversity were significant, and of substantial magnitude, in forests, grasslands, and wetlands. Changes in plant diversity could alter decomposition rates by as much as climate change is projected to alter them. Specifically, diversifying plant litter from mono- to mixed-species increases decomposition rate by 34.7% in forests worldwide, which is comparable in magnitude to the 13.6-26.4% increase in decomposition rates that is projected to occur over the next 50 years in response to climate warming. Thus, biodiversity changes cannot be solely viewed as a response to human influence, such as climate change, but could also be a non-negligible driver of future changes in biogeochemical cycles and climate feedbacks on Earth.
生物多样性的丧失会改变生态系统的功能;然而,它如何改变分解作用——生物圈中生物地球化学循环的一个关键组成部分,仍然不清楚。在这里,我们提供了一项全球范围内的荟萃分析,以量化源自植物的有机物(即凋落物)多样性变化如何影响分解速率。我们发现,多样性的“来世效应”在森林、草原和湿地中具有重要意义。植物多样性的变化可能会改变分解速率,其幅度与气候变化预计将改变的幅度相当。具体来说,将植物凋落物从单一物种多样化到混合物种会使全球森林的分解速率增加 34.7%,这与预计未来 50 年内由于气候变暖而导致的分解速率增加 13.6-26.4%的幅度相当。因此,生物多样性的变化不能仅仅被视为对人类影响(如气候变化)的一种反应,而可能是未来生物地球化学循环变化和地球气候反馈的一个不可忽视的驱动因素。