Key Laboratory of Biometallurgy of Ministry of Education, School of Minerals Processing and Bioengineering, Central South University, Changsha, China.
Institute for Environmental Genomics, University of Oklahoma, Norman, OK, USA.
Nat Ecol Evol. 2019 Apr;3(4):612-619. doi: 10.1038/s41559-019-0848-8. Epub 2019 Mar 25.
Determining the temporal scaling of biodiversity, typically described as species-time relationships (STRs), in the face of global climate change is a central issue in ecology because it is fundamental to biodiversity preservation and ecosystem management. However, whether and how climate change affects microbial STRs remains unclear, mainly due to the scarcity of long-term experimental data. Here, we examine the STRs and phylogenetic-time relationships (PTRs) of soil bacteria and fungi in a long-term multifactorial global change experiment with warming (+3 °C), half precipitation (-50%), double precipitation (+100%) and clipping (annual plant biomass removal). Soil bacteria and fungi all exhibited strong STRs and PTRs across the 12 experimental conditions. Strikingly, warming accelerated the bacterial and fungal STR and PTR exponents (that is, the w values), yielding significantly (P < 0.001) higher temporal scaling rates. While the STRs and PTRs were significantly shifted by altered precipitation, clipping and their combinations, warming played the predominant role. In addition, comparison with the previous literature revealed that soil bacteria and fungi had considerably higher overall temporal scaling rates (w = 0.39-0.64) than those of plants and animals (w = 0.21-0.38). Our results on warming-enhanced temporal scaling of microbial biodiversity suggest that the strategies of soil biodiversity preservation and ecosystem management may need to be adjusted in a warmer world.
在全球气候变化的背景下,确定生物多样性的时间尺度,通常用物种-时间关系(STR)来描述,是生态学的一个核心问题,因为它是生物多样性保护和生态系统管理的基础。然而,气候变化是否以及如何影响微生物 STR 仍然不清楚,主要是因为长期实验数据的缺乏。在这里,我们在一个长期的多因素全球变化实验中,研究了土壤细菌和真菌的 STR 和系统发育时间关系(PTR),该实验包括增温(+3°C)、减半降水(-50%)、加倍降水(+100%)和刈割(每年去除植物生物量)。在 12 种实验条件下,土壤细菌和真菌都表现出强烈的 STR 和 PTR。引人注目的是,增温加速了细菌和真菌 STR 和 PTR 的指数(即 w 值),导致时间尺度率显著升高(P<0.001)。虽然降水、刈割及其组合显著改变了 STR 和 PTR,但增温起着主要作用。此外,与以前的文献相比,我们发现土壤细菌和真菌的总体时间尺度率(w=0.39-0.64)明显高于植物和动物(w=0.21-0.38)。我们关于变暖增强微生物生物多样性时间尺度的研究结果表明,在一个更温暖的世界里,土壤生物多样性保护和生态系统管理的策略可能需要进行调整。