State Key Laboratory of Grassland and Agro-ecosystems, School of Life Sciences, Lanzhou University, Lanzhou, 730000, China.
Department of Biology, University of New Mexico, Albuquerque, New Mexico, 87103, USA.
Ecol Appl. 2020 Jul;30(5):e02096. doi: 10.1002/eap.2096. Epub 2020 Jun 2.
Plant community responses to global environmental change focus primarily on aboveground vegetation; however, the important role of the seed bank is frequently neglected. Specifically, the direct and indirect effects of changes in temperature and precipitation on seed banks remain poorly understood, yet seed banks provide a vital source of ecosystem resilience to global environmental change. We used a structural equation model to explore the direct and indirect effects of temperature, precipitation, and other biotic and abiotic factors on soil seed bank community composition using 1,026 soil seed bank samples from 57 sites along an elevation gradient that served as a space-for-time substitution for changing climate in the Tibetan Plateau. Seed bank richness was negatively correlated with both precipitation and temperature, but neither climate factor affected seed bank density. Temperature was also negatively correlated with vegetation species richness, which was positively correlated with seed bank richness and density. Both precipitation and temperature were positively correlated with soil total N, and total N was negatively correlated with vegetation richness. Both precipitation and temperature were negatively correlated with soil pH, and soil pH was negatively correlated with vegetation richness, but positively correlated with seed bank richness and density. Increasing precipitation and temperature would decrease seed bank diversity through direct effects as well as indirectly by decreasing vegetation diversity. Soil pH and total N emerged as the most important soil abiotic factors for seed bank diversity. Increasing precipitation and temperature under climate change may increase the extinction risk of some species in the seed bank by altering bet-hedging and risk-spreading strategies, which will degrade natural restoration ability and ultimately ecosystem resilience. This research is important because it identifies the potential underlying mechanistic basis of climate change impacts on seed banks through effects of aboveground vegetation and belowground biotic and abiotic factors.
植物群落对全球环境变化的响应主要集中在地上植被上;然而,种子库的重要作用经常被忽视。具体来说,温度和降水变化对种子库的直接和间接影响仍知之甚少,但种子库为生态系统对全球环境变化的恢复力提供了重要来源。我们使用结构方程模型,利用青藏高原海拔梯度上 57 个地点的 1026 个土壤种子库样本,探讨了温度、降水和其他生物及非生物因素对土壤种子库群落组成的直接和间接影响,这些样本可作为随气候变化的时间替代空间。种子库丰富度与降水和温度均呈负相关,但气候因子均不影响种子库密度。温度与植被物种丰富度呈负相关,而植被物种丰富度与种子库丰富度和密度呈正相关。降水和温度均与土壤总氮呈正相关,总氮与植被丰富度呈负相关。降水和温度均与土壤 pH 值呈负相关,土壤 pH 值与植被丰富度呈负相关,但与种子库丰富度和密度呈正相关。降水和温度的增加将通过直接效应以及通过降低植被多样性间接降低种子库多样性。土壤 pH 值和总氮是影响种子库多样性的最重要的土壤非生物因素。气候变化下降水和温度的增加可能会改变避险和风险分散策略,从而增加种子库中某些物种的灭绝风险,降低自然恢复能力,并最终降低生态系统的恢复力。这项研究很重要,因为它通过地上植被和地下生物及非生物因素的影响,确定了气候变化对种子库影响的潜在潜在机制基础。