Department of Environmental Science, Policy, and Management, University of California, Berkeley, California, 94720, USA.
Department of Integrative Biology, University of California, Berkeley, California, 94720, USA.
Ecology. 2020 Sep;101(9):e03107. doi: 10.1002/ecy.3107. Epub 2020 Jun 26.
Climate warming is facilitating the expansion of many cold-sensitive woody species in woodland-grassland ecotones worldwide. Recent research has demonstrated that this range expansion can be further enhanced by positive vegetation-microclimate feedbacks whereby woody canopies induce local nocturnal warming, which reduces freeze-induced damage and favors the establishment of woody plants. However, this local positive feedback can be counteracted by biotic drivers such as browsing and the associated consumption of shrub biomass. The joint effects of large-scale climate warming and local-scale microclimate feedbacks on woody vegetation dynamics in these ecotones remain poorly understood. Here, we used a combination of experimental and modeling approaches to investigate the effects of woody cover on microclimate and the consequent implications on ecological stability in North American coastal ecosystems. We found greater browsing pressure and significant warming (~2°C) beneath shrub canopies compared to adjacent grasslands, which reduces shrub seedlings' exposure to cold damage. Cold sensitivity is evidenced by the significant decline in xylem hydraulic conductivity in shrub seedlings when temperatures dropped below -2°C. Despite the negative browsing-vegetation feedback, a small increase in minimum temperature can induce critical transitions from grass to woody plant dominance. Our framework also predicts the threshold temperature of -7°C for mangrove-salt marsh ecotones on the Atlantic coast of Florida. Above this reference temperature a critical transition may occur from salt marsh to mangrove vegetation, in agreement with empirical studies. Thus, the interaction between ongoing global warming trends and microclimate feedbacks may significantly alter woody vegetation dynamics and ecological stability in coastal ecosystems where woody plant expansion is primarily constrained by extreme low temperature events.
气候变暖正在促进许多对寒冷敏感的木本物种在林地-草原生态交错带的扩张。最近的研究表明,这种范围的扩大可以通过积极的植被-小气候反馈进一步增强,其中木本树冠诱导局部夜间升温,减少冻害并有利于木本植物的建立。然而,这种局部正反馈可以被生物驱动因素抵消,如啃食和相关的灌木生物量消耗。在这些生态交错带中,大规模气候变暖与局部小气候反馈对木本植被动态的联合影响仍知之甚少。在这里,我们使用了实验和建模相结合的方法来研究木本覆盖对小气候的影响以及对北美沿海生态系统生态稳定性的相应影响。我们发现,与相邻草地相比,灌木树冠下的啃食压力更大,温度升高(约 2°C),这减少了灌木幼苗受到寒冷伤害的暴露。当温度下降到-2°C以下时,灌木幼苗木质部水力传导率显著下降,证明了其对寒冷的敏感性。尽管存在负面的啃食-植被反馈,但最小温度的微小增加可能会导致从草本植物到木本植物优势的关键转变。我们的框架还预测了佛罗里达州大西洋沿岸红树林-盐沼生态交错带的临界温度为-7°C。高于这个参考温度,盐沼到红树林植被可能会发生关键转变,这与实证研究一致。因此,持续的全球变暖趋势和小气候反馈之间的相互作用可能会显著改变沿海生态系统中的木本植被动态和生态稳定性,在这些生态系统中,木本植物的扩张主要受到极端低温事件的限制。