Rocky Mountain Biological Laboratory, P.O. Box 519, Crested Butte, Colorado 81224 USA.
Am J Bot. 2010 Sep;97(9):1431-7. doi: 10.3732/ajb.1000095. Epub 2010 Aug 23.
Climate change has affected species worldwide, including alterations in phenology, migration patterns, distribution, and survival. Because Erythronium grandiflorum is an early-season bloomer, alterations in its phenology may have serious implications for many North American Rocky Mountain communities, including changes in resource availability for pollinators and herbivores. •
We investigated whether changes in the snowmelt date, summer temperature, and summer precipitation have altered the timing and abundance of flowering in E. grandiflorum by collecting long-term data on floral abundance from 1975-2008 in a series of 2 × 2 m plots at the Rocky Mountain Biological Laboratory (RMBL) in Gothic, Colorado in the United States. •
Snowmelt date and mean summer temperature were negatively correlated. Over the 30-yr study, the snowmelt date advanced by 4.14 d/decade, and mean summer temperature increased by 0.38°C/decade. Summer precipitation was variable, showing no change. The first, peak, and last flowering dates of E. grandiflorum advanced an average of 3.2 d/decade. Furthermore, earlier snowmelt and greater summer precipitation in the previous year led to earlier flowering in E. grandiflorum. There was no change in flowering abundance in this species, indicating it may be controlled by a complex set of abiotic and biotic variables. •
Our study indicates that snowmelt is arriving earlier at the RMBL, which has caused earlier flowering in E. grandiflorum. Because alterations in phenology can disrupt important ecological interactions, information on potential phenological shifts in species that interact with E. grandiflorum is essential in determining the net effect of climate-driven alterations in phenology.
气候变化已经影响到了全球的物种,包括物候、迁徙模式、分布和生存的变化。由于大花杓兰是早春开花的植物,其物候的变化可能对许多北美落矶山地区的社区产生严重影响,包括传粉者和食草动物资源可用性的变化。
我们通过在美国科罗拉多州哥特的落矶山生物实验室(Rocky Mountain Biological Laboratory,RMBL)的一系列 2×2 米的样地中,从 1975 年至 2008 年收集了大花杓兰花朵丰度的长期数据,调查了融雪日期、夏季温度和夏季降水的变化是否改变了大花杓兰的开花时间和数量。
融雪日期与平均夏季温度呈负相关。在 30 年的研究中,融雪日期提前了 4.14 天/十年,平均夏季温度升高了 0.38°C/十年。夏季降水是多变的,没有变化。大花杓兰的首次、峰值和末次开花日期平均提前了 3.2 天/十年。此外,前一年更早的融雪和更多的夏季降水导致大花杓兰更早开花。该物种的开花丰度没有变化,表明它可能受到一系列复杂的非生物和生物变量的控制。
我们的研究表明,RMBL 的融雪时间提前了,这导致了大花杓兰更早开花。由于物候的变化会破坏重要的生态相互作用,因此了解与大花杓兰相互作用的物种潜在的物候变化信息,对于确定由物候变化引起的气候变化的净效应至关重要。