Milbau Ann, Graae Bente Jessen, Shevtsova Anna, Nijs Ivan
Research Group of Plant and Vegetation Ecology, Department of Biology, University of Antwerp, Universiteitsplein 1, Wilrijk, Belgium.
Ann Bot. 2009 Aug;104(2):287-96. doi: 10.1093/aob/mcp117. Epub 2009 May 13.
In a future warmer subarctic climate, the soil temperatures experienced by dispersed seeds are likely to increase during summer but may decrease during winter due to expected changes in snow depth, duration and quality. Because little is known about the dormancy-breaking and germination requirements of subarctic species, how warming may influence the timing and level of germination in these species was examined.
Under controlled conditions, how colder winter and warmer summer soil temperatures influenced germination was tested in 23 subarctic species. The cold stratification and warm incubation temperatures were derived from real soil temperature measurements in subarctic tundra and the temperatures were gradually changed over time to simulate different months of the year.
Moderate summer warming (+2.5 degrees C) substantially accelerated germination in all but four species but did not affect germination percentages. Optimum germination temperatures (20/10 degrees C) further decreased germination time and increased germination percentages in three species. Colder winter soil temperatures delayed the germination in ten species and decreased the germination percentage in four species, whereas the opposite was found in Silene acaulis. In most species, the combined effect of a reduced snow cover and summer warming resulted in earlier germination and thus a longer first growing season, which improves the chance of seedling survival. In particular the recruitment of (dwarf) shrubs (Vaccinium myrtillus, V. vitis-idaea, Betula nana), trees (Alnus incana, Betula pubescens) and grasses (Calamagrostis lapponica, C. purpurea) is likely to benefit from a warmer subarctic climate.
Seedling establishment is expected to improve in a future warmer subarctic climate, mainly by considerably earlier germination. The magnitudes of the responses are species-specific, which should be taken into account when modelling population growth and migration of subarctic species.
在未来亚北极地区气候变暖的情况下,夏季散布种子所经历的土壤温度可能会升高,但由于积雪深度、持续时间和质量的预期变化,冬季土壤温度可能会降低。由于对亚北极物种的休眠打破和萌发要求了解甚少,因此研究了气候变暖如何影响这些物种的萌发时间和水平。
在可控条件下,测试了23种亚北极物种在较冷冬季和较暖夏季土壤温度下对萌发的影响。冷层积和温育温度来自亚北极苔原实际土壤温度测量数据,并随时间逐渐变化以模拟一年中的不同月份。
适度的夏季升温(+2.5摄氏度)除4个物种外,显著加速了所有物种的萌发,但不影响萌发率。最适萌发温度(20/10摄氏度)进一步缩短了3个物种的萌发时间并提高了萌发率。较冷的冬季土壤温度使10个物种的萌发延迟,4个物种的萌发率降低,而在无毛女娄菜中则发现相反情况。在大多数物种中,积雪减少和夏季升温的综合作用导致萌发提前,从而使第一个生长季节延长,这提高了幼苗存活的机会。特别是(矮)灌木(笃斯越桔、红豆越桔、矮桦)、乔木(灰毛桤木、柔毛桦)和禾本科植物(拉普兰拂子茅、紫拂子茅)的更新可能受益于亚北极地区气候变暖。
预计在未来亚北极地区气候变暖的情况下,幼苗建立情况将得到改善,主要是因为萌发大幅提前。响应程度因物种而异,在模拟亚北极物种的种群增长和迁移时应考虑这一点。