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Microsite conditions in retrogressive thaw slumps may facilitate increased seedling recruitment in the Alaskan Low Arctic

机译:逆行解冻滑坡中的微地点条件可能有助于增加阿拉斯加低北极地区的幼苗招募

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摘要

In Low Arctic tundra, thermal erosion of ice‐rich permafrost soils (thermokarst) has increased in frequency since the 1980s. Retrogressive thaw slumps (RTS) are thermokarst disturbances forming large open depressions on hillslopes through soil wasting and vegetation displacement. Tall (>0.5 m) deciduous shrubs have been observed in RTS a decade after disturbance. RTS may provide conditions suitable for seedling recruitment, which may contribute to Arctic shrub expansion. We quantified in situ seedling abundance, and size and viability of soil seedbanks in greenhouse trials for two RTS chronosequences near lakes on Alaska's North Slope. We hypothesized recent RTS provide microsites for greater recruitment than mature RTS or undisturbed tundra. We also hypothesized soil seedbanks demonstrate quantity–quality trade‐offs; younger seedbanks contain smaller numbers of mostly viable seed that decrease in viability as seed accumulates over time. We found five times as many seedlings in younger RTS as in older RTS, including birch and willow, and no seedlings in undisturbed tundra. Higher seedling counts were associated with bare soil, warmer soils, higher soil available nitrogen, and less plant cover. Seedbank viability was unrelated to size. Older seedbanks were larger at one chronosequence, with no difference in percent germination. At the other chronosequence, germination was lower from older seedbanks but seedbank size was not different. Seedbank germination was positively associated with in situ seedling abundance at one RTS chronosequence, suggesting postdisturbance revegetation from seedbanks. Thermal erosion may be important for recruitment in tundra by providing bare microsites that are warmer, more nutrient‐rich, and less vegetated than in undisturbed ground. Differences between two chronosequences in seedbank size, viability, and species composition suggest disturbance interacts with local conditions to form seedbanks. RTS may act as seedling nurseries to benefit many Arctic species as climate changes, particularly those that do not produce persistent seed.
机译:自1980年代以来,在低北极冻原上,富含冰的多年冻土(热岩溶)的热侵蚀频率增加了。逆行融化坍落度(RTS)是热喀斯特扰动,通过土壤浪费和植被移位在山坡上形成大的开放洼地。扰动十年后,在RTS中观测到高(> 0.5 m)的落叶灌木。 RTS可能提供适合苗木招募的条件,这可能会促进北极灌木的扩张。我们在阿拉斯加北坡湖泊附近的两个RTS时序序列的温室试验中量化了实地幼苗的丰度,土壤种子库的大小和生存能力。我们假设,与成熟的RTS或未受干扰的苔原相比,最近的RTS提供的微型网站招募更多。我们还假设土壤种子库表现出数量-质量的权衡。较年轻的种子库包含较少数量的主要是可行的种子,随着种子随着时间的积累,生存力会降低。在较年轻的RTS中,我们发现较早的RTS(包括桦树和柳树)的幼苗数量是旧的RTS的五倍,而在未受干扰的冻原中没有发现任何幼苗。较高的幼苗数与裸露的土壤,温暖的土壤,较高的土壤有效氮和较少的植物覆盖率有关。种子库的生存能力与大小无关。较旧的种子库在一个时间序列上更大,发芽百分比没有差异。在其他时间序列上,发芽率低于较旧的种子库,但种子库大小没有变化。在一个RTS时序上,种子库萌发与原位幼苗丰度呈正相关,这表明干扰后种子库中的植被恢复。通过提供裸露的微地点,使热蚀对于苔原的征募可能很重要,因为这些微地点比未受干扰的地面更温暖,营养丰富且植被更少。种子库大小,生存力和物种组成两个时间序列之间的差异表明干扰与当地条件相互作用形成种子库。随着气候变化,RTS可以作为苗圃来使许多北极物种受益,尤其是那些不会产生持久种子的北极物种。

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