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Soil microbial responses to fire and interacting global change factors in a California annual grassland

机译:加利福尼亚年度草原上土壤对火和相互作用的全球变化因子的微生物响应

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Wildfire in California annual grasslands is an important ecological disturbance and ecosystem control. Regional and global climate changes that affect aboveground biomass will alter fire-related nutrient loading and promote increased frequency and severity of fire in these systems. This can have long-term impacts on soil microbial dynamics and nutrient cycling, particularly in N-limited systems such as annual grasslands. We examined the effects of a low-severity fire on microbial biomass and specific microbial lipid biomarkers over 3 years following a fire at the Jasper Ridge Global Change Experiment. We also examined the impact of fire on the abundance of ammonia-oxidizing bacteria (AOB), specifically Nitrosospira Cluster 3a ammonia-oxidizers, and nitrification rates 9 months post-fire. Finally, we examined the interactive effects of fire and three other global change factors (N-deposition, precipitation and CO2) on plant biomass and soil microbial communities for three growing seasons after fire. Our results indicate that a low-severity fire is associated with earlier season primary productivity and higher soil-NH4 + concentrations in the first growing season following fire. Belowground productivity and total microbial biomass were not influenced by fire. Diagnostic microbial lipid biomarkers, including those for Gram-positive bacteria and Gram-negative bacteria, were reduced by fire 9- and 21-months post-fire, respectively. All effects of fire were indiscernible by 33-months post-fire, suggesting that above and belowground responses to fire do not persist in the long-term and that these grassland communities are resilient to fire disturbance. While N-deposition increased soil NH4 +, and thus available NH3, AOB abundance, nitrification rates and Cluster 3a AOB, similar increases in NH3 in the fire plots did not affect AOB or nitrification. We hypothesize that this difference in response to N-addition involves a mediation of P-limitation as a result of fire, possibly enhanced by increased plant competition and arbuscular mycorrhizal fungi–plant associations after fire.
机译:加州一年生草原的野火是重要的生态扰动和生态系统控制。影响地上生物量的区域和全球气候变化将改变与火有关的养分含量,并加剧这些系统着火的频率和严重性。这可能对土壤微生物动力学和养分循环产生长期影响,特别是在氮有限的系统(例如一年生草地)中。在贾斯珀里奇全球变化实验中,大火过后3年,我们研究了低度烈火对微生物生物量和特定微生物脂质生物标志物的影响。我们还检查了火灾对氨氧化细菌(AOB)含量(特别是亚硝基螺菌簇3a氨氧化剂)的影响,以及火灾后9个月的硝化率。最后,我们研究了火灾和三个其他全局变化因子(N沉积,降水和CO 2 )对火灾后三个生长季节植物生物量和土壤微生物群落的相互作用的影响。我们的结果表明,低烈度火灾与较早季节的初级生产力和火灾后第一个生长季节较高的土壤-NH 4 + 浓度有关。地下生产力和微生物总生物量不受火的影响。诊断微生物脂质生物标志物,包括革兰氏阳性细菌和革兰氏阴性细菌的微生物标志物,分别在火灾后9个月和21个月后被减少。火灾后33个月,所有火势的影响都无法识别,这表明长期和长期地下的火势响应不会持续,这些草原社区具有抵抗火势的能力。虽然氮沉降增加了土壤NH 4 + ,从而使土壤NH 3 ,AOB丰度,硝化率和簇3a AOB升高,但火场中的NH 3 不会影响AOB或硝化作用。我们假设这种对N加成反应的差异涉及火引起的P限制介导,可能是由于植物竞争加剧和火后丛枝菌根真菌与植物的联系而增强。

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