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Inter-annual variation in soil extra-cellular enzyme activity in response to simulated global change and fire disturbance

机译:响应模拟的全球变化和火灾干扰,土壤细胞外酶活性的年际变化

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The interactive effects of global change drivers (e.g. climate change, nitrogen deposition, and elevated CO_2) on soil microbial activity have important implications for ecosystem carbon and nutrient cycling. However, these interactions have primarily been explored in single-year, single-factor studies despite the reality of multiple simultaneous global changes. We measured the activity of six enzymes (Β-glucosidase, α-glucosidase, cellobiohydrolase, xylosidase, acid phosphatase, and N-acetylglucosaminidase) for 3 years (2004-2006) following wildfire (2003) at the Jasper Ridge Global Change Experiment (JRGCE), a long-term multi-factor global change experiment in a California annual grassland. JRGCE manipulations include climate change (elevated temperature and precipitation), nitrogen addition, and elevated CO_2. In general we found only minimal interactions among treatments and found the strongest main effects from nitrogen addition and burning. Enzyme activities increased under elevated nitrogen, a response that persisted throughout the 3 years of the study. Wildfire was slightly related to decreased enzyme activities (by 10-20%) in 2004, with a larger decrease (by 25-50%) in 2005. The response was gone by 2006, suggesting that the microbial community was able to recover by 3 years following wildfire. Finally, enzyme responses to treatments, even where statistically significant, were of smaller magnitude than annual variation in activity. We propose that overall decreases in enzyme activity from 2004 to 2006 were due to decreased temperature and increased precipitation in 2005 and 2006 relative to 2004. Our results suggest that while it is important to assess response to specific global change treatment and treatment interactions, these responses (A) may change over time and (B) should be characterized within the context of inter-annual fluctuation in microbial community function.
机译:全球变化驱动因素(例如,气候变化,氮沉降和CO_2升高)对土壤微生物活动的互动影响对生态系统碳和养分循环具有重要意义。然而,尽管存在多个同时发生的全球变化,但这些相互作用主要是在单年,单因素研究中进行了探索。我们在贾斯珀里奇全球变化试验(JRGCE)进行野火(2003年)之后的三年(2004年至2006年),测量了6种酶(β-葡萄糖苷酶,α-葡萄糖苷酶,纤维二糖水解酶,木糖苷酶,酸性磷酸酶和N-乙酰氨基葡萄糖苷酶)在3年后(2004-2006年)的活性。 ),这是一项在加利福尼亚年度草原上进行的长期多因素全球变化实验。 JRGCE操纵包括气候变化(温度和降水升高),氮添加和CO_2升高。通常,我们发现各处理之间的相互作用极小,而氮添加和燃烧产生的主要作用最强。在氮含量升高的情况下,酶的活性增加,这种反应在整个研究的3年中一直持续。在2004年,野火与酶活性降低(10-20%)略有相关,在2005年降低幅度更大(25-50%)。2006年这种反应消失了,这表明微生物群落能够在3年前恢复。野火过了多年。最后,酶对治疗的反应,即使具有统计学意义,其幅度也小于活性的年度变化。我们建议从2004年到2006年,酶活性的总体下降是由于温度降低和2005年和2006年相对于2004年的降水增加。我们的结果表明,尽管评估对特定的全球变化治疗和治疗相互作用的反应很重要,但这些反应(A)可能随时间而变化,并且(B)应该在微生物群落功能的年际波动范围内表征。

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