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Glasshouse vs field experiments: do they yield ecologically similar results for assessing N impacts on peat mosses?

机译:温室实验与野外实验:在评估氮对泥炭苔藓的影响方面,它们是否得出生态上相似的结果?

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摘要

• Peat bogs have accumulated more atmospheric carbon (C) than any other terrestrial ecosystem today. Most of this C is associated with peat moss () litter. Atmospheric nitrogen (N) deposition can decrease production, compromising the C sequestration capacity of peat bogs. The mechanisms underlying the reduced production are uncertain, necessitating multifactorial experiments. • We investigated whether glasshouse experiments are reliable proxies for field experiments for assessing interactions between N deposition and environment as controls on N concentration and production. We performed a meta-analysis over 115 glasshouse experiments and 107 field experiments. • We found that glasshouse and field experiments gave similar qualitative and quantitative estimates of changes in N concentration in response to N application. However, glasshouse-based estimates of changes in production – even qualitative assessments – diverged from field experiments owing to a stronger N effect on production response in absence of vascular plants in the glasshouse, and a weaker N effect on production response in presence of vascular plants compared to field experiments. • Thus, although we need glasshouse experiments to study how interacting environmental factors affect the response of to increased N deposition, we need field experiments to properly quantify these effects.
机译:•泥炭沼泽所积累的大气碳(C)比当今任何其他陆地生态系统都要多。大部分C与泥炭苔藓()凋落物有关。大气氮(N)的沉积会降低产量,损害泥炭沼泽的碳固存能力。降低产量的潜在机制尚不确定,因此需要进行多因素实验。 •我们调查了温室实验是否是现场实验的可靠代表,用于评估氮沉降与环境之间的相互作用,以此作为氮浓度和产量的控制。我们对115个温室实验和107个现场实验进行了荟萃分析。 •我们发现,温室和田间试验对氮肥的施用量做出了相似的定性和定量估算,以估算氮含量的变化。但是,基于温室的生产变化估算(甚至是定性评估)与田间试验不同,这是因为在温室中不存在维管植物的情况下,氮对生产响应的影响更强,而在存在维管植物的情况下,氮对生产响应的影响较弱与现场实验相比•因此,尽管我们需要进行温室实验来研究相互作用的环境因素如何影响氮沉降增加的响应,但我们仍需要进行现场实验以正确量化这些影响。

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