Above and below-ground nutrient cycling: a criteria for assessing the biogeochemical functioning of a constructed fen

生物地球化学循环 植被恢复 自行车 环境科学 营养物 营养循环 泥炭 生物量(生态学) 泥炭藓 苔藓 生态学 生产力 地下水 生态演替 农学 生物 化学 林业 地质学 经济 宏观经济学 有机化学 岩土工程 地理
作者
Felix Nwaishi,Richard M. Petrone,Merrin L. Macrae,Jonathan S. Price,Maria Strack,Robin M. Slawson,Roxane Andersen
出处
期刊:Applied Soil Ecology [Elsevier]
卷期号:98: 177-194 被引量:18
标识
DOI:10.1016/j.apsoil.2015.10.015
摘要

Recent peatland restoration studies have highlighted the need to modify the conventional approach of monitoring the recovery of biogeochemical functions through above-ground processes by integrating below-ground components, which are potentially sensitive indicators of reclamation trajectory in long-term monitoring programs. In this study, the recovery of nutrient cycling processes were assessed from both above and below-ground perspectives in a fen constructed on a post-mining landscape in the Athabasca oil sands region, Canada. The goal of this study was to understand if and how different revegetation strategies (seedlings (SDL); moss layer transfers (MLT); seedlings with moss transfer (SMLT) and a control treatment (CTRL)) influence the evolution of biogeochemical functions in the constructed fen relative to a natural reference (REF). The treatments were replicated 6 times and monitored over 2 growing seasons. Our results showed that revegetation facilitated both above-ground productivity and the cycling of below-ground nutrients, especially in the species-rich SMLT plots. Supply of labile substrates in the re-vegetated plots increased microbial potential activity. This was reflected in higher rates of respiration (c.7.8 g CO2 m−2 day−2), nutrient acquisition (net immobilization) and productivity (c. −16.3 g CO2 m−2 day−2) among revegetated plots relative to the CTRL. Nutrient dynamics within the constructed fen suggest that phosphorus limitation (N:P ratio > 20) could hamper the establishment of a diverse plant community, whereas the build-up of microbial biomass appears to be NO3− limited. Our results also emphasize the need to track the evolution of nutrients cycling processes through long-term monitoring programs, and identify the potential use of ammonification, nitrogen mineralization and phosphorus availability as functional indicators of a fen’s recovery trajectory towards conditions present in natural fens.
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