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Turnover of labile and recalcitrant soil carbon differ in\ud response to nitrate and ammonium deposition in an\ud ombrotrophic peatland

By Pauline M. Currey, David Johnson, Lucy J. Sheppard, Ian D. Leith, Hannah Toberman, Rene Van Der Wal, Lorna A. Dawson and Rebekka R.E. Artz


The effects of 4 years of simulated nitrogen deposition, as nitrate (NO3\ud ) and ammonium\ud (NH4\ud 1), on microbial carbon turnover were studied in an ombrotrophic peatland. We\ud investigated the mineralization of simple forms of carbon using MicroRespt measurements\ud (a multiple substrate induced respiration technique) and the activities of four soil enzymes\ud involved in the decomposition of more complex forms of carbon or in nutrient acquisition: Nacetyl-\ud glucosaminidase (NAG), cellobiohydrolase (CBH), acid phosphatase (AP), and phenol\ud oxidase (PO). The potential mineralization of labile forms of carbon was significantly\ud enhanced at the higher N additions, especially with NH4\ud 1 amendments, while potential\ud enzyme activities involved in breakdown of more complex forms of carbon or nutrient\ud acquisition decreased slightly (NAG and CBH) or remained unchanged (AP and PO) with\ud N amendments. This study also showed the importance of distinguishing between NO3\ud and\ud NH4\ud 1 amendments, as their impact often differed. It is possible that the limited response on\ud potential extracellular enzyme activity is due to other factors, such as limited exposure to the\ud added N in the deeper soil or continued suboptimal functioning of the enzymes due to the\ud low pH, possibly via the inhibitory effect of low phenol oxidase activity

Topics: Botany, Agriculture and Soil Science, Biology and Microbiology, Atmospheric Sciences
Year: 2010
DOI identifier: 10.1111/j.1365-2486.2009.02082.x
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