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

The effects of 4 years of simulated nitrogen deposition, as nitrate (NO₃⁻) and ammonium (NH₄⁺), on microbial carbon turnover were studied in an ombrotrophic peatland. We investigated the mineralization of simple forms of carbon using MicroResp[trade mark sign] measurements (a multiple substrate indu...

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Published inGlobal change biology Vol. 16; no. 8; pp. 2307 - 2321
Main Authors CURREY, PAULINE M, JOHNSON, DAVID, SHEPPARD, LUCY J, LEITH, IAN D, TOBERMAN, HANNAH, van derWAL, RENÉ, DAWSON, LORNA A, ARTZ, REBEKKA R.E
Format Journal Article
LanguageEnglish
Published Oxford, UK Oxford, UK : Blackwell Publishing Ltd 01.08.2010
Blackwell Publishing Ltd
Wiley-Blackwell
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Summary:The effects of 4 years of simulated nitrogen deposition, as nitrate (NO₃⁻) and ammonium (NH₄⁺), on microbial carbon turnover were studied in an ombrotrophic peatland. We investigated the mineralization of simple forms of carbon using MicroResp[trade mark sign] measurements (a multiple substrate induced respiration technique) and the activities of four soil enzymes involved in the decomposition of more complex forms of carbon or in nutrient acquisition: N-acetyl-glucosaminidase (NAG), cellobiohydrolase (CBH), acid phosphatase (AP), and phenol oxidase (PO). The potential mineralization of labile forms of carbon was significantly enhanced at the higher N additions, especially with NH₄⁺ amendments, while potential enzyme activities involved in breakdown of more complex forms of carbon or nutrient acquisition decreased slightly (NAG and CBH) or remained unchanged (AP and PO) with N amendments. This study also showed the importance of distinguishing between NO₃⁻ and NH₄⁺ amendments, as their impact often differed. It is possible that the limited response on potential extracellular enzyme activity is due to other factors, such as limited exposure to the added N in the deeper soil or continued suboptimal functioning of the enzymes due to the low pH, possibly via the inhibitory effect of low phenol oxidase activity.
Bibliography:http://dx.doi.org/10.1111/j.1365-2486.2009.02082.x
ArticleID:GCB2082
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ISSN:1354-1013
1365-2486
DOI:10.1111/j.1365-2486.2009.02082.x