The relative importance of exogenous and substrate-derived nitrogen for microbial growth during leaf decomposition
dc.contributor.author | Cheever, B. M. | en |
dc.contributor.author | Webster, Jackson R. | en |
dc.contributor.author | Bilger, E. E. | en |
dc.contributor.author | Thomas, S. A. | en |
dc.contributor.department | Biological Sciences | en |
dc.date.accessed | 2014-03-11 | en |
dc.date.accessioned | 2014-03-27T13:05:59Z | en |
dc.date.available | 2014-03-27T13:05:59Z | en |
dc.date.issued | 2013-07 | en |
dc.description.abstract | Heterotrophic microbes colonizing detritus obtain nitrogen (N) for growth by assimilating N from their substrate or immobilizing exogenous inorganic N. Microbial use of these two pools has different implications for N cycling and organic matter decomposition in the face of the global increase in biologically available N. We used sugar maple leaves labeled with N-15 to differentiate between microbial N that had been assimilated from the leaf substrate (enriched with N-15) or immobilized from the water (natural abundance N-15:N-14) in five Appalachian streams ranging in ambient NO3-N concentrations from about 5 to 900 g NO3-N/L. Ambient NO3- concentration increased sugar maple decomposition rate but did not influence the proportion of microbial N derived from substrate or exogenous pools. Instead, these proportions were strongly influenced by the percentage of detrital ash-free dry mass (AFDM) remaining. Substrate-derived N made up a large proportion of the microbial N after the first 24 h in all streams. Detrital and microbial isotopic N-15 signatures approached that of the water as decomposition progressed in all streams, suggesting that exogenous N may be the predominant source of N for meeting microbial requirements even when exogenous N concentrations are low. Our results support predictions of more rapid decomposition of organic matter in response to increased N availability and highlight the tight coupling of processes driving microbial N cycling and organic matter decomposition. | en |
dc.description.sponsorship | NSF DEB-0823293, DEB-02218001, DEB-478406 | en |
dc.format.mimetype | application/pdf | en |
dc.identifier.citation | B. M. Cheever, J. R. Webster, E. E. Bilger, and S. A. Thomas 2013. The relative importance of exogenous and substrate-derived nitrogen for microbial growth during leaf decomposition. Ecology 94:1614-1625. http://dx.doi.org/10.1890/12-1339.1 | en |
dc.identifier.doi | https://doi.org/10.1890/12-1339.1 | en |
dc.identifier.issn | 0012-9658 | en |
dc.identifier.uri | http://hdl.handle.net/10919/46815 | en |
dc.identifier.url | http://www.esajournals.org/doi/pdf/10.1890/12-1339.1 | en |
dc.language.iso | en | en |
dc.publisher | Ecological Society of America | en |
dc.rights | In Copyright | en |
dc.rights.holder | Ecological Society of America | en |
dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | en |
dc.subject | n-15 | en |
dc.subject | assimilation | en |
dc.subject | chloroform fumigation | en |
dc.subject | heterotrophic microbes | en |
dc.subject | immobilization | en |
dc.subject | nitrogen availability | en |
dc.subject | nitrogen cycling | en |
dc.subject | organic matter | en |
dc.subject | decomposition | en |
dc.subject | streams | en |
dc.subject | forest litter decomposition | en |
dc.subject | soil-nitrogen | en |
dc.subject | woodland stream | en |
dc.subject | chloroform | en |
dc.subject | fumigation | en |
dc.subject | phosphorus dynamics | en |
dc.subject | foliar litter | en |
dc.subject | nutrient | en |
dc.subject | carbon | en |
dc.subject | release | en |
dc.subject | lignin | en |
dc.title | The relative importance of exogenous and substrate-derived nitrogen for microbial growth during leaf decomposition | en |
dc.title.serial | Ecology | en |
dc.type | Article - Refereed | en |
dc.type.dcmitype | Text | en |
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