Premium
The relative importance of exogenous and substrate‐derived nitrogen for microbial growth during leaf decomposition
Author(s) -
Cheever B. M.,
Webster J. R.,
Bilger E. E.,
Thomas S. A.
Publication year - 2013
Publication title -
ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.144
H-Index - 294
eISSN - 1939-9170
pISSN - 0012-9658
DOI - 10.1890/12-1339.1
Subject(s) - detritus , substrate (aquarium) , decomposition , heterotroph , organic matter , environmental chemistry , nitrogen , chemistry , maple , dissolved organic carbon , nitrogen cycle , bacterial growth , sugar , ecology , nutrient cycle , cycling , nutrient , botany , biology , bacteria , food science , organic chemistry , genetics , history , archaeology
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 15 N to differentiate between microbial N that had been assimilated from the leaf substrate (enriched with 15 N) or immobilized from the water (natural abundance 15 N: 14 N) in five Appalachian streams ranging in ambient NO 3 ‐N concentrations from about 5 to 900 μg NO 3 ‐N/L. Ambient NO 3 − 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 15 N 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.