Abstract
Increases in nitrogen (N) availability reduce decay rates of highly lignified plant litter. Although microbial responses to N addition are well documented, the chemical mechanisms that may give rise to this inhibitory effect remain unclear. Here, we ask: Why does increased N availability inhibit lignin decomposition? We hypothesized that either (1) decomposers degrade lignin to obtain N and stop producing lignin-degrading enzymes if mineral N is available, or (2) chemical reactions between lignin and mineral N decrease the quality of lignin and limit the ability of decomposers to break it down. In order to test these hypotheses, we tracked changes in carbon (C) mineralization, microbial biomass and enzyme activities, litter chemistry, and lignin monomer concentrations over a 478-day laboratory incubation of three maize genotypes differing in lignin quality and quantity (F292bm3 (high lignin) < F2 (medium lignin) < F2bm1 (low lignin)). Maize stem internodes of each genotype were mixed with either an acidic or neutral pH sandy soil, both with and without added N. Nitrogen addition reduced C mineralization, microbial biomass, and lignin-degrading enzyme activities across most treatments. These dynamics may be due to suppressed fungal growth and reduced microbial acquisition of lignin-shielded proteins in soils receiving N. However, N addition alone did not significantly alter the quantity or quality of lignin monomers in any treatment. Our results suggest that abiotic interactions between N and phenolic compounds did not influence lignin chemistry, but mineral N does alter microbial enzyme and biomass dynamics, with potential longer-term effects on soil C dynamics.






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Acknowledgments
This research was supported by an NSF Ecosystems Program Grant (# 0918718) to MNW and ASG and the NSF Research Coordination Network on Enzymes in the Environment Grant (# 0840869). For field and laboratory assistance, we thank Bethany Chidester, Dashanne Czegledy, Michael Elk, Mallory Ladd, Ryan Monnin, Steve Solomon, Heather Thoman, Logan Thornsberry, Eric Wellman, Travis White, and Megan Wenzel. We also thank three anonymous reviewers whose suggestions greatly improved this work.
Author contributions
MNW and IB conceived the project. Microbial analyses were conducted by ZLR. CuO analyses were performed by BZA and IB. ASG and KW provided the py-GCMS data. ZLR and BZA analyzed the data. ZLR wrote the article with input from the other authors.
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Supplementary Fig. 1
Microbial biomass-C (MB-C) for all genotypes in both soil types (acidic and neutral pH) with and without added N after day 0. Values represent the mean ± SE for each treatment over the final 9 incubation harvests (n = 36). Units are mg-C g dry litter−1. Significant nitrogen (N− > N+) and pH (neutral > acidic) effects predominated between days 27–478. Supplementary material 1 (TIFF 328 kb)
Supplementary Fig. 2
Cn/V ratio on days 120 and 478 during a laboratory incubation of low (A), medium (B), and high (C) lignin maize genotypes. Each genotype was mixed with either an acidic or neutral pH sandy soil, both with and without added N. Nitrogen addition had no significant effect on Cn/V ratios. Supplementary material 2 (TIFF 486 kb)
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Rinkes, Z.L., Bertrand, I., Amin, B.A.Z. et al. Nitrogen alters microbial enzyme dynamics but not lignin chemistry during maize decomposition. Biogeochemistry 128, 171–186 (2016). https://doi.org/10.1007/s10533-016-0201-0
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DOI: https://doi.org/10.1007/s10533-016-0201-0