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Biology subjects

Zak, D. R.

Publications and source records attributed to Zak, D. R..

2 recordsLinked to original sources

Anthropogenic nitrogen deposition decouples relationships with decomposing microbes, altering SOM molecular composition, but not molecular complexity or diversity

Soil organic matter (SOM) consists of diverse biochemical constituents, spanning a spectrum of chemical complexity, and the relative abundance of these substrates influences microbial metabolism and soil carbon persistence. However, mechanistic controls governing these processes and how they may be affected by environmental change remains incomplete. This study aims to assess (1) the molecular-level changes that occur across stages of root decomposition, from undecayed plant root litter to 1-year decomposed root litter, to mineral SOM and (2) how these changes are altered by anthropogenic nitrogen (N) deposition by using SOM biochemical and microbiome datasets and a long-term field experiment. N deposition did not significantly alter undecomposed or 1-year decomposed root litter, but did alter decomposing microbial communities and mineral SOM biochemical composition, specifically in lignin- and lipid-derived compounds. Taken together, this restructuring of microbial communities and alteration of SOM biochemistry likely contributed to the previously observed reduction in SOM decomposition.

ecology↗

Gains in soil C storage under anthropogenic N deposition are rapidly lost following its cessation

Anthropogenic nitrogen (N) deposition enhanced the global terrestrial carbon (C) sink and partially offset anthropogenic CO2 emissions. This was driven by the suppression of microbial activity associated with the breakdown of soil organic matter. However, since the implementation of emission abatement policies in the 1970s, atmospheric N deposition has declined globally, and the consequences of this decline are unknown. Here, we assessed the response of soil C storage, and associated microbial activities, in a long-term field study that experimentally increased N deposition for 24-years. We measured soil C and N, parameters of microbial activity, and compared effect sizes of soil C in response to, and in recovery from, the N deposition treatment across the history of our experiment (1994-2022). Our results demonstrate that the accumulated C in the organic horizon has been lost and exhibit additional deficits 5-years post-termination of the N deposition treatment. These findings, in part, arise from mechanistic changes in microbial activity. Soil C in the mineral soil was less responsive thus far in recovery. If these organic horizon C dynamics are similar in other temperate forests, the Northern Hemisphere C sink will be reduced and climate warming will be enhanced.

ecology↗