Journal
BIOGEOCHEMISTRY
Volume 142, Issue 2, Pages 299-313Publisher
SPRINGER
DOI: 10.1007/s10533-018-00535-4
Keywords
Forest soil; Carbon storage; Carbon biogeochemistry; Phospholipid fatty acids; Organic matter biomarkers; Lignin; Cutin; Suberin; Forest soils
Funding
- Natural Sciences and Engineering Research Council (NSERC) of Canada [2015-05760, 478038-15]
- Allegheny College
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Forest soil organic carbon (SOC) is one of the largest reservoirs of terrestrial carbon (C) and is a major component of the global C cycle. Yet there is still uncertainty regarding how ecosystems, and the SOC they store, will respond to changes due to anthropogenic processes. Current and future reactive nitrogen (N) deposition to forest soils may alter biogeochemical processes and shift both the quantity and quality of stored SOC. We studied SOC storage and molecular-level composition after 22years of N additions (100kgNha(-1)y(-1)) in a temperate deciduous forest. SOC storage in surface soils increased by 0.93kgm(-2) due to a decline in microbial biomass (phospholipid fatty acids) and litter decomposition. N additions resulted in the selective preservation of a range of plant-derived compounds including steroids, lignin-derived, cutin-derived, and suberin-derived compounds that have anti-microbial properties or are non-preferred microbial substrates. This overall shift in SOC composition suggests limited sustainability and a decline in soil health. The reduction in microbial biomass and increase in specific SOC components demonstrate that long-term N fertilization negatively alters fundamental C cycling in forest soils. This study also demonstrates unequivocally that anthropogenic impacts onC and N cycling in forests at the molecular-level must be considered more holistically.
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