Abstract

Litter decomposition is a key process that drives carbon and nutrient cycles in forest soils. The decomposition of five different substrate types was analyzed in hemiboreal coniferous forests, focusing on the mass loss and nutrient (N, P, and K) release of fine roots (FR) and needle litter in relation to the initial substrate and soil chemistry. A litterbag incubation experiment with site-specific FR and needle litter and three standard substrates (green and rooibos tea, α-cellulose) was carried out in four Norway spruce and four Scots pine-dominated stands in Estonia. Substrate type was the primary driver of mass loss and the decay rate of different substrates did not depend on the dominant tree species of the studied stands. Alpha-cellulose lost 98 ± 1% of the mass in 2-years, while the FR mass loss was on average 23 ± 2% after 3-years of decomposition. The FR decomposition rate could be predicted using a corresponding model of green tea, although the rate of FR decomposition is approximately five times lower than the rate of green tea in the first 3-years. The annual decomposition rate of the needle litter is rather constant in hemiboreal coniferous forests in the first 3 years. The initial substrate of fine roots or needle litter and soil chemistry jointly had a significant effect on mass loss in the later stage of decomposition. The critical N concentration for N release was lower for pine FR and needle litter (0.9–1.3% and 0.7–1.1%) compared to spruce (1.2–1.6% and 1.5–1.9%, respectively). The release rate of K depended on the initial K of substrate, while the release of N and P was significantly related to the initial C:N and N:P ratios, respectively. The results show the central role of soil and substrate initial chemistry in the decomposition of fine roots and needle litter across hemiboreal forests, especially at later stage (after 2 years) of decomposition. The slower decomposition and higher retention of N in the fine roots relative to needle litter suggests that fine roots have a substantial role in the carbon and nitrogen accumulation in boreal and hemiboreal forest ecosystems.

Highlights

  • Decomposition is a crucial process in forest soil regulating long-term storage of carbon and nutrient availability and determining soil fertility (Aerts, 1997; Berg and McClaugherty, 2008)

  • The average content of TOC and the C:N ratio was significantly higher and the concentration of K was significantly lower in the pine needles compared to the spruce needles, while there were no significant differences in the chemical composition of the incubated fine roots between tree species

  • Results from Redundancy analysis (RDA) analysis with manual selection showed that the decomposition time, sites and stand productivity (B), and the average K content in the soil organic layer explained approximately 76% of the variation in mass loss of all substrates over 3 years of the study period (p < 0.05; Supplementary Figure 1)

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Summary

Introduction

Decomposition is a crucial process in forest soil regulating long-term storage of carbon and nutrient availability and determining soil fertility (Aerts, 1997; Berg and McClaugherty, 2008). Litter quality, which is mainly determined by the relative content of recalcitrant organic compounds (e.g., lignin or phenols) and macronutrients, is of particular importance in controlling the mass loss and dynamics of litter nutrients during decay under similar climatic conditions (Prescott et al, 2000; Berg and McClaugherty, 2008). In addition to climate (temperature, precipitation), local site conditions (fertility, litter and soil chemistry, decomposer community) influence litter decomposition through the combined effect of nutrient availability and the soil moisture regime (Chapin et al, 2002). The main chemical soil properties include pH, organic carbon content and nutrients, of which soil nitrogen and phosphorus have been reported to be regulating and limiting factors (Coleman et al, 1999; DeLuca and Boisvenue, 2012)

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