Root litter decomposition slows with soil depth. (October 2018)

• Record Type: Journal Article
• Authors: Hicks Pries, Caitlin E.; Sulman, Benjamin N.; West, Corinna; O'Neill, Caitlin; Poppleton, Erik; Porras, Rachel C.; Castanha, Cristina; Zhu, Biao; Wiedemeier, Daniel B.; Torn, Margaret S.
• Is Part Of: Soil biology and biochemistry. Volume 125(2018)
• Page Start: 103
• Page End: 114
• Publication Date: 2018-10
• Subjects: Soil organic matter -- Carbon -- Decomposition -- Soil depth -- 13C -- Fine root -- Density fractionation -- PLFA; Soil biochemistry -- Periodicals; Soil biology -- Periodicals; Sols -- Biochimie -- Périodiques; Sols -- Biologie -- Périodiques; Sols -- Microbiologie -- Périodiques; Bodembiologie; Biochemie; 631.46
• DOI: 10.1016/j.soilbio.2018.07.002
• Languages: English
• ISSNs: 0038-0717

Abstract

Abstract: Even though over half of the world's soil organic carbon (SOC) is stored in subsoils (>20 cm deep), and the old ages of subsoil OC indicate its cycling differs from surface SOC, there are few studies examining in situ decomposition processes in deep soils. Here, we added 13 C-labeled fine roots to 15, 55, and 95 cm depths of a well-characterized coniferous forest Alfisol and monitored the amount of root-derived C remaining over 6, 12, and 30 months. We recovered the root-derived C in microbial phospholipid fatty acids (PLFAs) after 6 months and in coarse (>2 mm) particulate, fine (<2 mm) particulate, and dense, mineral-associated pools after 6, 12, and 30 months. Overall, root decomposition in the first 6 months was similar among all depths but significantly diverged at 30 months with faster decomposition at 15 cm than at 95 cm. There were more fungal and Gram negative-associated PLFAs at 15 cm than at 95 cm, and 13 C analysis revealed those microbial groups preferred the added root carbon to native SOC. Mineral-associations were not the cause of slower decomposition at depth because similar amounts of applied root C was recovered in the dense fraction at all depths. The largest difference among depths was in the amount of root C recovered in the coarse particulate fraction, which was greater at 95 cm (50%) than at 15 cm (15%). Slower decomposition of the particulate pool at depth likely contributed to the increase in C:N ratios and depletion of δ 13 C values below 60 cm depth in our soil profiles. Simulations of these soils using the CORPSE model, which incorporates microbial priming effects and mineral stabilization of SOC, reproduced patterns of particulate and mineral-associated SOC over both time and depth and suggested that a lack of priming by root exudates at depth could account for the slower decomposition rate of particulate root material. Decomposition of deep particulate SOC may increase if root exudation or dissolved OC transport to depth increases. Highlights: Fine root decay was similar across depths at first but then stalled at 95 cm. Organo-mineral associations were not the cause of slower decomposition at depth. Fine root litter at depth was stuck in the coarse particulate fraction. The CORPSE model showed how a lack of root exudates could slow decay at depth.