Carbon and nitrogen recycling from microbial necromass to cope with C:N stoichiometric imbalance by priming. (March 2020)

• Record Type: Journal Article
• Authors: Cui, Jun; Zhu, Zhenke; Xu, Xingliang; Liu, Shoulong; Jones, Davey L.; Kuzyakov, Yakov; Shibistova, Olga; Wu, Jinshui; Ge, Tida
• Is Part Of: Soil biology and biochemistry. Volume 142(2020)
• Publication Date: 2020-03
• Subjects: Soil carbon -- Priming effects -- Glucose mineralization -- Compound-specific 13C-PLFA analysis -- Necromass recycling -- Stoichiometric imbalance; Soil biochemistry -- Periodicals; Soil biology -- Periodicals; Sols -- Biochimie -- Périodiques; Sols -- Biologie -- Périodiques; Sols -- Microbiologie -- Périodiques; Bodembiologie; Biochemie; 631.46
• DOI: 10.1016/j.soilbio.2020.107720
• Languages: English
• ISSNs: 0038-0717

Abstract

Abstract: The impact of increasing amounts of labile C input on priming effects (PE) on soil organic matter (SOM) mineralization remains unclear, particularly under anoxic conditions and under high C input common in microbial hotspots. PE and their mechanisms were investigated by a 60-day incubation of three flooded paddy soils amended with 13 C-labeled glucose equivalent to 50–500% of microbial biomass C (MBC). PE (14–55% of unamended soil) peaked at moderate glucose addition rates (i.e., 50–300% of MBC). Glucose addition above 300% of MBC suppressed SOM mineralization but intensified microbial N acquisition, which contradicted the common PE mechanism of accelerating SOM decomposition for N-supply (frequently termed as "N mining"). Particularly at glucose input rate higher than 3 g kg −1 (i.e., 300–500% of MBC), mineral N content dropped on day 2 close to zero (1.1–2.5 mg N kg −1 ) because of microbial N immobilization. To cope with the N limitation, microorganisms greatly increased N-acetyl glucosaminidase and leucine aminopeptidase activities, while SOM decomposition decreased. Several discrete peaks of glucose-derived CO2 (contributing >80% to total CO2 ) were observed between days 13–30 under high glucose input (300–500% of MBC), concurrently with CH4 peaks. Such CO2 dynamics was distinct from the common exponential decay pattern, implicating the recycling and mineralization of 13 C-enriched microbial necromass driven by glucose addition. Therefore, N recycling from necromass was hypothesized as a major mechanism to alleviate microbial N deficiency without SOM priming under excess labile C input. Compound-specific 13 C-PLFA confirmed the redistribution of glucose-derived C among microbial groups, i.e., necromass recycling. Following glucose input, more than 4/5 of total 13 C-PLFA was in the gram-negative and some non-specific bacteria, suggesting these microorganisms as r -strategists capable of rapidly utilizing the most labile C. However, their 13 C-PLFA content decreased by 70% after 60 days, probably as a result of death of these r -strategists. On the contrary, the 13 C-PLFA in gram-positive bacteria, actinomycetes and fungi (K-strategists) was initially minimal but increased by 0.5–5 folds between days 2 and 60. Consequently, the necromass of dead r -strategists provided a high-quality C–N source to the K-strategists. We conclude that under severe C excess, N recycling from necromass is a much more efficient microbial strategy to cover the acute N demand than N acquisition from the recalcitrant SOM. Highlights: Priming effects (PEs) have a unimodal relationship to amount of added glucose. Microbial acquisition of N at high glucose amounts was intensified without increasing PEs. 13 C-PLFA reflects recycling of necromass C between microbial groups. 13 C-enriched CO2 peaks violating exponential decay suggest necromass decomposition. Necromass-N recycling was necessary to overcome N deficiency without priming other SOM pools.