Microbial interactions affect sources of priming induced by cellulose

纤维素 微生物 生物量(生态学) 微生物种群生物学 分解 分解者 化学 细菌 有机质 溶解有机碳 基质(水族馆) 生物 环境化学 植物 食品科学 生态学 生物化学 生态系统 遗传学
作者
Еvgenia Blagodatskaya,Nikita Khomyakov,Olga Myachina,И. Н. Богомолова,Sergey Blagodatsky,Yakov Kuzyakov
出处
期刊:Soil Biology & Biochemistry [Elsevier]
卷期号:74: 39-49 被引量:146
标识
DOI:10.1016/j.soilbio.2014.02.017
摘要

The recently developed 3-source-partitioning approach: addition of 14C labeled organics to soil after C3–C4 vegetation changes, was used to distinguish C sources in three compartments, namely CO2, microbial biomass and dissolved organic C (DOC) during decomposition of labeled cellulose. Microbial community structure (based on PLFA composition) and functions (based on enzyme activities and on microbial growth parameters) revealed mechanisms and drivers of priming effects (PE) induced by cellulose addition. 14C-cellulose input caused negative PE within the first week and was accompanied by fast consumption of unlabelled DOC and its incorporation into microbial biomass. Microbial activation however, was not confirmed by substrate-induced respiration, nor by hydrolytic enzymes activity or by PLFA changes. A remarkable exception was a 2-fold increase in protozoan PLFA. Such an increase indicates that microorganisms feeding on cellulose and on DOC were quickly grazed by protozoans acting as a driver of microbial succession. This experimentally demonstrates the functioning of the microbial interactions: protozoan grazers provided for rapid recycling of nutrients and facilitated the succession of cellulose-degrading microorganisms during the second week of cellulose decomposition. An increase in the activity of cellulolytic enzymes caused short-term real PE accompanied by increase in abundance of slow-growing fungi and G(−) bacteria. Long-term real PE observed between 14 and 60 days after cellulose input was due to decomposition of SOM-originated hemicelluloses by fungi and G(+) bacteria. The CO2 released by primed soil organic matter (SOM) decomposition was originated mainly from C younger than 12 years (63%) and only 37% were older than 12 years despite the recent and old C contributed almost equally (51 and 49%, respectively) to SOM under Miscanthus giganteus. This indicates that the SOM pools are involved in PE according to their availability. Despite 71% of the applied cellulose-C was sequestered in the soil, the net soil C-gain amounted only for 28% of the applied cellulose-C after factoring in the C losses by the PE. Our study emphasizes the role of food webs in the PE dynamics: cellulose input served as a driver activating the food chain through the microbial loop.
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