Institute of Microbiology of the CAS, Vídeňská 1083, 14220, Praha 4, Czech Republic.
Faculty of Science, Charles University, Albertov 6, 128 43, Praha 2, Czech Republic.
Microbiome. 2017 Sep 18;5(1):122. doi: 10.1186/s40168-017-0340-0.
Evergreen coniferous forests contain high stocks of organic matter. Significant carbon transformations occur in litter and soil of these ecosystems, making them important for the global carbon cycle. Due to seasonal allocation of photosynthates to roots, carbon availability changes seasonally in the topsoil. The aim of this paper was to describe the seasonal differences in C source utilization and the involvement of various members of soil microbiome in this process.
Here, we show that microorganisms in topsoil encode a diverse set of carbohydrate-active enzymes, including glycoside hydrolases and auxiliary enzymes. While the transcription of genes encoding enzymes degrading reserve compounds, such as starch or trehalose, was high in soil in winter, summer was characterized by high transcription of ligninolytic and cellulolytic enzymes produced mainly by fungi. Fungi strongly dominated the transcription in litter and an equal contribution of bacteria and fungi was found in soil. The turnover of fungal biomass appeared to be faster in summer than in winter, due to high activity of enzymes targeting its degradation, indicating fast growth in both litter and soil. In each enzyme family, hundreds to thousands of genes were typically transcribed simultaneously.
Seasonal differences in the transcription of glycoside hydrolases and auxiliary enzyme genes are more pronounced in soil than in litter. Our results suggest that mainly fungi are involved in decomposition of recalcitrant biopolymers in summer, while bacteria replace them in this role in winter. Transcripts of genes encoding enzymes targeting plant biomass biopolymers, reserve compounds and fungal cell walls were especially abundant in the coniferous forest topsoil.
常绿针叶林含有大量的有机物质。这些生态系统中的凋落物和土壤中会发生大量的碳转化,使它们成为全球碳循环的重要组成部分。由于光合作用产物会季节性地分配到根系中,因此表土中的碳供应会随季节而变化。本文旨在描述 C 源利用的季节性差异以及土壤微生物组的不同成员在这一过程中的参与情况。
我们发现,表土中的微生物编码了一套多样化的碳水化合物活性酶,包括糖苷水解酶和辅助酶。虽然在冬季土壤中,用于降解储备化合物(如淀粉或海藻糖)的酶的基因转录水平较高,但在夏季,木质素降解酶和纤维素酶的转录水平较高,这些酶主要由真菌产生。真菌在凋落物和土壤中的转录均占主导地位,而细菌和真菌的贡献相等。由于针对真菌生物量降解的酶活性较高,真菌生物量的周转率似乎在夏季比冬季更快,这表明凋落物和土壤中的真菌生长迅速。在每个酶家族中,通常有数百到数千个基因同时转录。
糖苷水解酶和辅助酶基因的转录在土壤中的季节性差异比凋落物中更为明显。我们的结果表明,主要是真菌在夏季参与了难降解生物聚合物的分解,而在冬季,细菌取代了它们的作用。编码针对植物生物量生物聚合物、储备化合物和真菌细胞壁的酶的基因的转录本在针叶林表土中特别丰富。