Are variations in heterotrophic soil respiration related to changes in substrate availability and microbial biomass carbon in the subtropical forests?
Are variations in heterotrophic soil respiration related to changes in substrate availability and microbial biomass carbon in the subtropical forests?
复制标题
异养土壤呼吸的变化是否与亚热带森林底物可用性和微生物生物量碳的变化有关?
DOI:
10.1038/srep18370
复制
发表时间:
2015-12-16
影响因子:
4.6
通讯作者:
Shen W
中科院分区:
文献类型:
--
作者:
Wei H;Chen X;Xiao G;Guenet B;Vicca S;Shen W
Soil temperature and moisture are widely-recognized controlling factors on heterotrophic soil respiration (Rh), although they often explain only a portion of Rhvariability. How other soil physicochemical and microbial properties may contribute to Rhvariability has been less studied. We conducted field measurements on Rhhalf-monthly and associated soil properties monthly for two years in four subtropical forests of southern China to assess influences of carbon availability and microbial properties on Rh. Rhin coniferous forest was significantly lower than that in the other three broadleaf species-dominated forests and exhibited obvious seasonal variations in the four forests (P< 0.05). Temperature was the primary factor influencing the seasonal variability of Rhwhile moisture was not in these humid subtropical forests. The quantity and decomposability of dissolved organic carbon (DOC) were significantly important to Rhvariations, but the effect of DOC content on Rhwas confounded with temperature, as revealed by partial mantel test. Microbial biomass carbon (MBC) was significantly related to Rhvariations across forests during the warm season (P= 0.043). Our results suggest that DOC and MBC may be important when predicting Rhunder some conditions and highlight the complexity by mutual effects of them with environmental factors on Rhvariations.