Climate Change Data Portal
DOI | 10.1016/j.geoderma.2023.116736 |
Decoupling of soil carbon mineralization and microbial community composition across a climate gradient on the Tibetan Plateau | |
Zheng, Jinyang; Mao, Xiali; van Groenigen, Kees Jan; Zhang, Shuai; Wang, Mingming; Guo, Xiaowei; Yu, Wu; Luo, Lun; Chang, Jinfeng; Shi, Zhou; Luo, Zhongkui | |
发表日期 | 2024 |
ISSN | 0016-7061 |
EISSN | 1872-6259 |
卷号 | 441 |
英文摘要 | Soil microbes drive soil organic carbon (SOC) mineralization. Because microbial groups differ in metabolic efficiency and respond differently to temperature variation, it is reasonable to expect a close association of SOC mineralization and its temperature sensitivity (Q(10) which is defined as the factor of the change of soil carbon mineralization induced by 10 degrees C temperature increase) with microbial community diversity and composition. However, these relations have rarely been tested. Here, we conducted an incubation experiment to assess the temperature responses of microbial alpha diversity and the relative abundance of microbial r- and K-strategists in soils from a wide range of ecosystems across a climate gradient in the southeast Tibet. The results indicated that the instantaneous alpha diversity and the relative abundance of r- and K-strategists are significantly (P < 0.05) influenced by temperature, but these microbial variables are poor predictors of SOC mineralization measured at the same time. Rather, microbial community diversity and the relative abundance of r- and K-strategists of fresh soils showed consistent and significant (P < 0.05) effects on both SOC mineralization and Q(10) at different incubation stages. Importantly, path analysis indicated that microbial alpha diversity and r- and K-strategists exerts no independent effects on SOC mineralization and Q(10) when variation in climate, SOC chemistry, physical protection, and edaphic properties are accounted for. Together, our results suggest that while soil microbial community diversity and composition are a strong proxy of SOC quality and availability, they are not a fundamental determinant of SOC mineralization and Q(10). |
关键词 | BacteriaCarbon fractionsFungiMicrobial diversityr/K strategistsSoil organic carbonTemperature sensitivity (Q (10) )Soil profile |
英文关键词 | TEMPERATURE SENSITIVITY; ORGANIC-MATTER; RESPIRATION; SUBSTRATE; BIOMASS; DECOMPOSITION; FRACTIONS; KNOWLEDGE; DYNAMICS; SYSTEM |
WOS研究方向 | Soil Science |
WOS记录号 | WOS:001138828700001 |
来源期刊 | GEODERMA |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/283626 |
作者单位 | Zhejiang University; University of Exeter; Tibet Agriculture & Animal Husbandry University; Zhejiang University; Zhejiang University |
推荐引用方式 GB/T 7714 | Zheng, Jinyang,Mao, Xiali,van Groenigen, Kees Jan,et al. Decoupling of soil carbon mineralization and microbial community composition across a climate gradient on the Tibetan Plateau[J],2024,441. |
APA | Zheng, Jinyang.,Mao, Xiali.,van Groenigen, Kees Jan.,Zhang, Shuai.,Wang, Mingming.,...&Luo, Zhongkui.(2024).Decoupling of soil carbon mineralization and microbial community composition across a climate gradient on the Tibetan Plateau.GEODERMA,441. |
MLA | Zheng, Jinyang,et al."Decoupling of soil carbon mineralization and microbial community composition across a climate gradient on the Tibetan Plateau".GEODERMA 441(2024). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。