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| DOI | 10.1016/j.soilbio.2024.109367 |
| The path from root input to mineral-associated soil carbon is dictated by habitat-specific microbial traits and soil moisture | |
| 发表日期 | 2024 |
| ISSN | 0038-0717 |
| EISSN | 1879-3428 |
| 起始页码 | 193 |
| 卷号 | 193 |
| 英文摘要 | Soil microorganisms help transform plant inputs into mineral-associated soil organic carbon (SOC) - the largest and slowest-cycling pool of organic carbon on land. However, the microbial traits that influence this process are widely debated. While current theory and biogeochemical models have settled on carbon-use efficiency (CUE) and growth rate as positive predictors of mineral-associated SOC, empirical tests are sparse, with contradictory observations. Using 13C-labeling of an annual grass (Avena barbata) under two moisture regimes, we found that microbial traits associated with formation of 13C-mineral-associated SOC varied by soil habitat, as did active microbial taxa and SOC chemical composition. In the rhizosphere, bacterial-dominated communities with fast growth, high biomass, and high extracellular polymeric substance (EPS) production were positively associated with 13C-mineral-associated SOC. In contrast, the detritusphere held communities dominated by fungi and more filamentous bacteria, and with greater exoenzyme activity; there, 13C-mineral-associated SOC was associated with slower microbial growth and lower microbial biomass. CUE was a negative predictor of 13C-mineralassociated SOC in both habitats. Using 13C-quantitative stable isotope probing, we found that the majority of 13C assimilation in the rhizosphere and detritusphere at week 12 of the experiment was performed by very few bacterial and fungal taxa (3-5% of the total taxa that assimilated 13C). Several complementary chemical analyses (13C-NMR, FTICR-MS, and STXM-NEXAFS) suggested that SOC in the rhizosphere had a more oxidized chemical signature, while SOC in the detritusphere had a less oxidized, more lignin-like chemical signature. Our findings challenge current theory by demonstrating that microbial traits linked with mineral-associated SOC are not universal, but vary with soil habitat and moisture conditions, and are shaped by a small number of active taxa. Emerging SOC models that explicitly reflect these interactions may better predict SOC storage, since climate change causes shifts in soil moisture regimes and the ratio of living versus decaying roots. |
| 英文关键词 | Soil carbon; Microbial traits; Mineral -associated organic carbon; Drought; Carbon cycle; Global change; Stable isotope probing |
| 语种 | 英语 |
| WOS研究方向 | Agriculture |
| WOS类目 | Soil Science |
| WOS记录号 | WOS:001218331000001 |
| 来源期刊 | SOIL BIOLOGY & BIOCHEMISTRY
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| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/305054 |
| 作者单位 | United States Department of Energy (DOE); Lawrence Livermore National Laboratory; Northern Arizona University; University of San Francisco; United States Department of Energy (DOE); Pacific Northwest National Laboratory; University of California System; University of California Berkeley; United States Department of Energy (DOE); Lawrence Berkeley National Laboratory; Yale University; University of California System; University of California Merced |
| 推荐引用方式 GB/T 7714 | . The path from root input to mineral-associated soil carbon is dictated by habitat-specific microbial traits and soil moisture[J],2024,193. |
| APA | (2024).The path from root input to mineral-associated soil carbon is dictated by habitat-specific microbial traits and soil moisture.SOIL BIOLOGY & BIOCHEMISTRY,193. |
| MLA | "The path from root input to mineral-associated soil carbon is dictated by habitat-specific microbial traits and soil moisture".SOIL BIOLOGY & BIOCHEMISTRY 193(2024). |
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