Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1111/gcb.15430 |
Divergent drivers of the microbial methane sink in temperate forest and grassland soils | |
Jana Tä; umer; Steffen Kolb; Runa S. Boeddinghaus; Haitao Wang; Ingo Schö; ning; Marion Schrumpf; Tim Urich; Sven Marhan | |
2020-11-22 | |
发表期刊 | Global Change Biology |
出版年 | 2020 |
英文摘要 | Aerated topsoils are important sinks for atmospheric methane (CH4) via oxidation by CH4‐oxidizing bacteria (MOB). However, intensified management of grasslands and forests may reduce the CH4 sink capacity of soils. We investigated the influence of grassland land‐use intensity (150 sites) and forest management type (149 sites) on potential atmospheric CH4 oxidation rates (PMORs) and the abundance and diversity of MOB (with qPCR) in topsoils of three temperate regions in Germany. PMORs measurements in microcosms under defined conditions yielded approximately twice as much CH4 oxidation in forest than in grassland soils. High land‐use intensity of grasslands had a negative effect on PMORs (−40%) in almost all regions and fertilization was the predominant factor of grassland land‐use intensity leading to PMOR reduction by 20%. In contrast, forest management did not affect PMORs in forest soils. Upland soil cluster (USC)‐α was the dominant group of MOBs in the forests. In contrast, USC‐γ was absent in more than half of the forest soils but present in almost all grassland soils. USC‐α abundance had a direct positive effect on PMOR in forest, while in grasslands USC‐α and USC‐γ abundance affected PMOR positively with a more pronounced contribution of USC‐γ than USC‐α. Soil bulk density negatively influenced PMOR in both forests and grasslands. We further found that the response of the PMORs to pH, soil texture, soil water holding capacity and organic carbon and nitrogen content differ between temperate forest and grassland soils. pH had no direct effects on PMOR, but indirect ones via the MOB abundances, showing a negative effect on USC‐α, and a positive on USC‐γ abundance. We conclude that reduction in grassland land‐use intensity and afforestation has the potential to increase the CH4 sink function of soils and that different parameters determine the microbial methane sink in forest and grassland soils. |
领域 | 气候变化 ; 资源环境 |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/304255 |
专题 | 气候变化 资源环境科学 |
推荐引用方式 GB/T 7714 | Jana Tä,umer,Steffen Kolb,et al. Divergent drivers of the microbial methane sink in temperate forest and grassland soils[J]. Global Change Biology,2020. |
APA | Jana Tä.,umer.,Steffen Kolb.,Runa S. Boeddinghaus.,Haitao Wang.,...&Sven Marhan.(2020).Divergent drivers of the microbial methane sink in temperate forest and grassland soils.Global Change Biology. |
MLA | Jana Tä,et al."Divergent drivers of the microbial methane sink in temperate forest and grassland soils".Global Change Biology (2020). |
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