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首页> 外文期刊>Soil Biology & Biochemistry >Additive effects of experimental climate change and land use on faunal contribution to litter decomposition
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Additive effects of experimental climate change and land use on faunal contribution to litter decomposition

机译:实验性气候变化和土地利用对垃圾分解的垃圾贡献的附加效应

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Litter decomposition is a key process determining the cycling of nutrients in ecosystems. Soil fauna plays an essential role in this process, e.g., by fragmenting and burrowing surface litter material, and thereby enhancing microbial decomposition. However, soil fauna-mediated decomposition might be influenced by interacting factors of environmental changes. Here we used a large-scale global change field experiment to test potential interacting effects between land-use type (croplands and grasslands differing in management intensity) and projected climate change on litter decomposition rates over a period of two years. For that, climate and land-use treatments were orthogonally crossed: (1) two climate scenarios: ambient vs. future; and (2) five land-use regimes: conventional fanning, organic farming, intensively used meadow, extensively used meadow, and extensively used pasture. Litterbags with two mesh sizes (5 mm and 0.02 mm) were used to differentiate contributions of microbes and fauna to the mass loss of standardized crop residues. Soil fauna accounted for more than 68% of surface litter mass loss. Future climate treatment decreased decomposition rates as a result of reduced precipitation and elevated temperature during summer months. Litter decomposition and the contribution of soil fauna to it were significantly higher in croplands than in grasslands, but did not differ due to management intensity within these land-use types. In grasslands, faunal contribution to decomposition decreased under future climate. There were no interacting effects between climate change and land use on decomposition rates. These findings indicate that predicted changes in precipitation patterns and temperature will consistently decelerate litter decomposition across land-used types via both microbial and faunal effects.
机译:垃圾分解是确定生态系统中营养循环的关键过程。土壤动物区系在该过程中起重要作用,例如,通过碎片和挖洞表面垫料材料,从而提高微生物分解。然而,土壤动物介导的分解可能受到环境变化的相互作用因素的影响。在这里,我们使用了一个大规模的全球变化现场实验,以测试土地使用类型(裁剪和管理强度不同的草原)之间的潜在相互作用效果,并在两年内对凋落物分解率的预计气候变化进行了预测的气候变化。为此,气候和土地利用治疗正交交叉:(1)两个气候情景:环境与未来; (2)五个土地使用制度:传统的扇形,有机农业,密集使用的草地,广泛使用的草地,广泛使用的牧场。使用两个网格尺寸(5 mm和0.02 mm)的地毯袋用于区分微生物和动物的贡献,以使标准作物残留物的质量损失。土壤动物占地表凋落物质量损失的68%以上。未来的气候治疗因减少沉淀和夏季的温度而降低分解率。垃圾分解和土壤动物的贡献在农田上的贡献比在草原上显着高,但由于这些土地使用类型内的管理强度没有不同。在草原,在未来的气候下,群体对分解的贡献减少。气候变化与分解率的土地使用之间没有相互作用的影响。这些发现表明,通过微生物和群效应,降水模式和温度的预测变化将一致地减速覆盖土地使用的垃圾分解。

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