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Leaf litter carbon, nitrogen, and phosphorus stoichiometric patterns as related to climatic factors and leaf habits across Chinese broad-leaved tree species

机译:叶凋落物碳,氮和磷化学计量模式与中国阔叶树种的气候因子和叶习惯有关

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Our understanding of how climate and leaf habit (evergreen vs. deciduous) drive leaf litter carbon (C), nitrogen (N), and phosphorus (P) stoichiometric patterns is largely limited but is particularly important for broad-leaved forests, since the forest is sensitive to climate change. Here, we investigated leaf litter C, N, and P stoichiometric ratios of broad-leaved tree species in relation to climate and leaf habit using previous publications and our additional samplings across China. We found that mean leaf litter C:N across Chinese broad-leaved tree species was within the range of the global flora, whereas C:P was lower and N:P higher. Evergreen species displayed higher leaf litter C:N, C:P, and N:P than their deciduous counterparts. Both leaf litter C:P and N:P for all species pooled were negatively correlated with latitude, driven by mean annual precipitation (MAP) and mean annual temperature, respectively, while leaf litter C:N displayed no clear latitudinal trend. The direction and magnitude of leaf litter C, N, and P stoichiometric ratios in response to climate diverged between leaf habits. For example, evergreen leaf litter C:N was negatively correlated with MAP, while deciduous counterparts did not respond significantly to MAP. We conclude that leaf litter C, N, and P stoichiometric ratios shifted along the climatic gradient, and the strength of such shifts differed between leaf habits. Therefore, leaf litter stoichiometric patterns across leaf habits suggest that any climate change-driven shift in species distribution may potentially alter the ecosystem's nutrient cycling processes of evergreen- and deciduous-dominated broad-leaved forests differentially.
机译:我们对气候和叶习合(常绿与落叶)驱动叶垃圾碳(C),氮(N)和磷(P)化学计量模式的理解在很大程度上是有限的,但对于自森林以来,对阔叶森林尤为重要对气候变化很敏感。在此,我们研究了与中国跨国公司的气候和叶习合相关的叶子凋落物C,N和P组化学计量比,以及我们在中国的其他采样。我们发现,中国阔叶树种类的平均叶垃圾c:n在全球植物区的范围内,而C:P较低,N:P高。常绿物种显示出更高的叶子垃圾c:n,c:p,n:p比其落叶同行。叶子垃圾c:p和n:p:汇集的所有物种的p与纬度都与平均年降水量(地图)和平均年度温度分别导致的纬度呈负相关,而叶子垃圾c:n显示无明显的纬度趋势。叶凋落物C,N和P化学计量比的方向和幅度响应于叶习合之间的气候分歧。例如,常绿叶垃圾c:n与地图呈负相关,而落叶同行对地图没有显着响应。我们得出结论,叶子凋落物C,N和P化学计量比沿着气候梯度移动,并且这种偏移的强度在叶习合之间不同。因此,叶片衬叶习惯的叶子垃圾化学计量模式表明,物种分布的任何气候变化驱动的转变可能会差异地改变常绿和落叶主导的阔叶林的生态系统的营养循环过程。

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