Faculty of Natural Resources Management, Lakehead University, 955 Oliver Rd, Thunder Bay, Ontario, Canada P7B 5E1.
Nat Commun. 2011 Jun 14;2:344. doi: 10.1038/ncomms1346.
Most water and essential soil nutrient uptake is carried out by fine roots in plants. It is therefore important to understand the global geographic patterns of fine-root nitrogen and phosphorus cycling. Here, by compiling plant root data from 211 studies in 51 countries, we show that live fine roots have low nitrogen (N) and phosphorus (P), but similar N:P ratios when compared with green leaves. The fine-root N:P ratio differs between biomes and declines exponentially with latitude in roots of all diameter classes. This is in contrast to previous reports of a linear latitudinal decline in green leaf N:P, but consistent with nonlinear declines in leaf litter N:P. Whereas the latitudinal N:P decline in both roots and leaves reflects collective influences of climate, soil age and weathering, differences in the shape of the response function may be a result of their different N and P use strategies.
大多数植物的水分和基本土壤养分摄取是由细根完成的。因此,了解细根氮磷循环的全球地理格局非常重要。在这里,我们通过汇编来自 51 个国家的 211 项研究中的植物根系数据,表明活的细根氮(N)和磷(P)含量较低,但与绿叶相比,其 N:P 比值相似。细根 N:P 比值在生物群系之间存在差异,并随着所有直径类别的根系纬度呈指数下降。这与先前关于绿叶 N:P 线性纬度下降的报告形成对比,但与叶凋落物 N:P 的非线性下降一致。尽管根和叶中的 N:P 纬度下降反映了气候、土壤年龄和风化的综合影响,但响应函数形状的差异可能是其不同氮和磷利用策略的结果。