Watanabe Toshihiro, Broadley Martin R, Jansen Steven, White Philip J, Takada Jitsuya, Satake Kenichi, Takamatsu Takejiro, Tuah Sehat Jaya, Osaki Mitsuru
Research Faculty of Agriculture, Hokkaido University, N9W9, Kita-ku, Sapporo 060-8589, Japan.
Plant Sciences Division, School of Biosciences, University of Nottingham, Sutton Bonington, Loughborough LE12 5RD, UK.
New Phytol. 2007;174(3):516-523. doi: 10.1111/j.1469-8137.2007.02078.x.
Leaf nitrogen (N) and phosphorus (P) concentrations are correlated in plants. Higher-level phylogenetic effects can influence leaf N and P. By contrast, little is known about the phylogenetic variation in the leaf accumulation of most other elements in plant tissues, including elements with quantitatively lesser roles in metabolism than N, and elements that are nonessential for plant growth. Here the leaf composition of 42 elements is reported from a statistically unstructured data set comprising over 2000 leaf samples, representing 670 species and 138 families of terrestrial plants. Over 25% of the total variation in leaf element composition could be assigned to the family level and above for 21 of these elements. The remaining variation corresponded to differences between species within families, to differences between sites which were likely to be caused by soil and climatic factors, and to variation caused by sampling techniques. While the majority of variation in leaf mineral composition is undoubtedly associated with nonevolutionary factors, identifying higher-level phylogenetic variation in leaf elemental composition increases our understanding of terrestrial nutrient cycles and the transfer of toxic elements from soils to living organisms. Identifying mechanisms by which different plant families control their leaf elemental concentration remains a challenge.
植物叶片中的氮(N)和磷(P)浓度相互关联。较高层次的系统发育效应会影响叶片中的氮和磷。相比之下,对于植物组织中大多数其他元素的叶片积累的系统发育变异,我们了解甚少,这些元素包括在新陈代谢中作用比氮小的元素,以及对植物生长非必需的元素。本文报道了来自一个统计结构不严谨的数据集的42种元素的叶片组成,该数据集包含2000多个叶片样本,代表了670个物种和138个陆生植物科。其中21种元素的叶片元素组成总变异的25%以上可归因于科级及以上水平。其余变异对应于科内物种之间的差异、可能由土壤和气候因素引起的地点之间的差异,以及由采样技术引起的变异。虽然叶片矿物质组成的大部分变异无疑与非进化因素有关,但识别叶片元素组成中的较高层次系统发育变异有助于我们理解陆地养分循环以及有毒元素从土壤到生物体的转移。确定不同植物科控制其叶片元素浓度的机制仍然是一个挑战。