Centre for Mined Land Rehabilitation, Sustainable Minerals Institute, The University of Queensland, Australia.
Université de Lorraine, INRA, Laboratoire Sols et Environnement, Nancy, France.
Ann Bot. 2020 Oct 30;126(6):1017-1027. doi: 10.1093/aob/mcaa119.
The aim of this study was to test the frequency distributions of foliar elements from a large dataset from Kinabalu Park (Sabah, Malaysia) for departure from unimodality, indicative of a distinct ecophysiological response associated with hyperaccumulation.
We collected foliar samples (n = 1533) comprising 90 families, 198 genera and 495 plant species from ultramafic soils, further foliar samples (n = 177) comprising 45 families, 80 genera and 120 species from non-ultramafic soils and corresponding soil samples (n = 393 from ultramafic soils and n = 66 from non-ultramafic soils) from Kinabalu Park (Sabah, Malaysia). The data were geographically (Kinabalu Park) and edaphically (ultramafic soils) constrained. The inclusion of a relatively high proportion (approx. 14 %) of samples from hyperaccumulator species [with foliar concentrations of aluminium and nickel (Ni) >1000 μg g-1, cobalt, copper, chromium and zinc >300 μg g-1 or manganese (Mn) >10 mg g-1] allowed for hypothesis testing.
Frequency distribution graphs for most elements [calcium (Ca), magnesium (Mg) and phosphorus (P)] were unimodal, although some were skewed left (Mg and Mn). The Ni frequency distribution was bimodal and the separation point for the two modes was between 250 and 850 μg g-1.
Accounting for statistical probability, the established empirical threshold value (>1000 μg g-1) remains appropriate. The two discrete modes for Ni indicate ecophysiologically distinct behaviour in plants growing in similar soils. This response is in contrast to Mn, which forms the tail of a continuous (approximately log-normal) distribution, suggestive of an extension of normal physiological processes.
本研究的目的是检验来自基纳巴卢公园(马来西亚沙巴)的大量数据集的叶片元素频率分布,以检验其是否偏离单峰分布,这表明与超积累相关的独特生理响应。
我们收集了来自超镁铁质土壤的叶片样本(n = 1533),包括 90 个科、198 个属和 495 个植物种;来自非超镁铁质土壤的叶片样本(n = 177),包括 45 个科、80 个属和 120 个种;以及来自基纳巴卢公园(马来西亚沙巴)的相应土壤样本(超镁铁质土壤 n = 393,非超镁铁质土壤 n = 66)。数据在地理上(基纳巴卢公园)和土壤上(超镁铁质土壤)受到限制。包括相对较高比例(约 14%)的超积累物种样本[叶片中铝和镍(Ni)浓度>1000μg g-1、钴、铜、铬和锌浓度>300μg g-1或锰(Mn)浓度>10mg g-1],以便进行假设检验。
大多数元素[钙(Ca)、镁(Mg)和磷(P)]的频率分布图呈单峰分布,尽管有些呈左偏分布(Mg 和 Mn)。Ni 的频率分布呈双峰分布,两个模态的分离点在 250 和 850μg g-1 之间。
考虑到统计概率,已建立的经验阈值(>1000μg g-1)仍然适用。Ni 的两个离散模态表明,在生长在相似土壤中的植物中存在不同的生理行为。这与 Mn 形成对比,Mn 形成连续(近似对数正态)分布的尾部,表明正常生理过程的延伸。