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Variation in leaf xeromorphism in the desert palm genus Washingtonia (Arecaceae)

机译:沙漠棕榈属华盛顿菊属植物(槟榔树)叶Xeromorphism的变异

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Washingtonia palms occur scattered in oases and canyons of the larger Sonoran Desert from lat. 24 degrees to lat. 34 degrees N. Northern oases have an arid temperate climate while those in the south experience seasonally dry, tropical conditions. A marked latitudinal cline in morphological characters has been described within the genus. We hypothesized that aridity-adapted leaf traits in Washingtonia palms, such as amphistomaty and isolaterality, could exhibit a predictable trend along the 1300-km-long gradient, allowing us to test whether the evolution of leaf xeromorphism is correlated with environmental aridity.We took measurements of anatomical and functional traits of leaves in 16 oases spanning the whole distributional range of the genus in Mexico and the US. Using regression models, we examined the response of specific leaf area, leaf greenness, delta C-13, stomatal size, and stomatal density to latitude, site, and landform. We used Principal Components Analysis and correlation matrices to identify bioclimatic variables that might be playing a role in the observed latitudinal patterns.Palms at northern sites have waxy, glaucous, thick, leaves and exhibit xeromorphic traits such as amphistomaty and isolaterality. Palms at more tropical sites have glossy green, thin leaves that do not show xeromorphic traits.Leaf xeromorphism, a morphological and physiological syndrome in Washingtonia palms, increases with aridity.
机译:华盛顿州的棕榈树散落在来自拉特的较大索诺兰沙漠的绿洲和峡谷中。 24度到拉特。 34度N. Northern Oases具有干旱的温带气候,而南方体验经季节性干燥,热带条件。在属中描述了一种标记的纬度曲线。我们假设华盛顿菊属植物(例如Amphistomaty和Issolatality)的干旱适应的叶状性状可能表现出沿1300公里长的梯度的可预测趋势,使我们能够测试叶Xeromorphism的演变是否与环境干燥相关。我们采取了在墨西哥和美国的全部分布范围内叶片中叶片叶片解剖学和功能性的测量。使用回归模型,我们检查了特定叶面积,叶片绿色,ΔC-13,气孔大小和气孔密度对纬度,场地和地形的响应。我们使用了主成分分析和相关矩阵来识别可能在观察到的纬度模式中发挥作用的生物媒体变量。北部地点的帕尔姆斯有蜡质,葡萄糖,厚,叶子,表现出Xeromorphic特征,如术式阳性和孤片性的Xeromorphic特征。棕榈树在更热带场所有光泽的绿色,薄叶不显示Xeromorphic traits.leaf Xeromorphism,华盛顿菊属植物的形态和生理综合征,含砷增加。

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