Dibán María José, Hinojosa Luis Felipe
Laboratory of Paleoecology, Department of Ecological Science, Faculty of Science, University of Chile, Santiago 7800003, Chile.
Plants (Basel). 2024 Jan 3;13(1):133. doi: 10.3390/plants13010133.
We assess the Tropical Niche Conservatism Hypothesis in the genus in South America using phylogeny, paleoclimate estimation and current niche modelling. We tested four predictions: (1) the climatic condition where the ancestor of grew is megathermal; (2) the temperate niche is a derived condition from tropical clades; (3) the most closely related species have a similar current climate niche (conservation of the phylogenetic niche); and (4) there is a range expansion from the northern Andes to high latitudes during warm times. Our phylogenetic hypothesis shows that originated 52.17 ± 0.85 My, in the early Eocene, with an annual mean temperature of 13.8 °C and annual precipitation of 1081 mm, corresponding to a microthermal to mesothermal climate; the species of the northern and central tropical Andes would be the ancestral ones, and the temperate species evolved between 32 and 20 My in a microthermal climate. The predominant evolutionary models were Brownian and Ornstein-Uhlenbeck. There was phylogenetic signal in 7 of the 9 variables, indicating conservation of the climatic niche. would have originated in the central and southern Andes and reached the other environments by dispersion.
我们利用系统发育、古气候估计和当前生态位建模,在南美洲对该属的热带生态位保守性假说进行了评估。我们检验了四个预测:(1)该属祖先生长的气候条件为高温多雨型;(2)温带生态位是从热带分支衍生而来的条件;(3)亲缘关系最密切的物种具有相似的当前气候生态位(系统发育生态位的保守性);(4)在温暖时期存在从安第斯山脉北部向高纬度地区的范围扩张。我们的系统发育假说表明,该属起源于始新世早期,距今5217±85万年,年平均温度为13.8℃,年降水量为1081毫米,对应微热到中热气候;安第斯山脉北部和中部热带地区的物种可能是祖先物种,温带物种在3200万至2000万年前的微热气候中进化而来。主要的进化模型是布朗运动模型和奥恩斯坦-乌伦贝克模型。9个变量中有7个存在系统发育信号,表明气候生态位具有保守性。该属可能起源于安第斯山脉中部和南部,并通过扩散到达其他环境。