Divergence time analyses suggest a Miocene origin of the narrow Amazonian endemic rheophytic Ceratolejeunea temnantha (Spruce) Reiner-Drehwald (Porellales, Lejeuneaceae)
A. Sierra, J. Bechteler, D. Cardoso, C. Zartman, J. C. Villarreal
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引用次数: 1
Abstract
The recent rediscovery of the rheophytic endemic Ceratolejeunea temnantha ~130 years after its original description, on the upper Rio Negro in the Brazilian Amazon, has enabled the assessment of its enigmatic phylogenetic position, estimates of its divergence time, and updates on its distribution and potential habitat threats. Phylogenetic analyses strongly supported its placement in the genus Ceratolejeunea in a geographically disparate clade including a Madagascar endemic C. saroltae and two Neotropical taxa, C. confusa and C. caducifolia. Divergence time estimates date the clade’s stem age to the late Miocene (8.92 [HPD: 12.39–6.04] Ma) offering further evidence that the evolution of rheophytes in northern South America is correlated with the expansion of cryptogams into novel ecological niches promoted by dramatic landscape changes during the Miocene. Major geomorphological and hydrological transformations contributing to such diversification are most likely the changing dynamics of the inundated mega lake system to the establishment of the Amazon River due to the Andean orogeny and the subsequent cessation of marine influences in the north-western portion of the Basin. Until recently, this rheophyte of seasonally inundated black-water forests was only known from its type collection from the Rio Negro near São Gabriel da Cachoeira (Brazil) as described by Richard Spruce in 1884. These new collections extend the distribution of this rare narrow endemic to the middle Rio Uaupés, a tributary of the upper Rio Negro near the Columbian border.
最近,在巴西亚马逊河上游里约热内卢Negro地区重新发现了一种距今约130年的流变性特有Ceratolejeunea temnanea,从而能够评估其神秘的系统发育位置,估计其分化时间,并更新其分布和潜在的栖息地威胁。系统发育分析有力地支持了其在Ceratolejeunea属中的位置,该分支包括马达加斯加特有的C. saroltae和两个新热带分类群C. confusa和C. caducifolia。据估计,该支系的分化时间可追溯到中新世晚期(8.92 [HPD: 12.39-6.04] Ma),这进一步证明了南美北部流变植物的进化与中新世剧烈的景观变化所促进的隐生植物向新生态位的扩张有关。促成这种多样化的主要地貌和水文变化很可能是由于安第斯造山运动和随后盆地西北部海洋影响的停止而导致的淹没大湖系统的动态变化,以及亚马孙河的形成。直到最近,这种季节性淹没的黑水森林的流生植物仅从它的类型收集中被人们所知,这些类型收集来自 o Gabriel da Cachoeira(巴西)附近的里约热内卢Negro,如Richard Spruce在1884年所描述的那样。这些新收集的标本将这种罕见的狭窄地方性植物的分布范围扩展到了哥伦比亚边界附近的上里约热内卢Negro的一条支流——中部里约热内卢uaupsamas。