Plastid phylogenomics clarifies broad-level relationships in Bulbophyllum (Orchidaceae) and provides insights into range evolution of Australasian section Adelopetalum

Lalita Simpson, M. Clements, Harvey K. Orel, D. Crayn, Katharina Nargar
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Abstract

The hyperdiverse orchid genus Bulbophyllum is the second largest genus of flowering plants and exhibits a pantropical distribution with a center of diversity in tropical Asia. The only Bulbophyllum section with a center of diversity in Australasia is sect. Adelopetalum. However, the phylogenetic placement, interspecific relationships, and spatio-temporal evolution of this section remain largely unclear. To infer broad-level relationships within Bulbophyllum, and interspecific relationships within sect. Adelopetalum, a genome skimming dataset was generated for 89 samples, which yielded 70 plastid coding regions and a nuclear ribosomal DNA cistron. For 18 additional samples, Sanger data from two plastid loci (matK and ycf1) and nuclear ITS were added using a supermatrix approach. The study provided new insights into broad-level relationships in Bulbophyllum, including phylogenetic evidence for the non-monophyly of sections Beccariana, Brachyantha, Brachypus, Cirrhopetaloides, Cirrhopetalum, Desmosanthes, Minutissima, Oxysepala, Polymeres, and Sestochilos. Section Adelopetalum and sect. Minutissima s.s. formed a highly supported clade that was resolved as a sister group to the remainder of the genus. Divergence time estimations based on a relaxed molecular clock model placed the origin of Bulbophyllum in the Early Oligocene (ca. 33.2 Ma) and sect. Adelopetalum in the Late Oligocene (ca. 23.6 Ma). Ancestral range estimations based on a BAYAREALIKE model identified the Australian continent as the ancestral area of the sect. Adelopetalum. The section underwent crown diversification from the mid-Miocene to the late Pleistocene, predominantly in continental Australia. At least two independent long-distance dispersal events were inferred eastward from the Australian continent to New Zealand and to New Caledonia from the early Pliocene onwards, likely mediated by predominantly westerly winds of the Southern hemisphere. Retraction and fragmentation of the eastern Australian rainforests from the early Miocene onwards are likely drivers of lineage divergence within sect. Adelopetalum facilitating allopatric speciation.
质体系统发生组学阐明了兰科植物球茎兰(Bulbophyllum)的广义关系,并提供了澳大拉西亚科球茎兰(Adelopetalum)分布区演化的见解
兰花属(Bulbophyllum)是第二大开花植物属,分布于泛热带地区,多样性中心位于亚洲热带地区。唯一在澳大拉西亚有多样性中心的球兰科是Adelopetalum。Adelopetalum。然而,该部分的系统发育位置、种间关系和时空演化在很大程度上仍不清楚。为了推断Bulbophyllum内的广义关系以及Adelopetalum科内的种间关系,研究人员利用基因组学方法进行了研究。Adelopetalum 的种间关系,对 89 个样本进行了基因组扦样,获得了 70 个质体编码区和一个核核糖体 DNA 组元。对于另外 18 个样本,利用超级矩阵方法添加了来自两个质体位点(matK 和 ycf1)和核 ITS 的 Sanger 数据。该研究为了解球叶植物的广泛关系提供了新的视角,包括Beccariana、Brachyantha、Brachypus、Cirrhopetaloides、Cirrhopetalum、Desmosanthes、Minutissima、Oxysepala、Polymeres和Sestochilos等科非单系的系统发生学证据。科 Adelopetalum 和 sect.Minutissima s.s.形成了一个支持率很高的支系,被认为是该属其余部分的姊妹群。根据一个宽松的分子钟模型进行的分化时间估计,Bulbophyllum 的起源时间为早渐新世(约 33.2 Ma),而 Adelopetalum 的起源时间则为早渐新世(约 33.2 Ma)。Adelopetalum起源于晚渐新世(约 23.6 Ma)。根据 BAYAREALIKE 模型进行的祖先分布区估算确定,澳大利亚大陆为 Adelopetalum 的祖先分布区。Adelopetalum。从中新世中期到更新世晚期,该门类主要在澳大利亚大陆经历了树冠分化。据推断,从上新世早期开始,至少有两次独立的长距离扩散活动,分别从澳大利亚大陆向东扩散到新西兰和新喀里多尼亚,可能主要是受南半球西风的影响。从中新世早期开始,澳大利亚东部雨林的退缩和破碎可能是导致Adelopetalum科内世系分化的原因。Adelopetalum 促进了同域物种的分化。
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