4.3 Article

Plastid phylogenomics shed light on intergeneric relationships and spatiotemporal evolutionary history of Melocanninae (Poaceae: Bambusoideae)

期刊

JOURNAL OF SYSTEMATICS AND EVOLUTION
卷 60, 期 3, 页码 640-652

出版社

WILEY
DOI: 10.1111/jse.12843

关键词

biogeography; diversification rate shift; Melocanninae; Paleotropical woody bamboo; phylogenomics; plastome; species radiation

资金

  1. National Natural Science Foundation of China [31670396, 31800181]
  2. Large-scale Scientific Facilities of CAS [2017-LSFGBOWS-02]
  3. West Light Foundation of CAS [Y8249411W1]
  4. Applied and Fundamental Research Project of Yunnan Province [202101AU070082]

向作者/读者索取更多资源

Melocanninae is a subtribe of Paleotropical woody bamboos with over 90 species mainly found in Asia. This study filled the gaps in plastome data of Melocanninae, reconstructed its phylogeny, estimated divergence time and ancestral distribution range. The results showed that the two major genera, Cephalostachyum and Schizostachyum, were paraphyletic. Different plastid regions provided inconsistent signals for the relationship between Melocanna and Pseudostachyum. It was inferred that Melocanninae originated in the East Himalaya to northern Myanmar in the early Miocene and dispersed to different regions through multiple routes.
Melocanninae is sister to other subtribes of Paleotropical woody bamboos with some 90 species mainly concentrated in Asia. However, phylogenetic relationships within the subtribe are poorly known. Here, we filled the gaps in complete plastome data of Melocanninae, reconstructed the phylogeny of Melocanninae, and further estimated divergence time and ancestral distribution range. Our results showed that the two major genera, Cephalostachyum Munro and Schizostachyum Nees, were paraphyletic. Species of Cephalostachyum were resolved in two successive basal clades, whereas Annamocalamus H. N. Nguyen, N. H. Xia, & V. T. Tran was embedded in the Schizostachyum clade. Different plastid regions provided inconsistent signals for the relationship of Melocanna and Pseudostachyum. Conservative loci supported a successive divergence rather than sister relationship between them and the difference may be caused by long-branch attraction. We infer that Melocanninae originated in the East Himalaya to northern Myanmar in the early Miocene. Three routes were revealed in forming its present biogeographic pattern: in situ diversification on the Asian mainland, dispersing southwest to Sri Lanka and to the Western Ghats in South India, and spreading southeast to Malesia and Oceania by way of the Indo-China Peninsula. The rapid uplift of the Tibetan Plateau and the intensification of Asian monsoons since the Miocene and the sea level fall events since the Late Miocene might be potential driving forces for diversification of Melocanninae and, particularly the latter event, for the species radiation of Schizostachyum.

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