Volume 52, Issue 4 pp. 988-997
Article
Free Access

ORIGIN AND BIOGEOGRAPHY OF AESCULUS L. (HIPPOCASTANACEAE): A MOLECULAR PHYLOGENETIC PERSPECTIVE

Qiu-Yun Xiang

Qiu-Yun Xiang

Department of Biological Sciences, Idaho State University, Pocatello, Idaho, 83209-8007

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Daniel J. Crawford

Daniel J. Crawford

Department of Plant Biology, The Ohio State University, 1735 Neil Avenue, Columbus, Ohio, 43210-1293

Corresponding author. E-mail: [email protected].Search for more papers by this author
Andrea D. Wolfe

Andrea D. Wolfe

Department of Plant Biology, The Ohio State University, 1735 Neil Avenue, Columbus, Ohio, 43210-1293

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Yan-Cheng Tang

Yan-Cheng Tang

Laboratory of Systematic and Evolutionary Botany, Chinese Academy of Sciences, Xiangshan, Beijing, 100093 China

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Claude W. DePamphilis

Claude W. DePamphilis

Department of Biology, Pennsylvania State University, University Park, Pennsylvania, 16802

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First published: 31 May 2017
Citations: 57

Abstract

Sequences of chloroplast gene matK and internal transcribed spacers of nuclear ribosomal RNA genes were used for phylogenetic analyses of Aesculus, a genus currently distributed in eastern Asia, eastern and western North America, and southeastern Europe. Phylogenetic relationships inferred from these molecular data are highly correlated with the geographic distributions of species. The identified lineages closely correspond to the five sections previously recognized on the basis of morphology. Ancestral character-state reconstruction, a molecular clock, and fossil evidence were used to infer the origin and biogeographic history of the genus within a phylogenetic framework. Based on the molecular phylogenetic reconstruction of the genus, sequence divergence, and paleontological evidence, we infer that the genus originated during the transition from the Cretaceous to the Tertiary (~65 M.Y.B.P.) at a high latitude in eastern Asia and spread into North America and Europe as an element of the “boreotropical flora”; the current disjunct distribution of the genus resulted from geological and climatic changes during the Tertiary.

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