Abstract

A primary aim of historical biogeography is to identify the causal factors or processes that have shaped the composition and distribution of biotas over time. Another is to infer the evolution of geographic ranges of species and clades in a phylogenetic context. To this end, historical biogeography addresses important questions such as: Where were ancestors distributed? Where did lineages originate? Which processes cause geographic ranges to evolve through time? Allium subgenus Anguinum comprises approximately twelve taxa with a disjunct distribution in the high mountains from south-western Europe to eastern Asia and in northeastern North America. Although both the systematic position and the geographical limits of Anguinum have been identified, to date no molecular systematic study has been performed utilizing a comprehensive sampling of these species. With an emphasis on the Anguinum eastern Asian geographical group, the goals of the present study were: (i) to infer species-level phylogenetic relationships within Anguinum, (ii) to assess molecular divergence and estimated the times of the major splits in Anguinum and (iii) to trace the biogeographic history of the subgenus. Four DNA sequences (ITS, matK, trnH-psbA, rps16) were used to reconstruct the phylogeny of Allium subgen. Anguinum RbcL sequences were used to estimate divergences time for Allium, and sequences of ITS were used to estimate the divergence times for Anguinum and its main lineages and to provide implications for the evolutionary history of the subgenus. Phylogenetic analyses for all Allium corroborate that Anguinum is monophyletic and indicate that Anguinum is composed of two sister groups: one with a Eurasian-American distribution, and the other restricted to eastern Asia. In the eastern Asian geographical group, incongruence between gene trees and morphology-based taxonomies was recovered as was incongruence between data from plastid and nuclear sequences. This incongruence is likely due to the combined effects of a recent radiation, incomplete lineage sorting, and hybridization/introgression. Divergence time estimates suggest that the crown group of Anguinum originated during the late Miocene (ca. 7.16 Mya) and then diverged and dispersed. Biogeographic analyses using statistical dispersal-vicariance analysis (S-DIVA) and a likelihood method support an eastern Asia origin of Anguinum It is inferred that in the late Pliocene/Early Pleistocene, with cooling climates and the uplift of the Himalayas and Hengduan Mountains, the ancestor of the eastern Asian alliance clade underwent a very recent radiation.

Highlights

  • A primary aim of historical biogeography is to identify the causal factors or processes that have shaped the composition and distribution of biotas over time (Sanmartın 2007)

  • To infer divergence times within Anguinum, 144 ITS sequences (34 sequences were generated in this study) that represented Anguinum and other subgenera and sections in Allium, plus two sequences of Nothoscordum gracile and Tulbaghia violacea were used, and the selection of Anguinum taxa is based on haplotype analysis, and sequences belong to the same haplotype form the same taxa are removed [see Supporting Information, Appendix S3]

  • ITS data show remarkably low levels of variability within Anguinum, and the variation is low in comparison to subgenus Melanocrommyum in the same evolutionary line (Gurushidze et al 2008)

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Summary

Introduction

A primary aim of historical biogeography is to identify the causal factors or processes that have shaped the composition and distribution of biotas over time (Sanmartın 2007) Another major focus is to infer the evolution of geographic ranges of species and clades in a phylogenetic context (Ree and Smith 2008). The Earth’s climate became cooler through the Tertiary (Zachos et al 2001), and the climate cooled gently from 50 to 35 million years (Myr) ago, fluctuated until 15 Myr ago, after which the climate cooled progressively, culminating in the Quaternary (2–0 Myr ago) glaciations (Milne and Abbott 2002) Cooling climates in the latter part of the Tertiary forced the boreotropical flora retreat southwards to large refugial regions that preserved the warm wet climate that they needed. At the same time western North America was connected to East Asia across the Bering land bridge (BLB), while eastern North

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