SEARCH

SEARCH BY CITATION

Keywords:

  • Ancestral area;
  • Bayes-DIVA;
  • Bering Land Bridge;
  • boreotropic hypothesis;
  • historical biogeography;
  • North Atlantic Land Bridge;
  • plant immigrants;
  • Tertiary

Abstract

Aim  Several recent studies have suggested that a substantial portion of today’s plant diversity in the Neotropics has resulted from the dispersal of taxa into that region rather than by vicariance. In general, three routes have been documented for the dispersal of taxa onto the South American continent: (1) via the North Atlantic Land Bridge, (2) via the Bering Land Bridge, or (3) from Africa directly onto the continent. Here a species-rich genus of Neotropical lowland rain forest trees (Guatteria, Annonaceae) is used as a model to investigate these three hypotheses.

Location  The Neotropics.

Methods  The phylogenetic relationships within the long-branch clade of Annonaceae were reconstructed (using maximum parsimony, maximum likelihood and Bayesian inference) in order to gain insight in the phylogenetic position of Guatteria. Furthermore, Bayesian molecular dating and Bayesian dispersal–vicariance (Bayes-DIVA) analyses were undertaken.

Results  Most of the relationships within the long-branch clade of Annonaceae were reconstructed and had high support. However, the relationship between the Duguetia clade, the XylopiaArtabotrys clade and Guatteria remained unclear. The stem node age estimate of Guatteria ranged between 49.2 and 51.3 Ma, whereas the crown node age estimate ranged between 11.4 and 17.8 Ma. For the ancestral area of Guatteria and its sister group, the area North America–Africa was reconstructed in 99% of 10,000 DIVA analyses, while South America–North America was found just 1% of the time.

Main conclusions  The estimated stem to crown node ages of Guatteria in combination with the Bayes-DIVA analyses imply a scenario congruent with an African origin followed by dispersal across the North Atlantic Land Bridge in the early to middle Eocene and further dispersal into North and Central America (and ultimately South America) in the Miocene. The phylogenetically and morphologically isolated position of the genus is probably due to extinction of the North American and European stem lineages in the Tertiary.