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Species relationships and divergence times in beeches: new insights from the inclusion of 53 young and old fossils in a birth–death clock model
Author(s) -
Susanne S. Renner,
Guido W. Grimm,
Paschalia Kapli,
Thomas Denk
Publication year - 2016
Publication title -
philosophical transactions of the royal society b biological sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.753
H-Index - 272
eISSN - 1471-2970
pISSN - 0962-8436
DOI - 10.1098/rstb.2015.0135
Subject(s) - biology , genus , clade , divergence (linguistics) , extinction (optical mineralogy) , paleontology , molecular clock , ecology , evolutionary biology , phylogenetics , biochemistry , linguistics , philosophy , gene
The fossilized birth-death (FBD) model can make use of information contained in multiple fossils representing the same clade, and we here apply this model to infer divergence times in beeches (genus Fagus), using 53 fossils and nuclear sequences for all nine species. We also apply FBD dating to the fern clade Osmundaceae, with about 12 living species and 36 fossils. Fagus nuclear sequences cannot be aligned with those of other Fagaceae, and we therefore use Bayes factors to choose among alternative root positions. The crown group of Fagus is dated to 53 (62-43) Ma; divergence of the sole American species to 44 (51-39) Ma and divergence between Central European F. sylvatica and Eastern Mediterranean F. orientalis to 8.7 (20-1.8) Ma, unexpectedly old. The FBD model can accommodate fossils as sampled ancestors or as extinct or unobserved lineages; however, this makes its raw output, which shows all fossils on short or long branches, problematic to interpret. We use hand-drawn depictions and a bipartition network to illustrate the uncertain placements of fossils. Inferred speciation and extinction rates imply approximately 5× higher evolutionary turnover in Fagus than in Osmundaceae, fitting a hypothesized low turnover in plants adapted to low-nutrient conditions.This article is part of the themed issue 'Dating species divergences using rocks and clocks'.

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