Dated molecular phylogenies are the basis for understanding species diversity and for linking changes in rates of diversification with historical events such as restructuring in developmental pathways, genome doubling, or dispersal onto a new continent. Valid fossil calibration points are essential to the accurate estimation of divergence dates, but for many groups of flowering plants fossil evidence is unavailable or limited. Arabidopsis thaliana, the primary genetic model in plant biology and the first plant to have its entire genome sequenced, belongs to one such group, the plant family Brassicaceae. Thus, the timing of A. thaliana evolution and the history of its genome have been controversial. We bring previously overlooked fossil evidence to bear on these questions and find the split between A. thaliana and Arabidopsis lyrata occurred about 13 Mya, and that the split between Arabidopsis and the Brassica complex (broccoli, cabbage, canola) occurred about 43 Mya. These estimates, which are two-to threefold older than previous estimates, indicate that gene, genomic, and developmental evolution occurred much more slowly than previously hypothesized and that Arabidopsis evolved during a period of warming rather than of cooling. We detected a 2-to 10-fold shift in species diversification rates on the branch uniting Brassicaceae with its sister families. The timing of this shift suggests a possible impact of the Cretaceous-Paleogene mass extinction on their radiation and that Brassicales codiversified with pierid butterflies that specialize on mustard-oil-producing plants.he most important genetic model in plant biology is Arabidopsis thaliana. It is the first plant to have its entire genome sequenced, and it serves as a key comparison point with other eukaryotic genomes. A. thaliana is diploid and has a small genome distributed on just five chromosomes, considerations in its choice as a model (1). The age of the Arabidopsis crown group (CG), previously estimated at 5.8-3 Mya (2, 3), and of splits within Brassicaceae have been used to understand the pace of evolution in genes affecting self-incompatibility (4, 5), the rate of change in signal transduction and gene expression (6, 7), the persistence of shared chromosomal rearrangements in A. thaliana and Brassica oleracea (8), the tempo of evolution of miRNA sequences (9), the evolution of pierid butterflies specializing in plants that produce mustard oils (10), and the ages of wholegenome duplication (WGD) events giving rise to gene pairs in Arabidopsis (11). As genomes of additional Brassicaceae (e.g., Capsella rubella) and other Brassicales (e.g., Carica papaya) (12) are sequenced, the importance of robust estimates of divergence dates relating these genomes to one another and to the geological record increases substantially.The accuracy of divergence times inferred from sequence data depends on valid, verifiable fossils to calibrate phylogenetic trees. Previous dates for the origin of Arabidopsis relied on the report of fossil pollen assigned to the genus Rori...

Modern survivors of previously more diverse lineages are regarded as living fossils, particularly when characterized by morphological stasis. Cycads are often cited as a classic example, reaching their greatest diversity during the Jurassic-Cretaceous (199.6 to 65.5 million years ago) then dwindling to their present diversity of ~300 species as flowering plants rose to dominance. Using fossil-calibrated molecular phylogenies, we show that cycads underwent a near synchronous global rediversification beginning in the late Miocene, followed by a slowdown toward the Recent. Although the cycad lineage is ancient, our timetrees indicate that living cycad species are not much older than ~12 million years. These data reject the hypothesized role of dinosaurs in generating extant diversity and the designation of today's cycad species as living fossils.