Plastome phylogenomic analysis reveals evolutionary divergences of Polypodiales suborder Dennstaedtiineae.

BACKGROUND: Polypodiales suborder Dennstaedtiineae contain a single family Dennstaedtiaceae, eleven genera, and about 270 species, and include some groups that were previously placed in Dennstaedtiaceae, Hypolepidaceae, Monachosoraceae, and Pteridaceae. The classification and phylogenetic relationships among these eleven genera have been poorly understood. To explore the deep relationships within suborder Dennstaedtiineae and estimate the early diversification of this morphologically heterogeneous group, we analyzed complete plastomes of 57 samples representing all eleven genera of suborder Dennstaedtiineae using maximum likelihood and Bayesian inference. RESULTS: The phylogenetic relationships of all the lineages in the bracken fern family Dennstaedtiaceae were well resolved with strong support values. All six genera of Hypolepidoideae were recovered as forming a monophyletic group with full support, and Pteridium was fully supported as sister to all the other genera in Hypolepidoideae. Dennstaedtioideae (Dennstaedtia s.l.) fell into four clades with full support: the Microlepia clade, the northern Dennstaedtia clade, the Dennstaedtia globulifera clade, and the Dennstaedtia s.s. clade. Monachosorum was strongly resolved as sister to all the remaining genera of suborder Dennstaedtiineae. Based on the well resolved relationships among genera, the divergence between Monachosorum and other groups of suborder Dennstaedtiineae was estimated to have occurred in the Early Cretaceous, and all extant genera (and clades) in Dennstaedtiineae, were inferred to have diversified since the Late Oligocene. CONCLUSION: This study supports reinstating a previously published family Monachosoraceae as a segregate from Dennstaedtiaceae, based on unique morphological evidence, the shady habitat, and the deep evolutionary divergence from its closest relatives.

New insights into the evolution of the fern family Dennstaedtiaceae from an expanded molecular phylogeny and morphological analysis.

Dennstaedtiaceae has 270 species, a worldwide distribution, and an edge-colonizing habit that is unusual among ferns. Aneuploidy, polyploidy, and hybrids are common in the family. Combining morphology, anatomy, chromosome number, and geographical distributions with our newly generated molecular phylogeny, we provide new insights into the evolution of the family. We paid special attention to Hypolepis. Our molecular dataset of five cpDNA markers is the most comprehensive to date, comprising 72 species (and a total of 98 taxa), of which 33 are Hypolepis (45 taxa). We also generated divergence-time estimates through BEAST with four fossil calibrations. We recovered three sub-families in Dennstaedtiaceae: Monachosoroideae (monogeneric), Dennstaedtioideae, and Hypolepidoideae. Monachosoroideae has a chromosome base number of x = 28; Hypolepidoideae of x = 26; while in Dennstaedtioideae this is still obscure, with different numbers ranging from 30 to 47. Dennstaedtioideae genera require re-circumscriptions because Dennstaedtia is polyphyletic. In Hypolepidoideae, the six genera are monophyletic. Within Hypolepis, seven geographically distinct clades were recovered; but we found no strong morphological characters to define them. Within the family, the long-creeping rhizome evolved with a change in habit: from shade-tolerant to edge-colonizers, to thicket-formers. Short or extremely large leaves are derived conditions. Sorus shape and position, glandular hairs, and prickles are homoplastic. Hybridization/allotetraploidy in Hypolepis can be suggested by the combined data. In our phylogenetic hypothesis, Dennstaedtiaceae originated around 135 Ma, with the split of Monachosoroideae around 94 Ma, and the split between Dennstaedtioideae/Hypolepidoideae around 78 Ma. All extant genera are inferred to be relatively young. Hypolepis started to diversify around 10 Ma, and it probably originated in east Asia and/or Oceania. Hypolepis reached the Neotropics twice: through elements of the Hypolepis rugosula clade (which originated at 7 Ma), and through the ancestor of the Neotropical clade, which originated at 3.1 Ma and was prickly.

Parallel polyploid speciation: distinct sympatric gene-pools of recurrently derived allo-octoploid Asplenium ferns.

Although polyploidy is widespread, its significance to the generation of biodiversity remains unclear. Many polyploids have been derived recurrently. For a particular polyploid, gene-flow between the products of independent origin is typical where they come into contact. Here, we use AFLP DNA-fingerprinting and chloroplast DNA sequences to demonstrate parallel polyploid speciation within both of the ferns Asplenium cimmeriorum and A. gracillimum. Both of these taxa comprise at least two allopolyploids, recurrently derived from the same progenitor pair. Each of these allopolyploids remain genetically distinguishable even with extensive sympatry, and could therefore be considered distinct species. To our knowledge, parallel speciation on this scale amongst recurrent polyploids has not been previously reported. With their parallel origins, these 'evolutionary replicates' provide an unrivalled opportunity to investigate how the reproductive barriers and ecological differentiation necessary for speciation arise following polyploidy.

Low-copy nuclear DNA sequences reveal a predominance of allopolyploids in a New Zealand Asplenium fern complex.

Recent generalisations about polyploidy in plants have been largely based on studies of angiosperms. A compelling group to compare with angiosperms is ferns, because of their high polyploidy. The bi-parental inheritance of nuclear DNA sequence markers makes them advantageous for investigating polyploid complexes, but few such markers have been available for ferns. We have used DNA sequences from the low-copy nuclear LFY locus to study an Asplenium polyploid complex. The New Zealand species of this Austral group comprise seven tetraploids and eight octoploids. LFY sequences indicate that allopolyploidy is much more predominant than previously thought, being implicated in the origins of seven of the octoploids. One of the tetraploids has had a central role, being a progenitor for five of the octoploids. All of the octoploids appear to have relatively recent origins, with the dynamic environmental conditions of the Pleistocene possibly playing a role in their formation and/or establishment.