Cytogenetics meets phylogenetics: a review of karyotype evolution in diprotodontian marsupials.

We have used a combined approach of phylogenetics and cytogenetics to describe karyotype evolution in Diprotodontia. Molecular relationships of diprotodontian marsupials have been clarified using a concatenation of 5 nuclear gene sequences from multiple exemplars of all extant genera. Our well-resolved phylogenetic tree has been used as a basis for understanding chromosome evolution both within this Order, as well as in marsupials in general. It is clear that the ancestral marsupial karyotype comprised 14 relatively large chromosomes of the form retained relatively unchanged in caenolestids, microbiotherians, peramelemorphians, vombatids, and pygmy possums. Four pericentric inversions occurred in the ancestral dasyuromorphian (chromosomes 1, 2, 4, and 6) and a different 4 in the ancestral didelphimorphian (chromosomes 1, 3, 5 and 6). Within Diprotodontia, although the ancestral marsupial karyotype has been retained in some families such as the extant wombats and pygmy possums, there have been major karytoypic repatternings early in the evolution of others. Chromosome rearrangements in diprotodontia include centric fissions and fusions, translocations, and centromere shifts. Karyotypic changes are discussed in the context of current hypotheses concerning centromeres, chromosomal fragile sites, and mobile elements in marsupials and the probable repeated involvement of these elements in karyotypic restructuring.

Bandicoot fossils and DNA elucidate lineage antiquity amongst xeric-adapted Australasian marsupials.

Bandicoots (Peramelemorphia) are a unique order of Australasian marsupials whose sparse fossil record has been used as prima facie evidence for climate change coincident faunal turnover. In particular, the hypothesized replacement of ancient rainforest-dwelling extinct lineages by antecedents of xeric-tolerant extant taxa during the late Miocene (~10 Ma) has been advocated as a broader pattern evident amongst other marsupial clades. Problematically, however, this is in persistent conflict with DNA phylogenies. We therefore determine the pattern and timing of bandicoot evolution using the first combined morphological + DNA sequence dataset of Peramelemorphia. In addition, we document a remarkably archaic new fossil peramelemorphian taxon that inhabited a latest Quaternary mosaic savannah-riparian forest ecosystem on the Aru Islands of Eastern Indonesia. Our phylogenetic analyses reveal that unsuspected dental homoplasy and the detrimental effects of missing data collectively obscure stem bandicoot relationships. Nevertheless, recalibrated molecular clocks and multiple ancestral area optimizations unanimously infer an early diversification of modern xeric-adapted forms. These probably originated during the late Palaeogene (30-40 Ma) alongside progenitors of other desert marsupials, and thus occupied seasonally dry heterogenous habitats long before the onset of late Neogene aridity.