During the
Oligocene, Africa was not connected to any of the other continents. The predominant theory suggests that rodents first evolved in
Laurasia, and expanded outward from there. Although
Europe,
Asia, and
North America were distinct landmasses during much of the
Eocene and Oligocene, they experienced intermittent migration events across the shallow sea separating Europe and Asia, via an ice-free
Greenland (Europe and North America), or across
Beringia (North America and Asia). The
southern continents were much more isolated, leading to the unique faunas of
Australia,
South America, and to a lesser degree Africa. Although the
hystricognath rodents may have evolved from an early
entodacryan ancestor in Asia, they migrated to Africa soon after. Phiomorpha represents the
clade that evolved as a result. Their success and diversification during the Oligocene is partially attributed to an early shift towards
herbivory, allowing them to survive off lower-quality foods and increasing their resilience to resource instability. Therefore, despite a decline in global temperatures and transition of African forests into savannahs and grasslands, Phiomorpha withstood this change and diversified within the new environments. Although once more diverse and widespread, this infraorder is now restricted to the
Old World porcupines, the
cane rats, the
dassie rat, the
naked mole-rat, and the
blesmols. == Families ==