The first known rodent
fossils in
South America are represented by the three taxa
Cachiyacuy contamanensis,
C. kummeli, and
Canaanimys maquiensis, as well as teeth from
Eobranisamys sp. (Dasyproctidae) and
Eospina sp., the latter two found also in the
Santa Rosa fauna from the late
Eocene or early
Oligocene. By the late
Oligocene, all superfamilies and most families of caviomorphs are present in the fossil record. During this time, South America was isolated from all other
continents. Several hypotheses have been proposed as to how hystricognath rodents colonized this island continent. Most require that a small group of these rodents traveled across ocean bodies atop a
raft of
mangroves or
driftwood. The most common hypothesis suggests that the ancestor to all modern caviomorphs
rafted across the
Atlantic Ocean (then narrower) from
Africa (Lavocat, 1969; Huchon and Douzery, 2000). This is supported by molecular results, which suggest that the
Phiomorpha (as restricted to
Bathyergidae,
Petromuridae, and
Thryonomyidae) are sister taxa to the Caviomorpha. All modern hystricognath families are restricted to South America, Africa, or had a range that included Africa (
Hystricidae).
New World monkeys appear to have colonized South America from Africa at a similar time. Caviomorphs went on to colonize the
West Indies as far as the
Bahamas, reaching the
Greater Antilles by the early Oligocene. This is commonly viewed as another example of oceanic dispersal, although a role for a possible
land bridge has also been considered. ==Diversity==