The evolutionary history of the passerine families and the relationships among them remained rather mysterious until the late 20th century. In many cases, passerine families were grouped together on the basis of morphological similarities that, it is now believed, are the result of
convergent evolution, not a close genetic relationship. For example, the
wrens of the Americas and Eurasia,
those of Australia, and
those of New Zealand look superficially similar and behave in similar ways, yet belong to three far-flung branches of the passerine family tree; they are as unrelated as it is possible to be while remaining Passeriformes. Advances in
molecular biology and improved
paleobiogeographical data gradually are revealing a clearer picture of passerine origins and evolution that reconciles molecular affinities, the constraints of morphology, and the specifics of the fossil record. The first passerines are now thought to have evolved in the
Southern Hemisphere in the late
Paleocene or early
Eocene, around 50 million years ago. Several more recent fossils from the
Oligocene of Europe, such as
Wieslochia,
Jamna,
Resoviaornis, and
Crosnoornis, are more complete and definitely represent early passeriforms, and have been found to belong to a variety of modern and extinct lineages. From the
Bathans Formation at the
Manuherikia River in
Otago, New Zealand,
MNZ S42815 (a
distal right
tarsometatarsus of a
tui-sized bird) and several bones of at least one species of
saddleback-sized bird have recently been described. These date from the Early to
Middle Miocene (Awamoan to
Lillburnian, 19–16 mya).
Early European passerines '' fossil In Europe, perching birds are not too uncommon in the fossil record from the
Oligocene onward, belonging to several lineages: •
Wieslochia (Early Oligocene of Frauenweiler, Germany) – suboscine • Passeriformes gen. et spp. indet. (Middle Miocene of France and Germany) – basal? • Passeriformes gen. et spp. indet. (Sajóvölgyi Middle Miocene of Mátraszőlős, Hungary) – at least 2 taxa, possibly 3; at least one probably Oscines. • Passeriformes gen. et sp. indet. (Middle Miocene of Felsőtárkány, Hungary) – oscine? • Passeriformes gen. et sp. indet. (Late Miocene of Polgárdi, Hungary) –
Sylvioidea (
Sylviidae?
Cettiidae?) That suboscines expanded much beyond their region of origin is proven by several fossils from Germany such as a presumed broadbill (
Eurylaimidae) humerus fragment from the Early
Miocene (roughly 20 mya) of
Wintershof, Germany, the Late Oligocene
carpometacarpus from France listed above, and
Wieslochia, among others. Extant Passeri super-families were quite distinct by that time and are known since about 12–13 mya when modern genera were present in the corvoidean and basal songbirds. The modern diversity of Passerida genera is known mostly from the Late Miocene onward and into the
Pliocene (about 10–2 mya).
Pleistocene and early
Holocene lagerstätten ( probably belongs to an extant family, most likely
passeroidean. ==Systematics and taxonomy==