Post-glacial fossil vertebrates from east-central Illinois / by Edwin C. Galbreath.

v.6:no.20(1938)

Ordovician vertebrates from Western United States / Robert H. Denison --

v.16:no.6(1967)

New and little known genera and species of vertebrates from the Lower Permian of Oklahoma / [by] Everett C. Olson -- [Patricia M. Williams, editor]

v.18:no.3(1970)

Early devonian vertebrates from the Keoydart formation of Nova Scotia.

v.37:no.17(1955)

Proposed Agate Fossil Beds National Monument, Nebraska.

"August 1963."

Structural function and evolution of the subarctometatarsus

Compares the metatarsal structural design (subarctometatarsus) of recently discovered Chinese feathered dinosaurs with the metatarsus (arctometatarsus) possessed by more advanced theropod dinosaurs and the metatarsus of more primitive forms. The subarctometatarsus was proved to be an intermediate structure. Additionally the metatarsus appears to co-incide with the evolution of the avian feather suggesting a possible relationship between the subarctometatarsus's evolution and the evolution of avian flight.

Estudo comparativo de restos fósseis e recentes de Amphisbaenia: abordagens filogenéticas, paleoecológicas, paleobiogeográficas

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

The vertebrate fauna of the Selma Formation of Alabama.

v.3:no.8(1970)

The vertebrate fauna of the Selma Formation of Alabama. Rainer Zangerl.

v.3:no.5(1960)

The vertebrate fauna of the Selma Formation of Alabama. Dale A. Russell.

v.3:no.7(1970)

Arctoryctes and some other Chadronian vertebrate microfossils from Nebraska / [by] William D. Turnbull -- and Charles A. Reed --.

v.14:no.3(1960)

The vertebrate fauna of the Selma Formation of Alabama. Rainer Zangerl.

v.3:no.3(1953)

The vertebrate fauna of the Selma Formation of Alabama. Wann Langston, Jr.

v.3:no.6(1960)

The vertebrate fauna of the Selma Formation of Alabama. Rainer Zangerl.

v.3:no.2(1948)

The Pleistocene of the middle region of North America and its vertebrated animals /

Mode of access: Internet.