Type-Species.—Telmatornis priscus Marsh, 1870, by subsequent designation (Hay, 1902:528).
Included Species.—Type species only.
Telmatornis priscus Marsh, 1870
Figures 5b-j, 6c,e,g, 7a,d,g,j,n
Telmatornis priscus Marsh, 1870:210. Telmatornis affinis Marsh, 1870:211. Graculavus pumilis Marsh, 1872:364. ?Palaeotringa vetus Marsh, 1870:209.
Holotype.—Distal end of left humerus ([Figure 5e,h]), YPM 840; collected in pits of the Cream Ridge Marl Company, near Hornerstown, New Jersey by J.G. Meirs. Navesink Formation, Maastrichtian, Late Cretaceous (Baird, 1967).
Referred Specimens.—Distal end of right humerus ([Figure 5f,g]), YPM 845 (holotype of Telmatornis affinis Marsh 1870); same data as holotype of T. priscus.
Proximal end of right humerus ([Figure 5b-d]), YPM 850, with distal end of right carpometacarpus ([Figure 5i]) and several fragments of shafts of long bones apparently associated (holotypical material of Graculavus pumilis Marsh, 1872); collected near Hornerstown, New Jersey, by J.G. Meirs; probably from the basal Hornerstown Formation, Maastrichtian, Late Cretaceous.
Distal end of left tibiotarsus ([Figure 7n]), ANSP 13361 (holotype of Palaeotringa vetus), collected near Arneytown, on the Monmouth-Burlington county boundary, New Jersey; Basal Hornerstown Formation, Maastrichtian, Late Cretaceous (Baird, 1967).
Left humerus lacking proximal end ([Figure 6c,e,g]), ANSP 15360; collected in 1971 from the Inversand Company marl pit, Sewell, Gloucester County, New Jersey, by Keith Madden. Basal Hornerstown Formation, Maastrichtian, Late Cretaceous.