Lithornithidae

Lithornithidae Temporal range: Paleocene-Eocene, 56–40 Ma PreЄ Є O S D C P T J K Pg N Possible Cretaceous record
Pseudocrypturus cercanaxius fossil cast, Zoologisk Museum, Copenhagen
Scientific classification
Kingdom:	Animalia
Phylum:	Chordata
Order:	†Lithornithiformes
Family:	†Lithornithidae Houde, 1988
Genera
Calciavis Fissuravis Lithornis Paracathartes Pseudocrypturus

Lithornithidae is an extinct, possibly paraphyletic^[1] (but see below) clade of early paleognath birds. They are known from fossils dating to the Upper Paleocene through the Middle Eocene of North America and Europe, with possible Late Cretaceous representatives.^[1][2] All are extinct today;^[3] the youngest specimen is the currently unnamed SGPIMH MEV1 specimen from the mid-Eocene Messel Pit site.^[4]

Woodcut of the Lithornis vulturinus holotype

Lithornithids had long, slender, bills for probing. They closely resembled modern tinamous. They possessed a rhynchokinetic skull with relatively unfused cranial bones, a weakly fused pygostyle and a splenial. The unguals were more curved than in tinamous and probably allowed better perching in trees.

The order Lithornithiformes was erected by Dr. Peter Houde in 1988. Three genera are included; Lithornis, Paracathartes, and Pseudocrypturus. There are eight named species.^[3] Promusophaga (Harrisson & Walker, 1977) originally considered a stem-turaco, is considered synonimous with Lithornis vulturinus. Fissuravis may also belong to the clade,^[5] and several unnamed remains are known.

Taxonomy

Lithornithiformes Houde 1988^[6][7]

• †Lithornithidae Houde 1988 (False tinamous)
  • †Calciavis grandei Nesbitt 2016
  • †Fissuravis weigelti Mayr 2007
  • †Paracathartes howardae Harrison 1979 (Early Eocene of WC US)
  • †Pseudocrypturus cercanaxius Houde 1988
  • †Lithornis Owen 1840 [Promusophaga Harrison & Walker 1977; Pediorallus Harrison 1984; Parvigyps Harrison & Walker 1977] (Paleocene – Early Eocene)
    • †L. celetius Houde 1988
    • †L. plebius Houde 1988
    • †L. promiscuous Houde 1988
    • †L. nasi (Harrison 1984) Houde 1988 [Pediorallus nasi Harrison 1984]
    • †L. hookeri (Harrison 1984) Houde 1988 [Pediorallus hookeri Harrison 1984]
    • †L. vulturinus Owen 1840 [Parvigyps praecox Harrison & Walker 1977; Promusophaga magnifica Harrison & Walker 1977; Pediorallus barbarae Harrison & Walker 1977a] (London Clay Early Eocene of England)

Several studies have shown conflicting status on the monophyly of the group. Some studies recover them as a paraphyletic assemblage leading to modern paleognaths,^[1] but more recent examinations group them in a single, natural group basal to the rest of Palaeognathae.^[8] Of issue is Paracathartes, which differs radically from other lithornithids and has been suggested to more closely related to extant paleognaths,^[9] though it is recently recovered as a derived lithornithid.^{[10][note 1]}

Lithornis itself may be paraphyletic in relation to Paracathartes and Pseudocrypturus.^[11]

Flight

Unlike modern paleognaths, lithornithids were generally decent flyers. Lithornis, Pseudocrypturus and Fissuravis all possess well developed keels, pectoral girdle elements and proportionally large wings, allowing for soaring flight akin to that of birds such as modern vultures and storks.^[12][13][1] By contrast, however, Paracathartes had shorter and more robust wing elements and a deeper keel, relating to a flight style more akin to that of modern gamefowl and tinamous, and was possibly far more terrestrial.^[1]

Unlike neognath birds, lithornithids had small pygostyles, and probably no tails.^[1] This may not have impaired their flight, however, since prehistoric birds like enantiornithes also generally had no tails.

Eggs

Several egg fossils have been attributed to lithornithid birds.^[1] Both Lithornis and Paracathartes have entire nests assigned to them.^[14] Their eggshells are, perhaps unsurprisingly, noted as being "ratite-like".^[15]

Notes

References