Puerto Rican quail-dove Temporal range: Early Holocene
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Bones of the Puerto Rican quail-dove | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Aves |
Order: | Columbiformes |
Family: | Columbidae |
Genus: | Geotrygon |
Species: | †G. larva
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Binomial name | |
†Geotrygon larva (Wetmore, 1920)
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Synonyms | |
Oreopela larva |
The Puerto Rican quail-dove (Geotrygon larva) is an extinct species of dove from the genus of quail-doves Geotrygon. It is only known by subfossil material from the Holocene.
Remains of the Puerto Rican quail-dove were unearthed in the Cueva Clara and Cueva Catedral near Morovis, in the Cueva Toraño at Utuado, and in a kitchen midden near Mayagüez on Puerto Rico. The holotype, a tarsometatarsus, was discovered in July 1916 by zoologist Harold Elmer Anthony in the Cueva Clara.
According to Alexander Wetmore[1] who described this species it was related to the grey-fronted quail-dove (Geotrygon caniceps), which occurs on Cuba. The tarsometatarsus of the Puerto Rican quail-dove, though, is longer than in the grey-fronted quail-dove. Compared with the ruddy quail-dove (G. montana), which occurs on Puerto Rico, too, the tarsometatarsi are more slender.
The large amount of unearthed material led to the assumption that the Puerto Rican quail-dove might have been a common bird before the initial arrival of humans to the island. Its extinction may have been due to deforestation.[citation needed]