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Through Bird, Fossil and Evolutionary radiation

Trogons are residents of tropical forests worldwide. The greatest diversity is in the Neotropics, where four genera, containing 34 species, occur. The genus Apaloderma contains the three African species. The genera Harpactes and Apalharpactes, containing twelve species, are found in southeast Asia.

They feed on insects and fruit, and their broad bills and weak legs reflect their diet and arboreal habits. Although their flight is fast, they are reluctant to fly any distance. Trogons are generally not migratory, although some species undertake partial local movements. Trogons have soft, often colourful, feathers with distinctive male and female plumage. They are the only type of animal with a heterodactyl toe arrangement. They nest in holes dug into trees or termite nests, laying 2–4 white or pastel-coloured eggs.

Evolution and taxonomy

The position of the trogons within the class Aves has been a long-standing mystery. A variety of relations have been suggested, including the parrots, cuckoos, toucans, jacamars and puffbirds, rollers, owls and nightjars. More recent morphological and molecular evidence has suggested a relationship with the Coliiformes. The unique arrangement of the toes on the foot (see morphology and flight) has led many to consider the trogons to have no close relatives; this would place them in their own order, possibly with the similarly atypical mousebirds as their closest relatives.

The earliest formally described remains of trogoniforms come from Fur Formation Lower Eocene in Denmark (54 mya), including a cranium assigned to Septentrogon, as well as the genus Daniatrogon known from a complete skeleton, which had a relatively narrow beak and lacks the reversed second toe characteristic of living trogons and other fossil trogons, as well as the London Clay at Walton-on-the-Naze, England (Eotrogon and ?Masillatrogon incertus) dating to around 54-56 mya. Other trogoniform fossils, assigned to the genus Masillatrogon, have been found in the Messel pit deposits from the mid-Eocene in Germany (49 mya), and in Oligocene and Miocene deposits from Switzerland and France respectively. The oldest New World fossil of a trogon is from the comparatively recent Pleistocene (less than 2.588 mya).

The family had been thought to have an Old World origin notwithstanding the current richness of the family, which is more diverse in the Neotropical New World. DNA evidence seemed to support an African origin for the trogons, with the African genus Apaloderma seemingly basal in the family, and the other two lineages, the Asian and American, breaking off 20–36 million years ago. More recent studies show that the DNA evidence gives contradictory results concerning the basal phylogenetic relationships; so it is currently unknown if all extant trogons are descended from an African ancestor, an American ancestor or neither.

The trogons are split into three subfamilies, each reflecting one of these splits. Apalodermatinae is the African subfamily and contains a single genus, Apaloderma. Harpactinae is the Asian subfamily and contains two genera, Harpactes and Apalharpactes. Apalharpactes, consisting of two species in Java and Sumatra, has only recently been accepted as a separate genus from Harpactes. The remaining subfamily, the Neotropical Trogoninae, contains the remaining four genera, Trogon, Priotelus, Pharomachrus and Euptilotis.

The two Caribbean species of Priotelus are extremely ancient. The two quetzal genera, Pharomachrus and Euptilotis are possibly derived from the final and most numerous genus of trogons in the Neotropics, Trogon. A 2008 study of the genetics of Trogon suggested the genus originated in Central America and radiated into South America after the formation of the Isthmus of Panama (as part of the Great American Interchange), thus making trogons relatively recent arrivals in South America.

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