| Charadriiformes | ||||||||
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| Crested Auklets (Aethia cristatella) | ||||||||
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Scolopacidae |
Charadriiformes is a diverse order of small to medium-large birds. It includes about 350 species and has members in all parts of the world. Most Charadriiformes live near water and eat invertebrates or other small animals; however, some are pelagic (sea birds), some occupy deserts and a few are found in thick forest.
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The order was formerly divided into three suborders:
The Sibley-Ahlquist taxonomy, which has been widely accepted in America, lumps all the Charadriiformes together with the seabirds and birds of prey into a greatly enlarged order Ciconiiformes. However, the resolution of the DNA-DNA hybridization technique used by Sibley & Ahlquist was not sufficient to properly resolve the relationships in this group, and indeed it appears as if the Charadriiformes consititute a single large and very distinctive lineage of modern birds of their ownFain & Houde (2004).
The auks, usually considered distinct because of their peculiar morphology, are more likely related to gulls, the "distinctness" being a result of adaptation for diving. Following recent researchEricson et al. (2003), Paton et al. (2003, Thomas et al. (2004a,b), van Tuinen et al. (2004), Paton & Baker (2006), a better arrangement may be as follows:
More conservatively, the Thinocori could be included in the Scolopaci, and the Chionidi in the Charadrii, or the Glareolidae could be placed in a tribe of their own. The buttonquails are of indeterminate, quite basal position in the Lari-Scolopaci sensu lato group. The arrangement as presented here is a consensus of the recent studies.van Tuinen et al. (2004), Paton & Baker (2006)
That the Charadriiformes are an ancient group is also borne out by the fossil record. Much of the Neornithes\' fossil record around the Cretaceous–Tertiary extinction event is made up of bits and pieces of birds which resemble this order. In many, this is probably due to convergent evolution brought about by semi-aquatic habits. Specimen VI 9901 (López de Bertodano Formation, Late Cretaceous of Vega Island, Antarctica) is probably a basal charadriiform somewhat reminiscent of a thick-knee[citation needed]. However, more complete remains of undisputed charadriiforms are known only from the mid-Paleogene onwards. Present-day orders emerged around the Eocene-Oligocene boundary, roughly 35-30 mya. Basal or unresolved charadriiforms are:
The "transitional shorebirds" ("Graculavidae") are a generally Mesozoic form taxon formerly believed to constitute the common ancestors of charadriiforms, waterfowl and flamingos. They are now assumed to be mostly basal taxa of the charadriiforms and/or "higher waterbirds", which probably were two distinct lineages 65 mya already[citation needed], and few if any are still believed to be related to the well-distinct weaterfowl. Taxa formerly considered graculavids are:
Other wader- or gull-like birds incertae sedis, which may or may not be Charadriiformes, are:
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