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A field guide to mesozoic birds and other winged dinosaurs

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Avians<br />

Avians, “(modern) <strong>birds</strong>”, represent the bird ‘crown group’, descendants<br />

of the most recent common ances<strong>to</strong>r of all <strong>birds</strong> alive <strong>to</strong>day. This<br />

ances<strong>to</strong>r seems <strong>to</strong> have existed as early as 130 million years ago, if fragmentary<br />

remains such as those classified as Gallornis are indeed avians.<br />

All known avians lack teeth, <strong>and</strong> instead have extensive, often fully-fused<br />

beaks. It is likely that teeth were lost completely in a predecessor <strong>to</strong> the<br />

common ances<strong>to</strong>r of all modern bird groups; however, it is also possible<br />

that two or more avian lineages lost teeth independently of one an<strong>other</strong>.<br />

Numerous species of avians have been identified from the Mesozoic,<br />

mainly from the latest Cretaceous, but are based on remains <strong>to</strong>o fragmentary<br />

<strong>to</strong> reconstruct their life appearance with any degree of confidence<br />

(see Appendix A). Due <strong>to</strong> this poor fossil record, there has his<strong>to</strong>rically been<br />

a debate regarding the timing of modern bird diversification. However, the<br />

likely presence of many modern bird “orders” in the Mesozoic suggests that<br />

avians had begun <strong>to</strong> diversify in<strong>to</strong> many of their modern forms by the time<br />

of the K-Pg extinction event that ended the Mesozoic era.<br />

Based on tentative interpretations of the fossil evidence, it is likely<br />

that members of the following modern bird groups existed before the K-Pg<br />

boundary: Charadriiformes (wading shore<strong>birds</strong> like Cimolopteryx), Anseriformes<br />

(including Vegavis, above), Galliformes (including Austinornis), Palaeognathae<br />

(ratites <strong>and</strong> allies represented by Limenavis <strong>and</strong> possibly some<br />

early lithornithids), <strong>and</strong> Pelecaniforms (including Torotix <strong>and</strong> some cormorant-like<br />

<strong>birds</strong>). Grebes <strong>and</strong> rail-like <strong>birds</strong> (possibly ancestral <strong>to</strong> Cenozoic<br />

“terror <strong>birds</strong>”) have also been reported from the latest Cretaceous. At least<br />

one species or lineage representing each of these groups survived the K-Pg<br />

extinction <strong>and</strong> diversified in<strong>to</strong> all the remaining groups of modern <strong>birds</strong><br />

in the Cenozoic Era. In the case of the anseriformes, at least two species or<br />

lineages survived the mass extinction (presbyornithids <strong>and</strong> the ances<strong>to</strong>rs of<br />

modern ducks <strong>and</strong> geese represented by Vegavis).<br />

In addition <strong>to</strong> these avian lineages, it is possible that one or more<br />

groups of non-avian <strong>birds</strong> also survived across the K-Pg boundary. One<br />

species from the Paleogene, Qinornis paleocenica, is known from fossils<br />

which show unfused bones in the tarsus, despite the interpretation of the<br />

specimen as an adult, a trait known only in non-avian <strong>birds</strong>. This species<br />

may represent a lineage of <strong>to</strong>othed carinate <strong>birds</strong> that survived for several<br />

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