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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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