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million years in the Cenozoic.<br />
Not included here is the diverse bird fauna of the Horners<strong>to</strong>wn Formation<br />
of New Jersey, which probably formed very shortly after the K-Pg<br />
boundary (as evidenced by an abundance of re-buried mosasaur remains).<br />
This ecosystem preserved an abundance of water<strong>birds</strong> including waders<br />
<strong>and</strong> representatives of most bird groups mentioned above, further evidence<br />
that the <strong>birds</strong> which survived the extinction were primarily water<strong>birds</strong>, <strong>and</strong><br />
which later evolved in<strong>to</strong> “higher l<strong>and</strong> <strong>birds</strong>” <strong>to</strong> fill the vacant niches left by<br />
enantiornitheans <strong>and</strong> <strong>other</strong> theropods.<br />
Above: Hypothetical res<strong>to</strong>rations of select Mesozoic avians. Clockwise from <strong>to</strong>p left: Austinornis<br />
lentus, Cimolopteryx rara, Limenavis patagonica, Torotix clemensi. Not <strong>to</strong> scale.<br />
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