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NUMBER 89 287<br />
and Australia by way of the Antarctic (Figure 4). A second<br />
wave of colonization of North America was possible later, independent<br />
of the colonization of Gondwana, in the Early Cretaceous<br />
(Valanginian).<br />
In Chiappe's (1991) opinion, the Enantiornithes evolved in<br />
Gondwana, whereas Zhou (1995a) claims that Laurasia was<br />
their cradle. In Chiappe's (1991) conception, the whole process<br />
of colonization of the earth ran in the opposite direction, which,<br />
from the viewpoint of the history of continents, also is possible.<br />
If the Enantiornithes separated in the Bajocian, they theoretically<br />
could have originated anywhere on the earth. Vorona berivotrensis<br />
Forster et al. (1996), discovered in Madagascar and considered<br />
to be a sister group of the Enantiornithes, speaks in<br />
favor of Chiappe's conception. On the other hand, the age of the<br />
remains and the differentiation of the forms from Laurasia seem<br />
to support Zhou's (1995a) opinion, and this is the reason for<br />
adopting my present course of reasoning. No matter which of<br />
these two theories is right, the history of continents indicates<br />
that the subclass Enantiornithes evolved in the Middle Jurassic,<br />
more than 25 million years before Archaeopteryx.<br />
The genera Nanantius and Enantiornis were first described<br />
from Gondwana in the Albian of Australia (Molnar, 1986) and<br />
the Maastrichtian of South America (Walker, 1981), respectively.<br />
The acceptance of land dispersal for the Enantiornithes<br />
against a background of the history of continents raises doubts<br />
that the Late Cretaceous remains mentioned from Uzbekistan<br />
and the Gobi Desert (Nesov and Panteleev, 1993; Kurochkin,<br />
1995a, 1996) could actually belong to these genera. Even if<br />
their flight abilities were considerably greater than in the Early<br />
Cretaceous Enantiornithes, at that time the oceans between all<br />
Bocheriski, Z.<br />
1997("1996"). Enantiornithes—dominuj^ca grupa ladowych ptakow kredowych<br />
[Enantiornithes—A Dominant Group of the Cretaceaous Terrestrial<br />
Birds]. Przegl^d Zoologiczny, 40(3^1): 175-184, 4 figures. [In Polish,<br />
with English summary. Date on title pages is 1996; actually published<br />
in 1997.]<br />
Chatterjee, S.<br />
1991. Cranial Anatomy and Relationships of a New Triassic Bird from<br />
Texas. Philosophical Transactions of the Royal Society of <strong>Lo</strong>ndon,<br />
Biological Sciences, 332(1265):277-342, 40 figures. <strong>Lo</strong>ndon: The<br />
Royal Society.<br />
1994. Protoavis from the Triassic of Texas: The Oldest Bird. [Abstract.]<br />
Journal fur Ornithologie, 135(3):330.<br />
Chiappe, L.M.<br />
1991. Cretaceous Birds of Latin America. Cretaceous <strong>Res</strong>earch,<br />
12:55-63.<br />
1993. Enantiornithine (Aves) Tarsometatarsi from the Cretaceous Lecho<br />
Formation of Northwestern Argentina. American Museum Novitates,<br />
3083: 27 pages, 13 figures.<br />
Dong, Zhi-Ming<br />
1993. A <strong>Lo</strong>wer Cretaceous Enantiornithine Bird from the Ordos Basin of<br />
Inner Mongolia, People's Republic of China. Canadian Journal of<br />
Literature Cited<br />
FIGURE 4.—Coastlines in the Albian, 105 Ma BP (modified from Smith et al.,<br />
1995, reprinted with the permission of Cambridge University Press). The star<br />
indicates the Albian locality of Nanantius in Queensland. Arrow indicates the<br />
latest possibility of colonization of Australia, assuming that the Antarctic was<br />
colonized earlier (not later than in the Tithonian). (IP=Indian Peninsula.)<br />
the places mentioned above were too wide to permit crossing<br />
(see Figure 4 and Rich, 1976). It also is doubtful that the genus<br />
Nanantius would have survived for 25 million years (i.e., from<br />
the Albian to the Campanian) or even longer.<br />
Earth Sciences, 30:2177-2179.<br />
Forster, C.A., L.M. Chiappe, D.W. Krause, and S.D. Sampson<br />
1996. The First Cretaceous Bird from Madagascar. Nature, 382:532-534,<br />
4 figures.<br />
Haq, B.W., and F.W.B. Van Eysinga<br />
1987. Geological Time Table. Fourth edition. Amsterdam: Elsevier Science<br />
Publishers. [Wall plate.]<br />
Hou, L.<br />
1995. Morphological Comparisons between Confuciusomis and Archaeopteryx.<br />
In A. Sun and Y. Wang, editors, Sixth Symposium on Mesozoic<br />
Terrestrial Ecosystems and Biota; Short Papers, pages<br />
193-202. Beijing: China Ocean Press.<br />
Kurochkin, E.N.<br />
1995a. The Assemblage of the Cretaceous Birds in Asia. In A. Sun and Y.<br />
Wang, editors, Sixth Symposium on Mesozoic Terrestrial Ecosystems<br />
and Biota; Short Papers, pages 203-208, 3 figures. Beijing:<br />
China Ocean Press.<br />
1995b. Synopsis of Mesozoic Birds and Early Evolution of Class Aves. Archaeopteryx,<br />
13:47-66.<br />
1996. A New Enantiornithid of the Mongolian Late Cretaceous, and a<br />
General Appraisal of the Infraclass Enantiornithes (Aves). 50<br />
pages, 13 figures, 3 plates. Moscow: Russian Academy of Sciences,