An enantiornithine bird from the Lower Cretaceous of Queensland, Australia
Current classification of birds recognizes four subclasses: the Archaeornithes, the Enantiornithes, the Odontornithes and the Neornithes. Three of these subclasses were proposed during the nineteenth century, but the Enantiornithes was proposed only five years ago, based on material from the Lecho Formation (Maas-trichtian) of Salt a Province in Argentina1. Further material from Asia (Mongolia) and North America (Mexico) has been referred to the Enantiornithes2, all of it from the Campanian. Now, in addition, a small tibiotarsus found in the Lower Cretaceous (Albian) of Queensland not only represents the first bony material of Mesozoic birds from Australia, but is also the first reported occurrence of an enantiornithine bird in the Lower Cretaceous.
The first Cretaceous bird from Madagascar
WE report the discovery of two exquisitely preserved specimens of a new, very primitive bird from the Late Cretaceous period of Madagascar. The new taxon, Vorona berivotrensis, is provisionally placed phylogenetically in an unresolved trichotomy with Enantiornithes and a clade consisting of Patagopteryx and Ornithurae. These specimens are the first known pre-Holocene birds from Madagascar and the first avian skeletal remains from the Mesozoic era of a large portion of Gondwana.
The pattern of tooth plate formation in the Australian lungfish, Neoceratodus forsteri Krefft
Tooth plate formation in the Queensland lungfish, Neoceratodus forsteri, Krefft begins with simple groups of isolated cusps, three in each tooth plate. The cusps fuse in ridges radiating from a point situated posterolingually. During growth, cusps are added to the labial ends of the ridges, and more ridges are added posteriorly, giving a total of seven in each tooth plate. Each tooth grows in thickness by the addition of layers of material, in line with the new cusps, beneath the tooth plate. The tooth plate grows outwards and is resorbed from the inner angle at the same time. The crushing surface is formed by the growth of cusps between the ridges. Angles between the ridges become progressively smaller, and angles between more posterior ridges are consistently less than between more anterior ridges. Similar but less pronounced changes in angles between ridges occur in a fossil genus, Sagenodus inaequalis, examined for comparison. Vomerine teeth grow in the same way, by fusion of isolated cusps and the addition of new cusps to one end (labial) of the tooth plate. Layers of material are also added beneath the tooth plate. The vomerine tooth plates are initially low-based with long cusps but develop into high-based low cusped incisiform tooth plates in fully grown adults. The labial dentition of the lower jaw starts to develop like the vomerine teeth, but degenerates by stage (vi) of tooth development. The single medial tooth is resorbed even earlier. The pattern of tooth plate formation described in this paper is consistent with illustrations published by Semon (1901) and Greil (1908, 1913) but the inferred developmental processes are different. Implications of the results for the Zahnreihe hypothesis of Edmund and for the phylogeny of Dipnoi are discussed.