The rhamphotheca of the Eocene pseudo-toothed birds from Antarctica

The Pelagornithidae are an extinct group of soaring birds that lived all over the world between the early Palaeocene and the Pliocene-Pleistocene and are characterised by the presence of hollow denticles along the tomial edges formed by the expansion of the premaxillary, maxillary, and dentary bones. The presence of distinctive sulci in the upper and lower jaws together with the absence of wearing signs on the denticles, attributable to the handling of the prey, indicates the development of a resistant and compound rhamphotheca. To reconstruct it, we turned to the evidence provided by extant representatives with similar configurations and the osteological correlates of the beak. As a result, we propose a model for the middle-latest Eocene Antarctic Pelagornithidae, in which the rhamphotheca would have been formed by thick horny plates. The <i>culminicorn</i> was separated from the <i>laternicorn</i> by an extense <i>sulcus nasi</i> that continuous caudally to the <i>apertura nasi ossea</i>, a sturdy and hooked <i>unguis maxillaris</i> covering the <i>rostrum</i>, with small nares opening at the cranial end of the <i>apertura nasi ossea</i>, dorsal and ventral <i>ramicorns</i>, and a thick <i>unguis mandibularis</i> with a pseudomental fold and a sulcus on the mandible.