THE OLDEST RECORD OF ARAMAYOICHNUS RHEAE FROM THE NEOGENE OF NORTHWESTERN ARGENTINA

DAVID E. TINEO; LEANDRO MARTÍN PÉREZ; PAULA BONA; MARCOS COMERIO; JORGE NORIEGA; DANIEL GUSTAVO POIRÉ

AMEGHINIANA

ASOCIACION PALEONTOLOGICA ARGENTINA

Lugar: Buenos Aires; Año: 2017

0002-7014

THE Argentinean fossil record of vertebrate footprints is significant and has been extensively studied; however sites with bird tracks are scarce and less known (Bonaparte, 1965; Aramayo, 1991, 2007; Galli et al., 1992; Aramayo and Manera de Bianco, 1987, 1990, 1996; de Balais and Melchor, 2008; Genise et al., 2009; Melchor, 2009; Alonso, 2012; Aramayo et al. 2015). Although, there are some studies of fossil footprints referred to Aves, there are no detailed descriptions or taxonomical assignations of such traces. A bird trackway with three footprints was found in the lower levels of the Guandacay Formation (upper Miocene-Pliocene) (Ayaviri, 1967), Grupo Chaco (Stebinger, 1920; White, 1925), at the ?Río Iruya? section, 62 Km NW of the city of San Ramón de la Nueva Orán (Salta Province, Argentina; Fig. 1.1). This unit is part of the fill of the Neogene foreland basin of the Sierras Subandinas Australes. This Subandean terrain is a thin-skinned fold-thrust belt system which represents the easternmost expression of the deformation of the central Andes. Compressive tectonics created a foreland basin with clastic sequences of continental rocks approximately 7500 m thick (Hernández et al., 1996; Ramos, 1999).The aim of this contribution is to report a new record of Aramayoichnus rheae Aramayo et al. 2015 from the Neogene of Northwestern Argentina, based on tridactyl - footprints attributed to bird activity. This fossil evidence expands the paleogeographical and temporal distribution of this ichnospecies, showing the presence of rheids in the Late Miocene in the Subandean region. The footprints were preserved as natural casts (convex hyporeliefs) in brownish-grey, fine to medium grain conglomerates; the base of the level is in contact with reddish - reddish brown mudstones and very fine sandstones (Fig. 1.2). The hypothesis that a rheiform bird could have registered this trackway is here considered in association with the fossil record of the group in a stratigraphic and biogeographic context.