"Bird-like tracks from northwest Argentina have been reported as being of Late Triassic age1. They were attributed to an unknown group of theropods showing some avian characters. However, we believe that these tracks are of Late Eocene age on the basis of a new weighted mean 206Pb/238U date (isotope dilutionthermal ionization mass spectrometry method) on zircons from a tuff bed in the sedimentary succession containing the fossil tracks. In consequence, the mentioned tracks are assigned to birds and its occurrence matches the known fossil record of Aves."
http://www.nature.com/nature/journal/v495/n7441/full/nature11931.html
The previous paper that gave a Triassic age was based on geologic relationships between different formations. They got those relationships wrong.
The age of the stratigraphic unit was considered to be Late Triassic on the basis of known fossil wood remains and geochronological information from basalt lava flows thought to be interbedded in this unit1, 3, 4. Further geological studies revealed that the Santo Domingo Formation contains several thrust sheets of different ages, and that the trace-fossil-bearing horizons belong instead to the recently proposed Laguna Brava Formation, in a thrust sheet separate from the one that contains the dated basalt and fossil wood remains5.
When they directly dated the rocks in the sediment bed containing the bird tracks, it turned out to be Eocene.
A 12-cm-thick crystal-rich ash-fall tuff within the thrust sheet with the bird-like footprints was sampled for this study for UPb zircon geochronology (supported by US National Science Foundation grant EAR 0931839 and ANPCyT PICT 13286 from Argentina). This tuff lies 38 m below the first layer with definite G. dominguensis and 124 m below the main horizon with hundreds of G. dominguensis6. There is no stratigraphic discontinuity between the tuff bed and the footprint-bearing levels. Zircon grains were separated from the tuff using conventional methods and were dated using high-precision chemical abrasionisotope dilutionthermal ionization mass spectrometry (CA-ID-TIMS)7, 8. The tuff yielded abundant clear, long bipyramidal (150 μm and 250 μm) and sharply faceted zircons. The five youngest analyses from a total of nine form a coherent cluster with a weighted-mean 206Pb/238U date of 37.222 ± 0.018/0.024/0.047 million years (Myr) ago (internal uncertainties/with tracer calibration uncertainties/with decay constant uncertainties; mean square of weighted deviation = 1.6) (Fig. 1 and Table 1). emphasis mine