Enigmatic glassy materials (escorias) and red bricklike materials (tierras
cocidas) occur at a restricted stratigraphic Level (the top of the Chapadma
lal Formation). Materials from one Locality near Mar del Plata are attribut
ed to a mid-Pliocene impact event with a radiometric and magnetostratigraph
ic age of 3.3 million years ago (Ma), An extinction of endemic fauna (inclu
ding the glyptodonts and flightless cariamid birds) correlates with the uni
t containing the impact glasses, Moreover, the age of the glasses is coinci
dent within dating uncertainties with a pulselike change in the oxygen isot
ope marine record in the Atlantic and Pacific Oceans just before the tate P
liocene deterioration of the climate.