Two dinosaur footprints levels are discovered in the 'Gres superieurs et Ar
gilites bariolees' Formation dated Late Triassic. These tracks form the Oto
zoum/Grallator association, never sharply defined in Europe. From ichnologi
cal comparisons with USA and South Africa, a norian age is inferred for the
french levels bearing the footprints. Otozoum grandcombensis nov. ichnosp.
names large tetradactyl hands and feet traces made by a bipedal Prosauropo
da, sometimes quadrupedal. It differs from Plateosaurus, frequent in the eu
ropean upper triassic, by a remarkable homopody. Grallator andeolensis nov.
ichnosp. are II-IV; tridactyl feet traces, probably due to a Ceratosauria
Coelophysidae. These two kind of dinosaurs lived together in a large flood
plain with flora and in which numerous clay-dolomite alternatings were depo
sited.