Abstract - A new tracksite located in the Mesozoic autochthonous series
covering the Aiguilles Rouges Massif, circa 7 km to the NNE of the tracksite of
the Vieux Emosson, is briefly described. The trampled bed is most likely coeval
with the outcrop in the Vieux Emosson area. Two poorly preserved quadrupedal
trackways, almost parallel, measure 9.8 and 8 m in length, respectively. They
are referred to the Chirotheriidae ABEL, 1835 form-family. A short and
well-preserved quadrupedal trackway, composed of two manus-pes couples, is
assigned to Chirotherium cf. barthii KAUP, 1835. A
reinterpretation of the Vieux Emosson ichnotaxa reveals that most tracks, if not
all, belong to indeterminate chirotheriid and that no clear evidence of dinosaur
footprints is observed. The trampled bed of the cover of the Aiguilles Rouges
Massif probably forms a megatracksite, which is Early or Middle Triassic in age.
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