ABSTRACT
Therian petrosals from the Milk River and Oldman formations of Alberta are described. The Milk River specimen is the earliest known ear structure of a therian from North America and has a cochlea with one and a quarter turns. Two of the Oldman specimens are from marsupials, probably Eodelphis. These specimens provide significant new evidence about the earliest known otic structures in marsupials, including: absence of the promontory and stapedial grooves on the promontorium, presence of a prominent rostral tympanic process of the petrosal, achievement of a fully coiled cochlear canal, and development of the radial innervation system of the cochlea. Implications of the new findings are: 1) absence of the stapedial artery is consistently distributed in marsupials; 2) the rostral tympanic process of the petrosal has evolved more than once in marsupials; 3) a fully coiled cochlear canal had evolved in the therian ear by the Late Cretaceous; 4) a radial innervation complex of the cochlea evolved along with the coiled cochlea in the therian ear during the Late Cretaceous.