. Bulletin of the Department of Geology. Geology. 1919] Merriam: Tertiary Mammalian Faunas of Mohave Desert 521 The metapodials are not distinctly different from those of Mcry- codus osborni figured by The ungual phalanges are sharply pointed anteriorly, and do not show the Roman-nose form seen in the Pliocene antelopes of Thousand Creek and to some extent in Capromeryx. A Tig. 133. Mcrycodus necatus? Leidy. Antler, no. 19832, X %. Barstow Miocene, Mohave Desert, California. Fig. 134. Mcrycodus necatus? Leidy. Antler, no. 22494, X %. Barstow Mio- cene, Mohave Desert, California. An


. Bulletin of the Department of Geology. Geology. 1919] Merriam: Tertiary Mammalian Faunas of Mohave Desert 521 The metapodials are not distinctly different from those of Mcry- codus osborni figured by The ungual phalanges are sharply pointed anteriorly, and do not show the Roman-nose form seen in the Pliocene antelopes of Thousand Creek and to some extent in Capromeryx. A Tig. 133. Mcrycodus necatus? Leidy. Antler, no. 19832, X %. Barstow Miocene, Mohave Desert, California. Fig. 134. Mcrycodus necatus? Leidy. Antler, no. 22494, X %. Barstow Mio- cene, Mohave Desert, California. An axis, no. 21499 (figs. 124ft, 124o), from the Barstow is nearly identical in form and dimensions with the axis of Capromeryx from the Pleistocene of Rancho La Brea. The spout of the Barstow speci- men is extended almost as far up on the sides as in Capromeryx, the Barstow form being in this respect possibly a trifle less advanced. M{?). coronatus Merriam. Univ. Calif. Publ., Bull. Dept. Geol., vol. 7, pp. 335-339, 1913. The type specimen-, consisting of a single fragmentary horn or antler, no. 20052, found by Buwalda and Mourning in 1913, repre- sents a horn or antler of peculiar type, unlike any form known to the writer. 35 Matthew, W. D., Bull. Am. Mus. Nat. Hist., vol. 20, pp. 117, 120. 133 134 MEEYCODUS ? CORONATUS Merriam. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original University of California, Berkeley. Dept. of Geology. Berkeley : The University Press


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