. Bulletins of American paleontology. PL. 28, Vol. 27 Bull. Amer. Paleont. No. 108, Pl. 2. Fig. 1.—Photo 3 of gray, slaty shale and gray nodular shale that weathers brownish gray. Some dark-gray quartzitic sandstones are interbedded with the shales. The locality is about at the top of the Cano del Oeste formation on the Cano Grande branch of Rio 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 Paleontological Resea
. Bulletins of American paleontology. PL. 28, Vol. 27 Bull. Amer. Paleont. No. 108, Pl. 2. Fig. 1.—Photo 3 of gray, slaty shale and gray nodular shale that weathers brownish gray. Some dark-gray quartzitic sandstones are interbedded with the shales. The locality is about at the top of the Cano del Oeste formation on the Cano Grande branch of Rio 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 Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ]
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