. Bulletins of American paleontology. Devonian Brachiopods of New Mexico: Cooper and Dutro 11 PERCHA TYPE AREA (composite). RINCON Wm Ha Des gg Miss ? or Contadero gd — 1 Wm N At Text-figure 6.—Correlated stratigraphic sections of Devonian rocks at selected localities west of the San Andres Mountains. New Mexico (See Text-figure 1 for location of sections and Text-figure 5 for explanations of abbreviations and lithic patterns). caenia. Hypotliyridinci Buckman (1906) and small in- dividuals of Wcirrenella floweri n. sp. At the westernmost known exposures of the Ohate Formation, near Hermosa, Rh
. Bulletins of American paleontology. Devonian Brachiopods of New Mexico: Cooper and Dutro 11 PERCHA TYPE AREA (composite). RINCON Wm Ha Des gg Miss ? or Contadero gd — 1 Wm N At Text-figure 6.—Correlated stratigraphic sections of Devonian rocks at selected localities west of the San Andres Mountains. New Mexico (See Text-figure 1 for location of sections and Text-figure 5 for explanations of abbreviations and lithic patterns). caenia. Hypotliyridinci Buckman (1906) and small in- dividuals of Wcirrenella floweri n. sp. At the westernmost known exposures of the Ohate Formation, near Hermosa, Rhyssovhonetes occurs in the lower 2 m (7 ft) and a characteristic assemblage is found in the upper I m (4 ft): Schizophoria. Nervo- strophia. Dicluicaenia, Hypothyridinu. Eleiitlicrokom- imi. and Desqiiaiiiatia. together with Cystodivtya. An interesting variant on the Onate brachiopod as- semblage occurs in the northern part of the San Andres Mountains where the formation is only about 3 m (10 ft) thick. Two species: Tropidoleptiis platys n. sp., occurring only on Capitol Peak and in Johnson Park Canyon, and Aciitoria angulata n. sp., found only in Johnson Park Canyon, are especially abundant. These occur with species found elsewhere in the Onate, in- cluding: Nervostrophia plana n. sp., Nervostrophia solida n. sp., Schizophoria lata Stainbrook (1940). and Platyterorhynchiis obscunun n. sp. Also present is Mucrospirifei'l aff. Ml sciilptilis (Hall, 1843) and Peii- tanwrella sp., both links to the Middle Devonian of the eastern United 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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