194 CAMBRIAN BRACHIOPODA. 



32c. (For stratigraphic position and association, see p. 152.) Middle Cambrian: About 60 feet (18.3 m.) above the 

 Brigham quartzite [Walcott, 1908a, p. 8], in green shale 1 mile (1.6 km.) northwest of Geneva (Copen- 

 hagen), east of Brigham, Boxelder County, Utah (L. D. Biirling, 1905). 

 Acrotreta cf . ophirensis. 



32d.. (For stratigraphic position and association, see p. 152.) Middle Cambrian: Shales about 150 feet (45.7 m.) 

 above the Brigham quartzite [Walcott, 1908a, p. 8], on the east side of the south fork of Paradise Dry Canyon 

 (locally known as East Fork), east of Paradise, Cache County, Utah (F. B. Weeks, 1905). 



Micromitra (Paterina) labradorica utahensis. 



Obelus (Westonia) ella. 



32e (same horizon as 31c and 54o). (For stratigraphic position and association, see p. 151.) Middle Cambrian: 

 About 900 feet (274.3 m'.) above the Brigham quartzite and 3,300 feet (1,005.8 m.) below the Upper Cambrian, 

 in limestone corresponding to that forming lb of the Ute limestone [Walcott, 1908f, p. 196], just south of the 

 south fork of Paradise Dry Canyon (locally known as East Fork), east of Paradise, Cache County, Utah 

 (L. D. Burling, 1905). 



Otusia utahensis. 



*Syntrophia cambria. 



32f. (For stratigraphic position and association, see p. 153.) Upper Cambrian: Thin-bedded siliceous limestone 

 near the top of the Upper Cambrian, about 2 miles (3.2 km.) southeast of Muskrat Spring, on the northwest 

 face of Grantsville Peak, Stansbury Range, Tooele County, Utah (F. B. Weeks and L. D. Burling, 1905). 



Lingulella manticula. 



Lingulella pogonipensis. 



32g. (For stratigraphic position and association, see p. 154.) Upper Cambrian: About 2,575 feet (784.9 m.) above 

 the Cambrian quartzitic sandstones, in a blue limestone about 2 miles (3.2 km.) southeast of Muskrat Spring, 

 on the northwest face of Grantsville Peak, Stansbury Range, Tooele County, Utah (L. D. Burling, 1905). 



Obolus mcconnelli pelias. I Lingulella isse. 



Lingulella desiderata. | Liunarssonella nitens. , 



321i. (For stratigraphic position and association, see p. 157.) Middle Cambrian: Shales in a canyon on the west 

 side of the Simpson Range, 4 miles (6.4 km.) south of Simpson Spring, about 20 miles (32.2 km.) west-south- 

 west of Vernon, Tooele County, Utah (F. B. Weeks and L. D. Burling, 1905). 

 Obolus (Westonia) ella. 



32j. (For stratigraphic position and association, see p. 157.) Middle Cambrian: 625 feet (190.5 m.) above the 

 Cambrian quartzitic sandstones, in pinkish-colored very fine grained arenaceous shale 2 miles (3.2 km.) 

 southeast of Muskrat Spring, on the northwest face of Grantsville Peak, Stansbury Range, Tooele County, 

 Utah (L. D. Burling, 1905). 

 Acrotreta cf. ophirensis. 



32k. (For stratigraphic position and association, see p. 156.) Middle? Cambrian: Limestones about 1,550 feet 

 (472.4 m.) above the top of the Cambrian quartzitic sandstones 2 miles (3.2 km.) southeast of Muskrat 

 Spring, on the northwest face of Grantsville Peak, Stansbury Range, Tooele County, Utah (L. D. Burling, 

 1905). 

 Obolus mcconnelli. 



32n. (For stratigraphic position and association, see p. 151.) Middle Cambrian: Shales about 725 feet (221 m.) 

 above the Brigham quartzite [Walcott, 1908a, p. 8], in the Wasatch Mountains, 1 mile (1.6 km.) northwest 

 of Geneva (Copenhagen), Boxelder County, Utah (L. D. Burling, 1905). 

 Obolus (Westonia) ella?. 



32o. (For stratigraphic position and association, see p. 158.) Middle Cambrian: Shale about 325 feet (99 m.) 

 above the Cambrian quartzitic sandstones 2 miles (3.2 km.) southeast of Muskrat Spring, on the northwest 

 face of Grantsville Peak, Stansbury Range, Tooele County, Utah (L. D. Burling, 1905). 

 Obolus (Westonia) ella. 



32p (=55e). (For stratigraphic position and association, see p. 152.) (L. D. Burling, 1905.) 

 Obolus (Westonia) ella. 

 Acrothele subsidua. 



32t. (For stratigraphic position and association, see p. 154.) Upper Cambrian: Limestone about 3,650 feet (1,112.5 

 m.) above the Cambrian quartzitic sandstones in Fandango Spring canyon, on the east side of the Dugway 

 Range, about 5 miles (8 km.) north of where the stage road between Vernon and Deep Creek crosses the 

 divide, Tooele County, Utah (L. D. Burling, 1905). 

 Linnarssonella girtyi. 



