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E. M. KINDLE 
Bay. The fauna of this lower division of the section comprises the 
following species :* 
Fusulina aff. F. longissima Moell. 
Crania sp. 
Schizophoria ? sp. 
Derbya aff. D. robusta Hall 
Chonetes sp. 
Chonetes aff. C. trapezoidalis Waagen 
Productus aff. P. humboldti D’Orb. 
Productus aff. P. porrectus Kut. 
Productus aff. P. semireticulatus Mar- 
tin 
Productus aff. P. schrenki Stuck 
Productus aff. P. koninckianus Vern. 
Productus cora D’Orb 
Spirifer aff. S. ufensis Tscherny. 
Spirifer cameratus Tscherny. non Mar- 
tin ? 
Squamularia n. sp. 
Martiniopsis sp. 
Rhynchopora aff. R. geinitziana 
Tscherny. 
Dielasma sp. 
Streblopteria sp. 
Aviculipecten aff. A. mccoyi M. and H. 
Aviculipecten, 2 spp. 
Entolium aff. E. aviculatum Meek. 
Solenopsis ? sp. 
In the upper division, }, occur the following species: 
Zaphrentis ? sp. 
Stenopora sp. 
Crinoid fragments 
Streptorhynchus aff. S. pelargonatum 
Schlot. 
Chonetes, 2 spp. 
Productus aff. P. timanicus Stuck. 
Productus aff. P. aagardi Toula. 
Productus aff. gruenewaldti Stuck. 
Productus aff. P. humboldti D’Orb. 
Productus aff. P. mammatus Keys. 
Productus aff. P. lineatus Waagen 
Productus aff. P. occidentalis New- 
berry 
Productus sp. 
Spirifer aff. S. alatus Schlot. 
Spirifer aff. S. blasii Vern. 
Spirifer arcticus Houghton 
Spirifer n. sp. aff. S. marcoui Waagen 
Spirifer aff. S. dieneri Tscherny. 
Spiriferina aff. S. cristata Schlot. 
Squamularia sp. 
Cleiothyris sp. 
Camarophoria margaritovi Tscherny. 
Camarophoria aff. C. purdoni David- 
son 
Rhynchopora aff. R. nikitini Tscherny. 
Rhynchopora aff. R. geinitziana 
Tscherny. 
Dielasma sp. 
Professor Schuchert published some notes on a collecton of Car- 
boniferous fossils from a locality near this section in 1896. The 
fossils were referred to Schuchert by Dr. Dall and Mr. J. A. Becker, 
and were collected near Point Cornwallis, which is about one mile 
from Halleck Harbor. Two of these, Spirifer sp. undet. and Pro- 
ductus longispinus var. alaskensis Schuchert, are reported to come 
from a yellow sandstone. The appearance of the fossils indicates 
that they came from a siliceous band in the limestone of the section. 
t Determined by Dr. G. H. Girty. 
