76 KANSAS ACADEMY OF SCIENCE. 
Nucula beyrichii ?? Schauroth, rr. 
Macrodon sp., rr. 
Lima retifera Shumard, rr. 
Bellerophon carbonaria Cox, rr. 
Bellerophon marcouana Geinitz, rr. 
Bellerophon montfortianus Norwood and Pratten, rr. 
Bellerophon ? cast, rr. 
Pleurotomaria sp., rr. 
Pleurotomaria subdecussata Geinitz, rr. 
Murchisonia sp., rr. 
Aclis sp., rr. 
Straparollus (Euomphalus) subrugosus Meek, rr. 
Loxonema rugosa Meek and Worthen, rr. 
Smali slender gastropod, rr. 
Dentalium meekianum Geinitz, rr. 
Cythere sp., a. 
Phillipsia scitula Meek and Worthen, rr. 
Nautilus forbesianus McChesney ??, rr. 
Several undetermined species of Mollusca and a fish tooth. 
The following were collected at the Minersville section: 
Fusulina secalica (Say) Fischer, aa. 
Rhombopora lepidodendroides (McChesney ) Meek, c. 
Bryozoa, 3 species, rr. 
Productus cora d’Orbigny, c. 
Productus semireticulatus Martin, rr. 
Productus costatus Sowerby, rr. 
Productus nebrascensis Owen, rr. 
Productus pertenuis Meek, a. 
Derbya crassa (Phillips) Hall and Clarke, a. 
Spirifer cameratus (Hall) Meek, r. 
Spiriferina cristata (Schlotheim ) Davidson, rr. 
Meekella striatocostata (Cox) White and St. John, rr. 
Chonetes glabra Geinitz, r. 
Chonetes granulifera Owen, aa. 
Amboccelia planoconvexa (Shumard) Hall and Clarke, a. 
Myalina perattenuata Meek and Worthen, rr. 
Allorisma sp., rr. 
Nucula ventricosa Hall ?, rr. 
Zeacrinus ? mucrospinus McChesney, rr. 
In collecting the fossils mentioned in these two lists no attempt was made to 
keep those of the different strata or groups of strata separate, except the two 
localities, as the matrix from which they were taken had been removed from its 
original position and mingled to a greater or less extent. Some of the species in 
the above list are not mentioned by Meek, while others that he found were not 
to be had at this time on account of the covering of the rocks that contained 
them. 
During the past summer the Burlingame limestone of the Wabaunsee forma- 
tion was traced from the Kansas river just west of Topeka, Kan., to the Nebraska 
line, where it seems to connect with Meek’s southern sections of the Missouri 
river bluffs. This seemed to be an additional evidence of the close relation of 
the Coal Measures of eastern Nebraska and Kansas, and led to a more close com- 
parison of the rocks and, fauna. 
