REPORT OF THE STATE PALEONTOLOGIST I9O3 



221 



a half inch shale seam lying immediately on the Tentaculite 

 band lo inches 



Gid The lowest portion is a 3 foot bed of solid limestone. This 

 is succeeded by a rather shaly limestone, 2 to 4 inches thick, alter- 

 nating with thin shaly seams, ^ to /^ inch thick 11^ feet 



The following fossils were gathered here: 



86 Spirifer vanuxemi Hall C 

 89 Stropheodonta varistriata (Con- 

 rad) 

 103 Whitfieldella? nncleolata (Hall) 

 C 



it6 Loxonema sp. 



128 Tentaculites gyracanthus (Eaton) 

 144 Beyrichia manliusensis ? Wel- 

 ter r 



Gie Chert is sparingly scattered through the lowest layer of 

 this 2 feet 



Section H 



Section H begins 5 rods northeast of section G. 



Hi Upper Manlius 13 feet 



Hia An exceedingly dense, finely grained, dark gray limestone 

 with very few fossils. Even where weathered from preglacial times, 

 there are very few fossil fragments shown ii feet 



Hib Alternately finely and rather coarsely grained, dark gray 

 limestone 2 feet 



Fossils are much more abundant than in the preceding bed. The 

 following were identified : 



Favosites? 

 86 Spirifer vanuxemi Hall r 

 103 Whitfieldella? nucleolata (Hall) 

 C 



116 Loxonema sp. 



144 Beyrichia manliusensis? (Weller) 



r 

 146 Leperditia alta (Conrad) c 



H2 Favosites bed. The lower 4 inches weather quite red. The 



whole bed is full of Stromatopora heads , i foot 



The following fossils were identified : 



2 Stromatopora concentrica? Gold- 

 fuss C 



6 Favosites helderbergiae Hall c 



7 F. sphaericus Hall r 



64 Rensselaeria cf. aequiradiata 



(Conrad) R 

 89 Stropheodonta varistriata (Con- 

 rad) 

 103 Whitfieldella? nucleolata (Hall) r 



