131 



Olad. 



Cladodiis a genus of fish of Carboniferous times of which 

 S. A. Miller catalogues the following species as described up 

 to 1884: Acuminatits^ alternatus^ angulatus^ hellifer^ carina- 

 tus^ Goncinmis^ costatus^ deflexus^ eecentrieus^ elegans, eugly- 

 pheus^ exiguus^ exilis^ Jerox^ fulleri^ gomphoides^ gracilis^ 

 grandis^ hertzerU inter go status^ ischypus^ lamnoides^ magiA- 

 Gus^ miGropics^ mortifer^ newmani^ OGGidentalis^ pandatus^ par- 

 vulus^ pattersoni^ politus^ proeyiuntius^ rariGOstatus^ rohustusy 

 romingeri^ spinosus^ sprmgerL steiioptis^ suhulatus^ suGGinGtuSj 

 turrittis^ vanhoriiei^ loaGhsmMthi^ and zygopits ; most of them 

 by Newberry in the Ohio Palaeontology ; many by St. John & 

 Worthen in that of Illinois; some by Tuomy, Alabama survey; 

 one by Leidy ; and most of them in the Lower Carboniferous 

 Strata. — In Pennsylvania, spines referable to this genus of fish 

 are frequently found in the Meadville upper limestone at Glen- 

 dale and elsewhere in Crawford Co. I. C. White's Rt. Q4, p. 

 83, 140. — Waverly or Pocono formation, X. — See also C aril's 

 Rt. I, p. 70. — And for such in the SubGonglomerate strata, see 

 I, p. 67. — XI? X? — For figure see Appendix. 



Cladopora caespitosa ? A Niagara polypoid coral (Hall, 

 1852, Pal. N. Y. Vol. 2), which seems to be represented by 

 specimen 610-8, in Billin's collections, 1876, from Warrior's 

 ridge, Barree township. Hunt. Co., in Lower Helderherg lime- 

 stone^ VL — For figure see Appendix, 



Cladopora laqueata. (Rominger, 1876, Foss. Corals, Ni- 

 agara formation). A. Winchell's GeoL 

 studies, 1886, page 224, fig. Ihl.— Ni- 

 agara formation. V a. — The figure 

 is a small part of the beautiful fig. 

 on plate 18, of Vol. 3, of the superb 

 work of the late State Geologist of 

 Michigan. 



Cladopora multipora? Hall. Pal. N. Y., Vol. 2, 1852, 

 Niagara limestone, VI). Doubtfully identified in Pennsyl- 

 vania by I. G. White, at Maurer's, Eck's, Limeridge and Apple- 

 ton's quarries in the Montour district, in Lower Helderberg 

 limestone, over the Bastard leds. Rt. G7, p. 89, 244, 247, 261, 

 300. — In Huntingdon Co., Coffl'ee run section, in Bastard led 

 44 T3, p. 172. Especially numerous in the McConnellsville 



