Identifier: annualrepo1517186264newy (find matches)
Title: Annual report of the regents of the university of the state of New York on the condition of the State Cabinet of Natural History and the historical and antiquarian collection annexed thereto
Year: 1853 (1850s)
Authors: New York State Museum
Subjects: Science
Publisher: Albany, Regents of the University of the State of New York
Contributing Library: Smithsonian Institution Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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50. Fig, 7. NucuLiTEs cuNEiFORMis : Conrad, Annual Report 1841, p. 50. Fig. 8. N. OBLONGATUS : Conrad, Annual Report 1841, p. 50. Fig. 9. AsAPHus ADSPECTANS : Courad, Annual Report 1841, p. 49. Fig. 10. Atrypa unisulcata : Conrad, Annual Report 1841, p. 56. Fig. 11. Atrypa peculiaris : Conrad, Annual Report 1841, p. 56. Fig. 12. PosiDONiA LiRATA : Courad, Annual Report 1838, p. 116. Fig. 13. AvicuLA BELLA : Conrad, Annual Report 1841, p. 54. Fig. 14. Atrypa elongata : Conrad, Annual Report 1839, p. 65. Fig. 15. Platyceras sulcatus : Conrad, Annual Report 1841, p. 56. Fig. 16. Orthostoma communis : Conrad, Annual Report 1838, p. 119. Fig. 17. Atrypa acutiplicata : Conrad, Annual Report 1841, p. 54. Fig. 18. Delthyris mucronata : Conrad, Annual Report 1841, p. 54. Fig. 19. Cyrtolites : Conrad, Annual Report 1838, p. 118. Fig. 20. Conularia laqueata : Conrad, Annual Report 1841, p. 57. Fig. 21. Cypricardites carinata : Conrad, Annual Report 1841, p. 53. Fig. 22. Dictuocrinites : Conrad.
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lo;pied. from, tixe Ori;inal Lith.o graphic Plate of T.A.Conrad.y.sq.) Swmtorv. lith.. NOTES AND CORRECTIONS. GENUS PHOLIDOPS. In the Addenda to Vol. iii, Palaeontology of New-York, p. 489, Ihave noticed and described a new genus under the name Pholidops ;expressing some doubt whether it may be a patellifbrm univalve,or a bivalve shell, since the only specimen where two valves wereshown in connexion was not entirely satisfactory. In the Thirteenth Report upon the State Cabinet, p. 92, I noticedthe genus, and described an additional species, expressing my beliefthat the shell was univalve. The numerous specimens observed inthe Hamilton group are all of single valves; and hence I was ledto the conclusion, that in the Oriskany sandstone species, showingtwo similar valves in contact, the relation was only accidental. During the last year, however, I have found among some collec-tions from the Niagara group in Indiana, another species with twosimilar valves closely conjoined; thus leaving

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