NOTES ON THE LORRAINE FAUNAS‘ OF NEW 
YORK AND THE PROVINCE OF QUEBEC 
Aug. F. Foerste 
1. Lingula clochensis 
2. Lingula rectilateralis, Emmons 
3. Pholidops subtruncata, Hall 
4. Glyptorthis insculpta, Hall 
5. Glyptorthis crispata, Emmons 
6. Dalmanella centrilineata, Hall 
7. Strophomena planumbona var, 
8. Rafinesquina nasuta, Conrad 
9. Rafinesquina squamula, James 
10. Rafinesquina mucronata 
11. Catazyga erratica, Hall 
12. Caritodens demissa, Conrad 
13. Byssonychia radiata, Hall 
14. Colpomya pusilla 
15. Pholadomorphapholadiformis, Hall 
16. Pholadomorpha pholadiformis — di- 
varicata 
17. Pholadomorpha chambliensis 
18. Modiolopsis modiolaris, Conrad 
19. Modiolopsis concentrica, Hall and 
Whitfield 
20. Modiolopsis postplicata 
21. Orthodesma approximatum 
22. Orthodesma nasutum, Conrad 
23. Orthodesma pulaskiensis 
24. Orthodesma prolatum 
25. Cymatonota lenior 
26. Cymatonota pholadis, Conrad 
27. Modiolodon poststriatus 
28. Psiloconcha subovalis, Ulrich 
29. Psiloconcha sinuata-borealis 
30. Cyrtodonta clochensis 
31. Ischyrodonta cur ta, Conrad 
32. Whitella securiformis 
33. Whitella complanata 
34. Whitella goniumbonata 
35. Clidophorus planulatus, Conrad 
36. Clidophorus praevolutus 
37. Ctenodonta lorrainensis 
38. Lyrodesma poststriatum, (Emmons) 
Hall 
39. Rhytimya oehana, Ulrich 
40. Cuneamya scapha-brevior 
41. Archinacella clochensis 
42. Archinacella pulaskiensis 
43. Lophospira beatrice 
44. Ruedemannia abbreviata, Hal 
45. Pterotheca cf. attenuata 
46. Pterotheca pentagona 
47. Cornulites sp. 
48. Technophorus quincuncialis 
49. Cryptolithus tessellatus, Green 
50. Calymene conradi, Emmons 
51. Proetus chambliensis 
52. Byssonychia carinata, Goldfuss 
During the summer of 1912, through the courtesy of the Direc- 
tor, Dr. R. W. Brock, I was given the privilege of carrying on 
investigations on the Richmond and Lorraine formations of the 
province of Quebec, under the auspices of the Geological Survey 
of Canada. These investigations revealed the presence of a 
great thickness of red clays occupying the stratigraphical position 
of the Queenstown red clay shales in western New York. These 
red clay shales were underlaid by fossiliferous strata readily corre- 
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