398 MR. S. S. BUCKMAN ON THE BAJOCIAN [Aug. 1895, 



ft. ins. ft. ins. 



Buckmani- 5. Sandy ragstone, mostly very shelly. 



grit. In places beds with numerous small 



lamellibranchiata in an intractable 



matrix. The bottom of this bed is 



very uneven 5 



6. Fine yellow sand — a marked horizon 



in the quarry 4"-6" 



7. Purplish-grey argillaceous mud, with 



numerous broken shells. Terebra- 



tula Buckmani, Dav., but scarce ... 3"-6" 



8. Shelly grey l-agstone, bored in places. 



At the very top of tbis bed Acan- 

 thothyris, n. sp., feebly spinose 1 6 



Lower Tri- 9. Yellowish, somewhat ironshot, shelly 

 gonia-grit. ragstone, with a few lamellibran- 



chiata ; much bored in places. 



Bhynchonella balinensis, Szaj 5 



10. Yellowish marl, with enclosed white 

 pebble-shaped humps 



Upper Free- 11. Oolitic debris 5 



stone equi- 12. White oolitic limestone 3 2 



valent, and 13. Brown marl 1 



Oolite Marl. 14. Greyish marl with Rhynch. Tatei, 

 Bhynch.,sp., Terebr. fimbria (scarce), 



Trigonia, sp 9 



15. Yellow argillaceous mud 1 



4 6 



16. White shelly oolite. 



At Stroud Hill about 10 feet, or perhaps more, 1 separated the 

 Notgrove Freestone and the Lower Trigonia-grit. Here the thick- 

 ness is 14 feet, with Gryphcece towards the top ; the latter fact 

 rather supports the suggestion about the Stroud Hill beds. 



The following is a section of the Frith quarry, 2 near Painswick, 

 whence Witchell obtained several ammonites indicative of the 

 discitce hemera. I have also obtained a poor ammonite therefrom. 3 

 For the section from beds 1 to 24 the present writer is responsible ; 

 but the details of the beds below 24 are copied from a section of 

 the quarry made by Mr. Upton, which he kindly placed at my 

 disposal. Mr. Upton has obtained a fine specimen of Hyperlioceras 

 discites from this quarry, thus confirming Witchell's finds. The 

 specimen was not in situ, but was lying in a part of the quarry 

 where it could only have come from beds 8-11. 



1 On account of the uncertain extent of the gap between the Workhouse 

 and the Coneygre quarries. 



2 No name on the Ordnance Survey map ; it is close to Wick Street. 



3 It is nearest to the Lioceras intermedium represented in pi. xi. figs. 2, 3, 

 ' Monogr. Inf. Ool. Ammonites,' Pal. Soc. vol. xli. (1888). 



