G02 BULLETIN: MUSEUM OF COMPARATIVE ZOOLOGY. 
11. Loptholepis schmidti Pander. 
12. Melittomelepis elegans Pander. 
13. Otontodus rootsikiillensis Pander. 
14. Prionacanthus brandti Pander. 
its! dubius Pander. 
16. Rytidolepis quenstedti Pander. 
17. Stigmolepis oweni Pander. 
18. Strosipherus indentatus Pander. 
19. laevis Pander. 
20. serratus Pander. 
21. Trachylepis formosus Pander. 
South of Attel are small exposures at Karral and Sarepa, but not 
more than four feet of thick-bedded gray limestone are shown at either 
place. The horizon is perhaps a little higher than the highest beds of 
Attel, but may be the same. At Sarepa Cyphaspis elegantula, 
Illaenus sulcatus Lindstrom and other fossils have been collected. At 
Hoheneichen, a few miles inland from Sarepa, a few feet of thick- 
bedded limestone are exposed in which Labechia conferta Lonsdale 
occurs in great abundance, and from which Phlebolepis elegans Pander 
and Schidiosteus mustelensis Pander have also been collected. 
(b) Kaugatoma zone. This zone is excellently exposed along the 
southern coast to the east of Arensberg and on the Sworbe, the south- 
western peninsular extension of Oesel. It is more fossiliferous than 
the Sagaristi zone. 
On the southern shore there are quite a number of important 
exposures of which the more extensive are those of Moritz, Kasti, 
Nessomay, and Lode, the last being west of Arensberg. 
The Moritz locality is on the road to Nessoma and is about four 
miles east of Arensberg. No rocks in place are now visible, the quarry 
having been abandoned, and it is at present largely overgrown. The 
strata appear to have been alternations of thin shales and coarsely 
crystalline, black and gray limestones. Corals and crinoid stems ex- 
cepted, good fossils do not appear to have been common. Corals 
are abundant, chiefly Clathrodictyon and Acervularia luxurians 
Eichwald. The crinoid stems belong to Crotallocrinus and the most 
common brachiopod is Whitfieldella prunum. Some of the limestones 
have the Caudigalli effect on their upper surfaces. 
Near Kasti two small quarries were examined, each about a mile 
westward from the dwelling of the Kasti estate. One is on the shore 
and exposes about three feet of gray crystalline limestone (beds four 
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