Review of the New York Geological Reports. 59 
. Semmamnmnr ay 
“i eae 
“s24p]00a)D sapsoan,y “V{ pur { “S1,] 
‘soqvtd ey1 Jo soSpe payejnuesd pur jeu 
Serg “gg pur ve ‘g ‘#][ewR] estoasuRd} ot) 
‘apis oy} uodn soiod jo moi ojqnop & Sunuos 
“DapUmYyIOyH “I '% 
“scot “d Suodey 38,]/"?H 
& 
9 snoyejedyjued oy) Farmoys ‘sumnjoo jeproulsa Jo syu9uL 
Gaimoys ‘ueuntoeds quioo-Aouoy B Woy jueWSey Y “4g 
-aid puv ‘aa1m} poylaseu oqny ojsuis y *7z; 
Perhaps no protozoic fossil has a wider range than Fig. 2 of 
this illustration, Favosites Gothlandica. Not only does it oceur 
in the limestones of Gothland, the Eifel and Groningen, as well 
as the magnesian limestones of Gerolstein in Europe, but also in 
the Wenlock limestones of England. In this country it is by no 
means confined to the State of New York, but is found in great 
perfection in the coralline beds in the vicinity of the Falls of the 
Ohio, in Kentucky, Tennessee and Indiana, and also in the mag- 
nesian limestone of the lead regions of lowa and Wisconsin. In- 
deed every locality in the West where the middle protozoic strata 
