CORALS FROM THE DEVONIAN FORMATION. 215 
found also at Nehou and Visé, in France ; at Millar, in Spain; at Paffrath, in the Eifel and 
in the Hartz Mountains; in the Oural, in Russia; in the States of Indiana, Ohio, and 
Kentucky, in America ; and (according to Mr. Lonsdale) at Yass plains, in New South Wales. 
This fossil was, till of late, confounded with 7. gothlandica,’ to which it bears in fact 
great resemblance exteriorly ; but it differs from it by the mural pores being more distant 
from each other, and arranged in two vertical lines on each side of the wall. In F. 
alveolaris’ and F. aspera’ these pores are always situated in the angles formed by 
the prismatic walls of the corallites, and in /. dasalticat and F. polymorpha’ they only 
form a single line, placed in the middle of each side of the wall. In mzdltipora® and 
F. Troosti,’ on the the contrary, there are always three series of pores on each side of the 
wall. #. parasitica’ and F. Forbesi® differ from F. Goldfussi by their calices being 
very unequal in size, and F. Hisingeri may be distinguished from the latter by the 
great development of the dissepiments. As to the ramose species of Favosites, they are 
sufficiently distinct from the above-described fossil, in consequence of their form. 
2. Favosires reticutata. Tab. XLVIII, figs. 1, la, 14. 
CALAMOPORA SPONGITES (var. RAMOSA), Goldfuss, Petref. Germ., vol. i, p- 80, tab. xxviii, 
fiz. 2a—yg, 1829. (Ccet. excl.) 
ALVEOLITES RETICULATA, De Blainville, Dict., vol. lx, p. 369, 1830.—Man., p- 404. 
CaLAMopPoRA SPoNGITES, Geinitz, Grundy. der Verst., pl. xxiii a, fig. 13, 1845-46. 
— — Keyserling, Reise in das Petsch., p. 178, 1846. 
ALVEOLITES sponairEs, D’ Orbigny, Prodr. de Paleont., vol. i, p. 108, 1850. (Not Steininger.) 
Favosires Orpianyana, De Verneuil and Jules Haime, Bull. Soc. Géol. de France, 2d ser., 
vol. vil, p. 162, 1850. 
= RETICULATA, Milne Edwards and Jules Haime, Pol. Foss. des Terr. Palzoz., 
p- 241, 1851. 
Corallum dendroid, composed of thick branches (from half a line to one line in * 
diameter), which intermingle much, and often coalesce. Calices almost equal in size, 
with thick walls, and having somewhat less than half a line in diameter. 
Found at Torquay in England, at Nehou and Brest in France, Palapaya and Ferrones 
in Spain, Eifel in Germany, and (according to M. Keyserling) at Uchta in Russia. 
1 Calamopora gothlandica (pars), Goldfuss, Petref. Germ., t. i, p. 78, pl. xxvi, figs. 3a and 3e, 1829. 
2 Calamopora alveolaris (pars), Goldfuss, ibid., p. 77, pl. xxvi, figs. la, le. 
8 Td. (pars.), Goldfuss, ibid., p. 77, pl. xxvi, fig. 10. 
4 Calamopora basaltica, Goldfuss, ibid., p. 78, pl. xxvi, figs. 4c, 4d. 
® Calamopora polymorpha, var. tuberosa, Goldfuss, ibid., p. 79, pl. xxvii, figs. 2b, 2c, 2d, 34, 3c. 
(Ccet. excl.) 
6 Lonsdale, Silur. Syst., p. 683, pl. xix, bis fig. 5, 1839. 
7 Milne Edwards and Jules Haime, Pol. Foss. des Terr. Palzeoz., p. 238, pl. xviii, fig. 1. 
8 Tab. xlix, fig. 2. 
9 Calamopora basaltica (pars), Goldfuss, Petref. Germ., t. i, p. 78, tab. xxvi, fig. 44, 1829. 
