14 Triassic Echinoderms of Bakony. 
of the markings, which appear to be relatively, as well as absolutely, more delicate. 
In E. granulosus the sutures are crenelate; or, if the crenellae cannot be seen, 
that is due to the presence of a peripheral rim, which structure does not occur in 
any of the present specimens. From all other species of Encrinus or Entrochus 
that I can find described, and certainly from all named Triassic species, E. can- 
cellistriatus differs in the same points as do the striate trochitae of E. granulosus. 
The relatively large number of specimens, their occurence at two localities, the 
absence of the striate form of the true E. granulosus, and the structural features 
just mentioned prevent me from regarding the columnals as derived merely from 
dwarfed individuals of E. granulosus. It is however possible that they represent a 
small race of a species as yet undescribed and living at a later date. Thus, a frag- 
ment of Hallstaétter Kalk from Steinbergkogel, preserved in the Hofmuseum at Vienna, 
is full of columnals closely resembling those of the present species, though the largest 
attains a diameter of 4°7 mm. with a height of 1°8 mm. A similar but much larger 
form from the Hallstatter Kalk of Leisling near Goisern, and from the Karnische 
Stufe, zone of 7ropites subbullatus, from Rapoltstein near Hallem, Salzburg, is also 
in that Museum. 
Encrinus sp. 
(Plate I, fig. 23.) 
A single columnal from the Cassian of Cserhat is placed with this genus 
because of its general resemblance to certain Entrochi assigned to E. cassianus by 
Lause (1865), especially that represented in Mtnster (1841) pl. V, fig. 4 c, and to 
a less extent that in Lause (1865) pl. VIII a, fig. Sg. 
Side-faces convex, with, in addition, a well-marked ridge, at about half the height, 
slightly wavy in outline and a little irregular. Ridges on joint-face not clear, about 15, 
apparently short. 
Diameter at ridge 1°65 mm. Diameter at joint-face 1°3 mm. Height 1°2 mm. 
Encrinus sp. 
Two columnals from Muschelkalk of Felséérs, and Tamashegy near Balatonfiired 
are too ill preserved to be further determined. Their measurements in millimetres are: 
Diameter’}.- :) ena Ors 88 
Height 2° so. sk 2k ete LOS 45 
Diameter of lumen. . . 0O°5 
Entrochus silesiacus. 
(Plate I, figs. 24—25.) 
1835. «Entrochiten... vielleicht zum Lxcrinites Schlottheimiz gehérig>. F A. QueNsTEDT: Archiv 
f. Naturges., Jahrg. I, Bd. II, p. 228, pl. IV, fig. 3. 
1858. Extrochus silesiacus H. E. Bevrich: Abh. Akad. Wiss. Berlin, 1857, Phys. Kl. No. 1, p. 46. 
1870. Encrinus silesiacus (Beyx.). — C. F, RoeMeR: Geologie von Oberschlesien, pl. XI, fig. 9—10. 
History of the species. — Other references might be given, but I am not 
convinced that all the forms assigned to this species by other authors really belong to it. 
The specimen figured by Quenstept (1835) appears to have been in the 
collection of H. von Decuen, and its locality and horizon are given merely as 
