with 490']. No. ‘ZH,’ 'I‘Ill‘l tAMHHO-ttlllNWllilAN BEDS. ll
From Virluria Head in his wurk lu'rvinuslt‘ menlinnedv "l’ulzeuulu- logy at the (Inns s ml the Arrlu- Lands elr". lilln‘ridg. . cnvery nl' Mmdurea umgmi I‘m-Venn. which is an ordinary tilmxy tin-m
in the southerly Nnrlh American regions,
repnrts the dis-
'l'hv locality from which llw hulk nl' Suu- cullerlinnx ul' lushllh
5 Marie
in these regions helnug. ix Norman lilik‘h'yl’l' Island m l’rinei- Ba}: outside the unuth at the little northerly hranclL l 'anklin Pierce Bay The island is lnrmed nl limcsluue with the same N-N-VV
dip as the hells farther snulh, 'l'he l'ussi . which lie in a gi'ey~l)1'uvv|i
limestone \Vllit'll is mostly very (‘uInp-‘u‘l. hut in places more crystallin
were arrurdiug In Snnm’s «II: has gathered on the east or south-east of the island. althuugh nu quite precise luenlily can he given.
The lulhmiug terms have heeu identified:
Ant/102ml.
Hnlysiles caleimlalus vain gracilis HM In
In one single specimen we find portions of this coral, nut par-tim- Ia'ly well preserved. We can however see the comparatively rerlangular hull of the coral tubes. which are characteristir of this varier nl'
s
H. mtenulams L. ('alapaeaia cauudensis ItiLLlNus One colony at a regular rounded term. Greatest diameter it em. Stn’ptelasma vorm‘culmn HALL. Various small specimens occur, mostly less than 2 Cllt long.
Bryozoav
Bryozoaus must have been extremely runlmmi in the limestone. We find numerous sumewhat large pieces 7 unfortunately not in a very good state of pre er atiou 7 at" a Mt'sotrg/pa, which seems nun-h tn agree with M. discoidea Umen vain orimmlis BASS '
In addition [here is a small piece of a small ranntied form, with a thickness of 3~ mm. the structure of which can he studied well. and which agrees entirely with Callopora angulan’s ULRICH.
‘ I um inclined to believe that the form described by Lmitheol. Sum Cnnadu 1907) as a r rul under the uauw Labyrinlhites clu'lltmn" is very i-luwly related to this species.
