A monograph of the British fossil corals - kreidefossilien.de
A monograph of the British fossil corals - kreidefossilien.de
A monograph of the British fossil corals - kreidefossilien.de
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64 BRITISH FOSSIL CORALS.<br />
<strong>of</strong> unequal size towards <strong>the</strong> calicular edge. Calice almost circular, or somewhat oval aud<br />
shallow. Columella fascicular, well <strong>de</strong>veloped, not prominent at its apex, and terminated<br />
by ten or fifteen papillae <strong>of</strong> equal size. Sqita forming four complete cycla and six wellmarked,<br />
equally <strong>de</strong>veloped systems, in which, however, <strong>the</strong> secondary ones differ but little<br />
from those <strong>of</strong> <strong>the</strong> first cyclum. The septa are slightly exsert, closely set, unequal, and<br />
ra<strong>the</strong>r thicker outwards than towards <strong>the</strong> columella. Pali narrow and unequal; those<br />
corresponding to <strong>the</strong> tertiary septa broad and ra<strong>the</strong>r stout ; <strong>the</strong> o<strong>the</strong>rs, and most especially<br />
those corresponding to <strong>the</strong> primary septa, narrow and thinner. Height <strong>of</strong> <strong>the</strong> corallum,<br />
seven or eight lines ; diameter <strong>of</strong> <strong>the</strong> calice, almost seven lines.<br />
This species belongs to <strong>the</strong> first section <strong>of</strong> <strong>the</strong> genus Trochoeyathus {T. simjjlices), and<br />
diifers from T. impari-2Mrtitus^ and T. BeUh)(jlienanus by not having a fifth cyclum<br />
<strong>of</strong> septa ;<br />
its general form distinguishes it from T. mitratus,^ T. crassus, T. simjjlew, and<br />
T. costulatus, -which are all short, broad, and curved ; and from T. elongatm, T. Komnckii,<br />
and T. gracilis, which are much elongated, curved, and very narrow towards <strong>the</strong> basis.<br />
It<br />
appears to resemble most, especially by its general form, T. ciqnda^ which is also conical<br />
and straight, but this last-mentioned species differs from it by <strong>the</strong> thickness and strong<br />
granulations <strong>of</strong> <strong>the</strong> septa, and by <strong>the</strong> breadth <strong>of</strong> <strong>the</strong> basis.<br />
Trochocyatlms conulus appears to have been very wi<strong>de</strong>ly spread in <strong>the</strong> seas where <strong>the</strong><br />
Gault formations were <strong>de</strong>posited.<br />
The specimens which we most particularly studied were<br />
'<br />
See our Monograph <strong>of</strong> Turbinolidse, loc. cit., p. 30".<br />
- Since <strong>the</strong> publication <strong>of</strong> our Monograph <strong>of</strong> <strong>the</strong> Turbinoli<strong>de</strong>e (in 1848) we have recognised that <strong>the</strong><br />
<strong>fossil</strong>s from Tortona, which M. Michelotti <strong>de</strong>signates un<strong>de</strong>r <strong>the</strong> name <strong>of</strong> TurbinoUa pHcata, do not differ<br />
specifically from <strong>the</strong> specimens existing in <strong>the</strong> Poppelsdorf Museum un<strong>de</strong>r <strong>the</strong> name <strong>of</strong> Tiirliinolia mitrata,<br />
Goldfuss. As we already expected, <strong>the</strong> latter specific name must <strong>the</strong>refore be substituted for <strong>the</strong> one<br />
employed by M. Michelotti, and M. Michelin.<br />
' This new species, <strong>de</strong>signated un<strong>de</strong>r <strong>the</strong> name <strong>of</strong> TurbinoUa cujmla, by M. Alex. Rouault, (Bulletin<br />
<strong>de</strong> la Soc. Geol. <strong>de</strong> France, 2""' serie, vol. ix, p. 206, 1848), was found by that geologist at Bos d'Arros, in<br />
<strong>the</strong> <strong>de</strong>partment <strong>of</strong> <strong>the</strong> Lower Pyrennees, and does not appear to differ from a <strong>fossil</strong> which exists in <strong>the</strong><br />
collection <strong>of</strong> M. Nyst, and was found in <strong>the</strong> Eocene formation at Lacken, near Brussels. Ti-ochoctjathus<br />
cvimla belongs to <strong>the</strong> first section <strong>of</strong> our genus Trachocyathus, and presents <strong>the</strong> following characters :<br />
Corallum straight, or almost so, subturbinate, but short, and having a broad peduncle, but not remaining<br />
adherent in <strong>the</strong> adult state. Costca distinct from <strong>the</strong> basis, straight, unequally <strong>de</strong>veloped alternately,<br />
ra<strong>the</strong>r prominent, especially near <strong>the</strong> cahce, granulated and striated transversely ; rudimentary costse, that<br />
do not correspond to any septa, are seen in <strong>the</strong> intercostal furrows. Calice circular; fossula not <strong>de</strong>ep.<br />
Columella crispate, well <strong>de</strong>veloped. Septa forming three complete cycla, and in general a fourth incomplete<br />
cyclum in one half <strong>of</strong> three <strong>of</strong> <strong>the</strong> systems ; exsert, ra<strong>the</strong>r unequal, strong, and presenting on <strong>the</strong>ir<br />
lateral surfaces large prominent granulations, which are arranged in lines nearly parallel to <strong>the</strong> upper edge.<br />
Pali thick, strongly granulated, and unequal ; those corresponding to <strong>the</strong> tertiary septa <strong>the</strong> largest in <strong>the</strong><br />
half sj'steras where <strong>the</strong> septa <strong>of</strong> <strong>the</strong> fourth cyclum exist, and those corresponding to <strong>the</strong> secondary septa<br />
most <strong>de</strong>veloped in <strong>the</strong> o<strong>the</strong>r part <strong>of</strong> <strong>the</strong> calice. Height <strong>of</strong> <strong>the</strong> corallum, three lines ; diameter <strong>of</strong> <strong>the</strong> calice<br />
almost as much. By <strong>the</strong> strong granulations <strong>of</strong> <strong>the</strong> septa, and <strong>the</strong> breadth <strong>of</strong> its basis, this species tends to<br />
establish a transition between <strong>the</strong> genus TrocJiocyatJuis and <strong>the</strong> genus Paraeijathus.