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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CORALS FROIM THE UPPER CHALK. 49<br />
We must also remark that, in a note just published, our able friend M. Alci<strong>de</strong><br />
d'Orbigny^ refers to <strong>the</strong> Caryoplnjllia<br />
or Parasmilia centralis as <strong>the</strong> type <strong>of</strong> a new genus,<br />
<strong>de</strong>signated un<strong>de</strong>r <strong>the</strong> name <strong>of</strong> Cyclosmilia, and characterised in <strong>the</strong> following terms<br />
" Cyclosmilia are Parasmilia, in which <strong>the</strong> loculi are but very little divi<strong>de</strong>d by dissepiments,<br />
<strong>the</strong> growth <strong>of</strong> <strong>the</strong> corallum is intermittent, <strong>the</strong> caHce circular instead <strong>of</strong> being oval, and<br />
<strong>the</strong> external costa? distant from each o<strong>the</strong>r." Now, with <strong>the</strong> exception <strong>of</strong> this last<br />
peculiarity, which is not even met with in P. ceniralis, all <strong>the</strong>se characters may be seen in<br />
every species belonging to our genus Parasmilia, and we <strong>the</strong>refore can find no reason for<br />
separating from it<br />
this new generic division.<br />
2. Parasmilia Mantelli. Tab. VHI, fig. 2, 2 a.<br />
We have as yet seen but one specimen <strong>of</strong> this species, which appears to be very distinct<br />
from all o<strong>the</strong>rs. Tt is a small corallum, nearly straight, adherent by a broad basis, regularly<br />
tm'binate, and not very tall ; but being in all probability susceptible <strong>of</strong> increasing much in<br />
height by progress <strong>of</strong> age, as is<br />
<strong>the</strong> case with <strong>the</strong> o<strong>the</strong>r species belonging to <strong>the</strong> same genus.<br />
The costce are narrow, sublamellar, closely set, distinct down to <strong>the</strong> basis <strong>of</strong> <strong>the</strong> corallum,<br />
very echinulate, and somewhat crispate. Those <strong>of</strong> <strong>the</strong> primary and secondary cycla are<br />
equally <strong>de</strong>veloped, and ra<strong>the</strong>r more prominent than <strong>the</strong> o<strong>the</strong>rs, especially towards <strong>the</strong> basis<br />
and <strong>the</strong> calicular luargin ; <strong>the</strong> tertiary ones also extend on <strong>the</strong> basal expansion <strong>of</strong> <strong>the</strong><br />
corallum, but are smaller ;<br />
and those <strong>of</strong> <strong>the</strong> fourth cyclum begin at a short distance above<br />
<strong>the</strong> basis, and are very narrow at <strong>the</strong>ir lower part.<br />
The intercostal furrows are broad, <strong>de</strong>ep,<br />
and divi<strong>de</strong>d by small transverse dissepiments, formed by rudiments <strong>of</strong> an exo<strong>the</strong>ca.<br />
Calice<br />
circular; fossula not <strong>de</strong>ep. Columella, as far as we can judge by <strong>the</strong> specimen here<br />
<strong>de</strong>scribed, very similar to that <strong>of</strong> P. centralis. Septa forming four complete cycla ; well<br />
<strong>de</strong>veloped, thin, straight, closely set, ra<strong>the</strong>r unequal, and presenting well-marked striae<br />
on <strong>the</strong>ir lateral surfaces. Height, seven or eight lines; diameter <strong>of</strong> <strong>the</strong> calice, nearly five lines.<br />
This <strong>fossil</strong> differs from <strong>the</strong> o<strong>the</strong>r species belonging to <strong>the</strong> same genus, and more<br />
especially from P. centralis and P. Fittoni, by its costse, which are equally prominent and<br />
subcrispate, whereas in <strong>the</strong> latter <strong>the</strong>y are smooth and never sublamellar. It resembles<br />
more closely P. Gravesiana, P. cylindrica, and P. elonyata ; but it differs from <strong>the</strong>m by <strong>the</strong><br />
strong granulations <strong>of</strong> <strong>the</strong> costse. In P. serpentina <strong>the</strong> basis is almost smooth, and <strong>the</strong><br />
septa do not form so many cycla.<br />
Parasmilia Mantelli was met with in <strong>the</strong> upper chalk at Bromley in Kent, by our<br />
friend Mr. J. S. Bowerbank.<br />
1 This paper, bearing <strong>the</strong> title <strong>of</strong> ' Note sur <strong>de</strong>s Polypiers Fossiles,' and published on tlie 1 0th <strong>of</strong><br />
October, 1 849, contains <strong>the</strong> exposition <strong>of</strong> <strong>the</strong> characters <strong>of</strong> a scries <strong>of</strong> new genera proposed by M. d'Orbio-nv.<br />
The author assigns to most <strong>of</strong> <strong>the</strong>se diyisions <strong>the</strong> date <strong>of</strong> 184 7, a period at which he appears to have adopted<br />
<strong>the</strong>m in <strong>the</strong> arrangement <strong>of</strong> his private collection ; but in referring to <strong>the</strong>m Jiere or elsewhere, we have<br />
consi<strong>de</strong>red it proper to quote <strong>the</strong> year <strong>of</strong> <strong>the</strong>ir publication, which is <strong>the</strong> only au<strong>the</strong>ntic date that could be<br />
ma<strong>de</strong> use <strong>of</strong> if any question <strong>of</strong> priority should arise concerning <strong>the</strong>m.