CORALS OF THE UPPER CHALK. 47 Family ASTREID^ (p. xxiii). Tribe EUSMILIN^ (p. xxiii). 1. Genus Parasmilia (p. xxiv). 1. Parasmilia centralis. Tab. VHI, figs. 1, la, 16, Ic. Ma<strong>de</strong>eporite, Parkinson, Organ. Remains <strong>of</strong>
48 BRITISH FOSSIL CORALS. very slightly flexuous, and presenting laterally a few large granulations. Lissephnents simple, almost horizontal, and few in number ; about three from <strong>the</strong> top to <strong>the</strong> bottom <strong>of</strong> each principal septum, as may be seen by means <strong>of</strong> a vertical section. Height varying from one to two inches ; diameter <strong>of</strong> <strong>the</strong> calice, four lines ; <strong>de</strong>pth <strong>of</strong> <strong>the</strong> fossula, two lines. The genus Parasmilia, circumscribed within <strong>the</strong> limits assigned to it in <strong>the</strong> Introduction to this Monograph, only contains seven species, all <strong>of</strong> which belong exclusively to <strong>the</strong> upper beds <strong>of</strong> <strong>the</strong> Chalk Formations. Three <strong>of</strong> <strong>the</strong>m (P. centralis, P. Gravesiana, and P. ehngatd) have already been <strong>de</strong>scribed in our Monograph <strong>of</strong> <strong>the</strong> Astreidse,^ and <strong>the</strong> four o<strong>the</strong>rs (P. MantelUi, P. Fittonii, P. cylindrica, and P. serpentina) will be ma<strong>de</strong> known in <strong>the</strong> present work. They all differ but little from each o<strong>the</strong>r, and in or<strong>de</strong>r to recognise <strong>the</strong>m, it is necessary that <strong>the</strong>y should be compared toge<strong>the</strong>r \d\\\ attention. P. centralis, which may be consi<strong>de</strong>red as <strong>the</strong> type <strong>of</strong> this small generic group, differs from P. Gravesiana, P. elongata, P. cylindrica, and P. MantelUi, by its costse being always straight, ra<strong>the</strong>r thick and never sub-lamellous, and ra<strong>the</strong>r flexuous, as in <strong>the</strong> four last-mentioned species ; it is also to be remarked, that its costae are ra<strong>the</strong>r more prominent near <strong>the</strong> basis than higher up, whereas <strong>the</strong> contrary is seen in <strong>the</strong> P. Gravesiana, and that <strong>the</strong> loculi are never subdivi<strong>de</strong>d by small dissepiments, as is <strong>the</strong> case in P. elongata, P. cylindrica, and P. MantelUi. P. serpentina, which bears more resemblance to it, is characterised by <strong>the</strong> septa forming only three cycla, and <strong>the</strong> costae being very <strong>de</strong>licate, and ra<strong>the</strong>r indistinct towards <strong>the</strong> basis. But it is with P. Fittonii that P. centralis is most closely allied ; <strong>the</strong> former, however, is <strong>of</strong> a thicker form, its tertiary costse are more <strong>de</strong>veloped and more <strong>de</strong>licately granulated, and its columella is much larger, and terminated by a sub-papillose surface. The specimens <strong>of</strong> P. centralis which we had <strong>the</strong> opportunity <strong>of</strong> examining were found in <strong>the</strong> Upper Chalk at Northfleet, near Gravesend, and at Norwich. Mr. Phillips mentions <strong>the</strong> existence <strong>of</strong> <strong>the</strong> same <strong>fossil</strong> at Dane's Dike;^ and Dr. Mantell has met with it at Brighton, Lewes/ Steyning, and Heytesbury.* Mr. Graves also allu<strong>de</strong>s to it as being found in <strong>the</strong> Challc Formation <strong>of</strong> <strong>the</strong> Parisian basin at Beauvais / but we have much reason to think that <strong>the</strong> species observed by that geologist is not <strong>the</strong> one here <strong>de</strong>scribed, and must be referred to our P. Gravesiana. M. Roemer and o<strong>the</strong>r authors equally apply <strong>the</strong> name <strong>of</strong> C. centralis^ to a <strong>fossil</strong> found in <strong>the</strong> north-west <strong>of</strong> Germany, but we have not been able as yet to verify <strong>the</strong> propriety <strong>of</strong> this <strong>de</strong>termination, not having seen any <strong>of</strong> <strong>the</strong> specimens discovered in that part <strong>of</strong> <strong>the</strong> Continent. ^ The species <strong>de</strong>scribed in that work un<strong>de</strong>r <strong>the</strong> names <strong>of</strong> Parasmilia pocuhim, P. Faitjasii, and P. punctata, must now be referred to our genus Coelosmilia, which is characterised by <strong>the</strong> entire absence <strong>of</strong> <strong>the</strong> cohimella. - Op. cit., parti, p. 119. ^ lUygt^ ^f tj^g Geol. <strong>of</strong> Sussex, p. ICO. * Geol. Trans., 2d series, vol. iii, p. 204, ^ Geogn. <strong>de</strong> I'Oise, p. 701. 8 Versteinerungen <strong>de</strong>s Nord<strong>de</strong>utschen Krei<strong>de</strong>birges, p. 26.