CALCAREA. 47 



basal ray, the paired rays arc .seen to Iw folded to one side ; the fold appears in some 

 cases to occur sharply ncnr the IMI.SC of the rays, which arc otherwise straight ; in other 

 OMBn the fold is gnulual, the rays being curved for the greater part of their length. 

 The apical ray springs from the junction of the facial rays on the side to which they 

 arc folded, but is immediately bent down nearly into line with the baaa! ray. Viewed 

 from the side the apical ray appears as a continuation of the Imsal ray, with a sharp 

 "set-over" at the junction. The amount of the set-over varies widely (see Streptocomut 

 australta and Meyapogon crucif(rus). The axis of the apical ray is usually slightly 

 inclined to the axis of the basal ray, sloping towards the side to which the paired rays 

 are folded. In facial view the chiactine does not differ much from the ordinary 

 quadriradiate, since the apical rays of the latter are usually curved orally, but in side 

 view the difference is wide. 



The ordinary position of quadriradiates in calcareous sponges is tangential to the 

 gastral surface, with the lsal ray downwards and the apical ray projecting into the 

 gastral cavity, so that the paired rays lie circumfcrcntially embracing the gastral 

 cavity. In Amphoriscu* and Syculmis there are quadriradiates which lie tangent ially 

 to the gastral surface with the apical ray pointing radially outwards, and in all the 

 Amphoricidat there are quadriradiates which lie tangentially to the dermal surface with 

 the apical ray pointing radially inwards. The chiactines lie in a plane perpendicular 

 to all these positions. Their l>asal ray is directed radially outwards, the paired rays 

 lie in the gastral cortex and the apical ray poiutu radially inwards and projects into 

 the gastral cavity. The plane of the facial rays is therefore perpendicular to the 

 gastral and dermal surfaces. The position of the paired rays is no longer fixed ; they 

 may lie circumferentially as l>efore, but they may turn round the axes of the Itasal ray 

 to any extent without coming out of the gastral cortex, and in fact they are found 

 lying in all positions between circumferential and longitudinal. 



The relation between the chiactines and the ordinary quadriradiates is an 

 interesting problem. All the nine new species containing chiactincs have ordinary 

 quadriradiates lying taugcntially round the oscule, and also lining the whole oscular 

 collar, if any. In six * of the new species the ordinary quadriradiates cease 

 entirely at the base of the collar and are replaced by the chiactines which form 

 the body skeleton. At the junction between the oscular collar and the body-wall 

 there is a short space in which quadriradiate spicules are found in every intermediate 

 position between tangential and centrifugal. This fact suggests most forcibly that the 

 spicules turn round. The top of the body appears to be the most recently developed, 

 and the spicules formed in the oscular collar might ! supposed to ! turned round 

 by the development of flagellated chambers under their basal rays. A very similar 

 tipping up of dermal triradiates, due to the growth under them of the flagellated 

 chambers, occurs at the base of the oscular collar in Tenthrenodet antarcticu*. There is 



In three of the new specie* the ordinary qnadriradiates in the oscular collar continue throughout the whole 

 gutral cavity in conjunction with the chiactines in the body. 



VOL. IT. 2 O 



