MF.SO/.OIC IM, ANIS FROM (Il IVA. 88 



M. Sha-ho-tzu, Ch'ang-tu, 

 Shéng-ching-Shêng-.' 



1. DIOONITES BRONGNIARTI (Mant). 



P]. XT. Fio-8. 1, 2. 



Dloonifci Jironr/nlarti Si:\vAnD, The Wenldeii Flora, p. 47. 

 Dioonitn Kokrl Vokoyama, Jurassic Plants, p. 44, pi. VU, tig. labe, 

 XIV. 14. 



This is the only fossil brought from the Sha-ho-tzu coal- 

 mine. It consists of several fragments, some belonging to the 

 apical portion (fig. 2) of a leaf, and some to the middle portion 

 (fig. 1) of the same. The segments are close together, long, 

 narrow, parallel-sided, either straight or very slightly curved 

 forward, attached to the upper surface of the rachis by the 

 whole base and more or less inclined forward, especially near 

 the apex of the le*if. Tlie apices of the segments are mostly 

 broken off, but judging from their form, they seem to have l)een 

 bluntly pointed. The most of the segments are about 3 mm. 

 l)road, pierced l>y 0-7 fine, equal, parallel veins. 



I formerly described a species of Diooniles found in the 

 Jurassic of Kaga and Echizen under the name of D. Kotœi 

 which Sewaed considers as probably identical with D. Brong- 

 niarti, an opinion to which I now quite agree. 



N. Ta-t*ai-shan, Ch'iian-yen-kou, 

 Shêng-ching-Shêng. ' 



1. PODOZAMITES LANCEOLATUS (Lindl. et Hutt.). 



PI. XI. Fig. 3. 

 Seven fragments of leaflets of Podozamites lanceolatus which 



-) &'^.^^ï^^ila\ii ('- l<il^ni. somh-west of T'ieh-linjrJ. 



