X CONTENTS 



VII. PITYOXYLON 219-231; VIII. PKOTOPICE- 

 OXYLON 231-234; IX. WOODWORTHIA 234, 235; 

 X. ARAUCARIOPITYS 235, 236; XI. PROTO- 

 CEDROXYLOSr 236-238; XII. XENOXYLON 238- 

 242 ; XIII. ANOMALOXYLON 242, 243 ; XIV. THYL- 

 LOXYLON 243 ; XV. PLANOXYLON 244. 



CHAPTER XLV 

 CONIFERALES (continued). Pp. 245—301. 



PAGE 



Araucarineae ■ 245-277 



DAMMARITES, PROTODAMMARA 245-252 ; Conites 

 252-256; ARAUOARITES 256-270 ; ELATIDES 270- 

 274; PAGIOPHYLLUM 274-277. 

 Palaeozoic Conifers exhibiting certain features sug- 

 gestive OF Araucarian affinity but which cannot be 

 definitely assigned to that or to any other family 

 of coniferales on the evidence at present available ' 277-301 

 WALCHIA 277-282; SCHIZODENDRON {Tylodendron) 

 282-286 ; HAPALOXYLON 286, 287; GOMPHOSTRO- 

 BUS 287, 288 ; VOLTZIA 289-295 ; SWEDENBORGIA 

 295, 296; Strobilites 296; ULLMANNIA 296-299; 

 ALBERTIA 300, 301. 



CHAPTER XLVI 

 CONIFERALES (continued). Pp. 302—335. 



CUPBESSINEAE 302-335 



CUPRESSINOCLADUS 303, 304, 307-310; THUITES 

 305; CUPRESSITES 305-307; ATHROTAXITES 

 311-315; BRACHYPHYLLUM 315-322, 324-328; 

 BRACHYOXYLON 322-324; TAXODITES 328-331; 

 CUNNINGHAMIOSTROBUS 331, 332;MORICONIA 

 332, 333; CRYPTOMERITES 334, 335; CRYPTO- 

 MERIOPSIS 335. 



CHAPTER XL VII 



CONIFERALES (continued). Pp. 336—367. 



Callitrineae ._ 336-346 



CALLITRITES 337-342 ; FRENELOPSIS 342-346. 



Sequoiineae 346-365 



SEQUOIITES 349-351, 352-357 ; Conites 351, 352 ; GEI- 

 NITZIA 357-361 ; EUGEINITZIA 361, 362 ; PSEUDO- 

 GEINITZIA 362; SPHENOLEPIDIUM 363-365. 



Sciadopitineae 365-36 



SCIADOPITYTES 366, 367. 



