LIST OF PUBLICATIONS. 



247 



GiLMORE, Charles W. — Continued. 



trachodont reptile Ilypacro- 

 saurus In the Judith River 

 (Belly River) beds is an- 

 nounced. 



GiRTY, George H. A report on Upper 

 Paleozoic fossils collected in China 

 in 1903-04. 



Carnegie Insk of Wash- 

 ington, Publ. No. 

 54, Research in 

 China, 3, 1913, pp. 

 297-334, pis. 27-29. 

 In this paper a detailed de- 

 scription of the Upper Paleozoic 

 fossils collected by the Car- 

 negie Institution expedition Is 

 given. The faunas are com- 

 pared with previously described 

 Carboniferous faunas from east- 

 ern Asia, and correlations are 

 made with Russian and Amer- 

 ican sections. The conclusions 

 are that Upper Carboniferous is 

 undoubtedly represented and 

 constitutes the major portion of 

 the collection. Lower Carbon- 

 iferous and Permian may be 

 present, but the evidence is incon- 

 clusive. One fauna is given a 

 possible range from Upper 

 Silurian to Lower Carboniferous. 

 The fossils described are the 

 property of the U. S: National 

 Museum. 



Hat, Oliver P. The extinct bisons of 

 North America ; with description of 

 one new species, Bison regius. 



Proc. U. S. Nat. Mus., 

 46, No. 2021, Dec. 6, 

 1913, pp. 161-200, 

 pis. 8-19, figs. 1-10. 

 Describes one new species and 

 discusses the American extinct 

 species of Bison, and also for 

 comparison the European species 

 B. priscus. The article contains 

 several valuable tables of com- 

 parative measurements and a 

 synopsis of the characters of 

 North American bisons. 



Camels of the fossil genus 



Camelops. 



Proc. U. 8. Nat. Mus., 

 46, No. 2025, Dec. 

 6, 1913, pp. 267- 

 277, pis. 25, 26. 1 



fig. 

 Reviews and discusses the 

 characters of the American Ple- 

 istocene camels variously re- 

 ferred to the genus Camelops. 

 Concludes that C. kansanns,' C. 

 hesternus, and C. huerfoncnsis 

 are distinct species ; that it is 



Hay, Oliver P. — Continued. 



not at present possible to de- 

 cide the status of Megaloinenjw 

 niobrarensis Leidy ; and accepts 

 the following species of Came- 

 lops as valid : C. kansanns, C. 

 calif ornicus, C. hesternus, C. 

 vitakerianus, O. niobrarensis,, C. 

 macrocephalus, and O. huerfan- 

 ensls. 



HuENE, Friedeich V. tJber die Zwei- 

 stammigkeit der Dinosaurier, mit 

 Beitragen zur Kenntnis einiger 



Schadel. 



Neues Jahrb. filr Min., 



Geol., und Pal., 



Bellage - Band 37, 



1914, pp. 577-589, 



pis. 7-12. 



Discusses the evidence as 



shown by the- skulls for the 



separation of the order Dino- 



sauria into the two suborders 



Saurischia and Ornithischia. 



The article is based in part on 



specimens belonging to the U. S. 



National Museum, some of which 



are figured. 



KiBK, Edwin. Notes on the fossil cri- 

 noid genus Homocriniis Hall. 



Proc. U. S. Nat. Mus., 

 46, No. 2038, Feb. 14, 

 1914, pp. 473-483, 

 pi. 42. 

 A study of the type species of 

 Eomocrinus, H. parvus Hall, 

 led to the discovery that the 

 genus is structurally quite dif- 

 ferent from what has been sup- 

 posed. In the present paper 

 Homocrinus is redefined, and a 

 new genus, Lasiocrinits, erected 

 for the reception of such forms 

 as Eomocrinus scopwrius Hall, 

 which has been chosen as the 

 type of the new genus. A new 

 family, Homocrinidifi, is pro- 

 posed. The material upon 

 which the studies were based is 

 in the Springer collection, de- 

 posited in the U. S. National 

 Museum. 



Knowlton, F. H. The Jurassic flora 

 of Cape Lisburne, Alaska. 



Prof. Paper, U. S. Oeol. 



8urv., 85-D, Jan. 28, 



1914, pp. 39-64, pis. 



5-8. 



The Jurassic section of Cape 



Lisburne, to which the name 



Corwin formation has been 



given, reaches the thickness of 



over 15,000 feet, fco far as at 



present known, the fossil 



flora is uniformly distributed 



