686 Review of North American Paleontology. 
U. P. James has “Genus Agelacrinus Vanuxem, Agelacrinus 
holbrooki,” in Jour. Cincinnati Soc. Nat. Hist., Vol. X., No. 1, 
p. 25. 
George F. Kunz has “Jasperized and Agatized Wood from Ari- 
zona” in Trans. N. Y. Acad. Sci., Vol. VI., p. 165. 
L’ Abbé J. C. Laflamme has “Note sur le contact des formations 
paleozoiques et archéennes de la province de Quebec” (Lu le 28 
Mai, 1886) in Trans. Roy. Soc. Canada for 1886, Section IV. 
p. 43. 
Chas. Lapworth publishes “ Fossils from Kicking Horse Pass, 
Manitoba,” in Science, Vol. IX., No. 217, p. 230; also, “ Prelim- 
inary Report on Some Graptolites from the Lower Paleozoic Rocks 
on the South Side of the St. Lawrence from Cape Rosier to Tar- 
tigo River, from the North Shore of the Island of Orleans, one 
mile above Cape Rouge, and from the Cave Fields, Quebec,” in 
Trans. Roy. Soc. Canada for 1886, Section IV., p. 167. 
Joseph Leidy has “ Fossil Bones from Florida” in Proc. Acad. 
Nat. Sci. Phila., Part III., p. 309. 
A. T. Lilley publishes “A Revision of the Section of Chemung 
Rocks exposed in the Gulf Broad Gorge, at Le Roy, in Bradford 
Co., Pennsylvania,” in Proc. Amer. Phil. Soc., Vol. XXII, 
p- 291. 
A. P. Law has “Preliminary Report on an Exploration of Coun- 
try between Lake Winnipeg and Hudson Bay” in Part F. Annual 
Report, 1886, Geological and Natural History Survey of Canada, 
E 
£ Richard Lydekker has an article on “The Order Ungulata, Sub- 
order Proboscidea,” in Catalogue of the Fossil Mammalia in the 
British Museum (Natural History), p. 1. ; 
A. McCharles has “The Footsteps of Time in the Red River 
Valley, with Special Reference to the Salt Springs and Flammg 
Wells to be Found in it,” in the Hist. and Sci. Soc. of Manitoba 
Trans., No. 27, Season, 1886-7, p. 1; in Trans. Geol. Soc. Edin- 
burgh, Vol. V., Part II., p. 331, he has “Notes on the Geology of 
the Winnipeg District, Manitoba.” ee 
R. G. McConnel, in Part D, Annual Report, 1886, Geological 
and Natural History Survey of Canada, p. 1, has “ Report on m 
Geological Structure of a Portion of the Rocky Mountains, aooo 
panied by a Section measured near the 51st Parallel.” 
