. Report on tertiary plants of British Columbia collected by Lawrence M. Lambe in 1906, together with a discussion of previously recorded tertiary floras [microform]. Géologie stratigraphique; Paleobotany; Paléobotanique; Geology, Stratigraphic. 68 fragmeiiU of eone., were brought together trom a iiuniberot loc-alitie«. From the T'llamoi there \vu a scale; from tlic Trunquille river there wtw an iinprewioii which wuh inti prcted 88 repreteiiting the end view of a .one, but the raoterial had been so cnwhed <- ot glia|)e u to leud to nolhinjf very definite ; from Quilcheiia tliero were
. Report on tertiary plants of British Columbia collected by Lawrence M. Lambe in 1906, together with a discussion of previously recorded tertiary floras [microform]. Géologie stratigraphique; Paleobotany; Paléobotanique; Geology, Stratigraphic. 68 fragmeiiU of eone., were brought together trom a iiuniberot loc-alitie«. From the T'llamoi there \vu a scale; from tlic Trunquille river there wtw an iinprewioii which wuh inti prcted 88 repreteiiting the end view of a .one, but the raoterial had been so cnwhed <- ot glia|)e u to leud to nolhinjf very definite ; from Quilcheiia tliero were obuiiied wed-lil bclieg wliith appeare<l to i)e those of a pine devoid ot the wings ; and u number of simili seed were obuinod Irom the lIorseHy river. As well defined remains of pines, of rei-o nizable speeies, occur in the fame deposits, these bodies undoubtedly belong to them, bi the precise specific correlation cannot be ascertained. Pinus columhiana, Penh. Bib : \orth American Oymnospcrras, 1907. Woo<l and cones of Pinu.'. rolumbiawi were obtainetl from the Kettle river in 1!»05, I Dr. R A. Daly. There is no other record of the species. Pinus lardyana, Ileer. Bib : Fl. Tert. Helv. Til, 161, pi. , f. 2. Two friijtmenU of cones from Quilcheiia, in the collections of 1900, reprexent u species < pine which cannot be fully identified because the elements of size an corresiK)ndence with respect to the size, shajie and configuration of the scales This correi pondence is to be observed with respect to the figures given in volume 111, plate CXLVl figure â¢> of the Tertiary flora of Helvetia, but it does not apply to figure 3, nor to the con depicted in volume I, plate XX, figure 5, both of which appear to me to be wholly diitincl. l-' \'.l. J'innr II,...r. .\ fni»fiiit-iit uf null- fnmi t^iili-hi-na. \ V\, Pinus stcen-ilriipiana, Ileer. Hib: Fl Foss. Arct. I, pi. XXIV, 28-26, 185. In the Quilchena collection of 1906 there were several
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