. 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. 5fl 829. expresfeil have not been removed by theQnilchcna material which is attoj/^ether too imperfect for that purpose. Sir William Duwboh'i 8|iefimcn from Stanley park, Vanconvor, was dorived from beds of Ko<!ene age, but four other specimcng enuiiicraleil l)y Knowlton are from the Cretaceous. Eijidsetiim sp. Uib: Trans. R. S, C, IV., I881;, i


. 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. 5fl 829. expresfeil have not been removed by theQnilchcna material which is attoj/^ether too imperfect for that purpose. Sir William Duwboh'i 8|iefimcn from Stanley park, Vanconvor, was dorived from beds of Ko<!ene age, but four other specimcng enuiiicraleil l)y Knowlton are from the Cretaceous. Eijidsetiim sp. Uib: Trans. R. S, C, IV., I881;, iv, 19-34. A specimen of Kquiaetinn from the Lignite Tertiary of Porcupine creek am' Great valley ghowg ill one caHO frugniciitB ot stems and in another remains of roots and tubers. These are treate<l separately by Sir William Dawson altlioiigh he considers there is reason to think they may be the same specie*. H'luisetum nrcticum, Ileer. Uib: Trans. K. 8. C, VIII, 1902, iv, 46; IV, 1H86, iv, 22: Mioc Fl. and Kann. of Spitzbergoii, 1870, 31. In collections from the Eocene forieatioii of lied Deer river, obtained in 1898, there were a few 8|iecimenB of E'liiiaehim oiciiciim. What is also probably the same species was obtained from the Lignite Tertiary of Pnrcupino creek and Great valley and recorded by Sir William Dawson in 188G, but tlicre is no further reeurd of it in sulpso(iiient collections. K. iirrlieum is a typo eommoii to the Miocene of Spitzbergen, and its resemblance to E, iryominijenae, liesip, from the Tertiary of (ireeii Uiver stafiim, \Vyoming, should be 11. A limiit li ^liowiiiK f;il?.4Mlii'litt>iii\. Tntn- KlM-r. \ I Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Penhallow, D. P. (David Pearce), 1854-1910; Geological Survey of Canada. Ottawa : Govt. Print. Bureau


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