134 



TITANOTHEBES OF ANCIENT WYOMING, DAKOTA, AND NEBRASKA 



Dawkins, W. Boyd. 



1880.1. The classification of the Tertiary period by means 

 of the Ivlammalia: Geol. Soc. London Quart. 

 Jour., 1880, pp. 379-405. 



Tertiary and Quaternary horizons and faunas of Great 

 Britain, France, and Italy correlatRd. 



Deperet, Charles. 



1893.1. Note sur la succession stratigraphique des faunes 

 de mammifcres pliocenes d' Europe et du Pla- 

 teau central en particulier: Soc. g<Sol. France 

 Bull., 3d ser., vol. 21, pp. 524-540, 1893. 

 1906.1. L'evolution des mammiferes tertiaires, importance 

 des migrations, epoque miocene: Compt. Rend., 

 vol. 143, No. 26, pp. 1120-1123, 1906. The 

 evolution of Tertiary mammals and the impor- 

 tance of their migrations (translation) : Am. 

 Naturalist, vol. 42, pp. 109-114, 166-170, 

 303-307. 



DOLLO, Loui.?. 



1909.1. The fossil vertebrates of Belgium [Correlation 

 Bull. No. 2] (translation by W. D. Matthew) : 

 New York Acad. Sci. Annals, vol. 19, No. 4, 

 pt. 1, pp. 99-119, pis. 4-10, July 31, 1909. 



DouGL.ASs, Earl. 



1S99.1. The Neocene lake beds of western Montana and 

 descriptions of some new vertebrates from the 

 Loup Fork: Montana LTniv. thesis, 27 pp., 

 4 pis., June, 1899. 



Geology, faunas, and correlation of White River, "Deep 

 River," and "Madison Valley." "Loup Fork" horizons in 

 Montana. Systematic descriptions of certain fossil camels, etc- 



1902.1. Fossil Mammalia of the White River beds of 



Montana: Am. Philos. Soc. Trans., new ser., 

 vol. 20, pp. 227-278, pi. 9, 1902. 



"Pipestone beds," "Toston beds," "Blaclitail Deer Creelc 

 beds." Geology and faunas; new genera and species of mam- 

 mals. 



1902.2. A Cretaceous and lower Tertiary section in south- 



central Montana: Am. Philos. Soc. Proc, vol. 

 41, No. 170, pp. 207-224, pi. 29, April, 1902. 



Sketch of the Jurassic and Cretaceous deposits. Probable 

 relations of the "Laramie" and overlying beds. Fossil mam. 

 mals of the Fort Union beds. Describes the Fort Union beds 

 of Montana; considers them as of practically the same age as 

 the Torrejon Tertiary. Places Puerco as Upper Cretaceous- 



1902.3. The discovery of Torrejon mammals in Montana: 



Science, new ser., vol. 15, No. 372, pp. 272-273, 

 Feb. 14, 1902. 



First record of mammals from Fort Union beds of Crazy 

 Mountains region. 



1903.1. New vertebrates from the Montana Tertiary: 

 Carnegie Mus. Annals, vol. 2, No. 2, pp. 

 145-199, pi. 2, 37 figs., November, 1903. 



"Sage Greek" (Eocene?), White River deposits, "Fort 

 'Logan beds" (upper Oligocene), "Deep" and "Flint Creek" 

 beds. New mammals described. 



1909.1. Preliminary descriptions of some new titanotheres 

 from the Uinta deposits: Carnegie Mus. Annals, 

 vol. 6, No. 2, pp. 304-313, pis. 13-15, 8 figs., 

 August, 1909. 

 Describes new faunas from liorizon B. 



Dow, John M. 



1867.1. Extracts from letters relating to Tapirus bairdi 

 (read by P. L. Sclater) : Zool. Soc. London Proc, 

 1867, p. 241, 1867. 



Earle, Charles. 



1895.1. See Osborn, Henry Fairfield, 1895.95. 



Emmons, Samuel Franklin. 



1907.1. Uinta Mountains: Geol. Soc. America Bull., vol. 

 17, pp. 287-302, pi. 24, 2 figs., July 13, 1907. 



Endlich, Frederic Miller. 



1877.1. Report on the San Juan region: U. S. Geol. and 

 Geog. Survey Terr. Ninth Ann. Rept., pp. 176- 

 191, 1877. 



Tertiary (p. 189). Puerco beds of Animas Valley, southern 

 Colorado (1,000 to 1,200 feet), are considered the basal member 

 of the Wasatch. 



1879.1. Report on the geology of the Sweetwater district: 

 U. S. Geol. and Geog. Survey Terr. Eleventh 

 Ann. Rept., pp. 5-158, 1879. ' 



Refers to the lower Bridger exposed in the northern part o! 

 the basin, Big Sandy^Creek, etc. (p. 132). Considers a portion 

 of the "Wasatch" of Beaver Creek, Wyo., as parallelwith the 

 Puerco marls. 

 Filhol, Henri. 



1885.1. Observations sur le memoire de M. Cope intitul(5 

 "Relations des horizons * * * d'animaux 

 vertebres fossiles en Europe et en Amerique": 

 Annales sci. g6ol., vol. 17, art. 2, pp. 1-18, pi. 

 6, 1885. 



FiNLAY, George Irving. 



1916.1. U. S. Geol. Survey Geol. Atlas, Colorado Springs 

 folio (No. 203), 17 pp., 3 maps. 

 Laramie, Dawson, and Denver of Colorado; flora, fauna. 



Fisher, Cassius Asa. 



1906.1. Geology and water resources of the Big Horn 

 Basin, Wyo.: U. S. Geol. Survey Prof. Paper 53, 

 72 pp., 16 pis., 1906. 



Discusses briefly the character, thickness, and distribution 

 of the Wasatch formation (p. 33) . 



Fraas, Eberhard. 



1901.1. On the aqueous vs. eolian deposition of the White 

 River Oligocene of South Dakota (translation 

 by H. F. Osborn): Science, new ser., vol. 14, 

 No. 345, pp. 210-212, Aug. 9, 1901. 



" Titanotherlum beds" formed by river and flood-pli.in 

 deposits exposed during dry season. Middle " Oreodon beds " 

 deposited by a shallow lake with dissolved materials of varying 

 concentration (cf. banded layers). Upper "Oreodon beds" 

 formed by eolian loess. 



Gardner, James Heney". 



1910.1. The Puerco and Torrejon formations of the 

 Nacimiento group: Jour. Geology, vol. 18, 

 pp. 702-741, 1 pi., 9 figs., 1910. 



Gives historical review. Topography, structure, and physi- 

 ographic record of the Puerco-Torrejon district described. 

 Considers that an unconformity exists between the two for- 

 mations, to which the group name Nacimiento is given. 



Gidley, James Williams. 



1904.1. See Matthew, William Diller, 1904.1. 



1917.1. [The 1910 collection near the Davis ranch, Powder 

 River valley, Wyo.] In Wegemann, C. H., 

 Wasatch fossils in so-called Fort Union beds of 

 the Powder River basin, Wyo., and their bear- 

 ing on the stratigraphy of the region: U. S. 

 Geol. Survey Prof. Paper 108, p. 59, 1917. 



Gilbert, Grove Karl. 



1898.1. The underground waters of the Arkansas Valley 

 in eastern Colorado: U. S. Geol. Survey 

 Seventeenth Ann. Rept., pt. 2, pp. 553-601, 

 pis. 56-68, figs. 45-49, 1896. 



Rocky Mountain deposits may be of fluviatile and not of 

 lacustrine origin. 



