Conifer Dominants in the Middle Tertiary of the John Day Basin, Oregon

Authors

  • Ralph W. Chaney Professor of Palaeontology, University of California, and Research Associate, Carnegie Institution of Washington

DOI:

https://doi.org/10.54991/jop.1952.377

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References

BRAUN. E. LUCY (1942). Forests of the Cumberland Mountains. Ecological Monographs. 12: 413-447.

CHANEY, RALPH W. (1924). Quantitative Studies of the Bridge Creek Flora. Am. Jour. Sci. 8: 127-144.

Idem(1925). Comparative Study of the Bridge Creek Flora and the Modern Redwood Forest. Carnegie Inst. Wash. Publ. 349: 1-22.

Idem (1927).Geology and Paleontology of the Crooked River Basin, with Special Reference to the Bridge Creek Flora. Ibid. 346:45-138.

Idem (1938). Ancient Forests of Oregon: A Study of Earth History in Western America. Ibid. 501: 631-648.

Idem (1947).Tertiary Centers and Migration Routes. Ecol. Monographs. 17 (2): 139-148.

Idem (1948). The Bearing of the Living Metasequia on Problems of Tertiary Paleobotany. Nat. Acad. Sci. 34(11): 503-515.

Idem (1948). Pliocene Flora from the Rattlesnake formation of Oregon. Bull. Geol. Soc. Am. 59: 1367.

Idem (1949). Evolutionary Trends in the Angiosperms. Genetics, Paleontology, and Evolution. 190-201.

Idem (1951). Revision of Fossil Sequoia and Taxodium in Western North America Based on the Recent Discovery of Metasequoia.Trans. Am. Phil. Soc. 40:169-263.

CHENG, W.C. (1939). Les Forets du Se-tchouan et du Si-kang oriental. Travaux du Laboratoire Forestier de Toulouse. 1(2): 1-212.

Idem (1949). Forest Communities. Unpublished manuscript.

CHU, KWEI-LING & WILLIAM S. COOPER (1950). An Ecological Reconnaissance in the Native Home of Metasequoia glyptostroboides. Ecology.

:260-278.

FLORIN, RUDOLF (1922). Zur alttertiaren Flora der sudlichen Mandschurei. Geol. Surv. China. 1 (1): 1-47.

Heer, O. (1855). Tertiare flora der Schweiz. l. Winterthur.

HOLLICK, ARTHUR (1936). The Tertiary Floras of Alaska. U.S. Geol. Surv. Prof. Paper 182: 1-175.

HU, HSEN-HSU & WAN-CHUN CHENG (1948). On the New Family Metasequoiaceae and on Metasequoia Glyptostroboides, a Living Species of the Genus Metasequoia Found in Szechuan and Hupeh. Bull. Fan. Mem. Inst. Of Biol. 1(2). 153-161.

KNOWLTON, F. H. (1898). The Fossil Plants of the Payette Formation. U.S. Geol. Survey, 18th Ann. Rept.: 721-736.

Idem (1926). Flora of the Latah Formation of Spokane, Washington, and Coeur D’Alene, Idaho. U.S. Geol. Surv. Prof. Paper 140: 17-82.

KRYSHTOFOVICH, A.N. (1929). Evolution of the Tertiary Flora in Asia. New Phytologist. 28(4): 303-312.

LAMOTTE, ROBERT SMITH (1936). Middle Cenozoic Floras of Western North America. Carn. Inst. Wash. Publ. 455: 29-148.

MACGINITIE, HARRY D. (1933). The Trout Creek Flora of Southeastern Oregon. Ibid. 416: 21-68.

MIKI, S. (1941). On the Change of Flora in Eastern Asia since Tertiary Period (I). The Clay or Lignite Beds Flora in Japan with Special Reference to the Pinus trifolia Beds in Central Hondo. Jap. Jour. Of Bot. 11: 237-303.

OLIVER, ELIZABETH (1934). A Miocene Flora from the Blue Mountains, Oregon. Carn. Inst. Wash. Publ. 455: 1-27.

STEBBINS, G.L. JR. (1948). The Chromosomes and Relationships of Metasequoia and Sequoia. Sci. 108: 95-98.

WILLIAMS, HOWEL (1948). The Ancient Volcanoes of Oregon. Ore. St. Syst. Of Higher Educ.: 1-64.

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Published

1952-12-31

How to Cite

Chaney, R. W. (1952). Conifer Dominants in the Middle Tertiary of the John Day Basin, Oregon. Journal of Palaeosciences, 1, 105–114. https://doi.org/10.54991/jop.1952.377

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Short Articles