Hostname: page-component-5c6d5d7d68-xq9c7 Total loading time: 0 Render date: 2024-08-22T13:12:50.838Z Has data issue: false hasContentIssue false
  • English
  • Français

The Effect of Vegetation Heterogeneity on Short Stratigraphic Sequences

Published online by Cambridge University Press:  26 July 2017

Ralph E. Taggart
Ralph E. Taggart*
Affiliation:
Department of Botany and Plant Pathology, Department of Geological Sciences, Michigan State University, East Lansing, MI 48824
Get access

Extract

Barring the immense and growing literature on Quaternary pollen analysis, the vast majority of the work on the paleoecology of terrestrial systems has concentrated on the Neogene floras of the Pacific Northwest. Study of these floras began with the pioneering exploratory surveys in the last quarter of the 19th century and assumed essentially its modern form with the work of R.W. Chaney, initiated in the 1920, the detailed contributions of H.D. MacGinitie, the continuing productivity of D.I. Axelrod, and, most recently, J. Wolfe. Such a short listing necessarily leaves out the many contributions of patient floristic monographers for I wish to concentrate on floristic treatments that include a major paleoecological element.

Type
Research Article
Information
The Paleontological Society Special Publications , Volume 3: Methods and Applications of Plant Paleoecology , 1988 , pp. 147 - 171
Copyright
Copyright © 1987 Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Axelrod, D. I., 1964. The Miocene Trapper Creek flora of southern Idaho. University of California Publication in Geological Science 51. 180 pp.Google Scholar
Axelrod, D. I., 1966. A method for determining the altitudes of Tertiary floras. Paleobotanist 14:144–171.Google Scholar
Axelrod, D. I., 1968. Tertiary floras and topographic history of the Snake River Basin, Idaho. Bull. Geol. Soc. Amer. 79:713–734.Google Scholar
Axelrod, D. I., and Bailey, H. P., 1969. Paleotemperature analysis of Tertiary floras. Paleogeography, Paleoclimatology, Paleoecology 6:163–195.Google Scholar
Chaney, R. W., 1948. The bearing of the living Metasequoia on the problems of Tertiary paleobotany. Proceedings National Academy of Sciences 34:503–515.CrossRefGoogle ScholarPubMed
Chaney, R. W., 1951. A revision of the fossil Sequoia and Taxodium in western North America based on the recent discovery of Metasequoia. Transactions American Philosophical Society 40:171–263.CrossRefGoogle Scholar
Chaney, R. W., and Axelrod, D. I., 1959. Miocene floras of the Columbia Plateau. Publications Carnegie Institute. Washington 617. 237 pp.Google Scholar
Cross, A. T. and Taggart, R. E., 1982a. A Miocene Nelumbo-Trapa lake, Southwestern Idaho. Botanical Society of America. Miscellaneous Series Publication 162:57; Abs. Google Scholar
Cross, A. T., and Taggart, R. E., 1982b. Causes of short-term sequential changes in fossil plant assemblages: some considerations based on a Miocene flora of the northwest United States. Annals Missouri Botanical Garden 69:679–734.Google Scholar
Graham, A., 1965. The Sucker Creek and Trout Creek Miocene floras of southeastern Oregon. Kent State University Bulletin of Research Series IX, 53. Kent, Ohio. 147 pp.Google Scholar
Imbrie, J., and Imbrie, K. P., 1979. Ice ages. Enslow Publishers, Sort Hill, NJ. 224 pp.Google Scholar
MacGinitie, H. D., 1962. The Kilgore flora - a late Miocene flora from northern Nebraska. University of California Publications in Geological Sciences 35:67–158.Google Scholar
McLeroy, C. A., and Anderson, R. Y., 1966. Laminations of the Oligocene Florissant lake deposits, Colorado. Geological Society of America Bulletin 77: 605–618.CrossRefGoogle Scholar
Milankovitch, M., 1930. Mathematische Kilmalehre und der astronomische Theorie der Klimaschwankungen. Pp 1–176 In Koppen, W. and Geiger, R. (eds.). Handbuch der Klimatologie, I(A). Gebruder Borntraeger, Berlin.Google Scholar
Satchell, L.S., 1984. Patterns of disturbance and vegetation change in the Miocene Succor Creek flora (Oregon-Idaho). PhD Dissert. (Botany), Michigan State University, E. Lansing. 153 pp.Google Scholar
Shotwell, J.A., 1968. Miocene mammalian faunas of southeastern Oregon. Bulletin University of Oregon Museum of Natural History 14:1–67.Google Scholar
Smiley, C. J., and Rember, W. C., 1985. Composition of the Miocene Clarkia flora. in Smiley, C.J. (ed.). Late Cenozoic history of the Pacific Northwest. Interdisciplinary studies on the Clarkia fossil beds of northern Idaho. Pacific Division, American Association for the Advancement of Science, San Francisco. p.95–112.Google Scholar
Smith, H. V., 1941. A Miocene flora from Thorn Creek, Idaho. American Midland Naturalist 25:473–522.Google Scholar
Taggart, R. E., and Cross, A. T., 1974. History of vegetation and paleoecology of Upper Miocene Sucker Creek beds of eastern Oregon. Birbal Sahni Inst. (Lucknow) Special Publication 3:125–132.Google Scholar
Taggart, R. E., and Cross, A. T., 1980. Vegetation change in the Miocene Sucker Creek flora of Oregon and Idaho: a case study in paleosuccession. Pp. 185–210 In Dilcher, D. L. and Taylor, T. N. (eds.). Biostratigraphy of fossil plants. Dowden, Hutchinson, and Ross, Inc., Stroudsburg, PA.Google Scholar
Wolfe, J. A., 1971. Tertiary climatic fluctuations and methods of analysis of Tertiary floras. Paleogeography, Paleoclimatology, Paleoecology 9:27–57.Google Scholar
Wolfe, J. A., 1978. A paleobotanical interpretation of Tertiary climates in the northern hemisphere. American Scientist 66:694–703.Google Scholar
Wolfe, J. A., 1979. Temperature parameters of humid to mesic forests of eastern Asia and relations to forests of other regions in the Northern Hemisphere and Australasia. U.S. Geological Survey Professional Paper 1106. 37 pp.CrossRefGoogle Scholar