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Age and origin of subalpine forest zone

Published online by Cambridge University Press:  08 April 2016

Daniel I. Axelrod
Daniel I. Axelrod*
Affiliation:
Department of Botany, University of California, Davis, California 95616
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Abstract

Genera of montane conifers first appeared in the fossil record in large numbers in the Middle Eocene (47-45 Ma) as widespread volcanism in the Cordilleran region provided scattered, cold upland tracts suited for them. Higher subalpine environments, generally above 2,000 m, probably were confined then to upper slopes of scattered strato-volcanos and basement highs covered with thick pyroclastic deposits. As relief increased in the middle Tertiary, and especially during the Pliocene-Quaternary, the area suited for a subalpine forest zone increased significantly, enabling montane conifers to spread into that higher, colder environment and form a new major forest zone. During glaciations the subalpine zone was much larger and probably from 900-1,000 m lower than at present. Spreading post-glacial warmth and drought account for its retreat to higher levels and for the discontinuous distribution of the forest and its species today. Recency of the subalpine adaptive zone is implied also by the close relations of its varieties and subspecies of herbaceous perennials, a few annuals, and pines to those in vegetation zones below it.

Type
Research Article
Information
Paleobiology , Volume 16 , Issue 3 , Summer 1990 , pp. 360 - 369
Copyright
Copyright © The Paleontological Society 

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References

Literature Cited

Alvin, K. L. 1960. Further conifers from the Wealden Formation of Belgium. Memoirs Institute Royal Society Natural Belgium 146:1–39.Google Scholar
Armstrong, R. L. 1978. Cenozoic igneous history of the U.S. Cordilleras from Lat. 42° to 49°N. Geological Society of America Memoir 152:265–282.Google Scholar
Axelrod, D. I. 1944a. The Oakdale flora. Carnegie Institution of Washington Publication 553:147–165.Google Scholar
Axelrod, D. I. 1944b. The Pliocene sequence in central California. Carnegie Institution of Washington Publication 553:207–224.Google Scholar
Axelrod, D. I. 1944c. The Alvord Creek flora. Carnegie Institution of Washington Publication 553:225–262.Google Scholar
Axelrod, D. I. 1956. Mio-Pliocene floras from west-central Nevada. University of California Publications in Geological Sciences 33.Google Scholar
Axelrod, D. I. 1957a. Late Tertiary floras and the Sierra Nevadan uplift. Geological Society of America Bulletin 68:19–46.Google Scholar
Axelrod, D. I. 1957b. Paleoclimate as a measure of isostasy. American Journal of Science 255:690–696.Google Scholar
Axelrod, D. I. 1958. The Pliocene Verdi flora of western Nevada. University of California Publications in Geological Sciences 34:91–160.Google Scholar
Axelrod, D. I. 1962. A Pliocene Sequoiadendron forest from western Nevada. University of California Publications in Geological Sciences 39:195–268.Google Scholar
Axelrod, D. I. 1965. A method for determining the altitudes of Tertiary floras. The Paleobotanist 14:144–171.Google Scholar
Axelrod, D. I. 1968. Tertiary floras and topographic history of the Snake River Basin, Idaho. Geological Society of America Bulletin 79:713–734.Google Scholar
Axelrod, D. I. 1976a. History of the conifer forests, California and Nevada. University of California Publications in Botany 70.Google Scholar
Axelrod, D. I. 1976b. Evolution of the Santa Lucia fir (Abies bracteata) ecosystem. Annals of the Missouri Botanical Garden 63:24–41.Google Scholar
Axelrod, D. I. 1980. The Mt. Reba flora from Alpine County. University of California Publications in Geological Sciences 121:13–74.Google Scholar
Axelrod, D. I. 1981. Altitudes of Tertiary forests estimated from paleotemperature. Proceedings of Symposium on Qinghai-Xizang (Tibet) Plateau (Beijing, China). Geological and Ecological Studies of Qinghai-Xizang Plateau. Vol. 1. Geology, Geological History and Origin of Qinghai-Xizang Plateau. Science Press, Beijing, and Gordon and Breach Science Publishers, Inc.; New York.Google Scholar
Axelrod, D. I. 1985. Miocene floras from the Middlegate Basin, west-central Nevada. University of California Publications in Geological Sciences 129.Google Scholar
Axelrod, D. I. 1986. Cenozoic history of some western pines. Annals of the Missouri Botanical Garden 73:565–641.CrossRefGoogle Scholar
Axelrod, D. I. 1988. An interpretation of high montane conifers in western Tertiary floras. Paleobiology 14:301–306.Google Scholar
Axelrod, D. I. 1990a. Environment of the Middle Eocene (45 Ma) Thunder Mountain flora, Idaho. National Geographic Research 6(3), in press.Google Scholar
Axelrod, D. I. 1990b. The Miocene Pyramid flora, western Nevada. University of California Publications in Geological Sciences.Google Scholar
Bailey, H. P. 1960. A method of determining the warmth and temperateness of climate. Geografisker Annaler 42:1–16.Google Scholar
Bailey, H. P. 1964. Toward a unified concept of the temperate climate. The Geographical Review 54:516–545.Google Scholar
Billings, W. D. 1974. Adaptations and origins of alpine plants. Arctic and Alpine Research 6:129–142.CrossRefGoogle Scholar
Billings, W. 1979. Alpine ecosystems of western North America. Pp. 6–21. In Johnson, D. A. (ed.), Special Management Needs of Alpine Ecosystems. Society for Range Management; Denver, Colorado.Google Scholar
Billings, W. 1988. Alpine vegetation. Pp. 391–420. In Barbour, M. G., and Billings, W. D. (eds.), North American Terrestrial Vegetation. Cambridge University Press; New York.Google Scholar
Brown, R. W. 1937. Additions to some fossil floras of the western United States. U.S. Geological Survey Professional Paper 186-J:163–206.Google Scholar
Cater, F. W., Pickney, D. M., Hamilton, W. B., Parker, R. L., Weldin, R. D., Close, T. J., and Zilka, N. T. 1973. Mineral deposits of the Idaho Primitive Area and vicinity, Idaho, with a section on the Thunder Mountain district by B. F. Leonard, and a section on aeromagnetic interpretation by W. E. Davis. U.S. Geological Survey Bulletin 1304.Google Scholar
Chabot, B. F., and Billings, W. D. 1972. Origins and ecology of the Sierran alpine flora and vegetation. Ecological Monographs 42:163–199.Google Scholar
Christiansen, R. L., and Lipman, P. W. 1972. Cenozoic volcanism and plate-tectonic evolution of the western United States. II. Philosophical Transactions of the Royal Society of London A 271:249–284.Google Scholar
Clements, F. E. 1920. Plant indicators: the relation of plant communities to process and practice. Carnegie Institution of Washington Publication 290.Google Scholar
Coney, P. J. 1978. Mesozoic-Cenozoic Cordilleran Plate tectonics. Geological Society of America Memoir 152:33–50.Google Scholar
Coney, P. J. 1983. The plate tectonic setting of Cordilleran deserts. Pp. 81–97. In Wells, S. G., and Haragan, D. R. (eds.), Origin and Evolution of Cordilleran Deserts. University of New Mexico Press; Albuquerque, New Mexico.Google Scholar
Epis, R. C., and Chapin, C. E. 1975. Geomorphic and tectonic implications of the post-Laramide, Late Eocene erosion surface in the southern Rocky Mountains. Geological Society of America Memoir 144:45–74.Google Scholar
Fields, P. F. 1983. A review of the Miocene stratigraphy of southwestern Idaho, with emphasis on the Payette Formation and associated floras. Unpublished M.A. thesis, University of California, Berkeley.Google Scholar
Franklin, J. F., and Dyrness, C. T. 1973. Natural Vegetation of Oregon and Washington. U.S. Department of Agriculture, Forest Service, General Technical Report PNW-8.Google Scholar
Graham, A. 1965. The Sucker Creek and Trout Creek Miocene floras of southeastern Oregon. Kent State University Bulletin, Research Series 9.Google Scholar
Griffin, J. R., and Critchfield, W. B. 1972. The distribution of forest trees in California. Pacific Southwest Forest and Range Experiment Station, Research Paper PSW-82/1972.Google Scholar
Hamilton, W., and Myers, W. B. 1966. Cenozoic tectonism of the western United States. Review of Geophysics 4:509–549.Google Scholar
Izett, G. A. 1975. Late Cenozoic sedimentation and deformation in northern Colorado and adjoining areas. Geological Society of America Memoir 144:179–209.Google Scholar
King, P. B. 1977. The Evolution of North America. Revised Edition. Princeton University Press; Princeton, New Jersey.Google Scholar
Knowlton, F. H. 1898. The fossil plants of the Payette Formation. U.S. Geological Survey 18th Annual Report, part 3:721–744.Google Scholar
Leonard, B. F., and Marvin, R. F. 1984. Temporal evolution of the Thunder Mountain caldera and related features, central Idaho. Idaho Bureau of Mines and Geology Bulletin 26:23–41.Google Scholar
Lipman, P. W., Protska, H. J., and Christiansen, R. L. 1972. Cenozoic volcanism and plate-tectonic evolution of the western United States. I, Early and middle Cenozoic. Philosophical Transactions of the Royal Society of London A 271:217–248.Google Scholar
Little, E. L. Jr. 1971. Atlas of United States Trees. Vol. 1. Conifers and Important Hardwoods. U.S. Department of Agriculture, Forest Service Miscellaneous Publication No. 1146.Google Scholar
MacGinitie, H. D. 1933. The Trout Creek flora of southeastern Oregon. Carnegie Institute of Washington Publication 416:21–68.Google Scholar
Major, J., and Taylor, D. W. 1977. Alpine. Pp. 601–675. In Barbour, M. G., and Major, J. (eds.), Terrestrial Vegetation of California. John Wiley & Sons; New York.Google Scholar
Miller, C. N. Jr. 1976. Two new pinaceous cones from the Early Cretaceous of California. Journal of Paleontology 50:821–832.Google Scholar
Miller, C. N. Jr. 1977. Mesozoic conifers. The Botanical Review 43:217–280.Google Scholar
Price, R. A., Olsen-Stokjovich, J., and Lowenstein, J. M. 1987. Relationships among the genera of Pinaceae: an immunological comparison. Systematic Botany 12:91–97.Google Scholar
Robinson, C. R. 1975. Pinaceous dwarf shoots from the Late Cretaceous Magothy Formation of Martha's Vineyard Island, Massachusetts. Unpublished Ph.D. Dissertation, University of Montana.Google Scholar
Robinson, C. R. 1977. Prepinus parlinensis, sp. nov., from the Late Cretaceous of New Jersey. Botanical Gazette 138:352–356.Google Scholar
Ross, C. P. 1935. Geology and ore deposits of the Casto quadrangle, Idaho. U.S. Geological Survey Bulletin 854.Google Scholar
Ross, C. P. 1937. Geology and ore deposits of the Bayhorse region, Custer County, Idaho. U.S. Geological Survey Bulletin 877.Google Scholar
Sawyer, J. O., and Thornburgh, D. A. 1977. Montane and subalpine vegetation of the Klamath Mountains. Pp. 699–732. In Barbour, M. G., and Major, J. (eds.), Terrestrial Vegetation of California. J. Wiley & Sons; New York.Google Scholar
Schorn, H. E. 1990. The Miocene Stewart Valley flora, Mineral County, Nevada. Unpublished manuscript.Google Scholar
Smith, H. V. 1941. A Miocene flora from Thorn Creek, Idaho. American Midland Naturalist 25:473–522.CrossRefGoogle Scholar
Steven, T. A. 1975. Middle Tertiary volcanic field in the southern Rocky Mountains. Geological Society of America Memoir 144:75–94.Google Scholar
Steven, T. A., and Epis, R. C. 1968. Oligocene volcanism in south-central Colorado. Colorado School of Mines Quarterly 63:241–258.Google Scholar
Steven, T. A., and Lipman, P. W. 1976. Calderas of the San Juan volcanic field, southwestern Colorado. U.S. Geological Survey Professional Paper 958.Google Scholar
Stewart, J. H. 1978. Basin-range structure in western North America: a review. Geological Society of America Memoir 152:1–32.Google Scholar
Stewart, J. H., and Carlson, J. E. 1978. Generalized maps showing distribution lithology, and age of Cenozoic igneous rocks in the western United States. Geological Society of America Memoir 152:263–265.Google Scholar
Stopes, M. C. 1915. Catalogue of the Mesozoic plants in the British Museum (Natural History). The Cretaceous Flora. Part II. Lower Greensand (Aptian) plants of Britain.Google Scholar
Taylor, D. W. 1976. Disjunction of Great Basin plants in the northern Sierra Nevada. Madroño 23:301–310.Google Scholar
Taylor, R. B. 1976. Neogene tectonism in south-central Colorado. Geological Society of America Memoir 175:211–226.Google Scholar
Wolfe, J. A. 1964. Miocene floras from Fingerrock Wash, southwestern Nevada. U.S. Geological Survey Professional Paper 454-N.Google Scholar