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Holocene Climatic Variations Inferred from Treeline Fluctuations in the White Mountains, California

Published online by Cambridge University Press:  20 January 2017

Valmore C. LaMarche Jr.
Valmore C. LaMarche Jr.*
Affiliation:
Laboratory of Tree-Ring Research, University of Arizona, Tucson, Arizona 85721 USA
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Abstract

Remains of dead bristlecone pine (Pinus longaeva Bailey) are found at altitudes up to 150 m above present treeline in the White Mountains. Standing snags and remnants in two study areas were mapped and sampled for dating by tree-ring and radiocarbon methods. The oldest remnants represent trees established more than 7400 y.a. Experimental and empirical evidence indicates that the position of the treeline is closely related to warm-season temperatures, but that precipitation may also be important in at least one of the areas. The upper treeline was at high levels in both areas until after about 2200 B.C., indicating warm-season temperatures about 3.5°F higher than those of the past few hundred years. However, the record is incomplete, relative warmth may have been maintained until at least 1500 B.C. Cooler and wetter conditions are indicated for the period 1500 B.C.-500 B.C., followed by a period of cool but drier climate. A major treeline decline occurred between about A.D. 1100 and A.D. 1500, probably reflecting onset of cold and dry conditions. High reproduction rates and establishment of scattered seedlings at high altitudes within the past 100 yr represents an incipient treeline advance, which reflected a general climatic warming beginning in the mid-19th century that has lasted until recent decades in the western United States. This evidence for climatic variation is broadly consistent with the record of Neoglacial advances in the North American Cordillera, and supports Antevs' concept of a warm “altithermal age” in the Great Basin.

Type
Original Articles
Information
Quaternary Research , Volume 3 , Issue 4 , December 1973 , pp. 632 - 660
Copyright
University of Washington

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References

Adam, D.P., (1967)Late-Pleistocene and recent palynology in the central Sierra Nevada, California. Cushing, E.J., Wright, H.E. Jr., Quaternary Paleoecology Yale University Press New Haven, Connecticut 275–301.Google Scholar
Andreev, V.N., (1954)Extension of arboreous plants into the tundra. Orig. Russian Botanical Journal Moscow .Google Scholar
Antevs, E., (1948)Climatic changes and pre-white man. The Great Basin, with Emphasis on Glacial and Postglacial Times. University of Utah Bulletin Vol. 38, 168–191no. 20, Salt Lake City.Google Scholar
Antevs, E., (1955)Geologic-climatic dating in the West. American Antiquity 20, 317–335.Google Scholar
Aschmann, H.H., (1958)Great Basin climates in relation to human occupance. University of California Archaeological Survey Reports 42, 23–40.Google Scholar
Bamberg, S., Schwarz, W., Tranquillini, W., (1967)Influence of daylength on the photosynthetic capacity of stone pine (Pinus cembra L.). Ecology 48, 264–269.Google Scholar
Benedict, J.B., (1968)Recent glacial history of an alpine area in the Colorado Front Range. II. Dating glacial deposits. Journal of Glaciology 7, 77–87.CrossRefGoogle Scholar
Billings, W.D., (1954)Temperature inversions in the pinvon-juniper zone of a Nevada moun-tain range. Butler University Botanical Studies 11, 112–118.Google Scholar
Billings, W.D., Thompson, J.H., (1957)Composition of a stand of old bristlecone pine in the White Mountains of California. Ecology 38, 158–160.Google Scholar
Birkeland, P.W., Crandell, D.W., Richmond, G.M., (1971)Status of correlation of Quaternary stratigraphie units in the western conterminous United States. Quaternary Research 1, 208–227.Google Scholar
Birkeland, P.W., Miller, C.D., (1973)Re-interpretation of the type Temple Lake Moraine, and other Neoglacial deposits, southern Wind River Mountains, Wyoming. Geological Society of America Abstracts with Programs 5, 465.Google Scholar
Birman, J.H., (1964)Glacial geology across the crest of the Sierra Nevada, California. Geological Society of America Special Paper 75, 1–80.Google Scholar
Bryson, R.A., (1966)Air masses, streamlines, and the boreal forest. Geographical Bulletin 8, 228–269.Google Scholar
Bryson, R.A., Irwing, W.N., Larsen, J.A., (1965)Radiocarbon and soil evidence of former forest in southern California tundra. Science 147, 45–48.Google Scholar
Curry, R.R., (1968)Quaternary climatic and glacial history of the Sierra Nevada, California. Ph.D. DissertationUniversity of California at Berkeley.Google Scholar
Curry, R.R., (1969)Holocene climatic and glacial history of the central Sierra Nevada, California. INQUA Volume, Geological Society of America Special Paper 123, 1–47.CrossRefGoogle Scholar
Dale, R.F., (1959)Climates of the States (California). U.S. Department of Commerce, Weather Bureau, Climatography of the United States 60, 1–29.Google Scholar
Daubenmire, R., (1954)Alpine timberlines in the Americas and their interpretation. Butler University Botanical Studies 11, 119–154.Google Scholar
Denton, G.H., Porter, S.C., (1970)Neoglaciation. Scientific American 222, 100–110.Google Scholar
Detterman, R.L., (1970)Early Holocene warm interval in northern Alaska. Arctic 23, 130–132.CrossRefGoogle Scholar
D'Ooge, C.L., (1955)Five years of weather observations on the White Mountain Range, California. Bulletin of the American Meteorological Society 36, 172–175.Google Scholar
Ferguson, C.W., (1969)A 7104-year annual treering chronology for bristlecone pine, Pinus aristata, from the White Mountains, California. Tree-Ring Bulletin 29, 1–29.Google Scholar
Fritts, H.C., (1969)Bristlecone pine in the White Mountains of California: growth and righ-width characteristics. Papers of the Laboratory of Tree-Ring Research No. 4 University of Arizona Press Tucson.Google Scholar
Griggs, R.F., (1937)Timberlines as indicators of climatic trends. Science 85, 251–255.Google Scholar
Griggs, R.F., (1938)Timberlines in the northern Rocky Mountains. Ecology 19, 548–564.Google Scholar
Haugen, R.K., (1965)Climatic implications of timberline in interior Alaska (abstract). Abstracts, International Association for Quaternary Research, VII International Congress Boulder, Colorado 197.Google Scholar
Hustich, I., (1958)On the recent expansion of the scotch pine in northern Europe. Fennia 82, 1–25.Google Scholar
Hustich, I., (1966)On the forest-tundra and northern tree-lines. Annals of The University of Turku A II, 36(Rep. Kevo Subarctic Station 3)Hustich, I., On the forest-tundra and northern tree-lines. Annals of The University of Turku A II, 7–47(Rep. Kevo Subarctic Station 3).Google Scholar
Jungerius, P.D., (1969)Soil evidence of postglacial tree line flucturations in the Cypress Hills area, Alberta, Canada. Arclic and Alpine Research 1, 235–245.Google Scholar
Kesseli, J.E., Beaty, C.B., (1959)Desert flood conditions in the White Mountains of California and Nevada. Quartermaster Research and Engineering Commission, U.S. Army Environmental Protection Research, Division, Technical Report EP-108 1–107.Google Scholar
Knopf, A., (1918)A geologic reconnaissance of the Inyo Range and the eastern slope of the southern Sierra Nevada with a section on the stratigraphy of the Inyo Range by Edwin Kirk. U.S. Geological Survey Professional Paper 110, 1–130.Google Scholar
Kozlowski, T.T., (1971)Growth and Development of Trees. Academic Press New York.Google Scholar
LaMarche, V.C. Jr., (1965)Distribution of Pleistocene glaciers in the White Mountains of California and Nevada. U.S. Geological Survey Professional Paper 525-C, 144–146.Google Scholar
LaMarche, V.C. Jr., (1968)Rates of slope degradation as determined from botanical evidence, White Mountains, California. Erosion and sedimentation in a semiarid environment. U.S. Geological Survey Professional Paper 325-I, 341–377.Google Scholar
LaMarche, V.C. Jr., (1969)Environment in relation to the age of bristlecone pines. Ecology 50, 53–59.Google Scholar
LaMarche, V.C. Jr., Mooney, H.A., (1967)Altithermal timberline advance in western United States. Nature (London) 213, 980–982.Google Scholar
LaMarche, V.C. Jr., Mooney, H.A., (1972)Recent climatic change and development of bristlecone pine (P. longaeva Bailey) krummholz zone, Mt. Washington, Nevada. Arctic and Alpine Research 4, 61–72.Google Scholar
LaMarche, V. C. Jr., Harlan, T. P., (in press). Accuracy of tree-ring dating of bristlecone pine for calibration of the radiocarbon time scale. Journal of Geophysical Research .Google Scholar
Lamb, H.H., (1964)Trees and climatic history in Scotland. Quarterly Journal of the Royal Meteorological Society 90, 382–394.CrossRefGoogle Scholar
Larson, P.R., (1964)Some indirect effects of environment on wood formation. Zimmerman, M.H., The Formation of Wood in Forest Trees Academic Press New York 345–365.Google Scholar
Lüdi, W., (1955)Die vegetationsentwicklung seit dem Ruckzug der Gletscher in den mittleren Alpen and ihrem Vorland. Ber. Geobotan Forschunginst. Rubel. (Zurich) 36–38.Google Scholar
Lundquist, G., (1959)C14-dated pine stumps from the high mountains in western Sweden. Sveriges Geol. Undersökning 53, 1–24Arsb.Google Scholar
Lundquist, G., (1962)Geological radiocarbon datings from the Stockholm station. Sveriges Geol. Undersökning 56, 1–23Arsb.Google Scholar
Mahaney, W.C., (1972)Audubon: new name for Colorado Front Bange Neoglacial deposits formerly called “Arikaree”. Arctic and Alpine Research 4, 355–358.Google Scholar
Mahaney, W.C., (1973)Neoglacial chronology in the Fourth of July cirque, central Colorado Front Range. Geological Society of America Bulletin 84, 161–170.Google Scholar
Martin, P.S., (1963)The last 10,000 years. University of Arizona Press Tucson.Google Scholar
McCulloch, D., Hopkins, D., (1966)Evidence for an early recent warm interval in northwestern Alaska. Geological Society of America Bulletin 77, 1089–1108.Google Scholar
Mitchell, J.M. Jr., (1961)Recent secular changes of global temperature. Annals of the New York Academy of Science 95, 235–250.Google Scholar
Mitchell, R.S., LaMarche, V.C. Jr., Lloyd, R.M., (1966)Alpine vegetation and active frost features of Pellisier Flats: White Mountains, California. American Midland Naturalist 75, 516–525.CrossRefGoogle Scholar
Mooney, H.A., St. Andre, G., Wright, R.D., (1962)Alpine and subalpine vegetation patterns in the White Mountains of California. American Midland Naturalist 68, 257–273.CrossRefGoogle Scholar
Mooney, H.A., West, M., Brayton, R., (1966)Field measurements of the metabolic responses of bristlecone pine and big sagebrush in the White Mountains of California. Botanical Gazette 127, 105–113.Google Scholar
Namias, J., (1972)Experiments in objectively predicting some atmospheric and oceanic variables for the winter of 1971–1972. Journal of Applied Meteorology 11, 1164–1174.Google Scholar
Nichols, H., (1967)The postglacial history of vegetation and climate at Ennadai Lake, Keewatin, and Lynn Lake, Manitoba (Canada). Eiszeitalter und Gegenwart 18, 176–197.Google Scholar
Pearson, G.A., (1931)Forest types in the Southwest as determined by climate and soil. United States Department of Agriculture Technical Bulletin 247, 1–143.Google Scholar
Porter, S.C., Denton, G.H., (1967)Chronology of Neoglaciation in the North American Cordillera. American Journal of Science 265, 177–210.CrossRefGoogle Scholar
Richardson, S.D., (1964)The external environment and tracheid size in conifers. Zimmerman, M.H., The Formation of Wood in Forest Trees Academic Press New York 367–388.Google Scholar
Richmond, G.M., (1962)Quaternary stratigraphy of the La Sal Mountains, Utah. U.S. Geological Survey Professional Paper 324, 1–135.Google Scholar
Richmond, G.M., (1972)Appraisal of the future climate of the Holocene in the Rocky Mountains. Quaternary Research 2, 315–322.CrossRefGoogle Scholar
Ritchie, J.C., Hare, F.K., (1971)Late Quaternary vegetation and climate near the Arctic treeline of northwestern North America. Quaternary Research 1, 331–342.CrossRefGoogle Scholar
Schubert, G.H., Reitveld, W.J., (1970)Bristlecone pine—its phenology, cone maturity, and seed production in the San Francisco Peaks, Arizona. U.S. Department of Agriculture Forest Service Research Note RM-180 Rocky Mountain Forest and Range Experimental Station 1–7.Google Scholar
Schulze, E.D., Mooney, H.A., Dunn, E.L., (1967)Wintertime photosynthesis of bristlecone pine (Pinus aristata) in the White Mountains of California. Ecology 48, 1044–1047.CrossRefGoogle Scholar
Sorenson, C.J., Knox, J.C., Larsen, J.A., Bryson, R.A., (1971)Paleosols and the forest border in Keewatin, N.W.T. Quaternary Research 1, 468–473.CrossRefGoogle Scholar
Stidd, C.K., (1967)The use of eigenvectors for climatic estimates. Journal of Applied Meterology 6, 255–264.Google Scholar
Stokes, M.A., Smiley, T.L., (1968)An Introduction to Tree-Ring Dating. University of Chicago Press Chicago.Google Scholar
Suess, H.C., (1970)Bristlecone-pine calibration of the radiocarbon time-scale 5200 B.C. to the present. Olsson, I.U., Radiocarbon Variations and Absolute Chronology Wiley New York 303–312.Google Scholar
Terjung, W.H., Kickert, R.N., Potter, G.L., Swarts, S.W., (1969)Energy and moisture balance of an alpine tundra in mid July. Arctic and Alpine Research 1, 247–266.Google Scholar
Tikhomirov, V.A., (1956)The Vegetation of the Far North and its Utilization. I. Academy of Science Moscow, U.S.S.R.,.Google Scholar
Tranquillini, W., (1964)The physiology of plants at high altitudes. Annual Review of Plant Physiology 15, 345–362.Google Scholar
Tranquillini, W., (1967)Über die physiologischen Ursachen der Wald-und Baumgrenze. Ökologie der Alpinen Waldgrenze Mitt. Forst. Bundes Wien, Austria.Google Scholar
Trewartha, G.T., (1966)The Earth's Problem Climates. University of Wisconsin Press Madison.Google Scholar
Wahl, E.W., (1968)A comparison of the climate of the eastern United States during the 1830's with the current normals. Monthly Weather Review 96, 73–82.Google Scholar
Wahl, E.W., Lawson, T.L., (1970)The climate of the mid-nineteenth century United States compared to the current normals. Monthly Weather Review 98, 259–265.2.3.CO;2>CrossRefGoogle Scholar
Wardle, P., (1968)Engelmann spruce (Picea engelmannii Engel.) at its upper limits on the Front Range, Colorado. Ecology 49, 483–495.Google Scholar
Willet, H.C., Saunders, F., (1959)Descriptive Meterology. Second Edition Academic Press New York.Google Scholar
Wright, R.D., Mooney, H.A., (1965)Substrate-oriented distribution of bristlecone pine in the White Mountains of California. American Midland Naturalist 73, 257–284.Google Scholar
Zahner, R., (1968)Water Deficits and Growth of Trees: Water Deficits and Plant Growth. Academic Press New York.Google Scholar