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Do Low CO2 Concentrations Affect Pollen-Based Reconstructions of LGM Climates? A Response to “Physiological Significance of Low Atmospheric CO2 for Plant–Climate Interactions” by Cowling and Sykes

Published online by Cambridge University Press:  20 January 2017

John W. Williams ,
Thompson Webb III ,
Bryan N. Shurman  and
Patrick J. Bartlein
John W. Williams
Affiliation:
National Center for Ecological Analysis and Synthesis, University of California, Santa Barbara, Santa Barbara, California 93101, E-mail: [email protected]
Thompson Webb III
Affiliation:
Department of Geological Sciences, Brown University, Providence, Rhode Island 02912, E-mail: [email protected], [email protected]
Bryan N. Shurman
Affiliation:
Department of Geological Sciences, Brown University, Providence, Rhode Island 02912, E-mail: [email protected], [email protected]
Patrick J. Bartlein
Affiliation:
Department of Geography, University of Oregon, Eugene, Oregon 97403, E-mail: [email protected]
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Abstract

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Type
Letter to the Editor
Information
Quaternary Research , Volume 53 , Issue 3 , May 2000 , pp. 402 - 404
Copyright
University of Washington

References

Bartlein, P.J., Prentice, I.C., Webb, T. III, (1986). Climatic response surfaces from pollen data for some eastern North American taxa. Journal of Biogeography 13, 35–57.Google Scholar
Bazzaz, F.A., (1990). The response of natural ecosystems to the rising global CO2 levels. Annual Review of Ecology and Systematics 21, 167–196.CrossRefGoogle Scholar
Berner, R.A., (1997). The rise of plants and their effect on weathering and atmospheric CO2 . Science 276, 544–546.Google Scholar
Brooks, A., Farquhar, G.D., (1985). Effect of temperature on the CO2/O2 specificity of ribulose-1,5-bisphosphate carboxylase/oxygenase and the rate or respiration in the light. Planta 165, 397–406.Google Scholar
Collatz, G.J., Berry, J.A., Clark, J.S., (1998). Effects of climate and atmospheric CO2 partial pressure on the global distribution of C4 grasses: Present, past, and future. Oecologia 114, 441–454.Google Scholar
Cowling, S.A., (1999). Simulated effects of low atmospheric CO2 on structure and composition of North American vegetation at the Last Glacial Maximum. Global Ecology and Biogeography Letters 8, 81–93.Google Scholar
Cowling, S.A., Sage, R.F., (1998). Interactive effects of low atmospheric CO2 and elevated temperature on growth, photosynthesis, and respiration in Phaseolus vulgaris. Plant, Cell and Environment 21, 427–435.Google Scholar
Cowling, S.A., Sykes, M.T., (1999). Physiological significance of low atmospheric CO2 for plant–climate interactions. Quaternary Research 52, 237–242.Google Scholar
Davis, M.B., (1989). Research questions posed by the paleoecological record of global change. Bradley, R.S., Global Changes of the Past UCAR Office for Interdisciplinary Earth Studies, Boulder.385–395.Google Scholar
Ehleringer, J.R., Sage, R.F., Flanagan, L.B., Pearcy, R.W., (1991). Climate change and the evolution of C4 photosynthesis. Trends in Ecology and Evolution 6, 95–99.Google Scholar
Ehleringer, J.R., Cerling, T.E., Helliker, B.R., (1997). C4 photosynthesis, atmospheric CO2, and climate. Oecologia 112, 285–299.CrossRefGoogle ScholarPubMed
Farquhar, G.D., Sharkey, T.D., (1982). Stomatal conductance and photosynthesis. Annual Review of Plant Physiology 33, 317–345.CrossRefGoogle Scholar
Field, C.B., Jackson, R.B., Mooney, H.A., (1995). Stomatal responses to increased CO2: Implications from the plant to the global scale. Plant, Cell, and Environment 18, 1214–1225.CrossRefGoogle Scholar
Fredlund, G.G., Tieszen, L.L., (1997). Phytolith and carbon isotope evidence for late Quaternary vegetation and climate change in the southern Black Hills, South Dakota. Quaternary Research 47, 206–217.CrossRefGoogle Scholar
Holliday, V.T., (1995). Stratigraphy and Paleoenvironments of Late Quaternary Valley Fills on the Southern High Plains. Geol. Soc. Am, Boulder.Google Scholar
Idso, S.B., (1989). A problem for paleoclimatology?. Quaternary Research 31, 433–434.CrossRefGoogle Scholar
Jackson, R.B., Sala, O.E., Field, C.B., Mooney, H.A., (1994). CO2 alters water use, carbon gain, and yield in a natural grassland. Oecologica 98, 257–262.Google Scholar
Jackson, S.T., Webb, R.S., Anderson, K.H., Overpeck, J.T., Webb, T.III, Williams, J.W., Hansen, B.C.S., (2000). Vegetation and environment in eastern North America during the last glacial maximum. Quaternary Science Reviews 19, 489–508.CrossRefGoogle Scholar
Jolly, D., Haxeltine, A., (1997). Effect of low glacial atmospheric CO2 on tropical African montane vegetation. Science 276, 786–788.Google Scholar
Jolly, D., Harrison, S.P., Damnati, B., Bonnefille, R., (1998). Simulated climate and biomes of Africa during the late Quaternary: Comparison with pollen and lake status data. Quaternary Science Reviews 17, 629–658.Google Scholar
Larcher, W., (1995). Physiological Plant Ecology. Springer, Berlin.CrossRefGoogle Scholar
Mahowald, N., Kohfeld, K., Hansson, M., Balkanski, Y., Harrison, S.P., Prentice, I.C., Shulz, M., Rodhe, H., (1999). Dust sources and deposition during the last glacial maximum and current climate: A comparison of model results with paleodata from ice cores and marine sediments. Journal of Geophysical Research 104, 895–916.Google Scholar
Muhs, D.R., Aleinikoff, J.N., Stafford, T.W. Jr., Kihl, R., Been, J., Mahan, S.A., Cowherd, S., (1999). Late Quaternary loess in northeastern Colorado: Part I—Age and paleoclimatic significance. GSA Bulletin 111.Google Scholar
Petit, J.R., Jouzel, J., Raynaud, D., Barkov, N.I., Barnola, J.-M., Basile, I., Bender, M., Chappellaz, J., Davis, M., Delaygue, G., Delmotte, M., Kotlyakov, V.M., Legrand, M., Lipenkov, V.Y., Lorius, C., Pepin, L., Ritz, C., Saltzman, E., Stievenard, , (1999). Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399, 429–436.Google Scholar
Polley, H.W., Johnson, H.B., Marino, B.D., Mayeux, H.S., (1993). Increase in C3 plant water-use efficiency and biomass over glacial to present CO2 concentrations. Nature 361, 61–64.Google Scholar
Polley, H.W., Johnson, H.B., Mayeux, H.S., (1995). Nitrogen and water requirements of C3 plants grown at glacial to present carbon dioxide concentrations. Functional Ecology 9, 86–96.Google Scholar
Prentice, I.C., Bartlein, P.J., Webb, T. III, (1991). Vegetation and climate changes in eastern North America since the last glacial maximum: A response to continuous climatic forcing. Ecology 72, 2038–2056.Google Scholar
Prentice, I.C., Guiot, J., Harrison, S.P., (1992). Mediterranean vegetation, lake levels and palaeoclimate at the last glacial maximum. Nature 360, 658–660.Google Scholar
Street-Perrott, F.A., Huang, Y., Perrott, R.A., Eglinton, G., Barker, P., Khelifa, L.B., Harkness, D.D., Olago, D.O., (1997). Impact of lower atmospheric carbon dioxide on tropical mountain ecosystems. Science 278, 1422–1426.Google Scholar
Webb, T. III, Anderson, K.H., Bartlein, P.J., Webb, R.S., (1998). Late Quaternary climate change in eastern North America: A comparison of pollen-derived estimates with climate model results. Quaternary Science Reviews 17, 587–606.Google Scholar
Webb, T. III, Bartlein, P.J., Harrison, S.P., Anderson, K.H., (1993). Vegetation, lake levels, and climate in eastern North America for the past 18,000 years. Wright, H.E. Jr., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J., Global Climates Since the Last Glacial Maximum Univ. of Minnesota Press, Minneapolis.415–467.Google Scholar