By Ghillean T. Prance, Scott A. Mori
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Additional info for Lecythidaceae - Part I. The Actinomorphic-flowered New World Lecythidaceae (Asteranthos, Gustavia, Grias, Allantoma, & Cariniana) (Flora Neotropica Monograph No. 21(I))
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Biochem. 5, 19-34. Johnson, D. W. (1992). Nitrogen retention in forest soils. J. Environ. Qual. 21, 1-12. Johnson, D. W. (1994). Role of carbon in the cycling of other nutrients in forest ecosystems. In "Carbon: Forms and Functions in Forest Soils" (J. M. Kelly and W. M. ). 8th North American Forest Soil Conference, Special publication, Soil Science Society of America (in press). 2. Effects of C02 and N on Ponderosa Pine 39 Johnson, D. , and Ball, J. T. (1996). Interactions between CO2 and Nitrogen in Forests: Can We Extrapolate from the Seedling to the Stand Level?
Stored carbon may buffer the plant against the benefits of an increased supply of carbon from the atmosphere. Whole-tree dry mass seemingly is the measure most relevant to questions about the effects of CO2 concentration on carbon storage in forests, and many short-term studies with tree seedlings have drawn conclusions about forest tree growth on the basis of differences in biomass at the end of the experiment. However, the analysis of oak response illustrates why a static measure such as difference in tree mass is not a good predictor of long-term response.
Comerau, P. , and Kimmins,J. P. (1989). Above- and below-ground biomass and production oflodgepole pine on sites with differing soil moisture regimes. J. Forest Res. 19, 447-454. , and Bottner, P. (1991). Increased atmospheric COz and litter quality decomposition of sweet chestnut litter with animal food webs of different complexities. Oikos 61, 54-64. Curtis, P. , Zak, D. , Pregitzer, K. , and Teeri, J. A. (1996). Linking aboveand below-ground responses to rising CO~ in northern deciduous forest species.