Relationships between C3 Plant Foliar Carbon Isotope Composition and Element Contents of Grassland Species at High Altitudes on the Qinghai-Tibet Plateau,China

Relationships of foliar carbon isotope composition (δ¹³C) with foliar C, N, P, K, Ca, Mg contents and their ratios of 219 C₃ species leaf samples, obtained in August in 2004 to 2007 from 82 high altitude grassland sites on the Qinghai-Tibet Plateau China, were examined. This was done with reference to the proposition that foliar δ¹³C increases with altitude and separately for the life-form groups of graminoids, forbs and shrubs and for the genera Stipa and Kobresia. For all samples, foliar δ¹³C was negatively related to foliar K, P and ∑_{K+ Ca+ Mg}, and positively correlated to foliar C, C/N and C/P. The significance of these correlations differed for the taxonomic and life-form groups. Lack of a relationship of foliar δ¹³C with foliar N was inconsistent with the majority of studies that have shown foliar δ¹³C to be positively related to foliar N due to a decrease of C_i/C_a (the ratio between intercellular and atmospheric concentration of CO₂) and explained as a result of greater photosynthetic capacity at higher foliar N concentration. However this inconsistency relates to other high altitude studies that have found that photosynthetic capacity remains constant as foliar N increases. After accounting for the altitudinal relationship with foliar δ¹³C, of the elements only the K effect was significant and was most strongly expressed for Kobresia. It is concluded that factors critical to plant survival and growth at very high altitudes, such as low atmospheric pressure and low temperatures, may preclude expression of relationships between foliar δ¹³C and foliar elements that have been observed at lower altitudes.