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The carbon and nitrogen isotope composition of Australian grasses in relation to climate

Citation

Murphy, BP and Bowman, DMJS, The carbon and nitrogen isotope composition of Australian grasses in relation to climate, Functional Ecology, 23, (6) pp. 1040-1049. ISSN 0269-8463 (2009) [Refereed Article]


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The definitive published version is available online at: http://interscience.wiley.com

DOI: doi:10.1111/j.1365-2435.2009.01576.x

Abstract

1. The carbon and nitrogen isotope composition of plants are known to be affected by environmental factors, especially water availability. While d13C of C4 plants is generally assumed to be much less responsive to environmental variables than that of C3 plants, it is unclear whether the response of d15N differs between the two photosynthetic pathways. 2. Focussing on differences in the response of members of the C3 and C4 photosynthetic pathways to climate variables, we examined the foliar d13C and d15N of grasses collected from natural vegetation in a wide range of climatic zones throughout Australia. 3. An index of water availability was clearly related to foliar d13C and d15N of both C3 and C4 grasses. There was a negative relationship between water availability and d13C of C3 grasses (r2 = 0∆21), similar to that documented extensively in other C3 plants. An opposite, positive relationship was found between water availability and d13C in C4 grasses (r2 = 0∆17), an effect that has been reported only infrequently. Accounting for differences in d13C between the different C4 types (NADP-ME, PCK, NAD-ME and Aristida) resulted in a substantial increase in the fit of the model relating d13C to water availability (R2 = 0∆48). 4. There was a negative relationship between water availability and d15N (r2 = 0∆40), that was similar in both C3 and C4 grasses, but temperature had no effect on d15N. This provides strong support for the theory that water availability is the dominant factor determining soil and plant d15N via its effect on the Ďopennessí of the nitrogen cycle. 5. We also found significant differences in d15N between the different C4 types, with the highest values for PCK, followed by NADP-ME and NAD-ME, and the lowest values for Aristida. The difference in d15N between PCK and Aristida was large, at 5∆1&. 6. The importance of water availability as a predictor of d13C in both C3 and C4 grasses suggests that variation in water availability should be considered when estimating C4 grass abundance based on d13C measurements (e.g. in herbivore diets or as a contributor to biospheric carbon sinks).

Item Details

Item Type:Refereed Article
Keywords:C3, C4, photosynthetic pathway, Poaceae, rainfall, stable isotope, water availability
Research Division:Environmental Sciences
Research Group:Ecological Applications
Research Field:Ecosystem Function
Objective Division:Environment
Objective Group:Flora, Fauna and Biodiversity
Objective Field:Sparseland, Permanent Grassland and Arid Zone Flora, Fauna and Biodiversity
Author:Murphy, BP (Dr Brett Murphy)
Author:Bowman, DMJS (Professor David Bowman)
ID Code:61786
Year Published:2009
Web of Science® Times Cited:34
Deposited By:Plant Science
Deposited On:2010-03-05
Last Modified:2012-12-12
Downloads:1 View Download Statistics

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