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  Annual rainfall does not directly determine the carbon isotope ratio of leaves of Eucalyptus species

Turner, N. C., Schulze, E. D., Nicolle, D., Schumacher, J., & Kuhlmann, I. (2008). Annual rainfall does not directly determine the carbon isotope ratio of leaves of Eucalyptus species. Physiologia Plantarum, 132(4), 440-445. doi:10.1111/j.1399-3054.2007.01027.x.

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Turner, N. C., Author
Schulze, E. D.1, Author           
Nicolle, D., Author
Schumacher, J.1, Author           
Kuhlmann, I.1, Author           
Affiliations:
1Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497751              

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Free keywords: Common garden Leaf-area Gradient Discrimination Australia
 Abstract: Leaf carbon isotope discrimination (delta C-13) was widely considered to directly reflect the rainfall environment in which the leaf developed, but recent observations have queried this. The relationship between delta C-13 and rainfall was explored in Eucalyptus species growing along a rainfall gradient in Australia. The leaves of 43 species of Eucalyptus and the closely related Corymbia species produced in 2003 were sampled in September 2004 at 50 sites and grouped into 15 locations along a rainfall gradient in southwest Western Australia. At 24 sites, the same species and same trees were sampled as in a study in September 2003 when leaves produced in 2002 were sampled. The rainfall in 2004 was on average 190 mm (range 135-270 mm) higher at all locations than in 2003. In the leaves sampled in 2004, the mean carbon isotope discrimination (delta C-13) across the 15 locations decreased 2.9 parts per thousand per 1000 mm of rainfall, the specific leaf area (SLA) increased by 2.9 m(2) kg(-1) per 1000 mm of rainfall and the nitrogen (N) content decreased by 1.56 g m(-2) per 1000 mm of rainfall. In contrast, a comparison between the leaves produced in the drier 2002 year compared with the wetter 2003 year showed that there was a strong correlation (r(2) = 0.85) between the SLA values between years and a trend for higher values with increasing SLA, but the values of delta C-13 were on average only 0.38 parts per thousand lower (more negative) at all locations in the wetter year, equivalent to a decrease of 2.0 parts per thousand per 1000 mm of rainfall. The results suggest that while there may be constitutive differences in leaf morphology, SLA and N content per unit area, increasing rainfall or cloudiness associated with higher rainfall increases SLA and decreases N content per unit area. We conclude that rainfall does not directly influence delta C-13, but induces leaf morphological and physiological changes that affect the resultant delta C-13. [References: 16]

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 Dates: 2008
 Publication Status: Issued
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 Identifiers: DOI: 10.1111/j.1399-3054.2007.01027.x
Other: BGC1096
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Title: Physiologia Plantarum
Source Genre: Journal
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Publ. Info: Copenhagen, DK : Munksgaard International Publishers
Pages: - Volume / Issue: 132 (4) Sequence Number: - Start / End Page: 440 - 445 Identifier: CoNE: https://pure.mpg.de/cone/journals/resource/110978977737153
ISSN: 0031-9317