Changes in the abundance of C3/C4 species of Inner Mongolia grassland: evidence from isotopic composition of soil and vegetation
Article first published online: 18 JUL 2009
© 2009 Blackwell Publishing Ltd
Global Change Biology
Volume 16, Issue 2, pages 605–616, February 2010
How to Cite
WITTMER, M. H. O. M., AUERSWALD, K., BAI, Y., SCHÄUFELE, R. and SCHNYDER, H. (2010), Changes in the abundance of C3/C4 species of Inner Mongolia grassland: evidence from isotopic composition of soil and vegetation. Global Change Biology, 16: 605–616. doi: 10.1111/j.1365-2486.2009.02033.x
- Issue published online: 4 JAN 2010
- Article first published online: 18 JUL 2009
- Received 29 January 2009; revised version received 18 May 2009 and accepted 9 July 2009
Table S1. Coefficients for the cubic polynomial models for the prediction of δ13Ca; the independent variable is the year/1000.
Fig. S1. Atmospheric carbon isotope composition (δ13Ca, circles, solid line) and atmospheric CO2 concentration (dashed line) (Keeling, 1979; Friedli et al., 1986; Conway et al., 1994; Francey et al., 1999; Gat et al., 2001; Allison et al., 2003; NOAA ESRL, 2008). Grey and white areas denote different fitting models (Table S1).
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