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. 2009 Dec 3;162(4):837–852. doi: 10.1007/s00442-009-1514-7

Table 2.

The linear relationship between mean C (δ13C) and N isotopic composition (δ15N) values and the C/N ratio from C3 plant sites and mean annual rainfall

Rainfall (Ln mm/year) β α n R 2 P
δ13Ca
 W −0.82 (−1.17) −22.95 (−20.76) 23 (17) 0.41 (0.67) <0.05 (<0.001)
 D −0.55 (−0.78) −22.88 (−21.74) 18 (15) 0.18 (0.44) 0.086 (<0.01)
 Dg −0.96 (−1.73) −20.75 (−15.97) 17 (14) 0.32 (0.79) <0.05 (<0.001)
 Dd −0.97 (−1.22) −21.74 (−20.19) 17 (16) 0.45 (0.61) <0.01 (<0.001)
 A −0.58 (−0.96) −23.59 (−21.21) 39 (30) 0.14 (0.33) <0.05 (<0.001)
δ15Nb
 W −2.60 (−3.47) 15.09 (20.43) 23 (17) 0.39 (0.70) 0.001 (<0.001)
 D −2.69 (−3.32) 15.38 (19.71) 16 (14) 0.58 (0.76) <0.001 (<0.001)
 A −2.59 (−3.45) 14.96 (20.69) 39 (28) 0.46 (0.76) <0.001 (<0.001)
C/Nb
 W 3.19 (2.99) 3.73 (4.84) 21 (15) 0.28 (0.21) <0.05 (0.087)
 D 4.67 (5.65) 12.32 (5.94) 20 (17) 0.43 (0.50) <0.01 (<0.01)

W Wet season; D dry season; Dg dry season green plants; Dd dry season dried plants; A annual, combined wet and dry period; n number of sites; β slope; α intercept

P values < 0.05 are marked in bold

aDry wash desert sites are excluded from the δ13C regression analysis, results are shown in parentheses

bExposed ridge sites are excluded from the δ15N and C/N analysis, results are shown in parentheses