Table 2.
αRMA (95% CI) | Log βRMA (95% CI) | r2 | |
---|---|---|---|
Boreal (n=229) | |||
Log MA vs. log MR | 1·08 (0·986, 1·17) | 0·476 (0·329, 0·622) | 0·563 |
Log MS vs. log MR | 1·12 (1·02, 1·22) | 0·384 (0·230, 0·538) | 0·549 |
Temperate (n=511) | |||
Log MA vs. log MR | 0·836 (0·796, 0·875) | 0·665 (0·615, 0·702) | 0·658 |
Log MS vs. log MR | 0·888 (0·847, 0·929) | 0·551 (0·498, 0·604) | 0·716 |
Subtropical (n=767) | |||
Log MA vs. log MR | 1·06 (1·04, 1·08) | 0·494 (0·466, 0·522) | 0·927 |
Log MS vs. log MR | 1·08 (1·06, 1·10) | 0·430 (0·400, 0·459) | 0·923 |
Tropical (n=27) | |||
Log MA vs. log MR | 1·06 (0·864, 1·26) | 0·239 (−0·065, 0·543) | 0·797 |
Log MS vs. log MR | 1·10 (0·892, 1·31) | 0·133 (−0·190, 0·455) | 0·788 |
MA vs. MR or MS vs. MR scaling exponents in bold type have 95% CIs that numerically include those reported at the level of individual plants (αRMA=1·06 and 1·08, respectively; see Niklas, 2005).