Equilibrium in soil respiration across a climosequence indicates its resilience to climate change in a glaciated valley, western Himalaya

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Soil Ecol. 145, 1 (2020).Article  Google Scholar  Page 2 Elevation (m) SOC (g Kg-1) ST (°C) SWC (m3 m-3) SR (µmol m-2 s-1) Q10 of SR 3300 33.29 ± 2.35b 15.21 ± 0.34c 0.076 ± 0.006a 2.38 ± 0.21a 0.47 3400 19.03 ± 1.91a 13.93 ± 0.75bc 0.070 ± 0.008a 2.05 ± 0.21a 1.42 3600 18.04 ± 2.68a 13.74 ± 0.61bc 0.081 ± 0.010ab 2.02 ± 0.17a 2.69 3700 26.10 ± 3.42ab 10.60 ± 0.86a 0.115 ± 0.012b 2.18 ± 0.20a 3.57 3800 19.12 ± 2.55a 11.49 ± 0.66ab 0.110 ± 0.014ab 1.92 ± 0.21a 4.97 3900 15.70 ± 0.92a 11.83 ± 0.78ab 0.106 ± 0.011ab 2.42 ± 0.23a 4.30 Growing season mean soil temperature (ST), volumetric soil water content (SWC), SR and Q10 of SR at different elevations. Values are mean ± standard error of mean with n = 48. Different letters indicate a significant difference in each parameter between elevations (p < 0.05).
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