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. 2015 Aug 31;65(9):906–921. doi: 10.1093/biosci/biv109

Table 1.

A summary of site characteristics and soil chemical and physical properties along the elevation gradient.

Total phosphorus (mg per gram)
Total nitroge n (%) Leaf litter C:N
Vegetation type Elevation (m asl) Mean annual air temp (°C) Mean annual precipitation (mm per year) Soil organic horizon depth (cm) Mean (M) Standard error (SE) M SE Soil pH M SE Relative recalcitrance of soil C
Lowland rainforest 194 26.4 2730 1 0.35 0.03 0.49 0.07 3.7 NA 0.91
210 26.4 3199 2 0.23 0.03 0.18 0.03 4.0 29.9 7.7 NA
Premontane rainforest 1000 20.7 3087 4 1.34 0.12 0.73 0.05 4.7 23.7 1.9 0.53
Lower montane cloud-forest 1500 17.4 2631 16 0.91 0.12 1.36 0.37 3.5 29.1 5.3 0.58
1750 15.8 2631 10 1.56 0.50 1.44 0.09 3.6 NA NA
1850 16.0 2472 16 1.86 0.24 0.76 0.06 3.5 NA NA
2020 14.9 1827 17 2.00 0.24 0.71 0.10 3.4 NA NA
Upper montane cloud-forest 2520 12.1 NA 14 1.73 0.34 0.98 0.14 3.7 NA NA
2720 11.1 2318 21 1.64 0.25 0.87 0.19 3.6 39.6 2.3 NA
3020 9.5 1776 17 1.57 0.21 0.92 0.13 3.4 NA NA
3025 11.1 1706 23 2.39 0.12 1.09 0.08 3.5 71.5 19.2 0.52
3200 8.9 NA 12 2.42 0.20 0.91 0.02 3.5 NA NA
3400 7.7 2555 14 2.49 0.17 1.09 0.09 3.4 NA NA
Grassland 3644 6.5 NA 4 1.44 0.07 0.92 0.13 3.4 NA NA

Note: Leaf-litter carbon-to-nitrogen ratios (C:N) are the average of three dominant species for respective plots (Salinas et al. 2011). Total nitrogen and phosphorus were determined for surface soil (0–10 centimeters, cm, in depth). Soil pH was measured in water. The relative recalcitrance of soil carbon is the ratio of the proportion of total soil carbon in recalcitrant carbon divided by the proportion in recent plant-derived carbon within surface mineral soils as determined by nuclear magnetic resonance (percentage of carbon in groups: alkyl/O-alkyl; Zimmermann et al. 2012). 
n = 5. Abbreviations: °C, degrees Celsius; cm, centimeters; m asl, meters above sea level; mg, milligrams; mm, millimeters; NA, data not available (Girardin et al. 2010, Rapp and Silman 2012, Whitaker et al. 2014b).