Skip to main content
. 2014 Sep 12;9(3):746–759. doi: 10.1038/ismej.2014.148

Table 2. Archaeal 16S rRNA pyrosequencing parameters, statistical estimators and gene abundance in different depths of the mofette and reference soils in June 2011.

Sample No. of sequencesa No. of OTUsb Coverage (%) Inverse Simpson's (1/D)c Chao 1 Shannon-Wienerc Archaeal 16S rRNA gene copies (g (dw)1)d
Mofette soil
 0–10 cm 545 (545) 38 98 4.3 (3.9; 4.8) 45 (40; 62) 2.0 (1.9; 2.1) 7.7±0.5 × 108
 10–25 cm 545 (3624) 22 98 1.9 (1.8; 2.1) 29 (24; 54) 1.2 (1.1; 1.3) 5.2±0.5 × 108
 25–40 cm 545 (4353) 23 98 2.7 (2.4; 3.0) 32 (25; 60) 1.4 (1.3; 1.5) 4.3±0.3 × 108
               
Reference soil
 0–10 cm 545 (2089) 66 93 4.2 (3.7; 4.9) 121 (91; 187) 2.2 (2.1; 2.4) 3.1±0.2 × 108
 10–25 cm 545 (676) 70 94 8.4 (7.5; 9.6) 93 (80; 126) 2.8 (2.7; 2.9) 2.7±0.1 × 108
 25–40 cm 545 (1434) 67 94 10.4 (9.3; 11.9) 98 (80; 141) 2.9 (2.8; 3.0) 7.6±0.4 × 106
a

Number of denoised sequences before normalization is given in brackets.

b

97% sequence similarity cutoff.

c

Higher numbers indicate more diversity; numbers in parentheses are 95% confidence intervals.

d

Mean±s.d.