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. 2010 Jul 22;5(1):150–160. doi: 10.1038/ismej.2010.100

Table 1. Cryoconite holes sampled during this study during 2006 and 2007 on glaciers AB, ML and VB.

Sample code Physico-chemical data Clone Library T-RFLP No. of peaks T-RFLP Shannon diversity index (H′) T-RFLP Gini coefficient (Gcorr)
AB601 + + ND ND ND
AB602 +   42 4.12 0.340
AB603 +   16 2.657 0.389
AB604 +   32 3.53 0.430
AB605 +   9 2.129 0.309
AB606 + + 17 2.845 0.322
AB701   + 35 3.926 0.301
AB702     17 2.751 0.369
AB703     20 2.878 0.422
AB704     7 1.767 0.416
AB705     16 2.709 0.358
AB706   + 12 2.364 0.362
AB mean     20.3 2.88 0.365
           
ML601 + + 33 3.53 0.426
ML602 +   47 4.261 0.469
ML603 +   37 3.635 0.500
ML604     12 2.283 0.448
ML605     37 3.679 0.484
ML606   + 39 3.721 0.488
ML701   + 24 3.15 0.406
ML702     15 2.55 0.439
ML703     14 2.537 0.391
ML704     8 1.886 0.419
ML705     13 2.458 0.375
ML706   + 12 2.307 0.407
ML mean     24.3 3.00 0.438
           
VB601 + + 43 4.115 0.366
VB602 +   7 1.763 0.421
VB603 +   34 3.767 0.388
VB604     35 3.613 0.445
VB605     21 3.005 0.386
VB606   + 41 3.87 0.440
VB701   + 39 3.892 0.368
VB702     30 3.555 0.376
VB703     24 3.227 0.387
VB704     6 1.532 0.469
VB705     25 3.237 0.366
VB706   + 7 1.775 0.380
VB mean     26.0 3.11 0.399
           
By glacier
 ANOVA (P)     0.558 0.787 0.001
 ANOVA (F)     0.59 0.24 9.24
           
By year
 ANOVA (P)     0.005 0.015 0.134
 ANOVA (F)     8.91 6.56 2.35

ND indicates low quality T-RFLP data.