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. 2012 Aug;78(15):5070–5076. doi: 10.1128/AEM.00400-12

Table 1.

Substrate additions and 2,4-D mineralization rates in long-term laboratory incubations of surface ice cores from GrIS and estimated 2,4-D degradation potential on the surface of GrIS

Microcosma No. of days Amt of 2,4-D added
Amt of 2,4-D mineralized (nmol) tfdA gene copy no. (104) 2,4-D degradation potential
dpm nmol nmol day−1 m−2 ng C day−1 m−2
1a 133 49,234 1.30 0.17 <1 0.65 16
1b 166 50,338 1.33 0.12 <1 0.38 9.0
1c 206 46,802 1.23 0.13 <1 0.31 7.4
2a 133 49,234 1.30 0.82 <1 3.07 74
2b 166 50,338 1.33 0.53 <1 1.60 38
2c 206 46,802 1.23 0.46 <1 1.12 27
3a 133 49,234 1.30 0.56 <1 2.09 50
3b 166 48,308 1.27 0.35 <1 1.05 25
3c 206 46,802 1.23 0.48 <1 1.16 28
Control a 133 49,234 1.30 0.13 NDb 0.49 12
Control b 166 48,308 1.27 0.14 ND 0.42 10
Control c 206 46,802 1.23 0.11 ND 0.27 6.5
4 451 48,252 1.27 0.22 <1 0.24 5.8
5 451 48,252 1.27 0.51 <1 0.57 14
6 451 48,252 1.27 0.91 <1-1.7 1.00 24
Control (4–6) 451 48,252 1.27 0.25 ND 0.28 6.8
7 451 53,358 1.32 0.29 1.5-3.1 0.32 31
8 451 53,358 1.32 0.13 <1 0.14 13
9 451 53,358 1.32 0.23 <1 0.26 25
Control (7–9) 451 53,358 1.32 0.13 ND 0.15 14
a

a, b, and c, 1st, 2nd, and 3rd additions, respectively.

b

ND, not determined.