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. 2015 Jul 21;9(8):1904. doi: 10.1038/ismej.2015.112

An active atmospheric methane sink in high Arctic mineral cryosols

M C Y Lau, B T Stackhouse, A C Layton, A Chauhan, T A Vishnivetskaya, K Chourey, J Ronholm, N C S Mykytczuk, P C Bennett, G Lamarche-Gagnon, N Burton, W H Pollard, C R Omelon, D M Medvigy, R L Hettich, S M Pfiffner, L G Whyte, T C Onstott
PMCID: PMC4511938  PMID: 26194094

Correction to: The ISME Journal (2015) 9, 1880–1891; doi:10.1038/ismej.2015.13; published online 14 April 2015

Since the publication of this article, the authors have identified an error in the reported values for CH4 oxidation rates calculated from the microcosm experiment (Table 1), which also affected the reported Q10 values (on page 7 and Figure 3):

At 66% and 100% saturations, the Q10 values fell within the range of 1.3–2.9 values previously reported from incubation experiments carried out at atmospheric or elevated CH4 concentrations (Figure 3). In contrast, the Q10 value was 8 at 33% saturation (Figure 3).

The revised text is:

At 100% saturations, the Q10 values fell within the range of 1.3–2.9 values previously reported from incubation experiments carried out at atmospheric or elevated CH4 concentrations (Figure 3). In contrast, the Q10 value was 6 at 33% and 66% saturations (Figure 3).

Table 1 and Figure 3 have been amended to reflect these changes.

The authors would like to apologize for any inconvenience this may have caused.


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