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. 2016 Oct 27;7:1705. doi: 10.3389/fmicb.2016.01705

Table 4.

Comparison between the physiological characteristics of heterotrophic microorganisms in SLW and those of other aquatic environments.

Location Climate Salinity Doubling time (days) Growth Efficiency Leu:TdR Reference
Subglacial Lake Whillans Polar (Antarctic) Fresh 118 0.08 3.6 This study
Ross Sea Polar (Antarctic) Saline 4.33 0.24 9.2 Carlson et al., 1999; Ducklow et al., 2001
McMurdo Ice Shelf Polar (Antarctic) Saline 23.1 0.70 11 Vick-Majors, 2016
Northeast Atlantic Ocean Subtropical Saline 0.78 (0.46) 0.16 (0.15) 19.7 (12.6) Alonso-Sáez et al., 2007
North Pacific Ocean Temperate Saline 0.33 (0.79) 0.15 (0.05) 8.9 (3.7) del Giorgio et al., 2011
Svalbard (Kongsfjorden) Polar (Arctic) Saline 3.69 0.13 7.9 Motegi et al., 2013
East Lake Bonney Polar (Antarctic) Fresh 15.5 (39.1) 0.29 (0.05)* 18.6 Vick and Priscu, 2012
West Lake Bonney Polar (Antarctic) Fresh 7.2 (8.7) 0.32 (0.04)* 39.7 Vick and Priscu, 2012
Lake Fryxell Polar (Antarctic) Fresh 33.6 (77.9) 0.49 (0.07)* 59.1 Vick and Priscu, 2012
Mackenzie River Polar (Arctic) Fresh 1.79 0.65* 4.92 Galand et al., 2008
Beaufort Sea Coast Polar (Arctic) Saline 6.16 0.47* 5.50 Galand et al., 2008
Greenland Polar (subarctic) Saline 0.44 0.11* 69.1 Kaartokallio et al., 2013
Deep subsurface sediments Temperate Saline ~1–1000 years Reviewed by Jørgensen (2011)

Leu:Tdr is the molar ratio of leucine to thymidine incorporation. Doubling times were determined from published growth rates as ln2/growth rate, or from growth rates calculated from published rates of carbon production and bacterial abundance.

*

indicates that published bacterial production data was used to estimate growth efficiency according to the relationship between bacterial respiration and bacterial production described by del Giorgio and Cole (1998) and used by Takacs et al. (2001) for Antarctic surface lakes. Parentheses indicate standard deviations calculated for studies that included multiple samples, either in space or time.