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. 2018 Jul 18;165(8):129. doi: 10.1007/s00227-018-3386-z

Table 7.

Overview of the average energetic densities of Bathylagus antarcticus

Season Location n Mean size (mm) WW (g) DW (g) Water content (%) Mean energy density Method Source
kJ g−1 WW kJ g−1 DW
Summer Macquarie 18 116.8 ± 35.4 SD 14.2 ± 14.2 SD 2.7 ± 2.8 SD 81.7 ± 1.9 SD 3.93 ± 1.17 SD 21.43 ± 4.88 SD BC Tierney et al. (2002)
Autumn Lazarev Sea 7 77.6 ± 23.4 SD 3.1 ± 3.6 SD 0.4 ± 0.4 85.6 ± 2.5 SD 2.92 ± 0.42 SD 20.36 ± 1.32 SD BC Van de Putte et al. (2006)
Weddell Sea 32 77.2 3.8 0.5 85.9 ± 2.0 SD 2.24 15.89 PC Donnelly et al. (1990)a
Winter Scotia Sea 16 90 7.8 0.9 88.4 ± 1.4 SD 1.72 14.83 PC Donnelly et al. (1990)
Spring Ross Sea (p) 151a ± 20 SE 38.6 ± 18.2 SE 4.9 87.3 2.9 22.83 BC Lenky et al. (2012)
Scotia Sea 8 99.4 5.8 0.9 85.1 ± 2.1 SD 2.22 14.89 PC Donnelly et al. (1990)

Energy density measurements were done using bomb calorimetry (BC) and proximate composition (PC). Energetic values in italics represent values that were converted using information from the given sources. n represents the number of samples measured. Where this expresses samples of pooled individuals, this is indicated with (p). The standard error (SE) or standard deviation (SD) as given in the original source is added where available. The mean size is given in standard length (SL) unless otherwise indicated

aMeasured in total length (TL)

bA factor of 4.19 was used to convert calories to joules