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. 2015 Jul 21;10(1):39–50. doi: 10.1038/ismej.2015.105

Table 1. Brief description of the study sites.

Station Date Depth (m) ML (m) Temp (°C) Chl a (μg l−1)a DOC (μM) BA (× 108 cells l−1) BHP (ng C l−1 h−1) μ (d−1)b
R-2 26 Oct 2450 105±15 2.1 0.3±0.1 48±0 2.7±0.3 2.6±0.1 0.02±0.00
A3-1 20 Oct 527 168±11 1.7 0.6±0.2 52c 3.9±0.1 5.0±1.6 0.02±0.00
A3-2 16 Nov 527 153±15 2.2 2.0±0.3 51±2 3.2±0.5 19.9±3.8 0.12±0.01
A3-3 19 Jand 527 52±12 3.5 1.3±0.3 NA 4.8±0.2 103±5 0.42±0.02
A3-4 12 Febd 527 84±19 3.9 1.0±0.1 NA 5.7± 0.6 69±14 0.23±0.04
F-L 07 Nov 2690 38±7 4.2 4.0±1.6 50±1 6.1c 65.7±1.6 0.21c
E-1 30 Oct 2050 72±38 2.5 0.9±0.1 48±1 4.3±0.1 15.2±0.7 0.07±0.00
E-3 04 Nov 1923 38±9 2.8 0.6±0.1 49±1 5.1c 24.9±1.7 0.09c
E-4E 13 Nov 2210 74±8 3.2 1.1±0.0 50±2 5.6c 41.5±2.6 0.14c
E-4W 10 Nov 1398 61±11 2.5 1.3±0.1 49±0 6.0±0.1 29.1±3.9 0.09±0.01

Abbreviations: BA, bacterial abundance; BHP, bacterial heterotrophic production; Chla, chlorophyll a; DOC, dissolved organic carbon; NA, not available; temp, temperature; μ, bacterial growth rate.

For all parameters mean values±s.d. for the mixed layer (ML) are provided.

b

Bacterial growth rate was determined by diving bacterial heterotrophic production by bacterial biomass. To convert bacterial abundance to biomass, a conversion factor of 12.3 fg C per cell was used (Fukuda et al., 1998).

c

Only one data point was available for the ML.

d

Samples were taken during the KEOPS1 cruise in January–February 2005 (Obernosterer et al., 2008).