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. 2008 Jan 25;74(6):1767–1779. doi: 10.1128/AEM.01668-07

TABLE 2.

Vertical profile of some bacterial subgroup abundances through the epi- and mesopelagic zones in the northwest Atlantic Ocean during cruise COCA-2, at station 32, 26.00°N, 26.00°Wa

Depth (m) Chl concn (mg m−3) TPA (no. of cells [105] ml−1) % HNA cells PHP (μg carbon liter−1 day−1) SGR (day−1) No. of CTC+ cells (104) ml−1 No. of “live” cells (105) ml−1 % CTC+ cells % “Live” cells
5 0.04 6.68 38.6 6.32 ± 0.65 0.398 4.79 4.61 7.2 69.6
50 0.05 6.76 37.2 6.18 ± 0.73 0.383 2.32 3.4
100 0.15 4.14 26.6 4.09 ± 0.39 0.416 2.38 4.06 5.7 61.0
120 0.25 5.24 24.2 1.99 ± 0.16 0.181 6.22 3.94 11.9 63.4
130 0.65 6.79 34.8 10.99 ± 1.42 0.580 6.59 4.41 9.7 46.0
150 0.45 6.11 53.0 21.22 ± 1.11 0.954 2.58 3.93 4.2 46.5
200 0.04 2.85 51.4 0.94 ± 0.04 0.158 1.05 2.59 3.7 49.6
300 <0.01 2.41 52.6 0.26 ± 0.05 0.053 1.04 1.49 4.3 44.0
400 <0.01 2.20 54.1 0.15 ± 0.03 0.034 0.98 44.7
500 <0.01 2.38 50.4 0.19 ± 0.04 0.040 0.68 28.5
600 <0.01 2.36 57.9 0.21 ± 0.07 0.042 0.83 0.46 3.5 31.4
700 <0.01 2.06 49.5 0.11 ± 0.04 0.026 0.69 42.4
800 <0.01 1.86 54.9 0.06 ± 0.01 0.015 0.30 21.9
900 <0.01 1.88 47.7 0.11 ± 0.01 0.030
1,000 <0.01 2.41 38.6 0.05 ± 0.02 0.011 0.57 0.24 2.4 21.1
a

Prokaryote heterotrophic production (PHP) is the average of leucine and thymidine incorporation values converted with empirically derived conversion factors. Chl, chlorophyll; TPA, total prokaryote abundance determined by SG1 staining; SGR, heterotrophic prokaryote specific growth rate.