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Table 1 Values of turbulent kinetic energy (k), dissipation rate of energy (ɛ) and length (η) and velocity (v t ) Kolmogorov scales at different discrete depths under different wind conditions (U 10) in the southern Gulf of Mexico

From: Vertical segregation of holoplanktonic molluscs in the epipelagic layer, southern Gulf of Mexico

Stratum (m)

Depth (m)

k (J kg−1)

ɛ (m2 s−3)

η (mm)

v t (cm s−1)

Zooplankton (ml 100 m−3)

Molluscs (ind 100 m−3)

May (U 10 = 3.8 m s−1)

 0–6

3

1.51 × 10−2

2.26 × 10−3

0.14

6.89 × 10−1

31.8 ± 23.8

281.0 ± 368.1

 6–12

6

8.54 × 10−3

1.28 × 10−3

0.17

5.98 × 10−1

41.8 ± 37.2

421.3 ± 591.5

 12–18

12

2.73 × 10−3

4.09 × 10−3

0.22

4.49 × 10−1

33.5 ± 28.9

221.8 ± 217.2

 45–55

45

5.17 × 10−6

7.75 × 10−7

1.06

9.38 × 10−2

14.2 ± 6.2

43.4 ± 37.6

 95–105

95

4.42 × 10−10

1.14 × 10−10

9.66

1.03 × 10−2

13.6 ± 16.0

28.3 ± 18.1

November (U 10 = 6.1 m s−1)

 0–6

3

3.27 × 10−2

4.19 × 10−3

0.12

8.04 × 10−1

37.7 ± 24.5

134.6 ± 159.3

 6–12

6

2.16 × 10−2

2.76 × 10−3

0.14

7.25 × 10−1

31.4 ± 25.7

218.4 ± 354.1

 12–18

12

9.40 × 10−3

1.20 × 10−3

0.17

5.89 × 10−1

21.0 ± 15.8

192.4 ± 283.5

 45–55

45

9.70 × 10−5

1.24 × 10−5

0.53

1.87 × 10−1

10.3 ± 6.3

54.1 ± 62.9

 95–105

95

1.18 × 10−7

3.32 × 10−8

2.34

4.27 × 10−2

8.4 ± 5.6

86.6 ± 148.2

  1. Mean zooplankton biomass (\( \overline{X} \) ± SD) and density of the holoplanktonic molluscs (\( \overline{X} \) ± SD) of each stratum are also shown