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. 2014 Jun 12;9(6):e99312. doi: 10.1371/journal.pone.0099312

Table 1. Physical and chemical properties of the studied regions.

Location Temp. NO3 [1%PAR] Δσt 1%PARz UMLz Inline graphic Inline graphic
Temperate N (n = 8) 15.9±3.5 6.7±1.6 0.6±0.5 68±23 64±35 28±29 1.4±0.8
Temperate S (n = 4) 13.4±4.5 9.8±4.2 0.4±0.2 57±22 50±15 33±26 1.2±0.3
Oligotrophic N (n = 5) 22.3±2.3 1.9±1.5 0.8±0.5 115±14 47±13 2.8±1.5 2.6±0.8
Oligotrophic S (n = 13) 24.4±2.9 0.9±1.2 0.9±0.6 126±24 59±22 1.1±1.5 2.6±1.4
Upwelling (n = 8) 27.3±1.4 14.0±2.1 3.2±0.6 83±13 29±12 4.4±0.9 3.3±1.6
Coastal (n = 26) 15.3±2.0 6.8±3.2 0.8±0.6 20±4 7±4 11.5±7.6 3.9±2.2
Soiree In (n = 6) 2.8±0.1 23.2±1.1 0.02±0.01 47±1 72±3 - -
Soiree Out (n = 2) 2.7±0.0 25.4±0.4 0.23±0.02 74±8 69±2 - -

Mean (± standard deviation) values of sea surface temperature (°C, Temp.), nitrate concentration at the base of the euphotic layer (NO3 [1%PAR], µmol L−1), density difference between the surface and the base of the euphotic layer (Δσt, kg m−3), euphotic layer depth (1%PARz, m), and upper mixed layer depth (UMLz, m) for each location. For the regions where the resource supply index was calculated, the mean values of NO3 [1%PAR] divided by Δσt and 1%PARz divided by UMLz are also given. n is the number of measurements conducted at each location. Nitrate concentration data for the Soiree study correspond to 40 m depth [31].