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Turbulence and hypoxia contribute to dense biological scattering layers in a Patagonian fjord system

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Figure

Figure 1. Study area in relation to South America and the PacificOcean shown in the inset
Figure 2. (a, c, e ,g) Profiles of temperature (a, b), salinity (c, d), dissolved oxygen (e, f) and nitrate (g) collected during different oceano-graphic campaigns in the northern central part of Puyuhuapi Fjord and (b, d, f) in the eastern region of the Jacaf Channel.
Table 1. Data set collected during oceanographic campaigns in Puyuhuapi Fjord and Jacaf Channel.
Figure 3. (a) Volume backscattering strength (plankton groups (and the times of in situ zooplankton sampling (black dots) carriedout during 25–26 May 2013.and 18:00 (local time) on 25 May andSv) calculated fromthe ADCP-1 backscatter signal in Puyuhuapi Fjo
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