Fig. 2
From: Subtropical coastal microbiome variations due to massive river runoff after a cyclonic event
A Trajectory of Uesi cyclone (Photography from Hinawara 8 satellite: https://himawari8.nict.go.jp/). B Dumbéa River flow during and after the cyclone passage, including the 6 days of sampling, and in relation with the other rivers considered in this study. C PCA performed on Euclidian distance and based on eight selected environmental descriptors (Temperature; Salinity; Ni: Particulate nickel concentration; HIX: Humification Index of FDOM; BIX: Biological Index of FDOM; S1: Molecular weight of CDOM; DON: Dissolved Organic Nitrogen; POC: Particulate Organic Carbon) and after D exclusion of the outgroup samples collected the first day after the cyclone passage at Dumbéa Bay (DB-B1). The data variance for the two first dimension of the PCA analyses are indicated on the axes. The different sampling stations are labeled according to the sample campaign and in color tones representing either the coastal-off shore gradients (dry season) or the sampling days sampled after the cyclone (D1-D6) in the different fixed point of the studied bays (DB: Dumbea bay; GR: Grand Rade) and the buoys (B1 and B2) trajectories