Water samples were collected at all the above stations from 8 to 27 September 2006 from Shiyan 3, the research ship of the South China Sea Institute of Oceanology, Chinese Academy of Sciences. The sampling layers were designated according to the methods of ‘The specification for marine monitoring’

(GB17378-1998, China), and some stations were selected according to their depths. The depths included 0 m, 25 m , 50 m , 75 m , 100 m , 150 m , 200 m , 300 m , 400 m , 500 m , 600 m , 800 m , 1000 m , 1200 m , 1500 m , 2000 m , 2500 m , 3000 m  and 3500 m . Water samples were analysed for nitrate (NO3-N), nitrite (NO2-N), ammonium (NH4-N), silicate (SiO3-Si), phosphorus (PO4-P), dissolved oxygen (DO), chlorophyll a (Chl a), temperature (T), salinity (S), and pH ( Wang et al. 2006, 2008, 2011). DO was determined using the Winkler titration method immediately on board. Temperature (T) and Selleckchem BEZ235 salinity (S) were measured with SBE911 plus Conductive Temperature Depth (CTD). The other samples were passed through 0.45 μm GF/F filters, then poured into 500 m l LDPE bottles; following the addition of three drops of trichloromethane, the samples were deep-frozen immediately at –20°C. All the samples were analysed within two weeks of the

end of this cruise. All the parameters were detected according to ‘The specification for marine monitoring’ (GB17378-1998, China). The data sets consisted Bortezomib purchase of 14 parameters for 32 stations, which contained different depths at different stations since the depths of the stations were different from each other. Only the following data sets were analysed: from the surface layers at all stations (Data1), from deep station 14 (Data2), and silicate from 0 m  to 200 m  of the stations which had homologous layers (Data3). The parameters selected included silicate (SiO3-Si), nitrate (NO3-N), nitrite (NO2-N), ammonia (NH4-N), phosphorus (PO4-P), Temperature (T), Salinity (S), pH, dissolved oxygen (DO), chlorophyll a (Chl a), TIN, the Acesulfame Potassium ratio TIN/PO4-P,

the ratio of SiO3-Si/PO4-P and the depth of stations (DP). Initially, Data1 was used to show the surface distributions of every parameter, except DP, and to indicate the regions of upwelling. CA was then applied to cluster the stations into two groups to find which group was higher in nutrients; finally, PCA was used to analyse the parameters to identify the source of the nutrients and to decide which parameter could be used to reliably demonstrate regions of upwelling. Data2 and Data3 were selected to show the vertical and horizontal distributions of silicate, respectively, in order to show how upwelling was forming. Data1 was processed using Multivariate statistical analysis methods, such as CA and PCA. CA is an unsupervised pattern detection method that partitions all cases into smaller groups or clusters of relatively similar cases that are dissimilar to other groups (Lattin et al.