“…These diatom species are also found in Antarctic waters (Gonçalves-Araujo et al, 2015), indicating that Antarctic and subantarctic communities have an important influence on the southern Patagonian region, through advection of subantactic water from the shelf-break region (Olguín et al, 2006;Olguín and Alder, 2011;Gonçalves-Araujo et al, 2012;Olguín Salinas et al, 2015). Such predominance of diatoms in spring has been described for other domains across the Argentine Sea such as the northern shelf, in the La Plata outflow region (Carreto et al, 2008), shelfbreak (Olguín et al, 2006;Garcia et al, 2008;Segura et al, 2013), farther offshore (Olguín et al, 2006;Olguín Salinas et al, 2015) and in subantarctic waters at the Brazil-Malvinas Confluence (Gonçalves-Araujo et al, 2012). Moreover, it is a tenet of phytoplankton ecology that the dominance of fast growing diatoms in temperate latitudes is mainly related to water column structure, through the establishment of sunlit surface waters containing winter-accumulated nutrients, which triggers massive spring phytoplankton blooms (Sverdrup, 1953).…”