Horizontal and vertical distribution of mesozooplankton species richness and composition down to 2,300 m in the southwest Atlantic Ocean

• Published in: Zoologia (Curitiba)
• Main Authors: Sérgio L.C. Bonecker, Adriana V. de Araujo, Pedro F. de Carvalho, Cristina de O. Dias, Luiz F.L. Fernandes, Alvaro E. Migotto, Otto M.P. de Oliveira
• Format: Article in Journal/Newspaper
• Language: English
• Published: Pensoft Publishers 2014
• Subjects: Deep sea; diversity; southeastern Brazil; zooplankton; Zoology; QL1-991; Antarctic; Antarc*; NADW; North Atlantic Deep Water; North Atlantic
• Online Access: https://doi.org/10.1590/S1984-46702014000500005; https://doaj.org/article/0e3c539011f842409fb893aa89b779bf

We describe the species richness, distribution and composition of mesozooplankton over the continental shelf and slope, and in the water masses in the Campos Basin, southwest Atlantic Ocean. We analyzed the mesozooplankton from two oceanographic cruises (rainy and dry seasons, 2009) with samples taken in five different water masses from the surface to 2,300 m depth. In the Subsurface Water (SS), in both sampling periods, more species were recorded over the slope (rainy: 100; dry: 128) than the continental shelf (rainy: 97; dry: 104). Over the slope, species richness decreased with increasing depth: the highest values were observed in the South Atlantic Central Water (SACW), and the lowest values in the North Atlantic Deep Water (NADW), in both sampling periods. We recorded 262 species in 10 groups (Hydrozoa, Siphonophora, Ctenophora, Branchiopoda, Copepoda, Euphausiacea, Decapoda, Chaetognatha, Appendicularia e Thaliacea), with 13 new occurrences for the southwest Atlantic. Copepoda was the group with the highest species richness, containing 138 species. In both periods, the samples from SS, SACW and Antarctic Intermediate Water (AAIW)/Upper Circumpolar Deep Water (UCDW) were clustered in different faunistic zones, based on species composition. This study confirmed that zooplankton richness in the southwest Atlantic Ocean is underestimated, and suggests that additional efforts must be directed toward a better understanding of this fairly unknown region.