FN Archimer Export Format PT J TI Spatial patterns in planktonic cnidarian distribution in the western boundary current system of the tropical South Atlantic Ocean BT AF Tosetto, Everton Giachini Bertrand, Arnaud Neumann-Leitão, Sigrid Costa da Silva, Alex Nogueira Júnior, Miodeli Irigoien, Xabier AS 1:1;2:1,2,3;3:1;4:1;5:4;6:; FF 1:;2:;3:;4:;5:;6:; C1 Departamento de Oceanografia, Universidade Federal de Pernambuco, Avenida Arquitetura, S/N, 50670-901, Recife, PE, Brazil Institut de Recherche pour le Développement (IRD), MARBEC, Univ Montpellier, CNRS, Ifremer, IRD, 34200 Sète, France Departamento de Pesca e Aquicultura, Universidade Federal Rural de Pernambuco, Rua D. Manuel de Medeiros, S/N, 52171-900, Recife, PE, Brazil Departamento de Sistemática e Ecologia, Universidade Federal da Paraíba, Cidade Universitária, 58051-900, João Pessoa, PB, Brazil C2 UNIV FED PERNAMBUCO UFPE, BRAZIL IRD, FRANCE UNIV FED RURAL PERNAMBUCO UFRPE, BRAZIL UNIV FED PARAIBA, BRAZIL UM MARBEC IN WOS Cotutelle UMR copubli-int-hors-europe copubli-sud IF 2.473 TC 13 UR https://archimer.ifremer.fr/doc/00678/79000/87020.pdf LA English DT Article CR ABRACOS BO Antea DE ;medusae;siphonophores;tropical Atlantic Ocean;South Equatorial Current;North Brazil Undercurrent;Fernando de Noronha chain;Northeast Brazil AB In marine western boundary systems, strong currents flowing coastward spread oceanic water masses over the continental shelves. Here we propose to test the hypothesis according to which oceanic cnidarian species may dominate western boundary system regions even in coastal waters. For that purpose we use a set of data collected above the shelf, slope and around oceanic seamounts and islands in the Western Tropical South Atlantic. Samples were acquired with a plankton net with 300 μm mesh size over 34 stations during an oceanographic cruise carried out in October 2015. Results reveal a diverse cnidarian assemblage in the area, extending the known distribution of many species. In addition, the Fernando de Noronha Chain and most of the narrow continental shelf presented a typical oceanic cnidarian community, dominated by holoplanktonic siphonophores. In this western boundary system, this condition was likely driven by the strong currents, which carry the oceanic tropical water and associated planktonic fauna toward the coast. A specific area with reduced influence of oceanic currents presented typical coastal species. The pattern we observed with the dominance of oceanic plankton communities up to coastal areas may be typical in western boundary systems characterized by a narrow continental shelf. PY 2021 PD MAR SO Journal Of Plankton Research SN 0142-7873 PU Oxford University Press (OUP) VL 43 IS 2 UT 000642325100013 BP 270 EP 287 DI 10.1093/plankt/fbaa066 ID 79000 ER EF