TY - JOUR
T1 - Small-scale effects of a river plume front on the distribution of salps and doliolids
AU - Höfer, Juan
AU - Weidberg, Nicolás
AU - Molina-Ramírez, Axayacatl
AU - Cañas-Rueda, Andrés
AU - García-Flórez, Lucía
AU - Fernández-Rueda, María Del Pino
AU - Acuna, Joséluis
N1 - Publisher Copyright:
© The Author 2015.
PY - 2015
Y1 - 2015
N2 - River plumes are important features in coastal ecosystems and more studies are necessary to improve our knowledge about their influence on the distribution and dispersion of plankton, especially at small scales. Four surveys were conducted in the Nalón River mouth (Spain, southern Bay of Biscay) to study the effect of the river plume front on the distribution of doliolids (Doliolum nationalis) and salps (Thalia democratica). During each survey, surface currents, physicochemical variables and plankton distribution were measured by means of several GPS-tracked drifters, a CTD probe and a surface floating bongo net. Thaliacean abundance was related mainly to the intensity of the offshore convergent flow at the plume front, and less to physicochemical or biological parameters. Surface thaliacean abundances were lower at the plume and higher on the oceanic side of the front, and peaked closer to the foam line in fronts with stronger convergent flow. the distance between the point of maximum thaliacean abundance and the front was significantly correlated with a ratio of individual swimming speed to convergent current velocity. We interpret this result in terms of their capacity to oppose convergent flow.
AB - River plumes are important features in coastal ecosystems and more studies are necessary to improve our knowledge about their influence on the distribution and dispersion of plankton, especially at small scales. Four surveys were conducted in the Nalón River mouth (Spain, southern Bay of Biscay) to study the effect of the river plume front on the distribution of doliolids (Doliolum nationalis) and salps (Thalia democratica). During each survey, surface currents, physicochemical variables and plankton distribution were measured by means of several GPS-tracked drifters, a CTD probe and a surface floating bongo net. Thaliacean abundance was related mainly to the intensity of the offshore convergent flow at the plume front, and less to physicochemical or biological parameters. Surface thaliacean abundances were lower at the plume and higher on the oceanic side of the front, and peaked closer to the foam line in fronts with stronger convergent flow. the distance between the point of maximum thaliacean abundance and the front was significantly correlated with a ratio of individual swimming speed to convergent current velocity. We interpret this result in terms of their capacity to oppose convergent flow.
KW - Bay of Biscay
KW - Convergent current
KW - Plume front
KW - Swimming ability
KW - Thaliacea
UR - http://www.scopus.com/inward/record.url?scp=84958235144&partnerID=8YFLogxK
U2 - 10.1093/plankt/fbv085
DO - 10.1093/plankt/fbv085
M3 - Article
AN - SCOPUS:84958235144
SN - 0142-7873
VL - 37
SP - 1166
EP - 1180
JO - Journal of Plankton Research
JF - Journal of Plankton Research
IS - 6
ER -