Turbulence as a driver for vertical plankton distribution in the subsurface upper ocean

  1. DIEGO MACÍAS 1
  2. ÁNGEL RODRÍGUEZ-SANTANA 2
  3. EDUARDO RAMÍREZ-ROMERO 3
  4. MIGUEL BRUNO 4
  5. JOSEP L. PELEGRI 5
  6. PABLO SANGRÀ 2
  7. BORJA AGUIAR-GONZÁLEZ 2
  8. CARLOS M. GARCÍA 3
  1. 1 European Commission, Joint Research Center, Institute for Environment and Sustainability, Water Research Unit, Via E. Fermi 2547, 21027-Ispra, Italy.
  2. 2 Departamento de Física, Universidad de Las Palmas de Gran Canaria, Campus Universitario de Tafira, 35017 Las Palmas de Gran Canaria, Spain
  3. 3 epartamento de Biología, University of Cadiz, 11510 Puerto Real, Cadiz, Spain
  4. 4 Departamento de Física Aplicada, University of Cadiz, 11510 Puerto Real, Cadiz, Spain
  5. 5 Institut de Ciències del Mar, CSIC, 08003 Barcelona, Spain.
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Revista:
Scientia Marina

ISSN: 0214-8358

Año de publicación: 2013

Volumen: 77

Número: 4

Páginas: 541-549

Tipo: Artículo

DOI: 10.3989/SCIMAR.03854.03A DIALNET GOOGLE SCHOLAR lock_openAcceso abierto editor

Otras publicaciones en: Scientia Marina

Resumen

La turbulencia como mecanismo forzante de la distribución vertical del plancton en el océano subsuperficial. – Las distribuciones verticales de la tasa de disipación de la energía turbulenta y de la fluorescencia han sido medidas simultáneamente usando un microperfilador de alta resolución en cuatro regiones oceánicas distintas, desde zonas templadas a polares y desde regiones costeras al océano abierto. Valores altos de fluorescencia, conformando un máximo profundo de clorofila (MPC) fueron detectados habitualmente en regiones poco estratificadas de la columna de agua y justo por debajo de capas con valores máximos de la tasa de disipación de la energía turbulenta. En las cercanías del MPC se encontró una relación estadísticamente significativa y negativa entre los valores de fluorescencia y energía turbulenta. En este trabajo se discuten los posibles mecanismos que pueden explicar estas relaciones, incluyendo el efecto de la variación vertical del coeficiente de difusión y la posible alteración de la velocidad de sedimentación de las células de fitoplancton por el movimiento turbulento. Estos resultados proporcionan un mayor conocimiento sobre los procesos que controlan la distribución vertical de la comunidad pelágica y la posición de los MPC

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