Foraminíferos bentónicos recientes en sedimentos de fondo de la cuenca de panamá (pacífico colombiano), como indicadores de productividad y oxigenación
Por:
Betancur M.J., Martínez I.
Publicada:
1 ene 2003
Resumen:
Thirteen deep-sea samples (core-tops) from the Panama Basin, Colombian Pacific, were analysed for benthonic foraminifera in the >150µm size fraction. Based on the microfaunal content, three zones are recognised in the Panama Basin: (1) northern euphrophic region (~8° to 5,5°N), characterized by a high concentration of organic matter flux to the seafloor, oxygenated sediments, and influence of the Panama Bight and the Costa Rica Dome upwelling systems, (2) mesotrophic region (~5,5 to 2°N), characterized by low fluxes of organic carbon to the seafloor, oxygenated sediments, terrigenous influence and fluctuations of the upwelling systems of the basin, and (3) southern euphotic region (south of ~2°N), characterized by a larger organic carbon flux to the seafloor, low oxygen content (disoxia) and influence of the Equatorial Divergence.
Filiaciones:
Betancur M.J.:
Area de Ciencias del Mar, Departamento de Geología, Universidad EAFIT, A.A. 3300, Medellín, Colombia
Martínez I.:
Area de Ciencias del Mar, Departamento de Geología, Universidad EAFIT, A.A. 3300, Medellín, Colombia
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