Pyridine nucleotide levels in zooplankton: laboratory work and field samples

[ES]La respiración es un proceso fisiológico común a todos los organismos marinos. En los estudios oceanográficos se ha determinado, comúnmente, mediante la cuantificación del consumo de oxígeno de organismos incubados en botellas. Esta metodología es tediosa y lenta, por lo que Packard et al. (1971) propusieron el uso del análisis bioquímico basado en la actividad de las enzimas implicadas en la respiración, el Sistema de Transporte de Electrones (ETS). Este análisis mide la velocidad máxima que dichas enzimas pueden tener, determinando la respiración potencial de los organismos. Dicha velocidad estará controlada por la disponibilidad intracelular de sus sustratos, los piridín nucleótidos (NADH y NADPH). En el presente trabajo, se ha analizado el metabolismo respiratorio, a través de medidas del ETS y de los piridín nucleótidos, tanto en el dinoflagelado Oxyrrhis marina en estudios de laboratorio, como en organismos recogidos del medio marino durante la campaña de circunnavegación MALASPINA 2010

Zooplankton, micronekton and biological pump: Beyond the mesopelagic zone

[EN] Migrant biota transports carbon to the mesopelagic zone due to their feeding at the shallower layers and their defecation, respiration, excretion and mortality at depth. The so-called active flux has been considered a small number compared to gravitational sinking. Recent assessments in subtropical waters show an important effect due to predation by interzonal diel vertical migrants (DVMs). The consumption and subsequent transport of epipelagic zooplankton by DVMs (mainly micronekton) to the mesopelagic zone seemed similar to the mean gravitational export. However, the consequences of this active transport to the bathypelagic zone are almost unknown. Here, we show the effect of the Atlantic and Pacific equatorial upwelling systems on the vertical distribution of acoustic backscatter from the surface to bathypelagic depths. The enhancement of the acoustic signal below the upwelling zone was observed to reach 4000 m depth, coinciding with high abundances and activity of bacteria at those depths. The results suggest an active carbon transport from the epipelagic driven by zooplankton and micronekton, enhancing the efficiency of the biological pump and giving an insight about the fate of an increased productivity at the shallower layers of the ocean

Zooplankton oxygen consumption and nutrient release in relation to species composition, animals size and enviromental conditions in the Baltic Sea during May and August

[EN] Zooplankton metabolism in terms of oxygen consumption and ñutrient reléase (ammonia, phosphate) were measiu'ed in the Baltic Sea, a températe área with high envirormiental changes both in space and in time. Plankton of the surface layer were analysed with balance measurements in 4 size classes between 50 and 1000 nm during spring in 1988, 1990 and 1991, in summer 19^8 and 1990 as well. The use of electrón transport system (ETS), and the Glutamate Dehydrogenase (GDH) activity as indicators for respiration and ammonia reléase respectively, enlarged the data density and made a three dimensional resolution available (May 1990, 1991). Data are in the range of the latitudinal dependend magnitude. They reflect slight interannual, more seasonal and regional aspects. Animáis size, temperature, food concentration, and species composition influence the specific rates

The use of image analysis systems for the assesment of zooplankton physiological rates and carbon fluxes

Trabajo realizado por: Garijo, J. C., Hernández León, S.

The use of AARS activity as a proxy for zooplankton and ichthyoplankton growth rates

Programa de doctorado en Oceanografía