Efectos potenciales del marisqueo sobre moluscos gasterópodos de interés comercial ("Osilinus" spp. y "Patella" spp.) en el Archipiélago Canario

Abstract.- This study assessed the effects of human influences over the abundance and size patterns of five species of gastropods (top-shell snails and limpets) commonly collected in the Canarian Archipelago: ‘burgado hembra’ (Osilinus atrata), ‘burgado macho’ (Osilinus sauciatus), ‘lapa blanca’ (Patella aspera), ‘lapa negra’ (Patella candei crenata) and ‘lapa de sol’ (Patella rustica). We studied patterns of abundance and size of these species across three islands (Lanzarote, La Graciosa and Alegranza) corresponding to three levels of human influence: high, medium and low, respectively; which were quantified through three indicators: human pressure (inhabitants km-1 d-1), accessibility to the coast (km of sealed and unsealed roads), and volumes of capture (kg). The abundances of O. atrata and P. aspera were statistically higher at Alegranza than at La Graciosa and Lanzarote, whereas the density was 10 to 15 times larger at Alegranza for four of the five studied species. Significant differences in the size structure of the species among islands (= levels of human influence) were also observed. Not only all large-sized individuals disappeared at Lanzarote and La Graciosa, yet there was a decrease in numbers for the majority of size ranges. Thought populations of top-shell snails and limpets were affected by natural variability, human activities turned out to be the major driver for the observed differences among islands. These results seriously question the effectiveness of the current shellfish regulations contained in the Regional Fish Law. Resumen.- Este estudio determinó los efectos de la influencia humana sobre la abundancia y la estructura de talla de cinco especies de moluscos gasterópodos comúnmente recolectados en el Archipiélago Canario: el ‘burgado hembra’ (Osilinus atrata), el ‘burgado macho’ (Osilinus sauciatus), la ‘lapa blanca’ (Patella aspera), la ‘lapa negra’ (Patella candei crenata) y la ‘lapa de sol’ (Patella rustica). Se analizaron tres islas (Lanzarote, La Graciosa y Alegranza) correspondientes a tres categorías de influencia humana: alta, media y baja, respectivamente; cuantificadas a través de tres indicadores: la presión humana (hab km-1 d-1), la accesibilidad a la costa (km de red viaria) y los volúmenes de extracción de los recursos (kg). La abundancia de O. atrata y P. aspera fue estadísticamente mayor en Alegranza que en La Graciosa y Lanzarote, mientras que los valores de densidad fueron de 10 a 15 veces superiores en Alegranza para cuatro de las cinco especies estudiadas. Para la estructura de talla, se detectaron notables diferencias entre islas (= niveles de influencia humana). En Lanzarote y La Graciosa no sólo desaparecieron los ejemplares de mayor talla, sino que disminuyeron los ejemplares para la mayoría de rangos de talla. A pesar que la variabilidad natural de las poblaciones de burgados y lapas es alta, la actividad humana parece ser la causa principal de las diferencias observadas entre islas. Estos resultados cuestionan seriamente la efectividad de las normas sobre marisqueo de la actual Ley de Pesca de Canarias.

Diazotrophic activity of Trichodesmium and unicellular cyanobacteria in the subtropical NE Atlantic

Programa de Doctorado en Oceanografía

Regional differences in modelled net production and shallow remineralization in the North Atlantic subtropical gyre

[EN] We used 5-yr concomitant data of tracer distribution from the BATS (Bermuda Time-series Study) and ESTOC (European Station for Time-Series in the Ocean, Canary Islands) sites to build a 1-D tracer model conservation including horizontal advection, and then compute net production and shallow remineralization rates for both sites. Our main goal was to verify if differences in these rates are consistent with the lower export rates of particulate organic carbon observed at ESTOC. Net production rates computed below the mixed layer to 110m from April to December for oxygen, dissolved inorganic carbon and nitrate at BATS (1.34±0.79 molO2 m?2, ?1.73±0.52 molCm?2 and ?125±36 mmolNm?2) were slightly higher for oxygen and carbon compared to ESTOC (1.03±0.62 molO2 m?2, ?1.42±0.30 molCm?2 and ?213±56 mmolNm?2), although the differences were not statistically significant. Shallow remineralization rates between 110 and 250m computed at ESTOC (?3.9±1.0 molO2 m?2, 1.53±0.43 molCm?2 and 38±155 mmolNm?2) were statistically higher for oxygen compared to BATS (?1.81±0.37 molO2 m?2, 1.52± 0.30 molCm?2 and 147±43 mmolNm?2). The lateral advective flux divergence of tracers, which was more significant at ESTOC, was responsible for the differences in estimated oxygen remineralization rates between both stations. According to these results, the differences in net production and shallow remineralization cannot fully explain the differences in the flux of sinking organic matter observed between both stations, suggesting an additional consumption of nonsinking organic matter at ESTOC.

Active mesopelagic prokaryotes support high respiration in the subtropical northeast Atlantic Ocean

[EN]Here we provide evidence, based on prokaryote metabolic proxies and direct estimates of oxygen consumption, that the mesopelagic prokaryote assemblage in the subtropical Northeast Atlantic is an active one. It supports a high respiration (0.22 ± 0.05 μmol O2 l−1 d−1, corresponding to 68 ± 8 mmol CO2 m−2 d−1), comparable to that of the epipelagic zone during the same period (64–97 mmol C m−2 d−1). Our findings suggest that mesopelagic prokaryotes in the NE subtropical Ocean, as well as in other eastern boundary regions, are important carbon sinks for organic matter advected from the highly productive coastal systems, and would play a key role in the global carbon cycle of the oceans.

Krill as a central node for iron cycling in the Southern Ocean

[EN] In order to establish the potential role of Antarctic krill (Euphausia superba) in the recycling of bioactive elements, we have quantified the release of iron, phosphate, and ammonia by these organisms along the Antarctic Peninsula sector of the Southern Ocean. The experimental results suggested that the presence of krill has a significant impact on ambient iron concentrations, as large amounts of this trace element were released by the krill (22–689 nmol Fe g Dry Weight−1 h−1, equivalent to 0.2 to 4.3 nmol Fe L−1 d−1). Half of this iron release occurred within the first hour of the experiment, and differences in iron and phosphate release rates (3.1 to 14.0 μmol PO43− g DW−1 h−1) seemed to reflect differences in food availability. These results identify krill as a major node in iron cycling in the Southern Ocean, potentially influencing iron residence time in the upper water column of this region.