Plastic debris in the open ocean

There is a rising concern regarding the accumulation of floating plastic debris in the open ocean. However, the magnitude and the fate of this pollution are still open questions. Using data from the Malaspina 2010 circumnavigation, regional surveys, and previously published reports, we show a worldwide distribution of plastic on the surface of the open ocean, mostly accumulating in the convergence zones of each of the five subtropical gyres with comparable density. However, the global load of plastic on the open ocean surface was estimated to be on the order of tens of thousands of tons, far less than expected. Our observations of the size distribution of floating plastic debris point at important size-selective sinks removing millimeter-sized fragments of floating plastic on a large scale. This sink may involve a combination of fast nano-fragmentation of the microplastic into particles of microns or smaller, their transference to the ocean interior by food webs and ballasting processes, and processes yet to be discovered. Resolving the fate of the missing plastic debris is of fundamental importance to determine the nature and significance of the impacts of plastic pollution in the ocean

Protocolos RADMED (versión: 1.01 – 2014). Procedimientos a seguir en las campañas del proyecto RADMED

Los protocolos RADMED se pueden considerar como una guía de mar de las operaciones a realizar en el desarrollo de una campaña de ese proyecto, en donde figuran: el montaje del equipamiento científico, las secuencias de las diferentes operaciones y muestreos, la identificación de las estaciones, cómo rellenar los diferentes estadillos, las determinaciones de variables oceanográficas a bordo y el post-procesado de los datos hidrográficos. Detrás de todo ello está la intención de homogeneizar la información, para facilitar el post-procesado y el fiel tratamiento de las muestras y análisis.[Abstract] The RADMED protocols can be considered as a guide to work at the sea in the development of a campaign of this project and to conduct its different operations. They include: installation of scientific equipment, the sequences of the different operations and sampling, identification of stations, the filling of the various work sheets, determinations of oceanographic variables on board and the post processing of hydrographic data. All this pretend to standardize the information to facilitate post processing and accurate treatment of the samples and analysis

Zooplankton abundance in subtropical waters: is there a lunar cycle?

Based on historical data of abundance, we report evidence of changes in zooplankton abundance in the 0-200 m layer related to the moon cycle confirming that this phenomenon is produced in the marine environment, similarly to the one described for freshwater ecosystems. A clear decrease in the abundance of copepodites plus copepods was observed from the second to the fourth quarter of the moon when the seasonal variability was suppressed. During the full moon phase the large zooplankton and micronekton of the deep scattering layers (DSL) would not reach the upper mixed layer in order to avoid predation because of the relatively high level of illumination. Thus epipelagic zooplankton abundance increases as the effect of a lower predatory pressure. Conversely, during the new moon phase the diel migrants reach the surface waters and epiplankton abundance considerably decreases. Recent oceanic sediment trap data in subtropical waters indicate that the particle flux increases at about 30 days period. Thus, the effect of diel vertical migrants could promote not only the variability in their resources and the intensity of the active flux, but could also drive the variability in the gravitational flux.No disponibl

Diel variations in the vertical distribution of copepods off the north coast of Spain

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Seasonal variability of copepod abundance in the Balearic region (Western Mediterranean) as an indicator of basin scale hydrological changes

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