Evolución del contenido de dióxido de carbono en aguas del norte de Canarias. Su impacto en el cambio climático global

[ES] En este artículo presentamos los resultados de un año de estudio del sistema del dióxido de carbono, dirigido a completar una red de resultados de 10 años en la estación ESTOC (European Station for Time series in the Ocean Canary Islands) localizada a 29º10´N,15º30´W, alrededor de 100 Km al norte de la isla de Gran Canaria. Para ello se ha analizado Alcalinidad, Carbono Inorgánico Total y CO2 en agua de mar y en la atmósfera, cuantificando la variabilidad estacional y temporal y el rol de este área en el cambio climático global.

Identificación visual en ambientes subacuáticos

[ES] Los erizos de mar han servido como modelo prototípico de organismo en el desarrollo de la Biología. La irrupción de este animal como especie invasora en los fondos canarios, combinada con el éxito reproductivo que ha tenido en nuestras aguas, ha creado un problema medioambiental importante que se ha intentado atajar con la puesta en marcha de proyectos e iniciativas orientados a su erradicación (matanzas masivas) o su contención con intentos de estimular su explotación comercial para uso gastronómico. En el transcurso de este trabajo se pretende explorar la robustez con la que se pueden clasificar visualmente diferentes tipos de erizos (principalmente Diadema antillarumy y Erizos autóctonos) a partir tanto de imágenes estáticas como de secuencias de vídeo para evaluar si, mediante el empleo de técnicas de visión por computador, es posible resolver estas tareas mediante la inspección automática de vídeos e imágenes.

Isolation and characterization of microsatellite loci in Sorbus aria (Rosaceae)

[EN] Sorbus aria (L) Crantz (Common Whitebeam) is native to Europe, east of the Balkans and in North Africa; it is also present in the Canary Islands. To evaluate the genetic diversity in natural populations of this vulnerable species, nine novel polymorphic microsatellite markers were isolated from enriched libraries. Microsatellite loci were screened in 97 individuals from La Palma (Canary Islands) and Sierra Nevada (Granada, Spain). Examination of the microsatellite profiles shows that S. aria individuals have up to three alleles per locus. The cloned sequences in microsatellite loci confirmed the polyploidy status of the plants. The number of alleles ranged from 5 to 14 per locus. The phenotype diversities across loci (H0 T) ranging from 0.653 to 0.847

Migración y ecología trófica de peces migradores verticales dominantes del Atlántico nordeste subtropical: implicaciones en el flujo activo de carbono

[EN]Diel vertical migrants (DVMs) are mainly zooplankton and micronekton that migrate upward from 400-700 m depth every night to feed in the productive epipelagic zone and come back at dawn to the mesopelagic zone, where they release the ingested carbon. DVMs should contribute to the biological pump in the ocean and, accordingly, to thevglobal CO2 balance. A large portion of the DVMs biomass are the lanternfishes (myctophidae), which might represent a pathway accounting for a substantial export of organic carbon to the deep ocean. Nevertheless, the magnitude of this transport is still poorly known. The combined study of migration and feeding ecology is a good approach to improve our knowledge of the DVMs role in this active carbon flux. Two dominant myctophids in the Subtropical Eastern North Atlantic Ocean (Hygophum hygomii (Lütken, 1892) and (Lobianchia dofleini (Zugmayer, 1911)) were studied from several surveys carried out around the Canary Islands during the last decade. Our results showed a marked diel vertical migration and a prevailing nocturnal feeding with predation mainly on copepods and euphausiids. The digestion state of prey suggested a slow stomach evacuation rate and that most of the ingested carbon in the epipelagic is efficiently transported to the mesopelagic zone.

Análisis espacio-temporal de las praderas de Cymodocea nodosa (Ucria) Ascherson en la isla de Gran Canaria

Máster Oficial en Gestión Costera

Aumento de fijación de nitrógeno en diazótrofos unicelulares versus Trichodesmium tras un evento de deposición de polvo atmosférico en las Islas Canarias

[ES]En este trabajo hemos estudiado la relación entre la deposición de polvo atmosférico, y la abundancia y tasas de fijación de nitrógeno asociadas a Trichodesmium y fijadores unicelulares en las Islas Canarias. La fijación de nitrógeno asociada a los fijadores unicelulares aumentó entre el 86 y el 92% tras un evento de deposición de polvo atmosférico, mientras que la asociada a Trichodesmium disminuyó entre el 34 y el 92%. Tras el evento de deposición de polvo, aumentó la abundancia de fijadores unicelulares y la mayoría de éstos aparecieron asociados a partículas de materia orgánica. Creemos que esta estrategia les permite ligar el hierro que contiene el polvo y así poder usar este nutriente limitante.

Antioxidant activities of different aloe barbadensis extracts

[EN] In the regions of Canary Islands, it is prevailing all the year a high level of solar radiation. This force plants to develop defence mechanisms against excessive production of free radicals through the accumulation of antioxidant substances. Plants contain a diverse group of phenolic compounds with the structural requirements of free radical scavengers. The effects of different extracting solvents have been tested for the extraction of phenolic compounds from plant material. On the present study we compare the total phenolic contents (TPC) and antioxidant activities of several extracts derived from Aloe vera plants. The phenolic compounds present in the extracts were identified and quantified by RP­HPLC techniques. 

Pastaje (grazing) del microzooplancton en aguas de las Islas Canarias

[EN]The impact of micrograzers upon primary production was measured north of the Canary Islands during 2010 and 2011 using the dilution technique. Grazing was estimated from chlorophyll a but also taking into account the different phototrophic organisms, that is, Synechococcus (Syn), Prochlorococcus (Pro), autotrophic picoeukaryotes (APE) and autotrophic nanoflagellates (ANF). Some experiments showed significant values of grazing upon Syn, Pro or APE although no significant grazing was measured on chlorophyll a. Furthermore, a positive relationship, this means growth instead of grazing, was observed in Syn and Pro in two experiments. Grazing on heterotrophic prokaryotes was also determined and the obtained values were always highly significant. These results showed that the impact of micrograzers upon primary production is a complex process which involves a different grazing pressure upon phytoplankton groups. Therefore, a detailed analysis of the pico, nano and microplanktonic community is essential to really understand the role of micrograzers and the trophic interactions among these groups in subtropical waters.

Sexualidad y reproducción del boquerón o longorón "Engraulis encrasicolus" (Osteichthyes: Clupeiformes: Engraulidae) en aguas de Gran Canaria

Máster en Gestión Sostenible de Recursos Pesqueros

Biología de la conservación de endemismos vagetales de los parques nacionales canarios

[ES]El presente proyecto se centra en aplicar técnicas de biología molecular, demográficas y de biología reproductiva en cuatro endemismos canarios amenazados que se encuentran total o parcialmente localizados en los parques nacionales de Canarias: Silene nocteolens Webb & Berthel. (Parque Nacional del Teide, Tenerife); Ilex perado ssp. lopezlilloi (G. Kunkel) A. Hansen & Sunding (Parque Nacional Garajonay, La Gomera), Sorbus aria (L.) Crantz (Parque Nacional de la Caldera de Taburiente, La Palma) y Bencomia exstipulata Svent. (parques nacionales del Teide y Caldera de Taburiente). Se estableció un estudio genético a través de marcadores moleculares hipervariables, microsatélites, y se determinó para cada taxón la variación genética de sus poblaciones, para su posterior aplicación en la gestión en el ámbito de la Biología de la conservación de estos taxones.

Energía Geotérmica, ¿la gran desconocida? : Estudio prospectivo del potencial geotérmico de la isla de Gran Canaria

[ES]En la actualidad, las Islas Canarias se abastecen energéticamente de combustibles fósiles aproximadamente en un 90%. La Energía Geotérmica es un recurso energético renovable con muchas posibilidades de explotación en el Archipiélago Canario para la producción de energía; así lo demuestra su naturaleza volcánica, registros históricos y actividad sismotectónica. Se analizan las características necesarias desde varios puntos de vista para evaluar y cuantificar el potencial geotérmico de la isla de Gran Canaria

Adaptación de la Directiva Europea de Gestión de la Calidad de Aguas de Baño a las playas de Canarias

[ES] Hemos realizado una serie de consideraciones con respecto a la Directiva 2006/7/CE para lograr su correcta aplicación en las playas de baño de Canarias. En nuestras aguas se producen algunos fenómenos que no se producen en el resto de la Unión Europea. Por esta razón hemos establecido una serie de conceptos que no están previstos de forma explicita en los artículos de la Directiva y que, con algunas matizaciones, podremos adaptarlos a la generalidad de la Directiva, o ?sensu contrario?, adecuar la Directiva a nuestra realidad ambiental. En este sentido, hemos adaptado conceptos como ?contaminación de corta duración?, ?tendencia a la proliferación de macroalgas?, ?tendencia a la proliferación de fitoplancton marino?, ?proliferación de cianobacterias? y otros a las especificidades que se producen en nuestras costas y que podrían alterar la calidad de las aguas de baño

Differences in diversity, structure, and variability between intertidal and subtidal meiofaunal assemblages

[EN] Meiofaunal assemblages from intertidal and shallow subtidal seabeds were studied at two sites (one dominated by volcanic sands and the other by organogenic sands) at Tenerife (Canary Islands, NE Atlantic Ocean) throughout an entire year (May 2000?April 2001). Specifically, we aimed (i) to test for differences in diversity, structure, and stability between intertidal and subtidal meiofaunal assemblages, and (ii) to determine if differences in the meiofaunal assemblage structure may be explained by environmental factors (granulometric composition, availability of organic matter, and carbonate content in sediments). A total of 103,763 meiofaunal individuals were collected, including 203 species from 19 taxonomic groups (Acari, Amphipoda, Cnidaria, Copepoda, Echinodermata, Gastrotricha, Isopoda, Insecta, Kinorrhyncha, Misidacea, Nematoda, Nemertini, Oligochaeta, Ostracoda, Polychaeta, Priapulida, Sipuncula, Tanaidacea, and Turbellaria). Nematodes were the most abundant taxonomic group. Species diversity was higher in the subtidal than in the intertidal zone at both sites, as a result of the larger dominance of a few species in the intertidal zone. The meiofaunal assemblage structure was different between tidal levels at both sites, the intertidal presenting greater temporal variability (multivariate dispersion) in the meiofaunal assemblage structure than the subtidal. Sediment grain size, here quantified by the different granulometric fractions, explained the variability in meiofaunal assemblage structure to a greater extent than the percentage of carbonates, a variable linked to sediment origin. This study revealed differences in diversity, assemblage structure, and variability between intertidal and subtidal meiofauna.

Meridional changes in water mass distributions off NW Africa during November 2007/2008

[EN] An optimum multiparameter analysis was applied to a data set for the eastern boundary of the North Atlantic subtropical gyre, gathered during November of two consecutive years and spanning from 16 to 36º N. This data set covers over 20º of latitude with good meridional and zonal resolution over the whole coastal transition zone. The contribution from six water types in the depth range between 100 and 2000 m is solved. In the 100 to 700 m depth range the central waters of southern and northern origin meet abruptly at the Cape Verde Frontal Zone. This front traditionally has been reported to stretch from Cape Blanc, at about 21.5º N, to the Cape Verde Islands, but in our case it penetrates as far as 24º N over the continental slope. South of 21º N latitude we actually find a less saline and more oxygenated variety of South Atlantic Central Water, which we ascribe to less diluted equatorial waters. In the 700 to 1500 m depth range the dominant water type is a diluted form of Antarctic Intermediate Water (AAIW), whose influence smoothly disappears north of the Canary Islands as it is replaced by Mediterranean Water (MW); at latitudes where both water masses coexist, we observe MW offshore while AAIW is found near-shore. North Atlantic Deep Water is the dominating water type below about 1300/1700 m depth south/north of the Canary Islands; this abrupt change in depth suggests the existence of different paths for the deep waters reaching both sides of the archipelago.

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.