Temporal and spatial distribution of the ichthyoplankton in the Canary Islands

A pesar del creciente interés en el estudio de las primeras fases de desarrollo de los peces, aún existen zonas donde esta comunidad es relativamente desconocida. Este es el caso de las Islas Canarias. En la presente tesis, gracias a una serie de muestreos semanales en la región costera de la isla de Gran Canaria durante más de dos años, se ha caracterizado de manera precisa la composición, estructura y variabilidad del ictioplancton presente en esta región subtropical. Clupeidos, Espáridos y Góbidos dominaron la comunidad neríticas, mientras que Mictófidos, Gonostomátidos y Photíctidos prevalecieron dentro de las familias oceánicas. La variabilidad temporal de la comunidad larvaria parece estar más relacionada con la temperatura y efectos a pequeña escala (hidrografía, productividad local, ciclo lunar), que con el aumento de productividad anual durante el bloom de finales de invierno. Se definieron dos asociaciones estacionales de larvas estrechamente ligadas a las características de la columna de agua: (1) invierno-primavera, en la que dominan Sardinella aurita, Boops boops y Cyclothone braueri, y son características especies como Pomacentridae sp1, Trachurus picturatus o Scomber colias; y (2) verano-otoño, donde Góbidos y Cyclothone braueri dominan, pero cuyas especies características son Ceratoscopelus warmingii, Pomacentridae sp2 y Anthias anthias, entre otras. Respecto a la variabilidad horizontal, se confirmó la presencia de dos zonas de retención para los huevos y larvas neríticas a barlovento y sotavento (estela cálida) de la isla. Sin embargo, no se encontraron diferencias significativas en la composición de la comunidad larvaria entre las diferentes zonas de la plataforma de la isla. La Zona de Transición Costera Canario-Africana se caracteriza por una gran actividad de mesoscala, que afectará a la distribución de las larvas neríticas de las costas africanas. Esta interacción resulta especialmente evidente en el caso de las larvas, principalmente sardina y anchoa, transportadas en filamentos de afloramiento generados en la región de Cabo Juby-Cabo Bojador. Estos filamentos pueden ser atrapados por remolinos ciclónicos situados al sur de Gran Canaria. Este sistema remolino-filamento podrá, en función de su evolución, actuar como un mecanismo de retención o dispersión para las larvas de especies neríticas africanas. Parte de estas larvas pueden llegar a las costas de Gran Canaria, suponiendo un aporte para las poblaciones larvarias locales, al menos durante el verano. A pesar de la gran cantidad de información obtenida a partir de esta tesis, es necesario continuar con este tipo de estudios para evaluar la importancia de este transporte larvario y su aplicación a la gestión pesquera.

Temporal and along-shelf distribution of the larval fish assemblage at Gran Canaria, Canary Islands

Temporal and spatial variations of the larval fish community off the island of Gran Canaria (Canary Islands) were studied in weekly surveys from October 2005 to June 2006. A total of 156 taxa, belonging to 51 families and 15 orders, were identified. Myctophidae was by far the most abundant family (30%), followed by Sparidae (11%), Clupeidae (9%) and Gonostomatidae (7%). As expected for an oceanic island, neritic and oceanic taxa contributed in similar proportions. Leeward and windward retention areas were found for total egg and neritic larval abundance. However, seasonality showed a stronger influence on the annual larval assemblage than sampling site, as the latter was not significant on a long time scale. Results suggest that there are two seasonal larval assemblages corresponding to the two main characteristic periods of the water column in these waters: mixing (winter) and stratification (summer). In addition, a significant relationship was recorded between lunar illumination and small mesozooplankton biomass, suggesting that this relationship may be extended to certain neritic families. The most abundant neritic larvae (Sparidae) showed this lunar pattern, which partially supports a recent hypothesis about the effect of lunar illumination on larval fish survival and development in subtropical waters.

Colectores artificiales para el estudio de los patrones de colonización de organismos bentónicos: de su selección y optimización a la cuantificación de patrones espacio-temporales de colonización.

Programa de Doctorado en Gestión Costera

Patrones de colonización de organismos bentónicos en hábitats litorales de Gran Canaria

Programa de doctorado en gestión costera

High-resolution reconstruction of Holocene climate variability and environmental changes in the North Pacific using bivalve shells

Bivalve mollusk shells are useful tools for multi-species and multi-proxy paleoenvironmental reconstructions with a high temporal and spatial resolution. Past environmental conditions can be reconstructed from shell growth and stable oxygen and carbon isotope ratios, which present an archive for temperature, freshwater fluxes and primary productivity. The purpose of this thesis is the reconstruction of Holocene climate and environmental variations in the North Pacific with a high spatial and temporal resolution using marine bivalve shells. This thesis focuses on several different Holocene time periods and multiple regions in the North Pacific, including: Japan, Alaska (AK), British Columbia (BC) and Washington State, which are affected by the monsoon, Pacific Decadal Oscillation (PDO) and El Niño/Southern Oscillation (ENSO). Such high-resolution proxy data from the marine realm of mid- and high-latitudes are still rare. Therefore, this study contributes to the optimization and verification of climate models. However, before using bivalves for environmental reconstructions and seasonality studies, life history traits must be well studied to temporally align and interpret the geochemical record. These calibration studies are essential to ascertain the usefulness of selected bivalve species as paleoclimate proxy archives. This work focuses on two bivalve species, the short-lived Saxidomus gigantea and the long-lived Panopea abrupta. Sclerochronology and oxygen isotope ratios of different shell layers of P. abrupta were studied in order to test the reliability of this species as a climate archive. The annual increments are clearly discernable in umbonal shell portions and the increments widths should be measured in these shell portions. A reliable reconstruction of paleotemperatures may only be achieved by exclusively sampling the outer shell layer of multiple contemporaneous specimens. Life history traits (e.g., timing of growth line formation, duration of the growing season and growth rates) and stable isotope ratios of recent S. gigantea from AK and BC were analyzed in detail. Furthermore, a growth-temperature model based on S. gigantea shells from Alaska was established, which provides a better understanding of the hydrological changes related to the Alaska Coastal Current (ACC). This approach allows the independent measurement of water temperature and salinity from variations in the width of lunar daily growth increments of S. gigantea. Temperature explains 70% of the variability in shell growth. The model was calibrated and tested with modern shells and then applied to archaeological specimens. The time period between 988 and 1447 cal yrs BP was characterized by colder (~1-2°C) and much drier (2-5 PSU) summers, and a likely much slower flowing ACC than at present. In contrast, the summers during the time interval of 599-1014 cal yrs BP were colder (up to 3°C) and fresher (1-2 PSU) than today. The Aleutian Low may have been stronger and the ACC was probably flowing faster during this time.