Growth and photosynthetic performance of Nostoc linckia (formerly N. calcicola) cells grown in BG11 and BG110 media.

The biotechnological potential of Nostoc linckia as a biofertilizer and source of bioactive compounds makes it important to study its growth physiology and productivity. Since nitrogen is a fundamental component of N. linckia biomass, we compared the growth and biochemical composition of cultures grown in BG11 (i.e., in the presence of nitrate) and BG110 (in the absence of nitrate). Cultures grown in BG11 accumulated more cell biomass reaching a dry weight of 1.65 ± 0.06 g L-1, compared to 0.92 ± 0.01 g L-1 in BG110 after 240 h of culture. Biomass productivity was higher in culture grown in BG11 medium (average 317 ± 38 mg L-1 day-1) compared to that attained in BG110 (average 262 ± 37 mg L-1 day-1). The chlorophyll content of cells grown in BG11 increased continuously up to (39.0 ± 1.3 mg L-1), while in BG110 it increased much more slowly (13.6 ± 0.8 mg L-1). Biomass grown in BG11 had higher protein and phycobilin contents. However, despite the differences in biochemical composition and pigment concentration, between BG11 and BG110 cultures, both their net photosynthetic rates and maximum quantum yields of the photosystem II resulted in similar.

Effect of plate distance on light conversion efficiency of a Synechocystis culture grown outdoors in a multiplate photobioreactor.

In this work, the performance of a vertical multiplate photobioreactor is analyzed and presented. The photobioreactor consisted of 20 vertical plates (1 m2 each) connected by manifolds and a working volume of 1300 L. The total area occupied (footprint) was 10 m2, while the illuminated area was 40 m2, therefore the ratio of illuminated area to volume ratio was about 30 m-1. The performance of the photobioreactor was evaluated using a culture of Synechocystis PCC 6803, circulated by a centrifuge pump. The results showed that the amount of light captured by the photobioreactor at a plate spacing of 0.5 m was 90.2 % of the light incident on the horizontal surface, while at a plate spacing of 1.0 m, 50.3 % was captured. The corresponding biomass yield, calculated based on the ground area occupied by the reactor, was 26.0 g m-2 day-1 and 7.2 g m-2 day-1, when the plates were spaced at 0.5 m and 1.0 m respectively. Therefore, the light conversion efficiency calculated based on the ground area was significantly higher in the configuration with a plate spacing of 0.5 m, reaching 5.43 % based on PAR (photosynthetically active radiation), and 2.44 % based on solar radiation, giving a value 3.7 higher than when the plates were spaced 1.0 m apart. It was concluded that the light conversion efficiency might be further improved by reducing the plate spacing while also reducing the culture light path.

Effect of high pH on growth of Synechocystis sp. PCC 6803 cultures and their contamination by golden algae (Poterioochromonas sp.).

Culturing cyanobacteria in a highly alkaline environment is a possible strategy for controlling contamination by other organisms. Synechocystis PCC 6803 cells were grown in continuous cultures to assess their growth performance at different pH values. Light conversion efficiency linearly decreased with the increase in pH and ranged between 12.5 % (PAR) at pH 7.5 (optimal) and decreased to 8.9 % at pH 11.0. Photosynthetic activity, assessed by measuring both chlorophyll fluorescence and photosynthesis rate, was not much affected going from pH 7.5 to 11.0, while productivity, growth yield, and biomass yield on light energy declined by 32, 28, and 26 % respectively at pH 11.0. Biochemical composition of the biomass did not change much within pH 7 and 10, while when grown at pH 11.0, carbohydrate content increased by 33 % while lipid content decreased by about the same amount. Protein content remained almost constant (average 65.8 % of dry weight). Cultures maintained at pH above 11.0 could grow free of contaminants (protozoa and other competing microalgae belonging to the species of Poterioochromonas).

Implicaciones sedimentológicas sobre el cambio en la cobertura del bosque de manglar en Boca Zacate, Humedal Nacional Térraba-Sierpe, Costa Rica / Sedimentological implications of the change in the coverage of mangrove forest in Boca Zacate, Térraba-Sierpe National Wetlands, Costa Rica

Resumen:En los últimos sesenta años han ocurrido cambios en el Humedal Nacional Térraba-Sierpe, Costa Rica. Los cambios en la geomorfología costera están asociados a la erosión o acreción de sedimentos, lo que ha favorecido la eliminación de sectores de bosque o a la formación de bancos de sedimentos que han sido colonizados por árboles de mangle. El estudio se realizó en los sectores Bocón, Brujo e isla Coco en Boca Zacate, Humedal Nacional Térraba-Sierpe, Costa Rica, entre 2008-2013, cuyo objetivo consiste en analizar el aporte de sedimentos y las implicaciones en la cobertura del bosque de mangle en el sector de Boca Zacate. Es este estudio se realizó un análisis multitemporal de la morfología litoral con fotografías aéreas e imágenes satelitales de 1948, 1960, 1974, 1978, 1984, 1992 y 2011. Y además, se cuantificó la tasa de sedimentación mensual (g/cm2/día) en los canales de los estuarios, la composición granulométrica y la concentración de elementos químicos en los sedimentos (mgL-1) en época seca y lluviosa durante los años de estudio. Los resultados indican que Boca Zacate ha mantenido en los últimos 60 años una tendencia hacia la erosión, perdiendo un 10.6 % de su espacio emergido entre 1948 y 2011 y aproximadamente un 8.9 % de su cobertura forestal; también ha experimentado una acreción en la zona de la isla Coco, uniéndose al continente por este sector. La tasa de sedimentación cuantificada en los esteros presentó diferencias con respecto al sitio y a la época. La mayor cantidad se presentó en el estero el Brujo y la menor cantidad en el estero Camíbar. Con respecto a la granulo-metría, el tipo de sedimento dominante es la arena, seguido por la arcilla y en menor cantidad el limo en todos los sitios de estudio. La mayor distribución de los elementos químicos corresponde al magnesio, calcio, potasio; mientras que el manganeso, hierro, aluminio, fósforo, zinc y cobre se encontraron en menor cantidad. El transporte, composición y cantidad de sedimentos en Boca Zacate aportados por el río Grande de Térraba asociados a las corrientes, mareas y oleaje, son factores determinantes en los cambios que han ocurrido en el litoral de la Boca, conllevando a un paisaje de bosque de mangle muerto en la zona. Por consiguiente, este tipo de análisis es importante para la recomendación de lineamientos y acciones en la conservación y la gestión integrada del espacio marino-costero en el Humedal Nacional Térraba Sierpe.

Abstract:In the last sixty years many geomorphological changes have occurred in Costa Rica's Térraba-Sierpe National Wetlands. Changes in coastal geomorphology are generally associated with erosion or accretion of sediment, which has led to the removal of sections of mangrove forests or sediment banks colonized by mangroves. The aim of this study was to analyze sedimentation as a leading process in the dynamics of coastal morphology and its implications for mangrove forest cover in the Boca Zacate area of Térraba-Sierpe wetlands. The study was conducted in the sectors of Bocón, Brujo and Coco Island in Boca Zacate, from 2008 to 2013. The research was based on a multi-temporal analysis of coastal morphology using aerial photographs from the years 1948, 1960, 1974, 1978, 1984, 1992 and 2011. The following measurements were also performed: monthly sedimentation rate (g/cm2/day), and granulometric composition and content of chemical elements in the sediments of the study area. These last two measurements were performed once each in the dry and rainy seasons during the years of study. The results indicated that over the past 60 years, Boca Zacate has witnessed a process of sustained erosion; from 1948 through 2001, losing 10.6 % of its land and approximately 8.9 % of its forest cover. It has also experienced accretion in the area of Coco Island. The Brujo sector showed the highest sedimentation rate and the Camibar estuary, the lowest. The dominant type of sediment in all study sites was sand, followed by clay and silt. The most widespread chemical elements (mg/L) included magnesium, calcium and potassium; others, such as manganese, iron, aluminum, phosphorus, zinc and copper, were measured in smaller amounts. Transport, composition and quantity of sediment in Boca Zacate are crucial to the changes that have occurred on the coastal area of La Boca, where the presence of dead trees was evident. This geomorphological analysis holds great importance for future guidelines and actions for the conservation and integrated management of the mangrove in Terraba- Sierpe National Wetlands.