Induction and characterization of oil palm (Elaeis guineensis Jacq.) pro-embryogenic masses.
Oil palm is one of the most economically valuable oil seed plants, but the expansion of plantations has been limited by availability of seedlings, as the conventional propagation is through seeds, which have low germination rates. One possible solution for the large-scale production is the use of somatic embryogenesis. The aim of this study was evaluate the effects auxins 2,4-D and picloram on the induction of pro-embryogenic masses in E.guineenesis hybrid leaf explants and characterize, regarding embryogenic characteristics, with cytochemical and ultrastructural analysis. Specifically, in vitro plantlets leaves fragments were inoculated in Y3 culture medium supplemented by 2.4-D or picloram at different concentrations (0.0, 1.0, 3.0, 6.0 and 9.0 mg l⁻¹). After 90 days the presence/ absence of cell masses were evaluated. Both growth regulators efficiently induced cellular masses regardless of the concentrations applied. As the cell masses were not homogeneously formed, they were classified according to color and shape into four types: TYPE 1--elongated and translucent, TYPE 2--uneven and translucent, TYPE 3--globular and beige, TYPE 4--globular and white. Based on the anatomical and ultrastructural features, TYPE 2, 3 and 4 cell masses were considered to have the highest embryogenic potential and therefore may be most suited to large-scale vegetative propagation of oil palm.
Embriogênese somática e regeneração de plantas a partir de embrião maduro de aveia
Embryogenic callus has been the most used target tissue for cereal genetic transformation. Therefore, the objective of this study was to investigate the establishment of embryogenic calli and the in vitro plant regeneration from mature embryos of oat genotypes (Avena sativa L.). Mature embryos were taken out of the seeds and placed on a culture medium MS (Murashige & Skoog), containing 30,0 mg L-1 of sucrose and 2,0 mg L-1 of 2,4-dichlorophenoxyacetic acid (2,4-D). From the induction period, embryogenic aggregates were isolated and subcultivated each 21 days into a fresh medium. After this period, embryogenic calli were transferred to a medium for shoot regeneration. Subsequently, the shoot was transferred to a medium for root induction. There was variability among genotypes for somatic embryogenesis and in vitro plant regeneration from mature embryos. This explant allowed the induction of calli with ability to multiply and regenerate high number of plants from genotypes as UFRGS 7 and UFRGS 19, what makes it capable for oat genetic transformation.
Observations of nearshore infragravity waves: Seaward and shoreward propagating components
[1] The variation of seaward and shoreward infragravity energy fluxes across the shoaling and surf zones of a gently sloping sandy beach is estimated from field observations and related to forcing by groups of sea and swell, dissipation, and shoreline reflection. Data from collocated pressure and velocity sensors deployed between 1 and 6 m water depth are combined, using the assumption of cross-shore propagation, to decompose the infragravity wave field into shoreward and seaward propagating components. Seaward of the surf zone, shoreward propagating infragravity waves are amplified by nonlinear interactions with groups of sea and swell, and the shoreward infragravity energy flux increases in the onshore direction. In the surf zone, nonlinear phase coupling between infragravity waves and groups of sea and swell decreases, as does the shoreward infragravity energy flux, consistent with the cessation of nonlinear forcing and the increased importance of infragravity wave dissipation. Seaward propagating infragravity waves are not phase coupled to incident wave groups, and their energy levels suggest strong infragravity wave reflection near the shoreline. The cross-shore variation of the seaward energy flux is weaker than that of the shoreward flux, resulting in cross-shore variation of the squared infragravity reflection coefficient (ratio of seaward to shoreward energy flux) between about 0.4 and 1.5.