Uso de marcadores morfológicos, bioquímicos y moleculares SRAP para diferenciar variedades de Cynara cardunculus L. (Asteraceae)

Dentro del complejo primario de Cynara cardunculus L. se encuentran diversas variedades botánicas: var. scolymus (alcaucil), var. altilis (cardo cultivado) y var. sylvestris (cardo silvestre). A lo largo de la historia del mejoramiento, la caracterización de los materiales ha evolucionado desde el uso de caracteres morfológicos hasta los modernos análisis moleculares, pasando por los marcadores bioquímicos. El objetivo del presente trabajo fue comparar la utilidad de los marcadores morfológicos, bioquímicos y moleculares para la caracterización de materiales pertenecientes a tres variedades botánicas de Cynara cardunculus. Tres cultivares de la var. scolymus, dos de la var. altilis y dos de la var. sylvestris fueron caracterizadas por variables morfovegetativas, proteínas de reserva y por marcadores moleculares a través de la técnica SRAP. Estas metodologías permitieron discriminar dos grupos: uno incluyendo las variedades de cardo cultivado y silvestre, y el otro, las variedades del alcaucil. Los datos moleculares y morfológicos permitieron además diferenciar los cultivares evaluados de la var. scolymus. Se concluye que los marcadores analizados son útiles para la caracterización intravarietal e intervarietal en programas de mejoramiento.

Cenozoic benthic foraminifers from ODP Leg 134 holes

This paper discusses the Paleobathymetric and paleoenvironmental history of the New Hebrides Island Arc and North d'Entrecasteaux Ridge during Cenozoic time based on benthic foraminiferal and sedimentological data. Oligocene and Pliocene to Pleistocene benthic foraminiferal assemblages from Sites 827, 828, 829, and 832 of Ocean Drilling Program (ODP) Leg 134 (Vanuatu) are examined by means of Q-mode factor analysis. The results of this analysis recognize the following bathymetrically significant benthic foraminiferal biofacies: (1) Globocassidulina subglobosa biofacies and Bulimina aculeata-Bolivinita quadrilatera biofacies representing the upper bathyal zone (600-1500 m); (2) Gavelinopsis praegeri-Cibicides wuellerstorfi biofacies, indicating the Pacific Intermediate Water (water depth between 1500 and 2400 m); (3) Tosaia hanzawai-Globocassidulina muloccensis biofacies, Valvulineria gunjii biofacies, and the Melonis barleeanus-Melonis sphaeroides biofacies, which characterize the lower bathyal zone; (4) the Nuttallides umbonifera biofacies, which characterizes the interval between the lysocline (approximately 3500 m) and the carbonate compensation depth (approximately 4500 m); and (5) the Rhabdammina abyssorum biofacies representing the abyssal zone below the carbonate compensation depth. Benthic foraminiferal patterns are used to construct Paleobathymetric and paleogeographic profiles of the New Hebrides Island Arc and North d'Entrecasteaux Ridge for the following age boundaries: late Miocene/Pliocene, early/late Pliocene, Pliocene/Pleistocene, and Pleistocene/Holocene.

Biostratigraphical investigations of Lago d'Averno, near Naples

Remains of diatoms, molluscs, ostracods, foraminifera and pollen exines preserved in the sediments of Lago d'Averno, a volcanic lake in the Phlegrean Fields west of Naples, allowed us to reconstruct the changes in the ecological conditions of the lake and of the vegetation around it for the period from 800 BC to 800 AD. Lago d'Averno was at first a freshwater lake, temporarily influenced by volcanic springs. Salinity increased slowly during Greek times as a result of subsidence of the surrounding land. Saline conditions developed only after the lake was connected with the sea by a canal, when Portus Julius was built in 37 BC. The first post-Roman period of uplift ended with a short freshwater phase during the 7th century after Christ. Deciduous oakwoods around the lake was transformed into a forest of evergreen oaks in Greek times and thrived there - apparently almost uninfluenced by man - until it was felled, when the Avernus was incorporated into the new Roman harbour in 37 BC, to construct a shipyard and other military buildings there. Land-use was never more intense than during Roman times and weakest in Greek and Early Roman times, when the Avernus was considered a holy place, the entrance to the underworld.