High-resolution marine record of sediment core MD99-2343 in the Balearic Sea

The IMAGES core MD99-2343, recovered from a sediment drift north of the island of Minorca, in the north-western Mediterranean Sea, holds a high-resolution sequence that is perfectly suited to study the oscillations of the overturning system of the Western Mediterranean Deep Water (WMDW). Detailed analysis of grain-size and bulk geochemical composition reveals the sensitivity of this region to climate changes at both orbital and centennial-millennial temporal scales during the last 50 kyr. The dominant orbital pattern in the K/Al record indicates that sediment supply to the basin was controlled by the insolation evolution at 40°N, which forced changes in the fluvial regime, with more efficient sediment transport during insolation maxima. This orbital control also modulated the long-term pattern of the WMDW intensity as illustrated by the silt/clay ratio. However, deep convection was particularly sensitive to climatic changes at shorter time-scales, i.e. to centennial-millennial glacial and Holocene oscillations that are well documented by all the paleocurrent intensity proxies (Si/Al, Ti/Al and silt/clay ratios). Benthic isotopic records (d13C and d18O) show a Dansgaard-Oeschger (D-O) pattern of variability of WMDW properties, which can be associated with changing intensities of the deep currents system. The most prominent reduction on the WMDW overturning was caused by the post-glacial sea level rise. Three main scenarios of WMDW overturning are revealed: a strong mode during D-O Stadials, a weak mode during D-O Interstadials and an intermediate mode during cooling transitions. In addition, D-O Stadials associated with Heinrich events (HEs) have a very distinct signature as the strong mode of circulation, typical for the other D-O Stadials, was never reached during HE due to the surface freshening induced by the inflowing polar waters. Consequently, the WMDW overturning system oscillated around the intermediate mode of circulation during HE. Though surface conditions were more stable during the Holocene, the WMDW overturning cell still reacted synchronously to short-lived events, as shown by increments in the planktonic d18O record, triggering quick reinforcements of the deep water circulation. Overall, these results highlight the sensitivity of the WMDW to rapid climate change which in the recent past were likely induced by oceanographic and atmospheric reorganizations in the North Atlantic region.

Stable isotope record of benthic and planktonic foraminifera in sediment cores of ODP Leg 177, Southern Ocean

While onboard ship during Leg 177, we used variations in sediment physical properties (mainly percent color reflectance) in conjunction with biomagnetostratigraphy to correlate among sites and predict the position of marine isotope stages (MISs) (e.g., see fig. F11 in Shipboard Scientific Party, 1999, p. 45). Our working assumption was that physical properties of Leg 177 sediments are controlled mainly by variations in carbonate content. Previous studies of Southern Ocean sediment cores have shown that carbonate concentrations are relatively high during interglacial stages and low during glacial stages at sites located within the Polar Frontal Zone (PFZ). Today, the PFZ marks a lithologic boundary in underlying sediment separating calcareous oozes to the north and silica-rich facies to the south (Hays et al., 1976). Although there is debate whether the position of the "physical" PFZ actually moved during glacial-interglacial cycles (Charles and Fairbanks, 1990; Matsumoto et al., 2001), the "biochemical" PFZ, as expressed by the CaCO3/opal boundary in sediments, certainly migrated north during glacials and south during interglacials. This gave rise to lithologic variations that are useful for stratigraphic correlation. At Leg 177 sites located north of the PFZ and at sublysoclinal depths, we expected the same pattern of carbonate variation because cores in the Atlantic basin are marked by increased carbonate dissolution during glacial periods and increased preservation during interglacials (Crowley, 1985).

Relevamiento de plagas y enemigos naturales en el cultivo de lechuga : : provincia de La Pampa (Argentina)

En la provincia de La Pampa son escasos los datos sobre relevamiento de plagas y de especies benéficas en lechuga, por ello resulta necesario conocer e investigar los organismos perjudiciales y sus enemigos naturales y las condiciones predisponentes al incremento de sus poblaciones. Los objetivos de este trabajo fueron determinar las especies fitófagas para dos variedades de lechuga, en dos sistemas de producción, e identificar las especies benéficas que puedan actuar como controladores biológicos. El estudio se realizó en la huerta de la Facultad de Agronomía de la UNLPam, con muestreos semanales, desde julio hasta octubre de 2004, a campo con riego complementario y bajo cubierta en macrotúnel con riego por goteo, con las variedades de lechuga Grand Rapid y Gallega de Invierno. En cada variedad y en cada sistema se revisaron 6 plantas al azar, registrándose: especie, número de individuos y su estado de desarrollo. Se comparó mediante ANOVA y test de Tukey (a = 0,05). Se detectó la presencia de dos especies de pulgones: Myzus persicae Sulzer (Homoptera: Aphididae) y Nasonovia ribisnigri (Mosley) (primera cita de N. ribisnigri para la provincia de La Pampa). El mayor número de pulgones se concentró en el cultivo protegido bajo cubierta. Se registraron dos enemigos naturales de los pulgones: un hongo entomopatógeno y un parasitoide: Aphidius ervi (Hymenoptera: Braconidae). También se encontraron, en bajas densidades, larvas de Naupactus leucoloma Boheman (Coleoptera: Curculionidae) que se alimentaban de las hojas.

Cochinilla negra del olivo : control mediante insecticidas

El objetivo del presente trabajo fue comparar la eficiencia de 4 pesticidas: dimetoato, metidation, etion y clorpirifos, en el control de la cochinilla H [Saissetia oleae Bernard (Homoptera, Coccoidea, Lecaniidae)] también llamada cochinilla negra del olivo. Estos productos, conocidos en Mendoza (Argentina), se utilizan localmente. El ensayo se realizó en Vistalba (Luján de Cuyo). Para la evaluación se tuvo en cuenta el porcentaje de mortalidad. El análisis estadístico se efectuó transformando los datos según arcsen ( x / 1 0 0 ) .