Quaternary coastal uplift along the Talara Arc (Ecuador, Northern Peru) from new marine terrace data

Marine Geology, v. 228, n. 1-4, p. 73-91, 2006. http://dx.doi.org/10.1016/j.margeo.2006.01.004International audienceMarine terrace sequences have been investigated along the Talara Arc, a 1000-km-long stretch of the coast of Ecuador and northern Peru, characterized by subduction with a concave plan-view. Seven areas were investigated, evidencing flights of up to seven marine terraces with elevations reaching up to 360 m above mean sea level (amsl). Dating of the terraces was made using the Infra Red Stimulated Luminescence (IRSL) technique on sands as old as MIS 9 (∼330 ka). 14 C and U-series dates were obtained from fossil shells for geochronological cross control. Mean uplift rates along the Talara Arc range from about 0.10 up to 0.50 mm/ yr. The strongest uplift is observed in the Manta Peninsula of Ecuador in front of the subduction of the Carnegie Ridge. The uplift rate tends to slow down towards the northern and southern ends of the Talara Arc and then the transition toward the stable or subsiding coasts of central Peru and northern Ecuador and Colombia is sharp. The uplift appears to be homogeneous and related to 1) the map view curvature of the Arc, 2) the concave subduction pattern and 3) the Carnegie Ridge subduction

Uplift of the Bolivian orocline coastal areas based on geomorphologic evolution of marine terraces and abrasion surfaces: preliminary results

The southern Pacific coast morphology and especially the presence of marine surfaces gives information on the dynamics of Andean forearc evolution from the Neogene. Along most of the Southern Peru and Northern Chilean coasts, discontinuous uplifts are recorded by marine terraces and marine abrasion surfaces; they have thus, preserved a record of eustatic sea level changes and the uplift history of the coastal area in the Andean forearc. One approach to study the tectonic history of the Andean forearc is to identify its effects in marine sedimentation or erosion patterns along the coastal area. To investigate these processes, the Neogene marine formations are studied in various coastal sections either in southern Peru, at Chala (15°50'S) and Ilo (17°32'S-17°48'S), situated above a steep subduction segment and at San Juan de Marcona (15°20'S), situated above the southern part of the Nazca ridge; or in Chile, from Tongoy (30°15'S) to Los Vilos (31°55'S), situated above a flat subduction segment (Fig.1). We chose various sites from each branch of the Arica bend in order to sample possibly different time spans during the Neogene and different response of the continental plate to the subduction process. Various studies were already undertaken on such problems either in Peru or Chile but mainly leaded to the datation of the 5th isotopic stage. So, differential GPS and cosmogenic datations are pursued in order to propose robust ages on these sites and subtract the effects of eustatic sea-level changes from local curves, identifying tectonic uplifts

Oscilaciones eustáticas e implicaciones climáticas en el tránsito Neógeno-Cuaternario en la isla de Sal (archipiélago de Cabo Verde)

Solution pipes interpreted as a cryptokarst separate large-scale cross-bedded megaforms of shallowmarine calcarenites deposited at the Neogene-Quatemary transition in Cape Verde Islands. This implies that depositional phases were followed by subaerial exposure of the cemented calcarenites during subsequent falls of sea level, and accumulation of unconsolidated eolianites which supported a vegetal cover that promoted the cryptokarst. The process was repeated several times. A widespread, more recent karstification with red silty clay filling of voids may represent the aridification of climate at the beginning oi the Quaternary and the increased supply of Saharan dust by Trade Winds

Specialized Literacy Professionals as Literacy Leaders: Results of a National Survey

This large-scale national survey of specialized literacy professionals was designed to answer questions about responsibilities, including leadership, and preparation for these roles. Questionnaires, completed by over 2,500 respondents, indicated that respondents had multiple responsibilities that included both instruction of struggling readers and support for teachers. Four distinct role-groups were identified: instructional/literacy coaches, reading/literacy specialists, reading teachers/interventionists, and supervisors. The findings indicated a need for more precise definitions of the roles of these professionals and for preparation programs to include experiences that address the tasks required. Themes discussed included: roles have changed and require more focus on leadership, specialists must be nimble, and they require more in-depth preparation to handle the leadership demands of their positions

2. Cambios climáticos del Holoceno

Existe una variabilidad natural del clima. Se debe tanto a factores externos (como el cambio de la órbita de la Tierra) como internos (como erupciones volcánicas o movimientos tectónicos entre otros). Los paleo-climatólogos estudian los cambios del clima del pasado a través de complejos análisis de sedimentos de lagos, de testigos de hielo de los glaciares o también de estalagmitas de las cavernas. Estos registros son como libros donde está escrita la historia del clima de la Tierra. Usando estos marcadores ambientales y gracias a los modelos climáticos a diferentes escalas espaciales y de tiempo, los investigadores buscan discriminar cual es la parte natural del cambio climático actual de la parte debida a la actividad humana y disminuir las incertidumbres en las proyecciones futuras del clima.Il existe une variabilité climatique naturelle. Elle est due aussi bien à des facteurs externes (comme le changement d’orbite de la Terre) qu’internes (comme les éruptions volcaniques ou les mouvements tectoniques entre autres). Les paléo-climatologues étudient les changements du climat du passé en réalisant des analyses complexes de sédiments de lacs, de carottes glaciaires ou encore de stalagmites des grottes. Ces registres sont comme des livres où est écrite l’histoire du climat de la Terre. A partir de ces marqueurs environnementaux et des modelés climatiques à différentes échelles d’espace et de temps, les chercheurs cherchent à connaître quelle part du changement climatique actuel est naturelle et quelle part est liée à l’activité humaine et réduire les incertitudes dans les projections climatiques.There is natural climate variability. It ¡s due to both external factors (such as changes in Earth’s orbit) as well as internal factors (such as volcanic eruptions and tectonic movements among others). Paleoclimatologists study historic climate changes performance by complex analysis of lake sediments, ice cores or stalagmite caves. These records are like books in where the history of Earth’s climate has been written. Thanks to these environmental markers and the climate models at different scales of space and time, researchers seek to differentiate which part of the current climate change is natural and which part is due to human activity, in order to reduce uncertainties in future climate projections

The Calcitonin Receptor Gene Is a Candidate for Regulation of Susceptibility to Herpes simplex Type 1 Neuronal Infection Leading to Encephalitis in Rat

Herpes simplex encephalitis (HSE) is a fatal infection of the central nervous system (CNS) predominantly caused by Herpes simplex virus type 1. Factors regulating the susceptibility to HSE are still largely unknown. To identify host gene(s) regulating HSE susceptibility we performed a genome-wide linkage scan in an intercross between the susceptible DA and the resistant PVG rat. We found one major quantitative trait locus (QTL), Hse1, on rat chromosome 4 (confidence interval 24.3–31 Mb; LOD score 29.5) governing disease susceptibility. Fine mapping of Hse1 using recombinants, haplotype mapping and sequencing, as well as expression analysis of all genes in the interval identified the calcitonin receptor gene (Calcr) as the main candidate, which also is supported by functional studies. Thus, using unbiased genetic approach variability in Calcr was identified as potentially critical for infection and viral spread to the CNS and subsequent HSE development