Las biozonas de nummulitidos del Paleoceno Superior-Eoceno Inferior de la Cuenca Pirenaica

A nummulitid biozonation for the Upper Paleocene-Lower Eocene Pyrenean Basin is proposed in this work, The main contributions are: a) a new biozone proposed for the early Thanetian, b) a better characterization of the late Thanetian biozone, and c) the recognition of  two different biozones within the Lower Ilerdian.The nummulitid biozones established for the Pyrenean Upper Paleocene-Lower Eocene interval were correlated with the corresponding larger foraminiferal biozones Shallow Benthic Zones (SBZ) and integrated in the standard Paleocene-Eocene Time Scale on the basis of magnetostratigraphic data from the Pyrenean Basin and by correlation with the biozonation of calcareous nannoplankton and planktonic foraminifera in the Eastern and Central part of Tethys.The new biozones defined for tbe Pyrenean Upper Paleocene-Lower Eocene are: Nummulites heberti-Ranikothalia sindensis (early Thanetian), N. catari-Assilina yvettae-A. azilensis (late Thanetian), N. gamardensis-A. dandotica (early Ilerdian l), N. bigurdensis-A. aff. Prisca (early Ilerdian 2), N. carcasonensis-A. arenensis (middle Ilerdian l), N. exilis-A. leymeriei (middle Ilerdian 2), N. involutus-A. pomeroli (late Ilerdian), N. planulatus-N. burdigalensis burdigalensis-A. placentula (early Cuisian), N. praelaevigatus-N, cantabricus-A. laxispira (middle Cuisian), and N. manfredi-N. campesinus-A. mnior (late Cuisian)

Modelado de Procesos de Neurorrehabilitación

La Neurorrehabilitación es un proceso clínico que se centra en el abordaje de la alteración del sistema nervioso. Existe una enorme variabilidad tanto en la tipología como en el grado de las lesiones neurológicas, lo que la convierte en un proceso extremadamente complejo de analizar y comprender. El presente trabajo se centra en el modelado de las principales actividades que se llevan a cabo en el contexto de la Neurorrehabilitación actual con el objetivo de detectar aquellos puntos en que puedan ser mejoradas, tanto a nivel organizativo como a nivel de ejecución. Por otra parte, se trata de comprenderlas en profundidad para tratar de transformarlas posteriormente en nuevas actividades automatizadas y monitorizadas que se ajusten al nuevo paradigma de rehabilitación ubicua, personalizada y basada en la evidencia

Identificación de Oportunidades de Mejora en Procesos de Neurorrehabilitación

El modelado de procesos es una técnica de gestión empresarial destinada a la mejora continua de los procesos de una organización, como base operativa y estructural de la misma. En el ámbito de la Neurorrehabilitación, crece el interés por los mapas de procesos como herramienta de comprensión, representación y análisis de los procesos clínicos. El presente trabajo se centra en la identificación de oportunidades de mejora de las actividades de rehabilitación, con el objetivo de definir nuevas estrategias de monitorización y automatización que permitan su evolución hacia el nuevo modelo de rehabilitación ubicua, personalizada y basada en la evidencia

Detection of a classical Delta Scuti star in the new eclipsing binary system HIP 7666

HIP 7666 is a variable star newly discovered during the Hipparcos mission and classified as of unknown type (ESA 1997). During 23 nights between July 2000 and November 2000, over 2300 CCD observations in the V band were obtained from Hostalets de Pierola and Monegrillo observatories in Spain. These data show that the new variable is a detached eclipsing binary system with an orbital period of 2.37229 days. In addition, one of the components undergoes very short-period oscillations with a main pulsation frequency of 24.46 or 25.47 c/d. HIP 7666 is therefore a new member of the presently very few known detached eclipsing binary systems with a Delta Scuti type component.Comment: 6 pages, 8 Postscript figure

Dynein structure and power stroke

Dynein ATPases are microtubule motors that are critical to diverse processes such as vesicle transport and the beating of sperm tails; however, their mechanism of force generation is unknown. Each dynein comprises a head, from which a stalk and a stem emerge. Here we use electron microscopy and image processing to reveal new structural details of dynein c, an isoform from Chlamydomonas reinhardtii flagella, at the start and end of its power stroke. Both stem and stalk are flexible, and the stem connects to the head by means of a linker approximately 10 nm long that we propose lies across the head. With both ADP and vanadate bound, the stem and stalk emerge from the head 10 nm apart. However, without nucleotide they emerge much closer together owing to a change in linker orientation, and the coiled-coil stalk becomes stiffer. The net result is a shortening of the molecule coupled to an approximately 15-nm displacement of the tip of the stalk. These changes indicate a mechanism for the dynein power stroke

An inventory of the marine and transitional Middle/Upper Eocene deposits of the Southeastern Pyrenean Foreland Basin (NE Spain)

In the southeastern Ebro Foreland Basin, the marine deposits of Lutetian and Bartonian age show excellent outcrop conditions, with a great lateral and horizontal continuity of lithostratigraphic units. In addition, the rich fossil record -mainly larger foraminifers-, provides iostratigraphic data of regional relevance for the whole Paleogene Pyrenean Basin, that can be used for the Middle Eocene biocorrelation of the western Tethys. This contribution is a sedimentary and biostratigraphic synthesis of the basic outcrops and sections of the Lutetian and Bartonian marine and transitional deposits in the southeastern sector of the Ebro Foreland Basin

Biostratigrafía y litostratigrafía del Paleoceno Superior-Eoceno Inferior del sector oriental de la Cuenca Surpirenaica

This work is a revision of the Upper Paleocene-Lower Eocene lithostratigraphic units in the Southpyrenean basin and their larger foraminiferal assemblages (nummulitids and alveolinids). We assign the various assemblages to their respective alveolinid and nummulitid biozones.In the eastern part of the Southpyrenean Basin the Cadi and Sagnari formations present a nummulitid assemblage with a chronostratigraphic range from the early Ilerdian to the lowermost Cuisian. The lower part of the Corones Formation hosts an alveolinid assemblage belonging to the early Cuisian, whereas the uppermost part of this unit belongs to the middle Cuisian shown by magnetostratigraphic data. The La Penya and Armhncies formations present a nurnmulitid assemblage with a chronostratigraphic range between the rniddle Cuisian and the lowermost Lutetian. Finally, the Campdevhol Formation includes a reworked nummulitid assemblage that allows us to state the chronostratigraphic position of this unit as being no older than the late early Lutetian