Evidence for different expression profiles for c-Met, EGFR, PTEN and the mTOR pathway in low and high grade endometrial carcinomas in a cohort of consecutive women. Occurrence of PIK3CA and K-Ras mutations and microsatellite instability.

Molecular and genetic investigations in endometrial carcinogenesis may have prognostic and therapeutic implications. We studied the expression of EGFR, c-Met, PTEN and the mTOR signalling pathway (phospho-AKT/phospho-mTOR/phospho-RPS6) in 69 consecutive tumours and 16 tissue microarrays. We also analysed PIK3CA, K-Ras mutations and microsatellite instability (MSI). We distinguished two groups: group 1 (grade 1 and 2 endometrioid cancers) and group 2 (grade 3 endometrioid and type II clear and serous cell cancers). We hypothesised that these histological groups might have different features. We found that a) survival was higher in group 1 with less aggressive tumours (P⟨0.03); b) EGFR (P=0.01), PTEN and the AKT/mTOR/RPS6 signalling pathway were increased in group 1 versus group 2 (P=0.05 for phospho-mTOR); c) conversely, c-Met was higher (P⟨0.03) in group 2 than in group 1; d) In group 1, EGFR was correlated with c-Met, phospho-mTOR, phospho-RPS6 and the global activity of the phospho-AKT/phospho-mTOR/phospho-RPS6 pathway. In group 2, EGFR was correlated only with the phospho-AKT/phospho-mTOR/phospho-RPS6 pathway, whereas c-Met was correlated with PTEN; e) survival was higher for tumours with more than 50% PTEN-positive cells; f) K-RAS and PIK3CA mutations occurred in 10-12% of the available tumours and MSI in 40.4%, with a loss of MLH1 and PMS2 expression. Our results for endometrial cancers provide the first evidence for a difference in status between groups 1 and 2. The patients may benefit from different targeted treatments, anti-EGFR agents and rapamycin derivatives (anti-mTOR) for group 1 and an anti c-MET/ligand complex for group 2.

Els Almogàvers: Les cares d'un mite.

Els almogàvers foren un grup de guerrers mercenaris que se singularitzava en el si dels exèrcits de la Corona d'Aragó. Esmentats per Jaume el Conqueridor i descrits per Desclot, són els protagonistes dels capítols en què Ramon Muntaner narra la seva màxima gesta: l'aventura en terres bizantines, a conseqüència de la qual els reis d'Aragó seran ducs d'Atenes i Neopàtria. Posteriorment el seu exemple serà al·legat en temps de dificultat Guerra de Successi, Guerra contra Napoleó fins que la Renaixença els reivindicarà i en farà un mite. El present article estudia com els tractà la literatura catalana, i també la castellana, des dels primers textos i sobretot durant els segles XIX i XX, en un recorregut en què es revela com un mite imperfecte, car els aspectes violents remarcats per la propaganda hel·lènica han estat un llast impossible d'eliminar.

Dots i llegats dels Baldrich de Valls (1768-1863)

Aquest article presenta les dificultats que van haver d’afrontar entre 1768 i 1863 els hereus de la casa Baldrich de Valls per liquidar els dots i les deixes testamentàries. Anton Baldrich Janer va nomenar hereu el fill gran del primer matrimoni amb l’obligació de pagar als seus germans i especialment als seus germanastres unes quantitats molt elevades de diners atorgats en un moment de grans expectatives econòmiques, gràcies al comerç amb Amèrica i el nord d’Europa. Durant la primera meitat del segle XIX, alguns anys de males collites, les contínues guerres i la independència de les colònies americanes feren minvar els recursos i van afeblir la hisenda familiar. Els successius hereus maldaven per pagar les contínues reclamacions dels cabalers i les cabaleres de les diferents generacions, fet que els impedia invertir en noves empreses per tal d’ampliar i modernitzar els seus negocis. L’any 1863, el darrer hereu Baldrich va morir sense descendència, havent pagat els darrers deutes familiars però sense haver creat nous horitzons per als seus successors.

La cultura material de Tarraco - Tarracona (Hispania Tarraconensis - Regnum Visigothorum): cerámica común y ánforas

Síntesis actualizada de los estudios monográficos realizados sobre las cerámicas comunes y ánforas de la ciudad de Tarraco desde finales del s. IV hasta inicios del s. VIII. Se hace especial hincapié en los últimos hallazgos del siglo VII que reflejan una intensificación de la presencia de materiales orientales en la ciudad.

Réunion internationale de physique, chimie, biologie, Congrès du Palais de la découverte, Paris, octobre 1937. 5, Chimie minérale / Van Arkel, U.-R. Evans, W.-L. Bragg... [et al.]

Collection : Actualités scientifiques et industrielles ; 722

Deep incision in an Aptian carbonate succession indicates major sea-level fall in the Cretaceous

Long-term relative sea-level cycles (0 5 to 6 Myr) have yet to be fully understood for the Cretaceous. During the Aptian, in the northern Maestrat Basin (Eastern Iberian Peninsula), fault-controlled subsidence created depositional space, but eustasy governed changes in depositional trends. Relative sea-level history was reconstructed by sequence stratigraphic analysis. Two forced regressive stages of relative sea-level were recognized within three depositional sequences. The first stage is late Early Aptian age (intra Dufrenoyia furcata Zone) and is characterized by foreshore to upper shoreface sedimentary wedges, which occur detached from a highstand carbonate platform, and were deposited above basin marls. The amplitude of relative sea-level drop was in the order of tens of metres, with a duration of <1 Myr. The second stage of relative sea-level fall occurred within the Late Aptian and is recorded by an incised valley that, when restored to its pre-contractional attitude, was >2 km wide and cut 115 m down into the underlying Aptian succession. With the subsequent transgression, the incision was back-filled with peritidal to shallow subtidal deposits. The changes in depositional trends, lithofacies evolution and geometric relation of the stratigraphic units characterized are similar to those observed in coeval rocks within the Maestrat Basin, as well as in other correlative basins elsewhere. The pace and magnitude of the two relative sea-level drops identified fall within the glacio-eustatic domain. In the Maestrat Basin, terrestrial palynological studies provide evidence that the late Early and Late Aptian climate was cooler than the earliest part of the Early Aptian and the Albian Stage, which were characterized by warmer environmental conditions. The outcrops documented here are significant because they preserve the results of Aptian long-term sea-level trends that are often only recognizable on larger scales (i.e. seismic) such as for the Arabian Plate.

Deep incision in an Aptian carbonate succession indicates major sea-level fall in the Cretaceous

Long-term relative sea-level cycles (0 5 to 6 Myr) have yet to be fully understood for the Cretaceous. During the Aptian, in the northern Maestrat Basin (Eastern Iberian Peninsula), fault-controlled subsidence created depositional space, but eustasy governed changes in depositional trends. Relative sea-level history was reconstructed by sequence stratigraphic analysis. Two forced regressive stages of relative sea-level were recognized within three depositional sequences. The first stage is late Early Aptian age (intra Dufrenoyia furcata Zone) and is characterized by foreshore to upper shoreface sedimentary wedges, which occur detached from a highstand carbonate platform, and were deposited above basin marls. The amplitude of relative sea-level drop was in the order of tens of metres, with a duration of <1 Myr. The second stage of relative sea-level fall occurred within the Late Aptian and is recorded by an incised valley that, when restored to its pre-contractional attitude, was >2 km wide and cut 115 m down into the underlying Aptian succession. With the subsequent transgression, the incision was back-filled with peritidal to shallow subtidal deposits. The changes in depositional trends, lithofacies evolution and geometric relation of the stratigraphic units characterized are similar to those observed in coeval rocks within the Maestrat Basin, as well as in other correlative basins elsewhere. The pace and magnitude of the two relative sea-level drops identified fall within the glacio-eustatic domain. In the Maestrat Basin, terrestrial palynological studies provide evidence that the late Early and Late Aptian climate was cooler than the earliest part of the Early Aptian and the Albian Stage, which were characterized by warmer environmental conditions. The outcrops documented here are significant because they preserve the results of Aptian long-term sea-level trends that are often only recognizable on larger scales (i.e. seismic) such as for the Arabian Plate.

Proceedings of the 1st Seminar on Higher Education Rankings and E-learning

First International Seminar on Higher EducationRankings and e-Learning. Proceedings