El confesor real en la Castilla de los Trastamara: 1366-1504

The knowledge about the figure of royal confessor has been, until recent times, very limited for the period of medieval Castile. A lot of studies have been done for Modern Age, when the institution of the kinǵs confessor played an important role in the Court of the Hispanic Crown. It is evident that this figure didńt appear ex nihilo in the Sixteenth Century and there existed some origins. Many historians mentioned some medieval confessors in their studies about any other subjects. Actually, it was not clear if those clerics could be properly considered as confessors. Our first aim has been to find all the references which exist in the sources and bibliography about kinǵs confessors in the Middle Ages and verify their nature as confessors. We fixed the beginning of the period of study with the reign of Enrique II, and its end with the death of Isabel I in 1504. The main reason is the fact that both sovereigns are the first and last monarchs of Trastamara dinasty, a very significant period in the origin of Modern State in Castile. The Church was an essential element in this process, on account of the service which many clerics enlisted to the Crown in different tasks (diplomacy, bureaucracy, Counsel and Counselling, etc.) and their ideological support to this endeavour. In this context, the royal confessor could perform an important work as personal advisor and a loyal subject to the person of the king in so many activities. This is well-known for Modern Age and also fort the reign of transition between this period and the precedent: the period of Catholic Kings. But it isńt for the times backwards...

Revisiting the Late Jurassic-Early Cretaceous of the NW South Iberian Basin: new ages and sedimentary environments

The study of the Upper Jurassic-Lower Cretaceous deposits (Higueruelas, Villar del Arzobispo and Aldea de Cortés Formations) of the South Iberian Basin (NW Valencia, Spain) reveals new stratigraphic and sedimentological data, which have significant implications on the stratigraphic framework, depositional environments and age of these units. Moreover, these new data encourage revising the previously proposed stratigraphic correlations between the studied units and those deposited in adjacent areas of the Iberian Basin. The Higueruelas Fm was deposited in a mid-inner carbonate platform where oncolitic bars migrated by the action of storms and where oncoid production progressively decreased towards the uppermost part of the unit. The overlying Villar del Arzobispo Fm has been traditionally interpreted as an inner platform-lagoon evolving into a tidal-flat. Here it is interpreted as an inner-carbonate platform affected by storms, where oolitic shoals protected a lagoon, which had siliciclastic inputs from the continent. The Aldea de Cortés Fm has been previously interpreted as a lagoon surrounded by tidal-flats and fluvial-deltaic plains. Here it is reinterpreted as a coastal wetland where siliciclastic muddy deposits interacted with shallow fresh to marine water bodies, aeolian dunes and continental siliciclastic inputs. The contact between the Higueruelas and Villar del Arzobispo Fms, classically defined as gradual, is interpreted here as gradual and rapid, because the transition between both units comprises few meters. More importantly, the contact between the Villar del Arzobispo and Aldea de Cortés Fms, previously considered as unconformable, is here interpreted as gradual. The presence of Alveosepta in the Villar del Arzobispo Fm suggests that at least part of this unit is Kimmeridgian, unlike the previously assigned Late Tithonian-Middle Berriasian age. Consequently, the underlying Higueruelas Fm, previously considered Tithonian, should not be younger than Kimmeridgian. Accordingly, sedimentation of the Aldea de Cortés Fm, previously considered Valanginian-Hauterivian, probably started during the Tithonian and it may be considered part of the regressive trend of the Late Jurassic-Early Cretaceous cycle. This is consistent with the dinosaur faunas, typically Jurassic, described in the Villar del Arzobispo and Aldea de Cortés Fms.