Reproductive phenology of three species of Gelidiales (Rhodophyta) in two macroalgal communities from Tenerife (Atlantic Ocean, Canary Islands, Spain)

[EN] The reproductive phenology of three species of Gelidiales, Gelidium canariense, Gelidium arbuscula and Pterocladiella capillacea, was analysed seasonally for a period of one year in two localities on the West coast of Tenerife Atlantic Ocean, Canary Islands, Spain. Considerations are provided on sex ratio, maximum length and branch order of uprights and on the length of the thalli for each sexual and asexual phase of the Canary Islands populations. The three species were characterized by a high percentage of tetrasporophytes, while female and male gametophytes have been observed only in little proportion. Only G. canariense showed gametophytes in all seasons while the occurrence of gametophytes in G. arbuscula and Pterocladiella capillacea demonstrated a clear seasonality.

Biodiversidad morfológico-reproductiva y genética del género endémico canario Parolinia Webb (Brassicaceae)

Tesis realizada en el Jardín Botánico Canario "Viera y Clavijo" en colaboración con el Departamento de Biología de la Universidad de Las Palmas de GRan Canaria, dentro del Programa de Doctorado: Biodiversidad y Conservación Vegetal

Morphogenesis of the Ourense plains:(NW of Spain)

[EN] We present a geomorphological analysis of Ourense Province (NW Spain) characterized by: a general narrowing of the fluvial network, highlands with smooth reliefs partially eroded and lowlands with residual reliefs, several extensive plains of erosion frequently limited by fractures -among which Tertiary grabens are inserted-, some ?Hollow Surface?-type morphology, absence of sedimentary deposits outside the grabens, and a generalized outcrop of the Hercynian Massif substratum. Traditionally, this ?piano?s keyboard morphology? has been interpreted as expression of block tectonics in tensile regimen; instead we suggest the existence of: an isostatic upheaval simultaneous to a sequence of tectonic pulses of compressive regimen with activity in favour of transcurrent faults, a General Surface (R600), several plains that present a ?Hollow Surface?-type morphology (R1600 R1400 R1000), a generalized alteration that correspond to a same process of decomposition associated to fluctuating conditions of redox equilibrium, a erosional terraces related principaly to the palaeo-fluvial nets; moreover, we propose the existence of two morphoestructural lineament: the first one represented by the Fault of Vila Real (NE-SW) -a ramification of the ?Basal Pyrenean Overthrust?-, that would have been active at an early moment of the tectonic sequence with a left transcurrent fault, secondly the lineament represented by the Fault of Maceda (NNW-SSE) that would be related to the ?Fault System NW-SE? and would have produced a right transcurrent fault during a late tectonic pulse.

La Real Hacienda y el control del gasto. La Tesorería General en la España del siglo XVIII

[ES] La evolución historiográfica ocurrida en los últimos años en relación con el mundo de las finanzas en general y las Haciendas reales en particular, ha generado grandes cambios en la percepción del interés por el gasto de los Estados. La potenciación del deseo de observar cómo las Monarquías del Antiguo Régimen gestionan la atención a sus necesidades, conlleva aparejada una creciente atención por el estudio de los organismos encargados de dicha actuación. Entre estas instituciones destaca en la España del siglo XVIII la Tesorería Mayor o Tesorería General. Su estudio permite conocer la evolución política de la Monarquía y de su relación con las finanzas privadas desde una perspectiva diferente. Los estudios centrados en la actuación de este organismo, su composición interna, su estructura territorial, los mecanismos de su ordenación contable y, en definitiva, cualquier tipo de actuación ocurrida dentro del ámbito de su gestión son el objeto del presente estudio.