Beyond the subject DP versus the subject pronoun divide in agreement switches

Producción CientíficaPrevious code-switching literature argues that no switch takes place between a pronoun and a verb, while Determiner Phrases (DPs) do code-switch. This paper uses code-switching acceptability judgment data elicited from three groups of English–Spanish bilinguals (2L1 children, L2 English children and L2 English adults) to test: (i) van Gelderen & MacSwan’s (2008) PF disjunction theorem intended to account for the DP/pronoun divide; and (ii) an agreement version of the analogical criterion (Liceras et al. 2008) which is based on Pesetsky & Torrego’s (2001) double-feature valuation mechanism intended to account for the different status of third person versus first and second person pronominal subjects. We show that the PF disjunction theorem is clearly rooted in the mind of the bilingual and that the Spanish dominant bilinguals can ‘relax’ its requirements to value person agreement features as predicted by the double-feature valuation mechanism.Ministerio de Ciencia e Innovación - FEDER (HUM2007-62213 and BFF2002-00442)Faculty of Arts of the University of Ottawa - Social Sciences and Humanities Research Council of Canada (410-2004-2034)International Council for Canadian Studies - Department of Foreign Affairs (10-CEA-A

Linguistic theory and bilingual systems: Simultaneous and sequential English/Spanish bilingualism

Producción CientíficaUsing data from simultaneous and sequential bilingualism, we address a series of learnability issues by investigating the acquisition of four different structures: (i) the [Gender] feature of the Spanish Determiner in the production of English/ Spanish mixed Determiner Phrases; (ii) the [Determiner] feature of Tense in the production of null/overt subjects; (iii) the morphosyntactic status of definite articles and clitics; and (iv) the morphosyntactic characteristics of Spanish deverbal compounds. We compare spontaneous and experimental data elicited from children and adults in order to show how these linguistic constructs can account for the differences and similarities between native and non-native bilingual systems. The data reveal clear-cut differences between native and non-native production/ interpretation. We attribute this to feature specification and the way in which both groups access the input.Ministerio de Ciencia y Tecnología de España - FEDER (BFF2002-00442)Faculty of Arts of the University of Ottawa - Social Sciences and Humanities Research Council of Canada (410-2004-2034

Geología y mineralogía del yacimiento polimetálico de Au-As (Ag-Pb-Zn-Cu-Sb) de Valiña-Azúmara (Lugo, NO de España)

Valiña-Azúmara is a polymetallic Au-As (Ag-Pb-Zn-Cu-Sb) deposit, located in the province of Lugo (NW Spain), that was mined for arsenic at the beginning of the 20th century. The mineralization is hosted in a Variscan thrust fault with a dip direction of N247-261ºE, and N-S and NE-SW Late-Variscan faults. These structures are hosted in black slates, Cambrian in age. To a lesser extent, the mineralization also occurs disseminated within narrow, weakly silicified and sericited selvages. Mineralization is divided into two hypogene stages. The first consists of quartz, calcite, rutile, sericite, arsenopyrite and pyrite. Two types of pyrite (Py-I and Py-II) are defined according to their chemical and textural characteristics. Py-II occurs as overgrowth of previous Py-I crystals. Py-II is As-rich (≤1.7 wt.%) and often contains traces of Te, Zn, Cu, Bi, Sb and Au. The mineralized drill core sections show a significant correlation between Au and As. This is due to Au occurring as invisible Au within the Py-II grains, with contents of up to 176 ppm. The Au/As ratios of Py-II indicate that Au was deposited as Au1+, as solid solution within the pyrite structure. The second stage of mineralization is enriched in Ag-Pb-Zn-Cu-Sb, replacing the first stage, and consists of quartz, calcite, chlorite, sphalerite, jamesonite, Ag-rich tetrahedrite, freibergite, chalcopyrite, pyrrhotite and galena. Although jamesonite shows traces of Ag, the Cu-Ag sulfosalts are the main carriers of the Ag mineralization in the deposit, with contents that vary from 13.7 to 23.9 wt.% of Ag. In the most superficial levels of the area, secondary Fe oxide and hydroxide, scorodite and anglesite developed due to the oxidation of the ore.Valiña-Azúmara es un yacimiento filoniano de Au-As (Ag-Pb-Zn-Cu-Sb) situado en la provincia de Lugo (NO España), que fue explotado por arsénico a principios del siglo XX. La mineralización se encuentra encajada en un cabalgamiento Varisco de dirección de buzamiento N247-261°E y en fracturas tardivariscas de dirección N-S y NE-SO que cortan a filitas negras de edad Cámbrica. En menor medida la mineralización también se encuentra diseminada en el encajante, en finas salbandas levemente sericitizadas y silicificadas. La mineralización se divide en dos etapas hipogénicas. La primera está constituida por cuarzo, calcita, rutilo, sericita, arsenopirita y pirita. En base a su composición y textura, se diferencian dos tipos de pirita, Py-I y Py II. La Py-II suele encontrarse recrecida sobre la Py I, formando bandas poligonales. Esta pirita está enriquecida en As (≤1,7% en peso) y contiene trazas de otros metales como Te, Zn, Cu, Bi, Sb y Au. Los tramos mineralizados de sondeo del yacimiento presentan correlación geoquímica entre los elementos Au y As, debido a que el Au se halla en forma de oro refractario dentro de los cristales de pirita arsenical (Py-II), los cuales llegan a presentar concentraciones en Au de hasta 176 ppm. La relación Au/As de la Py-II sugiere que el oro se encuentra en forma de Au+1, en solución sólida dentro de la estructura cristalina del mineral. La segunda etapa de mineralización está enriquecida en Ag-Pb-Zn-Cu-Sb y consiste en cuarzo, calcita, clorita, esfalerita, jamesonita, cobres grises (tetraedrita argentífera y freibergita), calcopirita, pirrotina y galena. Esta etapa se encuentra rellenando fracturas y cavidades intersticiales en los minerales de la etapa anterior, reemplazándolos en parte. Los principales minerales portadores de Ag son los cobres grises, con contenidos que varían entre 13,7 y 23,9% en peso. En la parte más superficial del yacimiento, la alteración supergénica de la mena primaria dio como resultado la formación de óxidos e hidróxidos de hierro, escorodita y anglesita

Design of a GIS-database for the management of the Courel Mountains UNESCO Global Geopark (Spain)

X Congreso Geológico de España, 5-7 Julio 2021, Vitoria - GasteizSe ha desarrollado una base de datos en un sistema de información geográfica (SIG) para la gestión del Geoparque Mundial de la UNESCO Montañas do Courel (NO de España). El SIG incluye 66 capas de información topográfica, geológica, minera, biológica, arqueológica y etnográfica, que pueden ser combinadas entre sí para elaborar mapas temáticos adaptados a la finalidad y al usuario. Los mapas generados son empleados en actividades de divulgación, en el diseño de cartografías técnicas de apoyo a los gestores del Geoparque, en el desarrollo de estudios científicos y en acciones de geoconservació

The granite‑hosted Variscan gold deposit from Santo António mine in the Iberian Massif (Penedono, NW Portugal): constraints from mineral chemistry, fuid inclusions, sulfur and noble gases isotopes

The study area is located in the Central Iberian Zone, a major tectonic unit of the Iberian Massif (Variscan belt). In this region the basement is composed of Cambrian-Ordovician sedimentary and minor volcanic rocks that underwent deformation and metamorphism during the Carboniferous. These metamorphic rocks host ca. 331–308 Ma granitic plutons emplaced during the D2 extensional and D3–D4 contractional deformation phases. The gold-bearing quartz veins from the Santo António mine (Penedono region) occur in granite formed at 310.1 ± 1.1 Ma and post-dated the peak of metamorphism. Gold–silver alloy is included in quartz, but mainly occurs in spaces between grains or micro-fractures within arsenopyrite of all three generations and less in pyrite. Late sulphides and sulphosalts were deposited along fractures mainly in arsenopyrite, and locally surrounding the gold–silver alloy grains. Ferberite, scheelite and stolzite replace arsenopyrite. The abundant aqueous carbonic fluids and the occurrence of a low-salinity fluid and their minimum possible entrapment temperature of 360–380 °C suggest that this gold-forming event began during the waning stages of the Variscan orogeny. The mean δ34S values of arsenopyrite and pyrite are − 4.7‰ and − 3.8‰, respectively. He–Ar–Ne isotopic data suggest a crustal origin. The ascent of the granite magma has provided the heat for remobilization of gold, other metals and metalloids from the metamorphic rocks. This gold-arsenopyrite deposit has thus similar characteristics as other selected gold-arsenopyrite deposits from the Iberian Massif, but it contains tungstates.El área de estudio está ubicada en la Zona Centroibérica, una importante unidad tectónica del Macizo Ibérico (cinturón varisco). En esta región el basamento está compuesto por rocas sedimentarias y volcánicas del Cámbrico-Ordovícico tectonizadas y metamorfzadas durante el Carbonífero. Estas rocas metamórfcas sirven como caja de los plutones graníticos datados en torno a 331–308 Ma y que fueron emplazados durante la fase de deformación extensional D2 y las fases de deformación contraccional D3 y D4. Las venas de cuarzo ricas en oro de la mina de Santo António (región de Penedono) que aparecen en un granito datado a los 310.1 ± 1.1 Ma son posteriores al pico metamórfco regional. La aleación de oro y plata se incluye en el cuarzo, pero se produce principalmente en los espacios entre granos o micro-fracturas dentro de arsenopirita de las tres generaciones y menos en pirita. Los sulfuros y sulfuros tardíos se depositaron a lo largo de las fracturas principalmente en arsenopirita, y alrededor de los granos de aleación de oro y plata. Ferberita, scheelita y la estolzita sustituyen a la arsenopirita. Los abundantes líquidos acuosos carbónicos y la presencia de un fuido de baja salinidad y su posible temperatura de atrapamiento mínima en torno de 360-380 ºC sugieren que este evento de formación de oro comenzó durante las etapas fnales de la orogenia varisca. Los valores medios de S de arsenopirita y pirita son − 4.7 ‰ y − 3.8 ‰, respectivamente. Los datos isotópicos de He–Ar–Ne sugieren que en el origen de los fuidos mineralizados participa la corteza continental. El ascenso del magma granítico ha provisto el calor para la movilización del oro, otros metales y metaloides desde las rocas metamórfcas. Este depósito de oroarsenopirita tiene así características similares a otros yaciamientos con arsenopirita y oro del Macizo Ibérico, pero sin embargo contienen tungstates.This research was financially supported by Fundação para a Ciência e Tecnologia through the projects GOLDGranites, Orogenesis, Long-term strain/stress and Deposition of ore metals—PTDC/GEO-GEO/2446/2012: COMPETE: FCOMP-01-0124-FEDER-029192 and UID/GEO/04035/2013

Diverse Large HIV-1 Non-subtype B Clusters Are Spreading Among Men Who Have Sex With Men in Spain

In Western Europe, the HIV-1 epidemic among men who have sex with men (MSM) is dominated by subtype B. However, recently, other genetic forms have been reported to circulate in this population, as evidenced by their grouping in clusters predominantly comprising European individuals. Here we describe four large HIV-1 non-subtype B clusters spreading among MSM in Spain. Samples were collected in 9 regions. A pol fragment was amplified from plasma RNA or blood-extracted DNA. Phylogenetic analyses were performed via maximum likelihood, including database sequences of the same genetic forms as the identified clusters. Times and locations of the most recent common ancestors (MRCA) of clusters were estimated with a Bayesian method. Five large non-subtype B clusters associated with MSM were identified. The largest one, of F1 subtype, was reported previously. The other four were of CRF02_AG (CRF02_1; n = 115) and subtypes A1 (A1_1; n = 66), F1 (F1_3; n = 36), and C (C_7; n = 17). Most individuals belonging to them had been diagnosed of HIV-1 infection in the last 10 years. Each cluster comprised viruses from 3 to 8 Spanish regions and also comprised or was related to viruses from other countries: CRF02_1 comprised a Japanese subcluster and viruses from 8 other countries from Western Europe, Asia, and South America; A1_1 comprised viruses from Portugal, United Kingom, and United States, and was related to the A1 strain circulating in Greece, Albania and Cyprus; F1_3 was related to viruses from Romania; and C_7 comprised viruses from Portugal and was related to a virus from Mozambique. A subcluster within CRF02_1 was associated with heterosexual transmission. Near full-length genomes of each cluster were of uniform genetic form. Times of MRCAs of CRF02_1, A1_1, F1_3, and C_7 were estimated around 1986, 1989, 2013, and 1983, respectively. MRCA locations for CRF02_1 and A1_1 were uncertain (however initial expansions in Spain in Madrid and Vigo, respectively, were estimated) and were most probable in Bilbao, Spain, for F1_3 and Portugal for C_7. These results show that the HIV-1 epidemic among MSM in Spain is becoming increasingly diverse through the expansion of diverse non-subtype B clusters, comprising or related to viruses circulating in other countries

The Lalin pegmatite field and their Sn, Ta, Nb associate mineralizations (Pontevedra, Galicia, Spain)

The aim of this paper is to present the most important mineralogical, textural and pretrological characteristics of the Lalin pegmatite field. We can establish two different types of zoned pegmatites, with Li and without Li. Both of them are mineralized in Sn, Nb and Ta. Also, based on textural and mineralogical features, we defined two different types of lithium pegmatites. On the other hand, we described de tin, niobium and tantalum mineralization on each established group. We point out the high cassiterite, columbite-tantalite and phosphates content in LCLP grou