Functional Studies of PTCHD3 During Spermatogensis

Paracrine factor Desert hedgehog (Dhh) is essential for mouse spermatogenesis. However, the specific receptor of Dhh during spermatogenesis is unknown. This study aims to test the hypothesis that Ptchd3, a male germ cell-specific gene acts as a receptor for Dhh in spermatogenesis. In this study, a transgenic mouse model with Ptchd3 gene deletion was first successfully established. Then, in vivo fertility assay and in vitro analysis were performed on Ptchd3 null mutant male mice. The data obtained from the in vivo fertility experiments indicates that there is no statistical significance in offspring litter number (p-value 0.7973) and litter size (p-value 0.3648) among mutant, heterozygote and wild-type male mice. The data of in vitro sperm assay reveals that the abnormality /normality ratio of sperm morphology in Ptchd3 null mice demonstrates no statistical difference with that in wild-type mice (Tukey test interval ±4.7 to ±12.8). Taken together, these findings clearly attest that Ptchd3 is not essential for mouse spermatogenesis and fertility. However, whether Ptchd3 functions as a Dhh receptor remains undetermined. The knowledge gained from this research into the function of Ptchd3 on spermatogenesis could give us a better understanding of the Dhh signaling pathway in testis

Predicción de la frescura del aceite de oliva virgen extra durante el almacenamiento mediante espectroscopía de fluorescencia

Virgin olive oil quality relates to flavor and unique health benefits. Some of these properties are at the most desirable level when the oil is just extracted, since it is not a product that improves with age. On the contrary, the concentrations of many compounds change during its shelf-life. These changes reveal the aging of the oil but do not necessarily mean decay in sensory properties, so in some cases an aged oil from healthy olives may be better qualified than a fresh one from olives affected by fermentation. The aim of this work is to analyze different methodologies proposed for assessing the quality of virgin olive oil with implications in freshness and aging of the oil, and to highlight the possibilities of rapid spectrofluorimetric techniques for assessing oil freshness by checking the evolution of pigments during storage. The observed change in the selected spectral features and mathematical modelling over time was compared with the accepted model for predicting the amount of pyropheophytin a, which is based on isokinetic studies. The best regression was obtained for 655 nm (adjustedR2 = 0.91) wavelength, which matches the distinctive band of pigments. The two mathematical models described in this study highlight the usefulness of pigments in the prediction of the shelf-life of extra virgin olive oil.La calidad del aceite de oliva virgen está relacionada con su flavor y sus beneficios únicos para la salud. Algunas de estas propiedades se encuentran en el nivel más deseable cuando el aceite está recién extraído, ya que no es un producto que mejore con el tiempo. Por el contrario, las concentraciones de muchos compuestos cambian a lo largo de la vida útil. Estos cambios revelan el envejecimiento del aceite, pero no implican necesariamente la alteración de las propiedades sensoriales, por lo que en algunos casos un aceite envejecido procedente de aceitunas sanas puede presentar mejor calidad que uno fresco procedente de aceitunas afectadas por procesos de fermentación. El objetivo de este trabajo es estudiar diferentes metodologías propuestas para evaluar la calidad del aceite de oliva virgen con implicaciones en la frescura y el envejecimiento del aceite, destacando las posibilidades de las rápidas técnicas espectrofluorométricas para evaluar la frescura del aceite verificando la evolución de los pigmentos durante el almacenamiento. El cambio observado en las características espectrales seleccionadas y su modelado matemático a lo largo del tiempo se comparó con el modelo aceptado para predecir la cantidad de pirofeofitina a, que se basa en estudios isocinéticos. Los dos modelos matemáticos descritos en este estudio pusieron de manifiesto la utilidad de los pigmentos en la predicción de la vida útil del aceite de oliva virgen extra. La mejor regresión se obtuvo para 655 nm (R2 -ajustado = 0,91), longitud de onda que coincide con la banda distintiva de pigmentos.Secretaría de Estado de Investigación, Desarrollo e Innovación de España-AGL2015-69320-

Predicción de la frescura del aceite de oliva virgen extra durante el almacenamiento mediante espectroscopía de fluorescencia

Virgin olive oil quality relates to flavor and unique health benefits. Some of these properties are at the most desirable level when the oil is just extracted, since it is not a product that improves with age. On the contrary, the concentrations of many compounds change during its shelf-life. These changes reveal the aging of the oil but do not necessarily mean decay in sensory properties, so in some cases an aged oil from healthy olives may be better qualified than a fresh one from olives affected by fermentation. The aim of this work is to analyze different methodologies proposed for assessing the quality of virgin olive oil with implications in freshness and aging of the oil, and to highlight the possibilities of rapid spectrofluorimetric techniques for assessing oil freshness by checking the evolution of pigments during storage. The observed change in the selected spectral features and mathematical modelling over time was compared with the accepted model for predicting the amount of pyropheophytin a, which is based on isokinetic studies. The best regression was obtained for 655 nm (adjustedR2 = 0.91) wavelength, which matches the distinctive band of pigments. The two mathematical models described in this study highlight the usefulness of pigments in the prediction of the shelf-life of extra virgin olive oil.La calidad del aceite de oliva virgen está relacionada con su flavor y sus beneficios únicos para la salud. Algunas de estas propiedades se encuentran en el nivel más deseable cuando el aceite está recién extraído, ya que no es un producto que mejore con el tiempo. Por el contrario, las concentraciones de muchos compuestos cambian a lo largo de la vida útil. Estos cambios revelan el envejecimiento del aceite, pero no implican necesariamente la alteración de las propiedades sensoriales, por lo que en algunos casos un aceite envejecido procedente de aceitunas sanas puede presentar mejor calidad que uno fresco procedente de aceitunas afectadas por procesos de fermentación. El objetivo de este trabajo es estudiar diferentes metodologías propuestas para evaluar la calidad del aceite de oliva virgen con implicaciones en la frescura y el envejecimiento del aceite, destacando las posibilidades de las rápidas técnicas espectrofluorométricas para evaluar la frescura del aceite verificando la evolución de los pigmentos durante el almacenamiento. El cambio observado en las características espectrales seleccionadas y su modelado matemático a lo largo del tiempo se comparó con el modelo aceptado para predecir la cantidad de pirofeofitina a, que se basa en estudios isocinéticos. Los dos modelos matemáticos descritos en este estudio pusieron de manifiesto la utilidad de los pigmentos en la predicción de la vida útil del aceite de oliva virgen extra. La mejor regresión se obtuvo para 655 nm (R2 -ajustado = 0,91), longitud de onda que coincide con la banda distintiva de pigmentos.Secretaría de Estado de Investigación, Desarrollo e Innovación de España-AGL2015-69320-

Taphonomy as a methodological framework for understanding surface funerary deposits: the human burial at the cave of El Espinoso (Ribadedeva, Asturias)

RESUMEN: Durante la Edad del Bronce en el norte de la Península Ibérica algunos grupos humanos inhumaban a sus congéneres sobre la superficie del suelo de cuevas de difícil acceso. Esta tradición cultural, muy arraigada en el País Vasco y en Cantabria, se extiende hasta la región oriental de Asturias. Este trabajo se centra en el estudio tafonómico de los restos humanos encontrados en 1993 en la cueva de El Espinoso (Ribadedeva, Asturias). La cueva fue utilizada como lugar de inhumación de un número mínimo de veinte individuos, de ambos sexos y diferentes edades. Este yacimiento constituye el único enterramiento múltiple en cueva de la Edad del Bronce documentado hasta ahora en Asturias, sumándose así a otros yacimientos de la Prehistoria Reciente de esta región, como son El Toral III, La Llana y Fuentenegroso y consolidando esta tradición funeraria a lo largo de dos mil años en el Oriente de Asturias. La tafonomía ha ofrecido un marco teórico y metodológico preciso para estudiar este tipo de yacimientos en superficie, afectados por complejos procesos post-deposicionales.ABSTRACT: During the Bronze Age the human groups of Cantabria buried their dead on the surface of narrow caves. This cultural tradition, common to the Basque Country and Cantabria, extends to eastern Asturias. This work focuses on the taphonomical study of the human remains found in 1993 in the cave of El Espinoso, located in Ribadedeva (Asturias). The cavity was used as a burial place for a minimum of twenty individuals of both sexes and different ages. This site constitutes the only collective burial cave currently known from the Bronze Age in Asturias (other later prehistoric burial caves in the region ?El Toral III, La Llana, Fuentenegroso, etc.? have single burials). A funerary tradition of cave burial lasted over two thousand years in eastern Asturias. The taphonomical analysis provides a theoritical and methodological framework adequate to the study this type of superficial deposits, affected by complex post-depositional processes.Este estudio se ha realizado a partir del Trabajo Fin de Máster del primero de los autores. La investigación ha sido apoyada por el Instituto Internacional de Investigaciones Prehistóricas de Cantabria y financiada por el Proyecto “Tracing Climatic Abrupt Change Events and Their Social Impact during the Late Pleistocene and Early Holocene (15–7 ky calBP) (HAR2013-46802-P)” financiado por el Ministerio de Economía y Competitividad de España

Presente-pasado. Definición y usos de una categoría historiográfica en historia de la ciencia: El arte prehistórico como paradigma.

In this paper we will investigate the potential for the application of the concept of “present-past” in the study of the history of archaeology. We suggest that this category provides archaeologists with a useful model in order to understand (A) the role of our present concepts and ideas in the definition of the past and (B) the impact of archaeological finds on modern Western societies. Taking the example of the cave of Altamira into account, we will analyse first the importance of assumptions deeply embedded in Western culture in the definition of Palaeolithic art at the end of nineteenth century. Secondly, we will show the influence (economic, cultural, political) that Palaeolithic art exerts on our modern societies. Through this examination, we will show the way in which the concept of “present-past” can be used in history of science.En este artículo exploramos las potencialidades de la categoría historiográfica “presente-pasado” en historia de la arqueología. Dicha categoría debe ser considerada como un instrumento que permita a los historiadores comprender (A) la importancia del presente en la definición del pasado y (B) el impacto que la arqueología ejerce sobre nuestras modernas sociedades occidentales. Tomando como ejemplo la cueva de Altamira, analizaremos en primer lugar la importancia que nuestras modernas categorías ejercieron sobre la definición del arte paleolítico a finales del siglo XIX. En segundo lugar, mostraremos la influencia (económica, cultural, política) que el arte paleolítico ejerce sobre nuestras modernas sociedades contemporáneas. De este modo, esperamos demostrar las potencialidades de la categoría “presente-pasado” en historia de la ciencia

Paleoclimatic inference of the mid-Holocene record of monk seal (Monachus monachus) in the Cantabrian Coast

The mid-Holocene has been widely used to test the performance of the numerical models that are commonly employed to estimate the future evolution of world climate. This period, as the pollen record shows, was characterized by higher temperatures than present in northern and Central Europe, while cooler conditions occurred in the south of the continent. This pattern is challenging numeric algorithms that widely fail to replicate the paleoclimate data of southern Europe. Here we report the discovery of a fragmented bone of a temperate water phocid (Monachus monachus) dated to 5540 ± 40 BP that was hunted and consumed on the Cantabrian Coast during that period. This find implies a hitherto unnoted phase of warm conditions associated with strengthened advention of subtropical waters to the region. As a consequence, the possibility that the oceanographic regime from that time in the Bay of Biscay was similar to the current one is reinforced, a fact that could modify our view of mid-Holocene climate in the Iberian Peninsula and have important implications in climate change studies

Palaeogenomics of Upper Palaeolithic to Neolithic European hunter-gatherers

Modern humans have populated Europe for more than 45,000 years1,2. Our knowledge of the genetic relatedness and structure of ancient hunter-gatherers is however limited, owing to the scarceness and poor molecular preservation of human remains from that period3. Here we analyse 356 ancient hunter-gatherer genomes, including new genomic data for 116 individuals from 14 countries in western and central Eurasia, spanning between 35,000 and 5,000 years ago. We identify a genetic ancestry profile in individuals associated with Upper Palaeolithic Gravettian assemblages from western Europe that is distinct from contemporaneous groups related to this archaeological culture in central and southern Europe4, but resembles that of preceding individuals associated with the Aurignacian culture. This ancestry profile survived during the Last Glacial Maximum (25,000 to 19,000 years ago) in human populations from southwestern Europe associated with the Solutrean culture, and with the following Magdalenian culture that re-expanded northeastward after the Last Glacial Maximum. Conversely, we reveal a genetic turnover in southern Europe suggesting a local replacement of human groups around the time of the Last Glacial Maximum, accompanied by a north-to-south dispersal of populations associated with the Epigravettian culture. From at least 14,000 years ago, an ancestry related to this culture spread from the south across the rest of Europe, largely replacing the Magdalenian-associated gene pool. After a period of limited admixture that spanned the beginning of the Mesolithic, we find genetic interactions between western and eastern European hunter-gatherers, who were also characterized by marked differences in phenotypically relevant variants.This project has received funding by the European Research Council under the European Union’s Horizon 2020 research and innovation programme under grant agreements no. 803147-RESOLUTION (to S.T.), no. 771234-PALEoRIDER (to W.H.), no. 864358 (to K.M.), no. 724703 and no. 101019659 (to K.H.). K.H. is also supported by the Deutsche Forschungsgemeinschaft (DFG FOR 2237). E.A. has received funding from the Van de Kamp fonds. PACEA co-authors of this research benefited from the scientific framework of the University of Bordeaux’s IdEx Investments for the Future programme/GPR Human Past. A.G.-O. is supported by a Ramón y Cajal fellowship (RYC-2017-22558). L. Sineo, M.L. and D.C. have received funding from the Italian Ministry of University and Research (MUR) PRIN 2017 grants 20177PJ9XF and 20174BTC4R_002. H. Rougier received support from the College of Social and Behavioral Sciences of CSUN and the CSUN Competition for RSCA Awards. C.L.S. and T. Saupe received support from the European Union through the European Regional Development Fund (project no. 2014-2020.4.01.16-0030) and C.L.S. received support from the Estonian Research Council grant PUT (PRG243). S. Shnaider received support from the Russian Science Foundation (no. 19-78 10053)

Vicia vulcanorum (Fabaceae), nueva especie para la isla de Lanzarote (Islas Canarias)

Vicia vulcanorum J. Gil & M. L. Gil (Fabaceae), a new species of subg. Cracca (Dumort.) Peterm., sect. Cracca Dumort. is described and illustrated from the island of Lanzarote, Canary Islands, north-west of Africa. It is related to and compared with Vicia cirrhosa C. Sm. ex Webb & Berthel. and Vicia filicaulis Webb & Berthel., two endemic species from the western and central group of the Canary Islands, and Vicia ferreirensis Goyder, an endemic species from Porto Santo Island, Madeira Archipelago.Se describe e ilustra Vicia vulcanorum J. Gil & M. L. Gil (Fabaceae), una nueva especie y endemismo de la isla de Lanzarote, Islas Canarias, perteneciente al subg. Cracca (Dumort.) Peterm., sect. Cracca Dumort. Se encuentra relacionada y es comparada con Vicia cirrhosa C. Sm. ex Webb & Berthel. y Vicia filicaulis Webb & Berthel., especies endémicas de las islas centrales y occidentales del archipiélago canario, y con Vicia ferreirensis Goyder, especie endémica de la isla de Porto Santo, en el archipiélago de Madeira

Fractionation and fluxes of metals and radionuclides during the recycling process of phosphogypsum wastes applied to mineral CO2 sequestration

The industry of phosphoric acid produces a calcium-rich by-product known as phosphogypsum, which is usually stored in large stacks of millions of tons. Up to now, no commercial application has been widely implemented for its reuse because of the significant presence of potentially toxic contaminants. This work confirmed that up to 96% of the calcium of phosphogypsum could be recycled for CO2 mineral sequestration by a simple two-step process: alkaline dissolution and aqueous carbonation, under ambient pressure and temperature. This CO2 sequestration process based on recycling phosphogypsum wastes would help to mitigate greenhouse gasses emissions. Yet this work goes beyond the validation of the sequestration procedure; it tracks the contaminants, such as trace metals or radionuclides, during the recycling process in the phosphogypsum. Thus, most of the contaminants were transferred from raw phosphogypsum to portlandite, obtained by dissolution of the phosphogypsum in soda, and from portlandite to calcite during aqueous carbonation. These findings provide valuable information for managing phosphogypsum wastes and designing potential technological applications of the by-products of this environmentally-friendly proposal.Junta de Andalucía P10-RNM-6300, P12- RNM-226