An updated biostratigraphy for the late Aragonian and the Vallesian of the Vallès-Penedès Basin (Catalonia)

The Vallès-Penedès Basin (Catalonia, Spain) is a classical area for the study of the Miocene land mammal faunas and includes one of the densest and most continuous records in Eurasia. Furthermore, it is the type area for the Vallesian European land mammal age. After decades of study a huge amount of bio- and magnetostratigraphic data have been collected, allowing an unprecedented dating accuracy. Here we provide an updated local biostratigraphy for the late Aragonian, Vallesian and Turolian of the Vallès-Penedès Basin. This new biostratigraphic scheme is almost exclusively based on fossil rodents, which are the most abundant and one of the best known mammal orders in the area. Our proposal represents a significant refinement compared to previous attempts and provides a formal diagnosis and description of each zone, as well as clear definition of boundaries and a reference locality and section. The chronology of zone boundaries and main bioevents is based on detailed magnetostratigraphic data. The defined biozones allow for the correlation of the sites without associated magnetostratigraphical data. Finally, the correlation of the Vallès-Penedès local zones with other detailed local biostratigraphies, such as those of the Calatayud-Montalbán and Teruel basins (east-central Spain) is discussed. The sequence and chronology of the main bioevents is roughly comparable, although the rodent succession and the structure of the assemblage show important differences between these areas

Los vertebrados fosiles del Abocador de Can Mata (els Hostalets de Pierola, l'Anoia, CataluÑa), una sucesion de localidades del Aragoniense superior (MN6 y MN7+8) de la cuenca del Valles-Penedes. CampaÑas 2002-2003, 2004-2005

Se presenta una síntesis del registro de vertebrados fósiles del Abocador de Can Mata (els Hostalets de Pierola, cuenca neógena del Vallès-Penedès), con especial énfasis en los aspectos taxonómico y bioestratigráfico. Este macroyacimiento incluye por el momento una sucesión de 91 localidades de micro- y/o macrovertebrados muestreadas, repartidas a lo largo de unos 300 m de serie estratigráfica, abarcando un intervalo de tiempo de más de un millón de años correspondiente al Aragoniense superior. Durante los 28 meses de trabajo de campo desarrollados a lo largo de las campañas 2002-2003, 2004 y 2005, se han recuperado más de 15.000 restos de macrovertebrados fósiles y más de 1.300 dientes de micromamíferos (cantidad que se verá incrementada en el futuro cuando haya finalizado el lavado y triado de los sedimentos acumulados). Se presenta por primera vez una lista exhaustiva del conjunto de localidades y su contextualización estratigráfica, además de una lista faunística actualizada y una propuesta de biozonación local. La gran riqueza fosilífera de la zona y el enorme esfuerzo de muestreo, combinados con los requerimientos de la legislación vigente sobre protección del patrimonio paleontológico, explican el éxito de la intervención paleontológica. En conjunto, la ampliación del vertedero de Can Mata, con el adecuado control paleontológico, proporciona una oportunidad única para investigar la composición faunística de los ecosistemas terrestres del Aragoniense superior en el suroeste de Europa

Ten years in the dump: An updated review of the Miocene primate-bearing localities from Abocador de Can Mata (NE Iberian Peninsula)

More than ten years of paleontological fieldwork during the enlargement of the Can Mata Landfill (Abocador de Can Mata [ACM]), in els Hostalets de Pierola (Vallès-Penedès Basin, NE Iberian Peninsula) led to the recovery of >60,000 Miocene vertebrate remains. The huge sampling effort (due to continuous surveillance of heavy machinery digging activity, coupled with manual excavation and screen-washing of sediments) enabled generally rare faunal elements such as pliopithecoid and hominoid primates to be found. Thanks to detailed litho-, bio- and magnetostratigraphic controls, accurate dating is possible for all the recovered primate remains from 19 of the 235 localities defined along the 234 m-thick composite stratigraphic sequence of the ACM. Here we report updated estimated (interpolated) ages for these paleontological localities and review the timing of the primate succession in this area. Our results indicate that the whole ACM sequence is late Aragonian in age (MN6 and MN7+8) and includes seven magnetozones that are correlated to subchrons C5Ar.1r to C5r.2r (ca. 12.6 to 11.4 Ma). Great apes (dryopithecines) are first recorded at 12.4-12.3 Ma, but most of the finds (Anoiapithecus, Pierolapithecus and Dryopithecus) cluster between 12.0 and 11.9 Ma, followed by some indeterminate dryopithecine remains between 11.7 and 11.6 Ma. Pliopithecoids first appear at 12.1 Ma, being subsequently represented by Pliopithecus between 11.9 and 11.7 Ma. The small-bodied hominoid Pliobates is the youngest ACM primate, with an estimated age of 11.6 Ma. Although these primates probably overlapped in time, their co-occurrence is recorded only twice, at 11.9 Ma (a dryopithecine with Pliopithecus) and at 11.6 Ma (a dryopithecine with Pliobates). The rare co-occurrence between great apes and small-bodied catarrhines might be attributable to sampling biases and/or to presumed diverging ecological preferences of these groups. In the future, more detailed analyses of the fauna recovered from the long and densely-sampled ACM sequence will hopefully throw new light on this long-standing, unresolved question

Kretzoiarctos gen. nov., the Oldest Member of the Giant Panda Clade

The phylogenetic position of the giant panda, Ailuropoda melanoleuca (Carnivora: Ursidae: Ailuropodinae), has been one of the most hotly debated topics by mammalian biologists and paleontologists during the last century. Based on molecular data, it is currently recognized as a true ursid, sister-taxon of the remaining extant bears, from which it would have diverged by the Early Miocene. However, from a paleobiogeographic and chronological perspective, the origin of the giant panda lineage has remained elusive due to the scarcity of the available Miocene fossil record. Until recently, the genus Ailurarctos from the Late Miocene of China (ca. 8–7 mya) was recognized as the oldest undoubted member of the Ailuropodinae, suggesting that the panda lineage might have originated from an Ursavus ancestor. The role of the purported ailuropodine Agriarctos, from the Miocene of Europe, in the origins of this clade has been generally dismissed due to the paucity of the available material. Here, we describe a new ailuropodine genus, Kretzoiarctos gen. nov., based on remains from two Middle Miocene (ca. 12–11 Ma) Spanish localities. A cladistic analysis of fossil and extant members of the Ursoidea confirms the inclusion of the new genus into the Ailuropodinae. Moreover, Kretzoiarctos precedes in time the previously-known, Late Miocene members of the giant panda clade from Eurasia (Agriarctos and Ailurarctos). The former can be therefore considered the oldest recorded member of the giant panda lineage, which has significant implications for understanding the origins of this clade from a paleobiogeographic viewpoint

Understanding the twist-bend nematic phase: the characterisation of 1-(4-cyanobiphenyl-4'-yloxy)-6-(4-cyanobiphenyl-4'-yl) hexane (CB6OCB) and comparison with CB7CB

Acknowledgements The FFTEM data were obtained at the (Cryo) TEM facility at the Liquid Crystal Institute, Kent State University, supported by the Ohio Research Scholars Program Research Cluster on Surfaces in Advanced Materials. ODL acknowledges the support of NSF DMR-1410378 grant. The authors are grateful for financial support from MINECO/FEDER MAT2015-66208-C3-2-P and from the Gobierno Vasco (GI/IT-449-10) OA via RSC Gold4GoldPeer reviewedPublisher PD

Intervenció paleontològica al jaciment oligocè del Talladell 3 (canal Segarra-Garrigues)

Altres ajuts: CERCA Programme/Generalitat de Cataluny

Bio- and magnetostratigraphic correlation of the Miocene primate bearing site of Castell de Barber a to the earliest Vallesian

Castell de Barberà, located in the Vallès-Penedès Basin (NE Iberian Peninsula), is one of the few European sites where pliopithecoids (Barberapithecus) and hominoids (cf. Dryopithecus) co-occur. The dating of this Miocene site has proven controversial. A latest Aragonian (MN7+8, ca. 11.88-11.18 Ma) age was long accepted by most authors, despite subsequent reports of hipparionin remains that signaled a Vallesian age. On the latter basis, Castell de Barberà was recently correlated to the early Vallesian (MN9, ca. 11.18-10.3 Ma) on tentative grounds. Uncertainties about the provenance of the Hippotherium material and the lack of magnetostratigraphic data precluded more accurate dating. After decades of inactivity, fieldwork was resumed in 2014-2015 at Castell de Barberà, including the original layer (CB-D) that in the past delivered most of the fossils. Here we report magnetostratigraphic results for the original outcrop and another nearby section. Our results indicate that CB-D is located in a normal polarity magnetozone at about midheight of a short (~20 m-thick) stratigraphic section. The composite magnetostratigraphic section (~50 m) has as many as four to six magnetozones. These multiple reversals, coupled with the in situ recovery of a Hippotherium humerus from CB-D in 2015, make it very unlikely the correlation of any of the sampled normal polarity magnetozones with the long normal polarity subchron C5n.2n (11.056-9.984 Ma), which is characteristic of the early Vallesian. Our results support instead a correlation of CB-D with C5r.1n (11.188-11.146 Ma), where the Aragonian/Vallesian boundary is situated, and therefore indicate an earliest Vallesian age of ~11.2 Ma for Castell de Barberà. Our results settle the longstanding debate about the Aragonian vs. Vallesian age of this site, which appears roughly coeval with the Creu de Conill 20 locality (11.18 Ma), where hipparionins are first recorded in the Vallès- Penedès Basi

Reingresos hospitalarios en un servicio de Medicina Interna de un hospital de tercer nivel

Objetivo principal: Identificar la tipología de pacientes que reingresan y los factores que intervienen en el reingreso hospitalario no planificado de un Servicio de Medicina Interna de tercer nivel. Metodología: Estudio observacional descriptivo con una muestra de 100 pacien-tes que reingresaron de forma consecutiva y no programada, antes de haber transcurrido 180 días. De cada uno de ellos se estudió variables demográficas, socio-familiares, salud-enfermedad, preocupación al alta anterior, continuidad asistencial y seguimiento terapéutico. Resultados principales: Los reingresos se produjeron en un 65% antes de 1 mes. Un 50% tenía más de 80 años y un 60% eran mujeres. El 40% convivía con personas de igual edad, siendo estas su principal cuidador. El principal motivo de ingreso, de reingreso y de proble-ma en domicilio fue la disnea. El diagnóstico mayoritario fue la infección respiratoria, con una media de comorbilidad de 4 y una media de cuidados al alta anterior de 3. Las personas se sintieron bien informadas al alta. Un 42 % recibió respuesta de su centro de atención primaria antes de las 48 horas y se sintió satisfecho por la atención que recibió. Un 18% de los pacientes no fueron cumplidores. Conclusión principal: los reingresos son más frecuentes en los primeros 30 días. Los mayores de 71 años con problemas respiratorios son los que presentaron mayor riesgo de reingreso

The STOP-AB trial protocol: efficacy and safety of discontinuing patient antibiotic treatment when physicians no longer consider it necessary

Desde 2011, la Sociedad Española de Medicina Familiar ha recomendado a los médicos de cabecera que pidan a sus pacientes que dejen de tomar antibióticos cuando sospechen una infección viral. El objetivo principal de este estudio es determinar si la interrupción del tratamiento con antibióticos cuando un médico de cabecera ya no lo considera necesario tiene algún impacto en el número de días con síntomas graves. Se realiza un ensayo clínico controlado aleatorizado, multicéntrico y abierto. El estudio se realizó en 10 centros de atención primaria en España. Los pacientes fueron asignados aleatoriamente a la estrategia habitual de continuar el tratamiento con antibióticos o suspender el tratamiento con antibióticos. Se calculó un tamaño de muestra de 240 pacientes por grupo sobre la base de una reducción de 1 día en la duración de los síntomas graves es un resultado clínicamente relevante. El resultado primario fue la duración de los síntomas graves, es decir, los síntomas puntuados 5 o 6 por medio de diarios de síntomas validados. Los resultados secundarios incluyeron antibióticos tomados, eventos adversos, satisfacción del paciente y complicaciones dentro de los primeros 3 meses.Since 2011, the Spanish Society of Family Medicine has recommended to GPs that focus on their patients to stop taking antibiotics when they suspect a viral infection. The main objective of this study is to determine whether interrupting antibiotic treatment when a GP is no longer considered necessary has an impact on the number of days with severe symptoms. A randomized, multicenter and open controlled clinical trial is carried out. The study was carried out in 10 primary care centers in Spain. The patients were randomly assigned to the usual strategy of continuing antibiotic treatment or discontinuing antibiotic treatment. A sample size of 240 patients per group is calculated based on a 1-day reduction in the duration of the sequential session is a clinically relevant result. The primary outcome was the duration of the severe symptoms, that is, the specific symptoms 5 or 6 by means of validated symptoms. The results include antibiotics taken, adverse events, patient satisfaction and difficulties within the first 3 mon