El paleógeno del sector suroccidental de la Cuenca del Duero: nueva división estratigráfica y controles sobre su sedimentación

A Paleogene four-fold stratigraphical division is proposed here as result from the detailed studies carried out during the elaboration of 22 sheets of the Geological Map of Spain (E. 1:50.000). This units (T.S.U.) are limited by regional discordances and they have a Upper Cretaceous to Oligocene ages. The previous stratigraphical schemes are rearranged due to the different stratigraphicalrelations observed between the lithostratigraphical units proPosed by other workers (Jiménez, 1970; Corrochano, 1977; Alonso, 1981 ...). An Upper Cretaceous-Paleocene age is assumed to T.S.U. MC which is mainly composed by siliciclastic sediments strongly silicified forming a FU megasequence. It is interpretated as braided streams that flowed downslope filling paleovalleys eroded onto Paleozoic materials. Mineralogical features point to a tropical climate. Lower Eocene (T.S.U. P1) is identified in the Salamanca area, where it was considered as lacking. It is composed by arkosic sediments forming a CU megasequence. Fossil faunas of this T.S.U. record a subtropical climate. It is observed a transition from high sinuosity streams to braided ones. T.S.U. P2 (Middle Eocene-Lower Oligocene) is composed of two lithostratigraphical units previously considered as bounded by a discordance (Alonso, 198 1). It has a subarkosic to lithic nature and forms a CU megasequence. This unit records a subtropical climate with short arid periods and is interpretated as braided streams showing an increasing stability and enviromental energy to the top. T.S.U. P3 (Upper Oligocene) is composed by arkosic sediments previously considered of Vallesian (Middle to Upper Miocene) age. They form a CU megasequence that records braided streams prograding basin ward from higher areas. Palinological associations and pedological features indicate an arid mediterranean climate with long arid periods and a short rainy season with strong floods. We consider that most of Lower Miocene sediments are of Paleogene age. They are afected by a widespread alteration profile developed along Lower Miocene that masked its more significative features. Sedimentological analysis of T.S.U. shows that its megasequentiality is related to the rates of tectonical uplift of source areas whereas a distensive regime developed in the sedimentation basin

GEICAM Guidelines for the Management of Patients with Breast Cancer During the COVID-19 Pandemic in Spain

Breast cancer (BC) is the most common cancer in women in Spain. During the COVID-19 pandemic caused by the SARSCoV-2 virus, patients with BC still require timely treatment and follow-up; however, hospitals are overwhelmed with infected patients and, if exposed, patients with BC are at higher risk for infection and serious complications if infected. Thus, health care providers need to evaluate each BC treatment and in-hospital visit to minimize pandemic-associated risks while maintaining adequate treatment efficacy. Here we present a set of guidelines regarding available options for BC patient management and treatment by BC subtype in the context of the COVID-19 pandemic. Owing to the lack of evidence about COVID-19 infection, these recommendations are mainly based on expert opinion, medical organizations’ and societies’ recommendations, and some published evidence. We consider this a useful tool to facilitate medical decision making in this health crisis situation we are facing

The Palaeolithic occupation of Europe as revealed by evidence from the rivers: data from IGCP 449

IGCP 449 (2000-2004), seeking to correlate fluvial records globally, has compiled a dataset of archaeological records from Pleistocene fluvial sequences. Many terrace sequences can now be reliably dated and correlated with marine oxygen isotope stages (MIS), allowing potentially useful patterns in artefact distribution to be recognised. This review, based on evidence from northwest European and German sequences (Thames, Somme, Ilm, Neckar and Wipper), makes wider comparisons with rivers further east, particularly the Vltava, and with southern Europe, especially Iberia. The northwest and southern areas have early assemblages dominated by handaxes, in contrast with flake-core industries in Germany and further east. Fluvial sequences can provide frameworks for correlation, based on markers within the Palaeolithic record. In northwest Europe the first appearance of artefacts in terrace staircases, the earliest such marker, dates from the mid-late Cromerian Complex. Flake-core industries may have significantly preceded handaxe industries in southern Europe. An important technological innovation - Levallois technique - occurs at the Lower-Middle Palaeolithic boundary, correlated with MIS 9-8. Humans deserted northern Europe during MIS 6, apparently returning to central Germany and northern France (Somme valley) by MIS 5e but not reaching southern England until the appearance of Mousterian culture during MIS 4-3

Estudios paleoclimáticos y paleoambientales en cuevas kársticas

© DE LOS AUTORES © INSTITUTO DE GEOCIENCIAS, IGEO (CSIC-UCM)Ministerio de Educación y Ciencia (España)Ministerio de Educación y Ciencia (España)Plan Nacional (España)Ministerio de Ciencia e Innovación (España)Ministerio de Ciencia e Innovación (España)Ministerio de Educación y Ciencia (España)Ministerio de Medio Ambiente y Medio Rural y Marino (España)Ministerio de Ciencia e Innovación (España)Depto. de Geodinámica, Estratigrafía y PaleontologíaFac. de Ciencias GeológicasTRUEpu

Fluvial deposits as an archive of early human activity

River terraces are well established as an important source of Lower and Middle Palaeolithic artefacts in Europe, large collections having been assembled there during the years of manual gravel extraction. Now that many terrace sequences can be reliably dated and correlated with the oceanic record, potentially useful patterns can be recognized in the distribution of artefacts. The earliest appearance of artefacts in terrace staircases, marking the arrival of the first tool-making hominins in the region in question, is the first of several archaeological markers within fluvial sequences. The Lower to Middle Palaeolithic transition, with the appearance of Levallois, is another. Others may be more regional in significance: the occurrences of Clactonian (Mode 1) industry, twisted ovate handaxes and bout coupé handaxes, for example. IGCP Project no. 449 instigated the compilation of fluvial records from all over the ‘old world’. Comparison between British and Central European sequences confirms the established view that there is a demarcation between handaxe making in the west and flake/core industries in the east. Other centres of activity reported here have been in the Middle East (Syria), South Africa and India. Data from such areas will be key in deciphering the story of the earlier ‘out-of-Africa’ migration, that by pre-Homo sapiens people. There is clear evidence for diachroneity between the first appearances of different industries, in keeping with the well-established idea of northward migration

Hydrochemical characterization of an acid mine drainage-affected water reservoir : the Sancho Dam (Huelva, SW Spain)

The present study has the following objectives: to discover the relation between variables and the hydrochemical variations related to acid mine drainage in a water reservoir, and to describe horizontal stratification relating to vertical salinity and variations in metals. The information obtained may be used for establishing risk evaluation criteria and to design future remediation strategies, which could be useful for new dams. The hydrochemical characterization was based on a sampling campaign performed in October, 2011. A total of 28 samples, at one-meter-deep intervals, were obtained. The hydrogeochemical study of the polluted reservoir showed that the dilution effect is not sufficient to neutralize Acid Mine Drainage contributions from mining activity. Sampling carried out from the surface water to the deepest points reveals the reservoir stratification, which allows it to be included in the group of monomictic and holomitic lakes.This study is a contribution to the projects (CICYT-REN2002-1,897/HID, CICYT-TIN20046,689-C03-03 and DGCICYT-CGL2010-21,268-C02-01) financed by the Spanish Ministry of Education and Science; and the Andalusian Autonomous Government Excellence Projects (project P06-RNM-2,167)

Gypsum resources of Spain: Temporal and spatial distribution

Spain is one of the main gypsum producers in the world. Spanish gypsum reserves are large and a good knowledge of the location of the ore reserves permits to establish better exploitation strategies. Plotting the Spanish major gypsum outcrops, using a GIS base, helps to classify them by age, establish the main depositional character and determine the factors controlling their origin. Evaporitic deposits from Cambrian to Quaternary are preserved throughout Spain. The evaporites are formed by chemical precipitation of natural brines, either of marine or continental origin. The oldest evaporite vestiges in the Spanish geological record have been described in carbonate materials, as gypsum and anhydrite pseudomorphs, in Cambrian deposits of the Cantabro–Iberian basin (northern Spain). The first properly identified evaporite formation in Spain is located in the Triassic deposits that characterize central and northern Europe. In Spain, evaporites of this age appear well represented in 4394.5 km2 of outcrop area in the eastern part of the Iberian Peninsula. The Lower Jurassic (covering 1068 km2 of outcrop area) and the Cretaceous (covering 706.9 km2 of outcrop area) are periods of intense evaporitic sedimentation, and outcrops appear concentrated towards central and eastern parts of the Peninsula. More recently, in the Cenozoic, numerous continental and marine basins resulted from the tectonic activity produced by the Alpine Orogeny. Here, a combination of different factors produced thick and wide evaporite accumulations (outcrop surface is 13592.7 km2). In the Quaternary, evaporitic conditions are common in Spain, including various saline lakes (covering 1092.1 km2 of outcrop area) mainly in the Ebro basin and La Mancha zone. In addition, there are many artificial marine salinas. The evaporitic conditions in a basin strongly depend on factors such as climate, tectonics and brine composition. A study of the spatial distribution and age of the gypsum-bearing units in Spain suggests a wide variation in factors controlling the origin of gypsum deposits. The Spanish evaporite precipitation from Permian to Jurassic times was controlled by global conditions such as climate. They were formed during a global warming period. On the other hand, evaporites formed from late Cretaceous to Neogene were more influenced by regional factors that were related to the tectonic activity produced by the Alpine Orogeny. At present evaporite precipitation occurs due to the endorheic character of lakes in some parts of Spain

GEICAM Guidelines for the Management of Patients with Breast Cancer During the COVID-19 Pandemic in Spain

Breast cancer (BC) is the most common cancer in women in Spain. During the COVID-19 pandemic caused by the SARSCoV-2 virus, patients with BC still require timely treatment and follow-up; however, hospitals are overwhelmed with infected patients and, if exposed, patients with BC are at higher risk for infection and serious complications if infected. Thus, health care providers need to evaluate each BC treatment and in-hospital visit to minimize pandemic-associated risks while maintaining adequate treatment efficacy. Here we present a set of guidelines regarding available options for BC patient management and treatment by BC subtype in the context of the COVID-19 pandemic. Owing to the lack of evidence about COVID-19 infection, these recommendations are mainly based on expert opinion, medical organizations’ and societies’ recommendations, and some published evidence. We consider this a useful tool to facilitate medical decision making in this health crisis situation we are facing