Holocene summer temperature reconstruction based on a chironomid record from Sierra Nevada, southern Spain

This study was supported by projects CGL2013-47038-R, CGL2017-85415-R and PID2021-125619OB-C21/C22, funded by the Ministerio de Ciencia e Innovación of Spain, the Agencia Estatal de Investigación and the Fondo Europeo de Desarrollo Regional FEDER MCIN/AEI/10.13039/501100011033/FEDER, UE”; Junta de Andalucía I + D + i Junta de Andalucía 2020 Retos P-20-00059, UGR-FEDER B-RNM-144-UGR18, UGR-FEDER A-RNM-336-UGR20, Project cofinanced by FEDER and LifeWatch-Eric LifeWatch-2019-10-UGR-01 and the research group RNM-190 (Junta de Andalucía). RSA acknowledges several travel grants from Northern Arizona University to support this work. JC thanks the Ministerio de Ciencia e Innovación of Spain for the Juan de la Cierva Formación postdoctoral fellowship. ALA acknowledges the predoctoral fellowship BES-2018-084293 provided by the MCIN/AEI/10.13039/501100011033/. CLB acknowledges the European Union for her Marie Sklodowska-Curie grant agreement number 892487 under Horizon 2020 funds. LJ acknowledges the Ministry of Universities of Spain for her Margarita Salas grant (MS2021-204) financed by the European Union -Next Generation EU funds.Obtaining accurate temperature reconstructions from the past is crucial in understanding the consequences of changes in external climate forcings, such as orbital-scale insolation or multidecadal to centennial-scale variability on the climate system and the environment. In addition, these reconstructions help in comprehending the amplitude of natural temperature changes in the past, which can assist in evaluating the amplitude and rate of recent anthropogenic global warming. Here we present the first detailed Holocene mean July air temperature reconstruction based on chironomid assemblages from sediments retrieved from Laguna de Río Seco, an alpine lake in Sierra Nevada, southern Spain. Coldest climate conditions are recorded during the last glacial maximum and the last deglaciation. Warming occurred in the Early Holocene and warmest summer temperature conditions and the Holocene thermal maximum (HTM) occurred in the interval roughly between 9000 and 7200 cal yr BP, concurrent with summer insolation maxima. Rapid cooling of ∼1.5 °C occurred after the warmest maximum and between ∼7200 and 6500 cal yr BP, and temperatures stabilized between ∼6500 and 3000 cal yr BP. A further cooling began ∼3000 cal yr BP and culminated with coldest summer conditions during the Dark Ages (DA) and Little Ice Age (LIA) at ∼1550 cal yr BP (∼400 CE) and ∼200 cal yr BP (∼1750 CE), respectively. This cooling temperature trend was interrupted by warmer conditions during the Iberian-Roman Humid Period (IRHP) ∼2000 cal yr BP and during the Medieval Climate Anomaly (MCA) at ∼1000 cal yr BP. Our reconstruction shows a greater than two-degree cooling during the Middle and Late Holocene, agreeing with global mean surface temperature (GMST) reconstructions. Modern climate warming (MCW) during summer exceeds the two-degree Celsius forecasted for the future due to anthropogenic greenhouse gases, suggesting that recent warming is amplified at high elevations. Alpine environments and the biodiversity contained there are thus in danger if the observed temperature trend continues in the next decades.Ministerio de Ciencia e Innovación of Spain CGL2013-47038-R, CGL2017-85415-R, PID2021-125619OB-C21/C22Agencia Estatal de InvestigaciónFondo Europeo de Desarrollo Regional FEDER MCIN/AEI/10.13039/501100011033/FEDER, UEJunta de Andalucía P-20-00059, UGR-FEDER B-RNM-144-UGR18, UGR-FEDER A-RNM-336-UGR20FEDERLifeWatch-Eric LifeWatch-2019-10-UGR-01Research group RNM-190 (Junta de Andalucía)Northern Arizona UniversityMinisterio de Ciencia e Innovación of SpainMCIN/AEI/10.13039/501100011033/ BES-2018-084293Horizon 2020 European Union Marie Sklodowska-Curie 892487European Union -Next Generation EU funds MS2021-20

Summer temperatures during the Holocene inferred from a chironomid record from Sierra Nevada, southern Spain

XXI INQUA 2023. Rome. july 14-20 2023Accurate and continuous quantitative paleotemperature records from the past are rare in southern Iberia, mostly due to the scarcity of continuous sedimentary sequences in terrestrial environments from that area. In this study we show the first Holocene mean July air temperature reconstruction based on fossil chironomids from a sedimentary sequence obtained from Laguna de Río Seco, an alpine lake in Sierra Nevada, southern Spain. Reconstructed summer temperatures agree with changes in summer insolation and other palaeotemperature records from alpine environments from southern Europe and show the Holocene thermal maximum between 10 to 8.0 ka (1 ka = 1000 cal yr BP). Rapid cooling occurred after the warmest maximum and between ~8.0-7.0 ka and temperatures stabilized between ~6.5 and 3.0 ka. A further cooling trend started ~3.0 ka, and coldest summer conditions were reached at 1.4 ka (~550 CE) and ~0.2 ka (~1750 CE), coinciding with the Dark Ages and Little Ice Age, respectively. This record also shows relatively warmer summer temperature conditions during the Iberian-Roman Humid Period ~2.0 ka and during the Medieval Climate Anomaly at ~0.9 ka. Summer climate warming of more than two degree Celsius is observed in the last decades showing that recent warming is amplified in high alpine environments

Paleoenvironmental evolution of Laguna Seca lake (Sierra Nevada, southern Iberia) since the Late Glacial

Comunicación oral en XXI INQUA Congress. Rome (Italy). 14-20th july 2023Laguna Seca lake at 2259 masl has provided the longest alpine sedimentary record in southern Iberia, registering the last ~18 kyr in a ~14-meter-long sediment core. The oldest part of the sedimentary record represents a phase of subaerial debris flows and a small glacier/nivation hollow. The sediment characteristics abruptly changed at ~15.7 cal kyr BP, when a lake environment was established. A multi-proxy approach (magnetic susceptibility, organic geochemical analyses in bulk sediment, XRF core scanner data, and algae identification) has allowed the characterization of three different environmental phases in this lake. Deep lake conditions are identified from ~15.7 to ~10.6 cal kyr BP, agreeing with overall increasing precipitation in southern Iberia coinciding with augmenting summer insolation. This part of the record is characterized by grey lutites with high total organic carbon (TOC) content, high algae productivity, high vascular plant inputs (high C/N ratio) from the catchment and low Fe/S ratio, suggesting low oxygen conditions in the water-sediment interphase. Between ~10.6 and 8.2-8.0 cal kyr BP higher TOC and low Fe/S ratio are also recorded as well as higher algae content and low C/N ratio suggesting high aquatic production and more algae contribution to the local organic matter pool. This period registered the highest lake levels agreeing with summer insolation maximum and highest precipitation in southern Iberia. An abrupt lowering of the lake level is recorded after 8.0 cal kyr BP in the area. This is deduced by the decrease in TOC and algae in the sediments and more siliciclastic contribution from the catchment basin, evidenced by a high increase in siliciclastic elements (Si, Al, K, Ti, among others), with increased oxic conditions in the water-sediment interphase pointed out by the high increase in Fe/S ratio. Additionally, a potential increase in north African aeolian inputs (rich in Fe cations and Fe compounds) can be interpreted for the Middle and Late Holocene, evidenced by high Fe/Al values. This environmental change agrees with an aridification trend previously observed in the southern Iberian Peninsula

Reconstruction of Past Environment and Climate Using Wetland Sediment Records from the Sierra Nevada

Understanding the effects of climate change and human activities on fragile mountain ecosystems is necessary to successfully managing these environments under future climate scenarios (e.g., global warming, enhanced aridity). This can be done through the study of paleoecological records, which can provide long paleoenvironmental databases containing information on how ecosystems reacted to climate change and human disturbances before the historical record. These studies can be particularly interesting when focusing on especially warm and/or dry past climatic phases. Biotic (pollen, charcoal) and abiotic (physical, geochemistry) analyses from wetland sediment records from the Sierra Nevada, southern Spain record changes in vegetation, fire history and lake sedimentation since ~11,700 years (cal yr BP). This multiproxy paleoecological study indicates that maxima in temperature and humidity occurred in the area in the Early and Middle Holocene, with a peak in precipitation between ~10,500 and 7000 cal yr BP. This is deduced by maxima in water runoff, the highest abundance of tree species and algae and high total organic carbon values recorded in the alpine wetland’s sedimentary records of the Sierra Nevada during that time period. In the last 7000 cal yr BP, and especially after a transition period between ~7000 and 5000 cal yr BP, a progressive aridification process took place, indicated by the decrease in tree species and the increase in xerophytic herbs in this region and a reduction in water runoff evidenced by the decrease in detritic input in the wetland sedimentary records. An increasing trend in Saharan dust deposition in the Sierra Nevada wetlands is also recorded through inorganic geochemical proxies, probably due to a coetaneous loss of vegetation cover in North Africa. The process of progressive aridification during the Middle and Late Holocene was interrupted by millennial-scale climatic oscillations and several periods of relative humid/droughty conditions and warm/cold periods have been identified in different temperature and/or precipitation proxies. Enhanced human impact has been observed in the Sierra Nevada in the last ~3000 cal yr BP through the increase in fires, grazing, cultivation, atmospheric pollution as well as reforestation by Pinus and the massive cultivation of Olea at lower altitudes.This study was supported by projects CGL2013-47038-R and CGL2017-85415-R funded by Ministerio de Economía y Competitividad of Spain and Fondo Europeo de Desarrollo Regional FEDER; Séneca Project 20788/PI/18; Junta de Andalucía I+D+i Junta de Andalucía 2020 Retos P-20-00059, FEDER Project B-RNM-144-UGR18, UGR-FEDER B-RNM-144-UGR18 Proyectos I + D + i del Programa Operativo FEDER 2018 and the research group RNM-190 (Junta de Andalucía). M.J.R.R. acknowledges the postdoctoral funding provided by the European Commission/H2020 (ERC-2017-ADG, project number 788616). J.C. acknowledges the postdoctoral funding provided by the Academy of Finland (project number 316702). A.G.-A. acknowledges the Ramón y Cajal fellowship RYC-2015-18966 provided by the Ministerio de Economía y Competitividad of the Spanish Government. M.R.G. acknowledges funding by the Juan de la Cierva-Incorporación program in the University of Granada (IJCI-2017-33755) from Secretaría de Estado de I+D+i, Spain. RSA acknowledges several travel grants from Northern Arizona University to support this work

Nueve jueces entran en diálogo con nueve hipótesis acerca de la prueba de los hechos en el contexto penal

This article formulates nine hypotheses concerning the proof of facts in criminal proceedings, which are analysed by nine judges of Chilean criminal Courts (Tribunal de Juicio Oral y de Garantía). Seven hypotheses aimed at describing different practices that take place in the courts and two of them concern how judges should act in certain hard cases. The matters are grouped in the following categories: a) scopes of the compromise that judges should have in order to operate with true stories as support of their decisions; b) difficulties that arise as consequence of the epistemic weakness of the evidence available in trials and the possible slants in their interpretation; c) requirements of the evaluation of the proof according to the sana crítica; and d) meaning that should have the standard of proof beyond reasonable doubt. In this way, a dialogue between the system of beliefs of judges and of jurists takes place

Repositioning of the global epicentre of non-optimal cholesterol

High blood cholesterol is typically considered a feature of wealthy western countries(1,2). However, dietary and behavioural determinants of blood cholesterol are changing rapidly throughout the world(3) and countries are using lipid-lowering medications at varying rates. These changes can have distinct effects on the levels of high-density lipoprotein (HDL) cholesterol and non-HDL cholesterol, which have different effects on human health(4,5). However, the trends of HDL and non-HDL cholesterol levels over time have not been previously reported in a global analysis. Here we pooled 1,127 population-based studies that measured blood lipids in 102.6 million individuals aged 18 years and older to estimate trends from 1980 to 2018 in mean total, non-HDL and HDL cholesterol levels for 200 countries. Globally, there was little change in total or non-HDL cholesterol from 1980 to 2018. This was a net effect of increases in low- and middle-income countries, especially in east and southeast Asia, and decreases in high-income western countries, especially those in northwestern Europe, and in central and eastern Europe. As a result, countries with the highest level of non-HDL cholesterol-which is a marker of cardiovascular riskchanged from those in western Europe such as Belgium, Finland, Greenland, Iceland, Norway, Sweden, Switzerland and Malta in 1980 to those in Asia and the Pacific, such as Tokelau, Malaysia, The Philippines and Thailand. In 2017, high non-HDL cholesterol was responsible for an estimated 3.9 million (95% credible interval 3.7 million-4.2 million) worldwide deaths, half of which occurred in east, southeast and south Asia. The global repositioning of lipid-related risk, with non-optimal cholesterol shifting from a distinct feature of high-income countries in northwestern Europe, north America and Australasia to one that affects countries in east and southeast Asia and Oceania should motivate the use of population-based policies and personal interventions to improve nutrition and enhance access to treatment throughout the world.Peer reviewe

4to. Congreso Internacional de Ciencia, Tecnología e Innovación para la Sociedad. Memoria académica

Este volumen acoge la memoria académica de la Cuarta edición del Congreso Internacional de Ciencia, Tecnología e Innovación para la Sociedad, CITIS 2017, desarrollado entre el 29 de noviembre y el 1 de diciembre de 2017 y organizado por la Universidad Politécnica Salesiana (UPS) en su sede de Guayaquil. El Congreso ofreció un espacio para la presentación, difusión e intercambio de importantes investigaciones nacionales e internacionales ante la comunidad universitaria que se dio cita en el encuentro. El uso de herramientas tecnológicas para la gestión de los trabajos de investigación como la plataforma Open Conference Systems y la web de presentación del Congreso http://citis.blog.ups.edu.ec/, hicieron de CITIS 2017 un verdadero referente entre los congresos que se desarrollaron en el país. La preocupación de nuestra Universidad, de presentar espacios que ayuden a generar nuevos y mejores cambios en la dimensión humana y social de nuestro entorno, hace que se persiga en cada edición del evento la presentación de trabajos con calidad creciente en cuanto a su producción científica. Quienes estuvimos al frente de la organización, dejamos plasmado en estas memorias académicas el intenso y prolífico trabajo de los días de realización del Congreso Internacional de Ciencia, Tecnología e Innovación para la Sociedad al alcance de todos y todas

Heterogeneous contributions of change in population distribution of body mass index to change in obesity and underweight NCD Risk Factor Collaboration (NCD-RisC)

From 1985 to 2016, the prevalence of underweight decreased, and that of obesity and severe obesity increased, in most regions, with significant variation in the magnitude of these changes across regions. We investigated how much change in mean body mass index (BMI) explains changes in the prevalence of underweight, obesity, and severe obesity in different regions using data from 2896 population-based studies with 187 million participants. Changes in the prevalence of underweight and total obesity, and to a lesser extent severe obesity, are largely driven by shifts in the distribution of BMI, with smaller contributions from changes in the shape of the distribution. In East and Southeast Asia and sub-Saharan Africa, the underweight tail of the BMI distribution was left behind as the distribution shifted. There is a need for policies that address all forms of malnutrition by making healthy foods accessible and affordable, while restricting unhealthy foods through fiscal and regulatory restrictions

Velocidad de secado de alfalfa bajo diferentes condiciones de secado artificial

El objetivo del presente estudio fue determinar la tasa de secado de alfalfa (Medicago sativa L.), simulando en laboratorio diferentes condiciones de temperatura, ventilación y densidad de hilerado. La pradera de alfalfa fue segada manualmente y las muestras obtenidas se dispusieron en horno con y sin ventilación forzada a tres densidades: 4,78; 3,62; y 2,17 kg m-2, y a tres temperaturas: 20, 30 y 40ºC. Se evaluaron 18 tratamientos con cuatro repeticiones, a las que se determinó MS cada 3 h durante el día y se evaluó por un total de 53 h. Se utilizaron seis hornos. El aumento de la densidad del forraje produjo una disminución en la tasa de secado (TS) (P < 0,0001), además la TS se incrementó con el aumento de la temperatura y la ventilación. La TS fue de 1,83; 2,20; y 3,25% MS h-1 para las densidades de 4,78; 3,62 y 2,17 kg m-2, respectivamente, cuando la temperatura fue de 30ºC. La TS fue de 1,49; 2,20 y 3,11% MS h-1 para las temperaturas de 20, 30 y 40ºC respectivamente, cuando la densidad fue de 3,62 kg m-2. La ventilación aumentó la TS entre 2 y 2,5 veces, dependiendo de la temperatura. A medida que aumentó la MS del forraje la TS disminuyó. Los datos obtenidos en laboratorio son una herramienta útil para elaborar modelos de simulación, ya que permiten estudiar diferentes factores climáticos sin interacciones entre ellos

INVESTIGACIÓN - VELOCIDAD DE SECADO DE ALFALFA BAJO DIFERENTES CONDICIONES DE SECADO ARTIFICIAL (Drying rate of alfalfa under different conditions of artificial drying)

The objective of the present study was to determine the drying rate (TS) of alfalfa (Medicago sativa L.), simulating under laboratory conditions different temperatures, ventilation rates and swath densities. The alfalfa pasture was harvested manually and the samples obtained were placed in ovens with and without forced ventilation, at three densities: 4.78, 3.62, and 2.17 kg m-2, and three temperatures: 20, 30 and 40ºC. Eighteen treatments were evaluated with four replicates; DM was determined every 3 h during the day and treatments were evaluated for 53 h. Six ovens were utilized. Increasing forage density produced a reduction in TS (P < 0.0001), as well TS increased with the increase in temperature and ventilation. TS was 1.83, 2.20 and 3.25% DM h-1 for forage densities of 4.78, 3.62 and 2.17 kg m-2, respectively, when the temperature was 30ºC. TS was 1.49, 2.20 and 3,11% DM h-1 for temperatures of 20, 30 and 40ºC, respectively, when the forage density was 3.62 kg m-2. Ventilation increased TS between 2 and 2.5 times depending on oven temperature. As forage DM increased, TS decreased. The data obtained under laboratory conditions are useful to elaborate simulation models since they permit to study different climatic factors without interactions between them. RESUMEN El objetivo del presente estudio fue determinar la tasa de secado de alfalfa (Medicago sativa L.), simulando en laboratorio diferentes condiciones de temperatura, ventilación y densidad de hilerado. La pradera de alfalfa fue segada manualmente y las muestras obtenidas se dispusieron en horno con y sin ventilación forzada a tres densidades: 4,78; 3,62; y 2,17 kg m-2, y a tres temperaturas: 20, 30 y 40ºC. Se evaluaron 18 tratamientos con cuatro repeticiones, a las que se determinó MS cada 3 h durante el día y se evaluó por un total de 53 h. Se utilizaron seis hornos. El aumento de la densidad del forraje produjo una disminución en la tasa de secado (TS) (P < 0,0001), además la TS se incrementó con el aumento de la temperatura y la ventilación. La TS fue de 1,83; 2,20; y 3,25% MS h-1 para las densidades de 4,78; 3,62 y 2,17 kg m-2, respectivamente, cuando la temperatura fue de 30ºC. La TS fue de 1,49; 2,20 y 3,11% MS h-1 para las temperaturas de 20, 30 y 40ºC respectivamente, cuando la densidad fue de 3,62 kg m-2. La ventilación aumentó la TS entre 2 y 2,5 veces, dependiendo de la temperatura. A medida que aumentó la MS del forraje la TS disminuyó. Los datos obtenidos en laboratorio son una herramienta útil para elaborar modelos de simulación, ya que permiten estudiar diferentes factores climáticos sin interacciones entre ellos