906 resultados para renal biological activity


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Accumulation rates of Mg, Al, Si, Mn, Fe, Ni, Cu, Zn, opal, and calcium carbonate have been calculated from their concentrations in samples from equatorial Deep Sea Drilling Project sites. Maps of element accumulation rates and of Q-mode factors derived from raw data indicate that the flux of trace metals to equatorial Pacific sediments has varied markedly through time and space in response to changes in the relative and absolute influence of several depositional influences: biogenic, detrital, authigenic, and hydrothermal sedimentation. Biologically derived material dominates the sediment of the equatorial Pacific. The distributions of Cu and Zn are most influenced by surface-water biological activity, but Ni, Al, Fe, and Mn are also incorporated into biological material. All of these elements have equatorial accumulation maxima similar to those of opal and calcium carbonate at times during the past 50 m.y. Detritus distributed by trade winds and equatorial surface circulation contributes Al, non-biogenic Si, Fe, and Mg to the region. Detrital sediment is most important in areas with a small supply of biogenic debris and low bulk-accumulation rates. Al accumulation generally increases toward the north and east, indicating its continental source and distribution by the northeast trade winds. Maxima in biological productivity during middle Eocene and latest Miocene to early Pliocene time and concomitant well-developed surface circulation contributed toward temporal maxima in the accumulation rates of Cu, Zn, Ni, and Al in sediments of those ages. Authigenic material is also important only where bulk-sediment accumulation rates are low. Ni, Cu, Zn, and sometimes Mn are associated with this sediment. Fe is almost entirely of hydrothermal origin. Mn is primarily hydrothermal, but some is probably scavenged from sea water by amorphous iron hydroxide floes along with other elements concentrated in hydrothermal sediments, Ni, Cu, and Zn. During the past 50 m.y. all of these elements accumulated over the East Pacific Rise at rates nearly an order of magnitude higher than those at non-rise-crest sites. In addition, factor analysis indicates that some of this material is carried substantial distances to the west of the rise crest. Accumulation rates of Fe in basal metalliferous sediments indicate that the hydrothermal activity that supplied amorphous Fe oxides to the East Pacific Rise areas was most intense during middle Eocene and late Miocene to early Pliocene time.

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The carbonate fraction of sediment core ODP 849, leg 138, located in the eastern equatorial Pacific, mostly consisting of coccoliths, was separated and analyzed for its Zn isotopic composition. The overall variation in Zn isotopic composition, as determined by multiple-collector, magnetic-sector, inductively coupled plasma mass spectrometry, was found to be on the order of 1? (expressed in delta66Zn, where deltaxZn=[(xZn/64Zn)sample/(xZn/64Zn)standard -1]*10**3 and x=66, 67 or 68) over the last 175 ka. The analytical precision was 0.04 per mil and the overall reproducibility was usually better than 0.07 per mil. The Zn isotopic composition signal exhibits several marked peaks and a high-frequency variability. A periodogram of the delta66Zn signal showed two periodicities of 35.2 and 21.2 ka. We suggest that the latter is caused by the precession of the Earth's axis of rotation. The periodogram exhibits a minimum at 41.1 ka, thus showing that the Zn isotopic composition is independent of the obliquity in the eastern equatorial Pacific. The range of delta66Zn values observed for the carbonate fraction of ODP 849 overlaps with the range observed for Fe-Mn nodules in the world's oceans, which suggests that seawater/carbonate Zn isotope fractionation is weak. We therefore assume that most of the Zn isotope variability is a result of the selective entrainment of the light isotopes by organic matter in the surface ocean. The ODP 849 delta66Zn record seems to follow the changes in the insolation cycles. Changes in the late summer/fall equatorial insolation modulate the intensity of the equatorial upwelling, hence the mixing between deep and surface waters. We propose that during decreased summer/fall equatorial insolation, when a steep thermocline can develop (El Niño-like conditions), the surface waters cannot be replenished by deep waters and become depleted in the lighter Zn isotopes by biological activity, thus resulting in the progressive increase of the delta66Zn values of the carbonate shells presumably in equilibrium with surface seawater.

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The present dataset contain source data for Figure 5a from Schilling et al., 2009. Cell fate decisions are regulated by the coordinated activation of signalling pathways such as the extracellular signal-regulated kinase (ERK) cascade, but contributions of individual kinase isoforms are mostly unknown. The authors combined quantitative data from erythropoietin-induced pathway activation in primary erythroid progenitor (colony-forming unit erythroid stage, CFU-E) cells with mathematical modelling, in order to predict and experimentally confirmed a distributive ERK phosphorylation mechanism in CFU-E cells. The authors found evidences that double-phosphorylated ERK1 attenuates proliferation beyond a certain activation level, whereas activated ERK2 enhances proliferation with saturation kinetics. Phosphorylation levels of JAK2 at 7 min after stimulation for Epo concentrations ranging from 0.1 to 1000 U/ml were simulated.

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The present dataset contain source data for Figure 5b from Schilling et al., 2009. Cell fate decisions are regulated by the coordinated activation of signalling pathways such as the extracellular signal-regulated kinase (ERK) cascade, but contributions of individual kinase isoforms are mostly unknown. The authors combined quantitative data from erythropoietin-induced pathway activation in primary erythroid progenitor (colony-forming unit erythroid stage, CFU-E) cells with mathematical modelling, in order to predict and experimentally confirmed a distributive ERK phosphorylation mechanism in CFU-E cells. The authors found evidences that double-phosphorylated ERK1 attenuates proliferation beyond a certain activation level, whereas activated ERK2 enhances proliferation with saturation kinetics. They show integrated responses of double-phosphorylated ERK1 and ERK2 that were calculated for different Epo concentrations for the original model as well as for models with elevated ERK1 or ERK2 levels.

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The present dataset data contain source data for Figure 5a from Schilling et al., 2009. Cell fate decisions are regulated by the coordinated activation of signalling pathways such as the extracellular signal-regulated kinase (ERK) cascade, but contributions of individual kinase isoforms are mostly unknown. The authors combined quantitative data from erythropoietin-induced pathway activation in primary erythroid progenitor (colony-forming unit erythroid stage, CFU-E) cells with mathematical modelling, in order to predict and experimentally confirmed a distributive ERK phosphorylation mechanism in CFU-E cells. The authors found evidences that double-phosphorylated ERK1 attenuates proliferation beyond a certain activation level, whereas activated ERK2 enhances proliferation with saturation kinetics. CFU-E cells were stimulated with the indicated Epo concentrations for 7 min and phosphorylation levels were determined by quantitative immunoblotting.

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Antarctic ice-free areas contain lakes and ponds that have interesting limnological features and are of wide global significance as early warning indicators of climatic and environmental change. However, most limnological and paleolimnological studies in continental Antarctica are limited to certain regions. There are several ice-free areas in Victoria Land that have not yet been studied well. There is therefore a need to extend limnological studies in space and time to understand how different geological and climatic features affect the composition and biological activity of freshwater communities. With the aim of contributing to a better limnological characterization of Victoria Land, this paper reports data on sedimentary pigments (used to identify the main algal taxa) obtained through a methodology that is more sensitive and selective than that of previous studies. Analyses were extended to 48 water bodies in ice-free areas with differing lithology, latitude, and altitude, and with different morphometry and physical, chemical, and biological characteristics in order to identify environmental factors affecting the distribution and composition of freshwater autotrophic communities. A wider knowledge of lakes in a limnologically important region of Antarctica was obtained. Cyanophyta was found to be the most important algal group, followed by Chlorophyta and Bacillariophyta, whereas latitude and altitude are the main factors affecting pigment distribution.

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Data contain source data for Figure 5c from Schilling et al., 2009. Cell fate decisions are regulated by the coordinated activation of signalling pathways such as the extracellular signal-regulated kinase (ERK) cascade, but contributions of individual kinase isoforms are mostly unknown. The authors combined quantitative data from erythropoietin-induced pathway activation in primary erythroid progenitor (colony-forming unit erythroid stage, CFU-E) cells with mathematical modelling, in order to predict and experimentally confirmed a distributive ERK phosphorylation mechanism in CFU-E cells. The authors found evidences that double-phosphorylated ERK1 attenuates proliferation beyond a certain activation level, whereas activated ERK2 enhances proliferation with saturation kinetics. Retrovirally transduced CFU-E cells were incubated with increasing Epo concentrations for 14 h and proliferation was measured by [3H]-thymidine incorporation.

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An analytical method for the determination of the alpha dicarbonyls glyoxal (GLY) and methylglyoxal (MGLY) from seawater and marine aerosol particles is presented. The method is based on derivatization with o-(2,3,4,5,6-Pentafluorobenzyl)-hydroxylamine (PFBHA) reagent, solvent extraction and GC-MS (SIM) analysis. The method showed good precision (RSD < 10%), sensitivity (detection limits in the low ng/l range), and accuracy (good agreement between external calibration and standard addition). The method was applied to determine GLY and MGLY in oceanic water sampled during the Polarstern cruise ANT XXVII/4 from Capetown to Bremerhaven in spring 2011. GLY and MGLY were determined in the sea surface microlayer (SML) of the ocean and corresponding bulk water (BW) with average concentrations of 228 ng/l (GLY) and 196 ng/l (MGLY). The results show a significant enrichment (factor of 4) of GLY and MGLY in the SML. Furthermore, marine aerosol particles (PM1) were sampled during the cruise and analyzed for GLY (average concentration 0.19 ng/m**3) and MGLY (average concentration 0.15 ng/m**3). On aerosol particles, both carbonyls show a very good correlation with oxalate, supporting the idea of a secondary formation of oxalic acid via GLY and MGLY. Concentrations of GLY and MGLY in seawater and on aerosol particles were correlated to environmental parameters such as global radiation, temperature, distance to the coastline and biological activity. There are slight hints for a photochemical production of GLY and MGLY in the SML (significant enrichment in the SML, higher enrichment at higher temperature). However, a clear connection of GLY and MGLY to global radiation as well as to biological activity cannot be concluded from the data. A slight correlation between GLY and MGLY in the SML and in aerosol particles could be a hint for interactions, in particular of GLY, between seawater and the atmosphere.

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Seasonality of biomarker baseline levels were studied in polar cod (Boreogadus saida), caught in Kongsfjorden, Svalbard, in April, July, September and December, 2006-2007. Physiological parameters (condition factor, gonado- and hepato-somatic indexes, energy reserves, potential metabolic activity and antifreeze activity) in polar cod were used to interpret the seasonality of potential biomarkers. The highest levels of ethoxyresorufin-O-deethylase (EROD) activity occurred concomitantly with the highest potential metabolic activity in July due to e.g. intense feeding. During pre-spawning, EROD showed significant inhibition and gender differences. Hence, its potential use in environmental monitoring should imply gender differentiation at least during this period. Glutathione S-transferase and catalase activities were stable from April to September, but changed in December suggesting a link to low biological activity. Knowledge of the biomarker baseline levels and their seasonal trends in polar cod is essential for a trustworthy interpretation of forthcoming toxicity data and environmental monitoring in the Arctic.

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Dissolved barium has been shown to have the potential to distinguish Eurasian from North American (NA) river runoff. As part of the ARK-XXII/2 Polarstern expedition in summer 2007, Ba was analyzed in the Barents, Kara, Laptev seas, and the Eurasian Basins as well as the Makarov Basin up to the Alpha and Mendeleyev Ridges. By combining salinity, d18O and initial phosphate corrected for mineralization with oxygen (PO4*) or N/P ratios we identified the water mass fractions of meteoric water, sea ice meltwater, and marine waters of Atlantic as well as Pacific origin in the upper water column. In all basins inside the lower halocline layer and the Arctic intermediate waters we find Ba concentrations close to those of the Fram Strait branch of the lower halocline (41-45 nM), reflecting the composition of the incoming Atlantic water. A layer of upper halocline water (UHW) with higher Ba concentrations (45-55 nM) is identified in the Makarov Basin. Atop of the UHW, the Surface Mixed Layer (SML), including the summer and winter mixed layers, has high concentrations of Ba (58-67 nM). In the SML of the investigated area of the central Arctic the meteoric fraction can be identified by assuming a conservative behavior of Ba to be primarily of Eurasian river origin. However, in productive coastal regions biological removal compromises the use of Ba to distinguish between Eurasian and NA rivers. As a consequence, the NA river water fraction is underestimated in productive surface waters or waters that have passed a productive region, whereas this fraction is overestimated in subsurface waters containing remineralised Ba, particularly when these waters have passed productive shelf regions. Especially in the Laptev Sea and small regions in the Barents Sea, Ba concentrations are low in surface waters. In the Laptev Sea exceptionally high Ba concentrations in shelf bottom waters indicate that Ba is removed from surface waters to deep waters by biological activity enhanced by increasing ice-free conditions as well as by scavenging by organic matter of terrestrial origin. We interpret high Ba concentrations in the UHW of the Makarov Basin to result from enrichment by remineralisation in bottom waters on the shelf of the Chukchi Sea and therefore the calculated NA runoff is an artefact. We conclude that no NA runoff can be demonstrated unequivocally anywhere during our expedition with the set of tracers considered here. Small contributions of NA runoff may have been masked by Ba depletion and could only be resolved by supportive tracers on the uptake history. We thus suggest that Ba has to be used with care as it can put limits but not yield quantitative water mass distributions. Only if the extra Ba inputs exceed the cumulative biological uptake the signal can be unequivocally attributed to NA runoff.

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The coastal upwelling system off the coast of Peru is characterized by high biological activity and a pronounced subsurface oxygen minimum zone, as well as associated emissions of atmospheric trace gases such as N2O, CH4 and CO2. From 3 to 23 December 2012, R/V Meteor (M91) cruise took place in the Peruvian upwelling system between 4.59 and 15.4°S, and 82.0 to 77.5°W. During M91 we investigated the composition of the sea-surface microlayer (SML), the oceanic uppermost boundary directly subject to high solar radiation, often enriched in specific organic compounds of biological origin like chromophoric dissolved organic matter (CDOM) and marine gels. In the SML, the continuous photochemical and microbial recycling of organic matter may strongly influence gas exchange between marine systems and the atmosphere. We analyzed SML and underlying water (ULW) samples at 38 stations focusing on CDOM spectral characteristics as indicator of photochemical and microbial alteration processes. CDOM composition was characterized by spectral slope (S) values and excitation-emission matrix fluorescence (EEMs), which allow us to track changes in molecular weight (MW) of DOM, and to determine potential DOM sources and sinks. Spectral slope S varied between 0.012 to 0.043 1 nm-1 and was quite similar between SML and ULW, with no significant differences between the two compartments. Higher S values were observed in the ULW of the southern stations below 15°S. By EEMs, we identified five fluorescent components (F1-5) of the CDOM pool, of which two had excitation/emission characteristics of amino-acid-like fluorophores (F1, F4) and were highly enriched in the SML, with a median ratio SML : ULW of 1.5 for both fluorophores. In the study region, values for CDOM absorption ranged from 0.07 to 1.47 m-1. CDOM was generally highly concentrated in the SML, with a median enrichment with respect to the ULW of 1.2. CDOM composition and changes in spectral slope properties suggested a local microbial release of DOM directly in the SML as a response to light exposure in this extreme environment. In a conceptual model of the sources and modifications of optically active DOM in the SML and underlying seawater (ULW), we describe processes we think may take place (Fig. 1); the production of CDOM of higher MW by microbial release through growth, exudation and lysis in the euphotic zone, includes the identified fluorophores (F1, F2, F3, F4, F5). Specific amino-acid-like fluorophores (F1, F4) accumulate in the SML with respect to the ULW, as photochemistry may enhance microbial CDOM release by (a) photoprotection mechanisms and (b) cell-lysis processes. Microbial and photochemical degradation are potential sinks of the amino-acid-like fluorophores (F1, F4), and potential sources of reworked and more refractory humic-like components (F2, F3, F5). In the highly productive upwelling region along the Peruvian coast, the interplay of microbial and photochemical processes controls the enrichment of amino-acid-like CDOM in the SML. We discuss potential implications for air-sea gas exchange in this area.

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Biological activity introduces variability in element incorporation during calcification and thereby decreases the precision and accuracy when using foraminifera as geochemical proxies in paleoceanography. This so-called 'vital effect' consists of organismal and environmental components. Whereas organismal effects include uptake of ions from seawater and subsequent processing upon calcification, environmental effects include migration- and seasonality-induced differences. Triggering asexual reproduction and culturing juveniles of the benthic foraminifer Ammonia tepida under constant, controlled conditions allow environmental and genetic variability to be removed and the effect of cell-physiological controls on element incorporation to be quantified. Three groups of clones were cultured under constant conditions while determining their growth rates, size-normalized weights and single-chamber Mg/Ca and Sr/Ca using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS). Results show no detectable ontogenetic control on the incorporation of these elements in the species studied here. Despite constant culturing conditions, Mg/Ca varies by a factor of similar to 4 within an individual foraminifer while intra-individual Sr/Ca varies by only a factor of 1.6. Differences between clone groups were similar to the intra-clone group variability in element composition, suggesting that any genetic differences between the clone-groups studied here do not affect trace element partitioning. Instead, variability in Mg/Ca appears to be inherent to the process of bio-calcification itself. The variability in Mg/Ca between chambers shows that measurements of at least 6 different chambers are required to determine the mean Mg/Ca value for a cultured foraminiferal test with a precision of <= 10%

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A clear statement in these lines textually cited (Byers et al., 1938) defines the framework of this special issue: “True soil is the product of the action of climate and living organism upon the parent material, as conditioned by the local relief. The length of time during which these forces are operative is of great importance in determining the character of the ultimate product. Drainage conditions are also important and are controlled by local relief, by the nature of the parent material or underlying rock strata, or by the amount of precipitation in relation to rate of percolation and runoff water. There are, therefore, five principal factors of soil formation: Parent material, climate, biological activity, relief and time. These soil forming factors are interdependent, each modifying the effectiveness of the others.” Due to these various processes associated to its formation and genesis soil dynamics reveals high complexity that creates several levels of structure using this term in a broad sense

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From the end of 2013 and during the following two years, 20 kt of CO2sc are planned to be injected in a saline reservoir (1500 m depth) at the Hontomín site (NE Spain). The target aquifers are Lower Jurassic limestone formations which are sealed by Lower Cretaceous clay units at the Hontomín site (NE Spain). The injection of CO2 is part of the activities committed in the Technology Development phase of the EC-funded OXYCFB300 project (European Energy Program for Recovery – EEPR, http://www.compostillaproject.eu), which include CO2 injection strategies, risk assessment, and testing and validating monitoring methodologies and techniques. Among the monitoring works, the project is intended to prove that present-day technology is able to monitor the evolution of injected CO2 in the reservoir and to detect potential leakage. One of the techniques is the measurement of CO2 flux at the soil–atmosphere interface, which includes campaigns before, during and after the injection operations. In this work soil CO2 flux measurements in the vicinity of oil borehole, drilled in the eighties and named H-1 to H-4, and injection and monitoring wells were performed using an accumulation chamber equipped with an IR sensor. Seven surveys were carried out from November 2009 to summer 2011. More than 4000 measurements were used to determine the baseline flux of CO2 and its seasonal variations. The measured values were low (from 5 to 13 g m−2 day−1) and few outliers were identified, mainly located close to the H-2 oil well. Nevertheless, these values cannot be associated to a deep source of CO2, being more likely related to biological processes, i.e. soil respiration. No anomalies were recognized close to the deep fault system (Ubierna Fault) detected by geophysical investigations. There, the CO2 flux is indeed as low as other measurement stations. CO2 fluxes appear to be controlled by the biological activity since the lowest values were recorded during autumn-winter seasons and they tend to increase in warm periods. Two reference CO2 flux values (UCL50 of 5 g m−2 d−1 for non-ploughed areas in autumn–winter seasons and 3.5 and 12 g m−2 d−1 for in ploughed and non-ploughed areas, respectively, in spring–summer time, and UCL99 of 26 g m−2 d−1 for autumn–winter in not-ploughed areas and 34 and 42 g m−2 d−1 for spring–summer in ploughed and not-ploughed areas, respectively) were calculated. Fluxes higher than these reference values could be indicative of possible leakage during the operational and post-closure stages of the storage project.

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La nueva legislación en materia fitosanitaria se dirige hacia una Gestión Integrada de Plagas (GIP). Estos programas dan preferencia a aquellos métodos más respetuosos y sostenibles con el medio ambiente, siendo piezas claves en ellos el control biológico, el físico y otros de carácter no químico. Sin embargo, el uso de insecticidas selectivos es a veces necesario para el adecuado manejo de plagas en cultivos hortícolas. Por ello, el objetivo general de este estudio es aportar conocimientos para mejorar el control de plagas en cultivos hortícolas, mediante la integración de tres estrategias de lucha: biológica, física y química. Una parte de este trabajo ha consistido en el estudio de los posibles efectos que mallas tratadas con insecticida (bifentrin) pudieran provocar mediante diferentes ensayos de laboratorio, invernadero y campo, en los enemigos naturales Orius laevigatus (Fieber) (Hemiptera: Anthocoridae) (depredador de trips), Nesidiocoris tenuis (Reuter) (Hemiptera: Miridae) (depredador de mosca blanca y Tuta absoluta (Meirick) (Lepidoptera: Gelechiidae)), y otros agentes de biocontrol comúnmente usados en cultivos hortícolas protegidos. Este tipo de mallas se han empleado con éxito en entomología médica para controlar mosquitos vectores de la malaria, y actualmente se está trabajando en su desarrollo para uso agrícola como método de exclusión, y método directo de control de plagas. En los ensayos realizados en laboratorio, O. laevigatus y N. tenuis no fueron capaces de detectar la presencia de bifentrin en el ensayo de preferencia. Además, no se produjo mortalidad a corto plazo (72 horas) en ambos chinches depredadores. Por el contrario, se registró una elevada mortalidad cuando se expusieron por contacto a la malla tratada durante 72 horas en cajas de dimensiones reducidas (10 cm de diámetro X 3 cm de altura). En ensayos llevados a cabo bajo condiciones más reales de exposición, en un invernadero experimental con jaulas de 25 X 25 X 60 cm de altura, no se produjo ningún efecto en la mortalidad a corto plazo (72 horas) o en los parámetros reproductivos de O. laevigatus y N. tenuis. Finalmente, en ensayos de campo realizados en túneles semi-comerciales (8 m de largo X 6,5 m de ancho X 2,6 m de altura), ni las condiciones ambientales [temperatura, humedad relativa, radiación ultravioleta (UV) y fotosintéticamente activa (PAR)], ni los enemigos naturales, se vieron afectados por la presencia de la malla tratada con bifentrin en el cultivo. Sin embargo, los resultados no fueron concluyentes, debido al bajo establecimiento de los agentes de biocontrol liberados. Por lo tanto, más estudios son necesarios en invernaderos comerciales para confirmar los resultados preliminares de compatibilidad. Además, en este trabajo se han evaluado los efectos letales (mortalidad) y subletales (parámetros reproductivos) de seis modernos insecticidas sobre los chinches depredadores O. laevigatus y N. tenuis, mediante ensayos de laboratorio y persistencia. Los ensayos se realizaron por contacto residual, aplicando los insecticidas a la dosis máxima de campo sobre placas de cristal (laboratorio) o plantas (persistencia). Los productos fitosanitarios se seleccionaron por representar a un grupo de modernos plaguicidas con modos de acción en principio más selectivos para los enemigos naturales que antiguos plaguicidas como organoclorados, oroganofosforados o carbamatos, y por su uso frecuente en cultivos hortícolas donde O. laevigatus y N. tenuis están presentes. Todos ellos están incluidos o en proceso de inclusión en la lista comunitaria de sustancias activas para uso agrícola, Anexo I de la Directiva 91/414/CEE: abamectina y emamectina (avermectinas neurotóxicas, activadoras del canal del cloro), deltametrina (piretroide neurotóxico, modulador del canal del sodio, control positivo), flubendiamida (neurotóxico, modulador del receptor de rianodina), spinosad (naturalito neurotóxico, agonistas/antagonistas del receptor de nicotínico acetilcolina) y spiromesifen (inhibidor de la acetil CoA carboxilasa). El estudio mostró que O. laevigatus fue más susceptible a los insecticidas que N. tenuis. Además, los resultados revelaron que flubendiamida y spiromesifen fueron compatibles con los dos enemigos naturales estudiados, y por tanto se podrían usar en programas de GIP. Por el contrario, los insecticidas abamectina, deltametrina, emamectina y spinosad no fueron selectivos para ninguno de los chinches depredadores. Sin embargo, los estudios de persistencia demostraron que a pesar de que estos insecticidas no proporcionaron selectividad fisiológica, pueden proporcionar selectividad ecológica en algunos casos. Abamectina, deltametrina, emamectina y spinosad podrían ser compatibles con N. tenuis si el enemigo natural es introducido en el cultivo 4 días después de su aplicación. En el caso de O. laevigatus, abamectina, deltametrina y spinosad se clasificaron como persistentes, por lo tanto es necesario completar el estudio con experimentos de semi-campo y campo que determinen si es posible su uso conjunto en programas de GIP. Por otro lado, emamectina podría ser compatible con O. laevigatus si el enemigo natural es introducido en el cultivo 7 días después de su aplicación. Por último, se ha comprobado la selectividad de tres insecticidas aceleradores de la muda (MACs) (metoxifenocida, tebufenocida y RH-5849) sobre O. laevigatus y N. tenuis. Además de realizar estudios para evaluar la toxicidad en laboratorio de los insecticidas por contacto residual e ingestión (principal modo de acción de los MAC´s), se extrajo RNA de los insectos y con el cDNA obtenido se secuenció y clonó el dominio de unión al ligando (LBD) del receptor de ecdisona correspondiente a O. laevigatus (OlEcR-LBD) y N. tenuis (NtEcR-LBD). Posteriormente, se obtuvo la configuración en tres dimensiones del LBD y se estudió el acoplamiento de las moléculas de los tres insecticidas en la cavidad que forman las 12 α-hélices que constituyen el EcR-LBD. En el caso de N. tenuis se debe mencionar que no fue posible la obtención de la secuencia completa del LBD. Sin embargo, se obtuvo una secuencia parcial (hélice 6-hélice 11), que mostró una alta conservación de aminoácidos con respecto a la obtenida en O. laevigatus. Los ensayos de toxicidad mostraron que metoxifenocida, tebufenocida y RH-5849 no produjeron ningún efecto nocivo en ambos depredadores. Además, los estudios de modelado por homología y acoplamiento molecular llevados a cabo con O. laevigatus, también indicaron que los MACs no produjeron ningún efecto deletéreo en este enemigo natural. Por lo tanto, estos compuestos pueden ser aplicados de manera segura en programas de GIP en los cuales O. laevigatus y N. tenuis estén presentes. ABSTRACT The new pesticide legislation on pest control is aimed at integrated pest management (IPM). These programs are based on the most environmentally sustainable approaches, where biological, physical control and other non-chemical methods are the cornerstone. However, selective pesticides are often required for pest management on horticultural crops. Therefore, the main goal of this study is to provide knowledge to improve pest control on horticultural crops through the integration of three strategies: biological, physical and chemical. Firstly, the effects of insecticide treated nets (bifenthrin) were evaluated in different laboratory, greenhouse and field experiments on the natural enemies Orius laevigatus (Fieber) (Hemiptera: Anthocoridae) (predator of thrips), Nesidiocoris tenuis (Reuter) (Hemiptera: Miridae) (predator of whiteflies and Tuta absoluta (Meirick) (Lepidoptera: Gelechiidae)), and other biocontrol agents commonly used on protected horticultural crops. These types of nets have been successfully used in medical entomology to control mosquito malaria vectors, and work is currently being done on their use as exclusion barriers and as a direct method of pest control in agriculture. In experiments made under laboratory conditions, O. laevigatus and N. tenuis were not able to detect the presence of bifenthrin in a dual-choice test. Furthermore, no shortterm mortality (72 hours) was recorded on both predatory bugs. In contrast, a high mortality rate was found when they were exposed by contact to the bifenthrin-treated net for 72 hours in small cages (10 cm diameter X 3 cm high). In assays carried out under more realistic conditions of exposure, in an experimental greenhouse with cages of 25 X 25 X 60 cm high, short-term mortality (72 hours) and reproductive parameters were not affected. Lastly, in field experiments carried out in semi-commercial tunnels (8 m long X 6.5 m width X 2.6 m high), neither environmental conditions [temperature, relative humidity, ultraviolet (UV) and photosynthetically active radiation (PAR)] nor natural enemies were affected by the presence of the bifenthrin-treated net on the crop. However, results were not conclusive, mainly due to a low settlement of the released biocontrol agents, and further studies are needed in commercial greenhouses to confirm our preliminary results of compatibility. Secondly, the lethal (mortality) and sublethal effects (reproductive parameters) of six modern pesticides on the predatory bugs O. laevigatus and N. tenuis has been evaluated through laboratory and persistence experiments. Trials were carried out by residual contact, applying the insecticides to the maximum field recommended concentration on glass plates (laboratory) or plants (persistence). Insecticides were chosen as representatives of modern pesticides with a more selective mode of action on natural enemies than organochlorine, organophosphorus and carbamate insecticides. Moreover, they were also chosen because of their frequent use on horticultural crops where O. laevigatus and N. tenuis are present. All of them have been included or have been requested for inclusion in the community list of active substances on the agricultural market, Annex I of the European Directive 91/414/EEC: abamectin and emamectin (neurotoxic avermectins, chloride channel activators), deltamethrin (neutotoxic pyrethroid, sodium channel modulator, positive commercial standard), flubendiamide (neurotoxic, rianodine receptor modulator), spinosad (neurotoxic naturalyte, nicotinic acetylcholine receptor allosteric activator) and spiromesifen (inhibitors of acetyl CoA carboxylase). The study showed that O. laevigatus was more susceptible to all the studied pesticides than N. tenuis. In addition, the research results indicated no impact of flubendiamide and spiromesifen on the two natural enemies studied under laboratory conditions. Consequently, both pesticides are candidates to be included in IPM programmes where these biocontrol agents are present. On the other hand, abamectin, deltamethrin, emamectin and spinosad were not selective for both predatory bugs in laboratory experiments. However, persistence test demonstrated that in spite of the lack of physiological selectivity, these pesticides can provide ecological selectivity in some cases. Abamectin, deltamethrin, emamectin and spinosad could be compatible with N. tenuis if the mirid bug is released 4 days after the insecticide treatment on the crop. With regard to O. laevigatus, abamectin, deltamethrin and spinosad were classified as persistent in our assays, thus the study should be completed with semi-field and field experiments in order to ascertain their possible joint use in IPM programs. In contrast, emamectin could be compatible with O. laevigatus if the pirate bug is released 7 days after the insecticide treatment on the crop. Finally, the selectivity of three moulting accelerating compounds (MACs) (methoxyfenozide, tebufenozide and RH-5849) has also been evaluated on O. laevigatus and N. tenuis. In addition to laboratory experiments to evaluate the toxicity of the insecticides by residual contact and ingestion, molecular approaches were used as well. RNA of both insects was isolated, cDNA was subsequently synthesized and the complete sequence of the ligand binding domain (LBD) of the ecdysone receptor of O. laevigatus (OlEcR-LBD) and N. tenuis (NtEcR-LBD) were determined. Afterwards, the three dimensional structure of LBD was constructed. Finally, the docking of the insecticide molecules in the cavity delineated by the 12 α-helix that composed the EcRLBD was performed. In the case of N. tenuis, it should be noted that in spite of intensive efforts, we did not manage to complete the sequence for the LBD.However, a partial sequence of the LBD was obtained (helix 6-helix 11), and a strong conservation between the amino acids of N. tenuis and O. laevigatus was observed. Results showed no biological activity of methoxyfenozide, tebufenozide and RH-5849, on both predatory bugs. Moreover, modeling of the OlEcR-LBD and docking experiments also suggested that MACs were devoid of any deleterious effect on O. laevigatus. Therefore, our results indicate that these compounds could be safely applied in IPM programs in which O. laevigatus and N. tenuis are present.