Effects of Estrogen on Muscle Damage in Response to an Acute Resistance Exercise Protocol

Creatine Kinase (CK) is used as a measure of exercise-induced muscle membrane damage. During acute eccentric (muscle lengthening) exercise, muscle sarcolemma, sarcoplasmic reticulum, and Z-lines are damaged, thus causing muscle proteins and enzymes to leak into the interstitial fluid. Strenuous eccentric exercise produces an elevation of oxygen free radicals, which further increases muscle damage. Muscle soreness and fatigue can be attributed to this membrane damage. Estradiol, however, may preserve membrane stability post-exercise (Brancaccio, Maffulli, & Limongelli, 2007; Carter, Dobridge, & Hackney, 2001; Tiidus, 2001). Because estradiol has a similar structure to Vitamin E, which is known to have antioxidant properties, and both are known to affect membrane structure, researchers have proposed that estrogen acts as an antioxidant to provide a protective effect on the post-exercise muscle of women (Sandoval & Matt, 2002). As a result, it has been postulated that muscles in women incur less damage in response to an acute strenuous exercise as compared to men. PURPOSE: To determine if circulating estrogen concentrations are related to muscle damage, as measured by creatine kinase activity and to determine gender differences in creatine kinase as a marker of muscle damage in response to an acute heavy resistance exercise protocol. METHODS: 7 healthy, resistance-trained, eumenhorrheic women (23±3 y, 169±9.1 cm, 66.4±10.5 kg) and 8 healthy, resistance-trained men (25±5 y, 178±6.7 cm, 82.3±9.33 kg) volunteered to participate in the study. Subjects performed an Acute Resistance Exercise Test (ARET) consisting of 6 sets of 5 repetitions Smith machine squats at 90% of their previously determined 1-RM. Blood samples were taken pre-, mid-, post-, 1 hour post-, 6 hours post-, and 24 hours post-exercise. Samples were stored at -80ºC until analyzed. Serum creatine kinase was measured using an assay kit from Genzyme (Framingham, MA). Serum estradiol was measured by an ELISA from GenWay (San Diego, CA). Estradiol b-receptor presence on granulocytes was measured via flow cytometry using primary antibodies from Abcam (Cambridge, MA) and PeCy7 antibodies (secondary) from Santa Cruz (Santa Cruz, CA). RESULTS: No significant correlations between estrogen and CK response were found after an acute resistant exercise protocol. Moreover, no significant change in estradiol receptors were expressed on granulocytes after exercise. Creatine Kinase response, however, differed significantly between genders. Men had higher resting CK concentrations throughout all time points. Creatine Kinase response increased significantly after exercise in both men and women (p=0.008, F=9.798). Men had a significantly higher CK response at 24 hours post exercise than women. A significant condition/sex/time interaction was exhibited in CK response (p=0.02, F=4.547). Perceived general soreness presented a significant condition, sex interaction (p=0.01, F=9.532). DISCUSSION: Although no estradiol and CK response correlations were found in response to exercise, a significant difference in creatine kinase activity was present between men and women. This discrepancy of our results and findings in the literature may be due to the high variability between subjects in creatine kinase activity as well as estrogen concentrations. The lack of significance in change of estradiol receptor expression on granulocytes in response to exercise may be due to intracellular estradiol receptor staining and non-specific gating for granulocytes rather than additional staining for neutrophil markers. Because neutrophils are the initial cells present in the inflammatory response after strenuous exercise, staining for estrogen receptors on this cell type may allow for a better understanding of the effect of estrogen and its hypothesized protective effect against muscle damage. Furthermore, the mechanism of action may include estradiol receptor expression on the muscle fiber itself may play a role in the protective effects of estradiol rather than or in addition to expression on neutrophils. We have shown here that gender differences occur in CK activity as a marker of muscle damage in response to strenuous eccentric exercise, but may not be the result of estradiol concentration or estradiol receptor expression on granulocytes. Other variables should be examined in order to determine the mechanism involved in the difference in creatine kinase as a marker of muscle damage between men and women after heavy resistance exercise.

The Relationship between Large Fiscal Adjustments and Short-Term Output Growth Under Alternative Fiscal Policy Regimes

A small, but growing, body of literature searches for evidence of non-Keynesian effects of fiscal contractions. That is, some evidence exists that large fiscal contractions stimulate short-run economic activity. Our paper continues this research effort by systematically examining the effects, if any, of unusual fiscal events - either non-Keynesian results within a Keynesian model or Keynesian results within a neoclassical model -- on short-run economic activity. We examine this issue within three separate models -- a St. Louis equation, a Hall-type consumption equation, and a growth accounting equation. Our empirical findings are mixed, and do not provide strong systematic support for the view that unusually large fiscal contractions/expansions reverse the effects of normal fiscal events. Moreover, we find only limited evidence that trigger points are empirically important.

OUT-OF-HOSPITAL CHILDBEARING CENTERS IN THE UNITED STATES: A DESCRIPTIVE STUDY OF THE DEMOGRAPHIC AND MEDICAL-OBSTETRIC CHARACTERISTICS OF WOMEN BEGINNING LABOR THEREIN 1972-1979

There is currently much interest in the appropriate use of obstetrical technology, cost containment and meeting consumers' needs for safe and satisfying maternity care. At the same time, there has been an increase in professionally unattended home births. In response, a new type of service, the out-of-hospital childbearing center (CBC) has been developed which is administratively and structurally separate from the hospital. In the CBC, maternity care is provided by certified nurse-midwives to carefully screened low risk childbearing families in conjunction with physician and hospital back-up.^ It was the purpose of this study to accomplish the following objectives: (1) To describe in a historical prospective study the demographic and medical-obstetric characteristics of patients laboring in eleven selected out-of-hospital childbearing centers in the United States from May 1, 1972, to December 15, 1979. Labor is defined as the onset of regular contractions as determined by the patient. (2) To describe any differences between those patients who require transfer to a back-up hospital and those who do not. (3) To describe administrative and service characteristics of eleven selected out-of-hospital childbearing centers in the United States. (4) To compare the demographic and medical-obstetric characteristics of women laboring in eleven selected out-of-hospital childbearing centers with a national sample of women of similar obstetric risk who according to birth certificates delivered legitimate infants in a hospital setting in the United States in 1972.^ Research concerning CBCs and supportive to the development of CBCs including studies which identified factors associated with fetal and perinatal morbidity and mortality, obstetrical risk screening, and the progress of technological development in obstetrics were reviewed. Information concerning the organization and delivery of care at each selected CBC was also collected and analyzed.^ A stratified, systematic sample of 1938 low risk women who began labor in a selected CBC were included in the study. These women were not unlike those described previously in small single center studies reported in the literature. The mean age was 25 years. Sixty-three per cent were white, 34 per cent Hispanic, 88 per cent married, 45 per cent had completed at least two years of college, nearly one-third were professionals and over a third were housewives. . . . (Author's abstract exceeds stipulated maximum length. Discontinued here with permission of school.) UMI ^

Escape performance of temperate king scallop, Pecten maximus under ocean warming and acidification

Among bivalves, scallops are exceptional due to their capacity to escape from predators by swimming which is provided by rapid and strong claps that are produced by the phasic muscle interspersed with tonic muscle contractions. Based on the concept of oxygen and capacity-limited thermal tolerance, the following hypothesis was tested: ocean warming and acidification (OWA) would induce disturbances in aerobic metabolic scope and extracellular acid-case status and impair swimming performance in temperate scallops. Following long-term incubation under near-future OWA scenarios [20 vs. 10 °C (control) and 0.112 kPa CO2 (hypercapnia) vs. 0.040 kPa CO2 (normocapnic control)], the clapping performance and metabolic rates (MR) were measured in resting (RMR) and fatigued (maximum MR) king scallops, Pecten maximus, from Roscoff, France. Exposure to OA, either alone or combined with warming, left MR and swimming parameters such as the total number of claps and clapping forces virtually unchanged. Only the duration of the escape response was affected by OA which caused earlier exhaustion in hyper- than in normocapnic scallops at 10 °C. While maximum MR was unaffected, warm exposure increased RMR in both normocapnic and hypercapnic P. maximus resulting in similar Q 10 values of ~2.2. The increased costs of maintenance and the observation of strongly reduced haemolymph PO2 levels indicate that at 20 °C scallops have reached the upper thermal pejus range with unbalanced capacities for aerobic energy metabolism. As a consequence, warming to 20 °C decreased mean phasic force during escape performance until fatigue. The observed prolonged recovery time in warm incubated scallops might be a consequence of elevated metabolic costs at reduced oxygen availability in the warmth.

Anelastic strain recovery and elastic properties of ODP Leg 123 oceanic basalt samples

A knowledge of rock stress is fundamental for improving our understanding of oceanic crustal mechanisms and lithospheric dynamic processes. However, direct measurements of stress in the deep oceans, and in particular stress magnitudes, have proved to be technically difficult. Anelastic strain recovery measurements were conducted on 15 basalt core samples from Sites 765 and 766 during Leg 123. Three sets of experiments were performed: anelastic strain recovery monitoring, dynamic elastic property measurements, and thermal azimuthal anisotropy observations. In addition, a range of other tests and observations were recorded to characterize each of the samples. One common feature of the experimental results and observations is that apparently no consistent orientation trend exists, either between the different measurements on each core sample or between the same sets of measurements on the various core samples. However, some evidence of correspondence between velocity anisotropy and anelastic strain recovery exists, but this is not consistent for all the core samples investigated. Thermal azimuthal anisotropy observations, although showing no conclusive correlations with the other results, were of significant interest in that they clearly exhibited anisotropic behavior. The apparent reproducibility of this behavior may point toward the possibility of rocks that retain a "memory" of their stress history, which could be exploited to derive stress orientations from archived core. Anelastic strain recovery is a relatively new technique. Because use of the method has extended to a wider range of rock types, the literature has begun to include examples of rocks that contracted with time. Strong circumstantial evidence exists to suggest that core-sample contractions result from the slow diffusion of pore fluids from a preexisting microcrack structure that permits the rock to deflate at a greater rate than the expansion caused by anelastic strain recovery. Both expansions and contractions of the Leg 123 cores were observed. The basalt cores have clearly been intersected by an abundance of preexisting fractures, some of which pass right through the samples, but many are intercepted or terminate within the rock matrix. Thus, the behavior of the core samples will be influenced not only by the properties of the rock matrix between the fractures, but also by how these macro- and micro-scale fractures mutually interact. The strain-recovery curves recorded during Leg 123 for each of the 15 basalt core samples may reflect the result of two competing time dependent processes: anelastic strain recovery and pore pressure recovery. Were these the only two processes to influence the gauge responses, then one might expect that given the additional information required, established theoretical models might be used to determine consistent stress orientations and reliable stress magnitudes. However, superimposed upon these competing processes is their respective interaction with the preexisting fractures that intersect each core. Evidence from our experiments and observations suggests that these fractures have a dominating influence on the characteristics of the recovery curves and that their effects are complex.

High-resolution multi-proxy record of the last glacial period from Lake Van, eastern Anatolian high plateau, Turkey

Detailed analyses of the Lake Van pollen, Ca/K ratio and stable oxygen isotope record allow the identification of millennial-scale vegetation and environmental changes in eastern Anatolia throughout the last glacial (~75-15 ka BP). The climate within the last glacial was cold and dry, with low arboreal pollen (AP) levels. The driest and coldest period corresponds to Marine Isotope Stage (MIS) 2 (~28-14.5 ka BP) dominated by the highest values of xerophytic steppe vegetation. Our high-resolution multi proxy record shows rapid expansions and contractions of tree populations that reflects variability in temperature and moisture availability. This rapid vegetation and environmental changes can be linked to the stadial-interstadial pattern of the Dansgaard-Oeschger (DO) events as recorded in the Greenland ice cores. Periods of reduced moisture availability were characterized by enhanced xerophytic species and high terrigenous input from the Lake Van catchment area. Furthermore, comparison with the marine realm reveals that the complex atmosphere-ocean interaction can be explained by the strength and position of the westerlies, which is responsible for the supply of humidity in eastern Anatolia. Influenced by diverse topography of the Lake Van catchment, larger DO interstadials (e.g. DO 19, 17-16, 14, 12 and 8) show the highest expansion of temperate species within the last glacial. However, Heinrich events (HE), characterized by highest concentrations of ice-rafted debris (IRD) in marine sediments, are identified in eastern Anatolia by AP values not lower and high steppe components not more abundant than during DO stadials. In addition, this work is a first attempt to establish a continuous microscopic charcoal record over the last glacial in the Near East, which documents an initial immediate response to millennial-scale climate and environmental variability and enables us to shed light on the history of fire activity during the last glacial.

Organic geochemical characteristics at DSDP Holes 76-534A and 44-391C

Pyrolysis assay, bitumen analysis, and elemental analysis of kerogen were used to characterize the organic matter of selected core samples from Hole 534A (Leg 76) and Hole 391C (Leg 44) on the Blake-Bahama Plateau. The organic matter throughout the stratigraphic section appears to be principally of a terrestrial origin. The data from several isolated horizons in the Hatteras and Blake-Bahama Formations imply the presence of significant quantities of autochthonous marine organic matter. However, these horizons appear so limited that they cannot be considered potential liquid hydrocarbon source rocks. All the analyzed samples are immature and have not evolved sufficiently to enter into the main stage of hydrocarbon generation. The temporal and spatial restrictions of strata rich in marine organic matter suggest that they do not represent major expansions and contractions of anoxic bottom-water masses, but represent limited occurrences of anoxic conditions.

U-Pb, trace element, and Hf isotope analysis for Macquarie Island detrital zircon

Oceanic zircon trace element and Hf-isotope geochemistry offers a means to assess the magmatic evolution of a dying spreading ridge and provides an independent evaluation of the reliability of oceanic zircon as an indicator of mantle melting conditions. The Macquarie Island ophiolite in the Southern Ocean provides a unique testing ground for this approach due to its formation within a mid-ocean ridge that gradually changed into a transform plate boundary. Detrital zircon recovered from the island records this change through a progressive enrichment in incompatible trace elements. Oligocene age (33-27 Ma) paleo-detrital zircon in ophiolitic sandstones and breccias interbedded with pillow basalt have trace element compositions akin to a MORB crustal source, whereas Late Miocene age (8.5 Ma) modern-detrital zircon collected from gabbroic colluvium on the island have highly enriched compositions unlike typical oceanic zircon. This compositional disparity between age populations is not complimented by analytically equivalent eHf data that primarily ranges from 14 to 13 for sandstone and modern-detrital populations. A wider compositional range for the sandstone population reflects a multiple pluton source provenance and is augmented by a single cobble clast with eHf equivalent to the maximum observed composition in the sandstone (~17). Similar sandstone and colluvium Hf-isotope signatures indicate inheritance from a similar mantle reservoir that was enriched from the depleted MORB mantle average. The continuity in Hf-isotope signature relative to trace element enrichment in Macquarie Island zircon populations, suggests the latter formed by reduced partial melting linked to spreading-segment shortening and transform lengthening along the dying spreading ridge.

Stable isotopic record of late Pliocene and Pleistocene foraminifera of ODP Site 114-704

We studied the stable isotopic and carbonate stratigraphy of ODP Hole 704A to reconstruct the paleoceanographic evolution of the eastern subantarctic sector of the South Atlantic Ocean. Site 704 is well positioned with respect to latitude (46°52.8'S, 7°25.3'E) and bathymetry (2532 m) to monitor past migrations in the position of Polar Front Zone (PFZ) and changes in deep-water circulation during the late Pliocene-Pleistocene. Several important changes occurred in proxy paleoceanographic indicators across the Gauss/Matuyama boundary at 2.47 Ma: (1) accumulation rates of biogenic sedimentary components increased by an order of magnitude (Froelich et al., this volume); (2) planktonic d1 8O values increased by an average of 0.5 per mil; (3) the amplitude of the benthic d18O signal increased; (4) the accumulation rate of ice-rafted detritus increased several fold (Warnke and Allen, this volume); and (5) carbon isotopic ratios of benthic foraminifers decreased by 0.5 per mil, as did the d13C of the fine-fraction carbonate by 1.5 per mil (Mead et al., 1991, doi:10.2973/odp.proc.sr.114.152.1991), but no change occurred in planktonic foraminiferal d13C values. Most of these changes are consistent with more frequent expansions and contractions of the PFZ over Site 704 after 2.47 Ma, bringing cold, nutrient-rich waters to 47°S that stimulated both carbonate and siliceous productivity. The synchronous increase in d18O values and ice-rafted detritus accumulation in Hole 704A indicates that the 2.4 Ma paleoceanographic event included ice volume growth on both Antarctica and Northern Hemisphere continents. The decrease in benthic d13C values indicates that the ventilation rate of Southern Ocean deep water decreased and the nutrient content increased during glacial events after 2.5 Ma. At the Gauss/Matuyama boundary, benthic d13C values of the Southern Ocean shifted toward those of the Pacific end member, indicating a decrease in the relative mixing ratio of Northern Component Water and Circumpolar Deep Water. During the early Matuyama (~2.3 to 1.7 Ma), the PFZ generally occupied a southerly position with respect to Site 704 and carbonate productivity prevailed. Exceptions to these general conditions occurred during strong glacial events of the early Matuyama (e.g., isotopic stages 82, 78, 74, and 70), when the PFZ migrated to the north and opal sedimentation predominated at Site 704. At 1.7 Ma, the PFZ migrated toward the equator and occupied a more northerly position for a prolonged interval between ~1.7 and 1.5 Ma. Beginning at ~1.5-1.4 Ma, surface and bottom water parameters (d18O, d13C, %CaCO3, and %opal) in the subantarctic South Atlantic became highly correlated such that glacial events (d18O maxima) corresponded to d13C and carbonate minima and opal maxima. This pattern is typical of the correlation found during the latest Pleistocene in the Southern Ocean (Charles and Fairbanks, in press). This event coincided with increased suppression of Northern Component Water during glacial events after 1.5 Ma (Raymo et al., 1990, doi:10.1016/0012-821X(90)90051-X), which may have influenced the climatology of the Southern Hemisphere by altering the flux of heat and salt to the Southern Ocean).

Petrography and geochemical composition of the Atlantis II Fracture Zone

SeaBeam echo sounding, seismic reflection, magnetics, and gravity profiles were run along closely spaced tracks (5 km) parallel to the Atlantis II Fracture Zone on the Southwest Indian Ridge, giving 80% bathymetric coverage of a 30- * 170-nmi strip centered over the fracture zone. The southern and northern rift valleys of the ridge were clearly defined and offset north-south by 199 km. The rift valleys are typical of those found elsewhere on the Southwest Indian Ridge, with relief of more than 2200 m and widths from 22 to 38 km. The ridge-transform intersections are marked by deep nodal basins lying on the transform side of the neovolcanic zone that defines the present-day spreading axis. The walls of the transform generally are steep (25°-40°), although locally, they can be more subdued. The deepest point in the transform is 6480 m in the southern nodal basin, and the shallowest is an uplifted wave-cut terrace that exposes plutonic rocks from the deepest layer of the ocean crust at 700 m. The transform valley is bisected by a 1.5-km-high median tectonic ridge that extends from the northern ridge-transform intersection to the midpoint of the active transform. The seismic survey showed that the floor of the transform contains up to 0.5 km of sediment. Piston-coring at two locations on the transform floor recovered more than 1 m of sand and gravel, which appears to be turbidites shed from the walls of the fracture zone. Extensive dredging showed that more than two-thirds of the crust exposed in the transform valley and its walls were plutonic rocks, principally gabbros and residual mantle peridotites. In contrast, based on dredging and seafloor morphology, only relatively undisrupted pillow basalt flows have been exposed on crust of the same age spreading away from the transform. Magnetic anomalies are well defined out to 11 m.y. over the flanking transverse ridges and transform valley, even where layer 2 appears to be absent. The total opening rate is 1.6 cm/yr, but the arrangement of the anomalies indicates that the spreading for each ridge is asymmetric, with the ridge flanks facing the transform spreading at a rate of 1.0 cm/yr. Such an asymmetric spreading pattern requires that both the northern and southern ridges migrate away from each other at 0.2 cm/yr, thus lengthening the transform at 0.4 cm/yr for the last 11 m.y. To the north, the fracture zone valley is oriented differently from the present-day transform, indicating a paleospreading direction change at 17 m.y. from N10°E to due north-south. This change placed the transform into extension for the 11-m.y. period required for simple orthogonal ridge-transform geometry to be reestablished and produced a large transtensional basin within the transform valley. This basin was split by continued transform slip after 11 m.y., with the larger half moving to the north with the African Plate.

Integral Bridge for High-Speed Railway

The structural continuity of fully integral bridges entails many advantages and some drawbacks. Among the latter, the cyclic expansions and contractions of the deck caused by seasonal thermal variations impose alternating displacements at the piers and abutments, with effects that may be difficult to establish reliably. The advantages include easier construction and cheaper maintenance but, especially, horizontal loads can be transmitted to the ground in a much better way than in conventional bridges. This paper first presents a methodology for dealing with the problems that the cyclic displacements imposed raise at the abutments and at the bridge piers. At the former, large pressures may develop, possibly accompanied by undesirable surface settlements. At the latter, the degree of cracking and the ability to carry the specified loads may be in question. Having quantified the drawbacks, simplified but realistic analyses are conducted of the response of an integral bridge to braking and seismic loads. It is shown that integral bridges constitute an excellent alternative in the context of the requirements posed by new high-speed railway lines.

El injerto en pepino corto tipo español (Cucumis sativus L.) recomencaciones para su empleo en la zona central española

El injerto en hortalizas es uno de los temas de más actualidad en el panorama hortícola, no solo español, sino occidental, y recalcamos occidental, pues en muchos países que no corresponden a ese ámbito, sobre todo asiáticos: Japón, Corea, China, Filipinas, etc., esta es una técnica que cuenta con una gran difusión desde hace décadas, siendo, por ejemplo en Japón, la mayoría de sus cultivos de cucurbitáceas y solanáceas realizados con planta injertada. A finales de los noventa quedó claro que el empleo de bromuro de metilo tenía una fecha de caducidad y que las zonas que tenían una fuerte dependencia de este desinfectante de suelo debían de buscar alternativas a un plazo lo más corto posible, con un punto añadido sobre etapas anteriores, debían ser alternativas lo más respetuosas posible con el medio ambiente y que no incrementaran, de forma importante, los costes de producción. En la zona centro y concretamente en los invernaderos de la Comunidad de Madrid y zonas cercanas de Toledo y Guadalajara el pepino era y es el cultivo predominante, los horticultores empleaban el bromuro de metilo de forma sistemática para desinfectar sus suelos y la desaparición de este producto les planteaba una gran incertidumbre, lo que llevó a que desde diferentes instancias se buscaran diferentes alternativas. Tras analizar las posibilidades que se podían implementar y conocido el buen resultado que había dado el injerto en sandía en Almería, se decidió acometer los trabajos que conforman esta Tesis Doctoral, planteando en la zona, diferentes ensayos con la idea de conocer, si el injerto en pepino, con los cultivares empleados habitualmente, podía ser una alternativa real para los horticultores, tanto de Madrid, como los de las zonas cercanas de Toledo y Guadalajara. Se pretendía conocer sobre todo las repercusiones agronómicas y si esta técnica podría emplearse en solitario o era necesario complementarla con otras alternativas: desinfectantes químicos, solarización, biofumigación e incluso desinfección con vapor de agua. Los ensayos fueron realizados de forma secuencial entre el año 1999 y el 2011, comprobándose en primer lugar que el empleo de portainjertos híbridos de calabaza era posible con los cultivares de pepino corto tipo español, mayoritariamente empleados en los últimos años del siglo XX y primeros del XXI, fundamentalmente: Serena. Tras los primeros ensayos, Shintoza parecía el portainjerto híbrido de calabaza (Cucurbita maxima x C. moschata) con mejores perspectivas de empleo, pues presentaba la ventaja adicional de ser bien conocido por los semilleros que producen planta injertada al ser, en esos momentos, el portainjerto más empleado en sandía, lo que garantizaba por su lado, su empleo en pepino, y que los horticultores pudiesen disponer de planta injertada. Más adelante los trabajos se encaminaron hacia la determinación de la densidad y tipo de poda más adecuado para la planta injertada, realizándose múltiples ensayos en esta dirección, que culminaron con la conclusión de que el extravigor que los portainjertos conferían a las plantas permitía conducir estas a dos o más brazos (se suelen emplear dos, por mejor adaptación a los trabajos de manejo de la planta por parte de los agricultores), con lo que se podría disminuir la densidad de planta y por tanto ahorrar en este capítulo, cosa que preocupaba y preocupa a los agricultores. Se llegó a determinar que es posible reducir la densidad de plantación en alrededor de un 25%, estando la densidad de brazos más adecuada entre 3 y 3.5 br•m-2. Tras las primeras decisiones tomadas sobre el portainjerto y la densidad más adecuada, se continuó con el estudio de adaptación de estas propuestas a los nuevos cultivares que las empresas de semillas iban proponiendo y los agricultores adoptando. Estas acciones se complementaron con la introducción de nuevos portainjertos susceptibles de sustituir a Shintoza o rotar con él para cambiar de sistema radicular, lo que es conveniente cuando se emplean, como es el caso, portainjertos que no son resistentes a nematodos, principalmente de la especie Meloidogyne incognita, el mayor problema en la zona, debido al suelo. Cultivares como Trópico, en un primer momento, y Urano y Motril más recientemente, se adaptaron muy bien a esta técnica. Entre los portainjertos que mostraron buena adaptación a la técnica de injerto y suficientemente buena compatibilidad con la mayoría de los cultivares ensayados destacan: RS-841, Strongtosa y Camel. Azman también mostró un comportamiento relevante, pero este portainjerto no podrá ser empleado, al ser recientemente retirado del mercado por la empresa que lo obtuvo y comercializó Aunque no era el objetivo principal de esta Tesis Doctoral, se ha comprobado que puede ser interesante combinar el empleo del injerto con otras técnicas alternativas al bromuro de metilo para superar los problemas debidos a enfermedades del suelo o nematodos, pero debe seguirse trabajando pues este es un tema en continua evolución, tanto si se trata de desinfectantes, a la mayoría de los cuales les está siendo retirado el permiso para su comercialización, como de otros métodos como la biofumigación o el empleo de vapor de agua. Queda muy claro que el injerto puede considerarse entre los métodos respetuosos con el medio ambiente, si no el que más, en lo que alternativas al bromuro de metilo se refiere. También en otro momento, se comprobó que con plantas injertadas es posible reducir el aporte de nutrientes, sobre todo nitrógeno, lo que además de un ahorro supone una mejora más desde el punto de vista medioambiental. En definitiva, queda demostrado que es factible el empleo del injerto en pepino corto tipo español, que las selecciones de los híbridos entre Cucurbita maxima y C. moschata que habitualmente se están empleando en sandía son también de aplicación en estos pepinos y que su empleo puede llevarnos a producciones suficientemente remuneradoras, alargándose en muchos casos el ciclo y no modificando, de forma apreciable, la calidad. Queda también demostrado que aunque los portainjertos no sean resistentes a nematodos, su extravigor les hace desarrollarse, desde el punto de vista productivo, suficientemente, llegando por tanto, a “convivir” con ese problema. Al no ser resistentes los portainjertos, y permanecer e incluso agravarse el problema de nematodos es conveniente poder contar con diferentes portainjertos que nos permitan rotar entre ellos y utilizar diferentes sistemas radiculares que harán menos fácil el parasitismo de los nematodos, como recomiendan los nematólogos que se haga. ABSTRACT Vegetable grafting is one of the most current practices in horticulture, not only in Spain, but also in other Western and Asian countries, such as Japan, South Korea, China, the Philippines, etc. This is a decades-old, widespread technique: In fact, most cucurbit and solanaceous crops in Japan and Korea are grafted. At the end of the 1990s, it was clear that methyl bromide had an expiry date. Consequently, the areas strongly dependant on this soil disinfectant had to look for alternatives as quickly as possible. Besides, these had to be as environmentally friendly as possible and should not increase production costs significantly. The cucumber has been and still is the most important crop in greenhouses of the Comunidad de Madrid and in areas near Toledo and Guadalajara. Cucumber growers used methyl bromide systematically to disinfect the soil. The banning of this chemical product brought about uncertainty, which encouraged the search for different alternatives. After analyzing the different possibilities and taking into account the good results of watermelon grafting in Almería, it was decided to carry out the works that make up this doctoral thesis. Different trials were made in order to know if the cultivars used in cucumber grafting might be a real alternative for farmers, not only in Madrid, but also in the areas near Toledo and Guadalajara. The main aim was to assess the agronomic repercussions and whether that technique could be used alone, or if other complementary alternatives, such as chemical disinfectants, solarisation, biofumigation, or even steam disinfection, were necessary. Trials were carried out sequentially from 1999 to 2011. It was observed that the use of pumpkin hybrid rootstocks could be applied to cultivars of Spanish short cucumbers, mainly grown in the late 20th and early 21st centuries eg Serena. After the early trials, Shintoza (Cucurbita maxima x C. moschata), a pumpkin hybrid rootstock, seemed to be the best option, as it had the additional advantage of being well known by nurseries growing grafting plants. Bearing this in mind, Shintoza was then the hybrid rootstock to be used in cucumbers and consequently growers could have grafted plants at their disposal. Later on, research was focused on density and the most adequate type of pruning, by carrying out several trials. These experiments showed that, the extra vigour the rootstocks gave to the plants, allowed them to have two or three stems, (normally nurserymen use two, as it is easier for them to manage the plants). These findings would lead to the lessening the density of the plant and thus reduce costs, something which worried and still worries farmers. It was stated that it would be possible to reduce the density of the plants by about 25%, the optimum density of the stems ranging from 3 to 3.5 stem-m-2. Once decisions were taken both on the rootstock and the appropriate density, we went on to study how to apply these proposals to the new cultivars which the seed companies were proposing and the farmers were applying. These measures were complemented with the introduction of new rootstocks capable of replacing Shintoza, or rotating with it in order to change the root system. This is particularly necessary when rootstocks, non-resistant to nematodes, mainly of the species Meloidogyne incognita, are used. This is the main problem due to the soil of that area. Cultivars such as Trópico, at first, and Urano and Motril, more recently, adapted quite well to this technique. Among the rootstocks which adapted well to grafting and which were compatible with most tested cultivars, were, in particular, RS-841 Strongtosa and Camel. The behaviour of Azman was worth studying, but this rootstock was removed from the market by the company which had bought and commercialized it. Although not the main purpose of the research, it was observed that combining grafting with other alternatives to methyl bromide in order to overcome problems due to soil diseases or nematodes may be worthwhile. However, further research is needed, as this topic is in constant evolution, not only when we come to disinfectants, most of which are being affected by the removal of the permit for commercialization, but also when we refer to other techniques such as biofumigation or the use of steam. Results also showed that grafted plants may reduce the amount of fertilizers, particularly nitrogen, used: This means both saving money and the protection of the environment. We may conclude by saying that grafting Spanish short cucumbers is feasible, that the selections of the hybrids between Cucurbita maxima and C. moschata, habitually used in watermelon grafting, can also be applied to these cucumbers. It can also be concluded that the use of these grafting techniques may lead to profitable yields, by lengthening the growing cycle in many cases and by maintaining the quality to a large extent. Although these rootstocks are not resistant to nematodes, the results showed that their extra vigour enables them to develop in terms of production, and thus they cope with this problem. Since these rootstocks are not resistant to nematodes and the problem with these nematodes may even worsen, it is recommended that different types of rootstocks should be available to enable both the rotation and the use of different root systems, which will encourage the parasitism of nematodes.

Selective maintenance of allozyme differences among sympatric host races of the apple maggot fly

Whether phytophagous insects can speciate in sympatry when they shift and adapt to new host plants is a controversial question. One essential requirement for sympatric speciation is that disruptive selection outweighs gene flow between insect populations using different host plants. Empirical support for host-related selection (i.e., fitness trade-offs) is scant, however. Here, we test for host-dependent selection acting on apple (Malus pumila)- and hawthorn (Crataegus spp.)-infesting races of Rhagoletis pomonella (Diptera: Tephritidae). In particular, we examine whether the earlier fruiting phenology of apple trees favors pupae in deeper states of diapause (or with slower metabolisms/development rates) in the apple fly race. By experimentally lengthening the time period preceding winter, we exposed hawthorn race pupae to environmental conditions typically faced by apple flies. This exposure induced a significant genetic response at six allozyme loci in surviving hawthorn fly adults toward allele frequencies found in the apple race. The sensitivity of hawthorn fly pupae to extended periods of warm weather therefore selects against hawthorn flies that infest apples and helps to maintain the genetic integrity of the apple race by counteracting gene flow from sympatric hawthorn populations. Our findings confirm that postzygotic reproductive isolation can evolve as a pleiotropic consequence of host-associated adaptation, a central tenet of nonallopatric speciation. They also suggest that one reason for the paucity of reported fitness trade-offs is a failure to consider adequately costs associated with coordinating an insect’s life cycle with the phenology of its host plant.

Decreased blood pressure response in mice deficient of the α1b-adrenergic receptor

To investigate the functional role of different α1-adrenergic receptor (α1-AR) subtypes in vivo, we have applied a gene targeting approach to create a mouse model lacking the α1b-AR (α1b−/−). Reverse transcription–PCR and ligand binding studies were combined to elucidate the expression of the α1-AR subtypes in various tissues of α1b +/+ and −/− mice. Total α1-AR sites were decreased by 98% in liver, 74% in heart, and 42% in cerebral cortex of the α1b −/− as compared with +/+ mice. Because of the large decrease of α1-AR in the heart and the loss of the α1b-AR mRNA in the aorta of the α1b−/− mice, the in vivo blood pressure and in vitro aorta contractile responses to α1-agonists were investigated in α1b +/+ and −/− mice. Our findings provide strong evidence that the α1b-AR is a mediator of the blood pressure and the aorta contractile responses induced by α1 agonists. This was demonstrated by the finding that the mean arterial blood pressure response to phenylephrine was decreased by 45% in α1b −/− as compared with +/+ mice. In addition, phenylephrine-induced contractions of aortic rings also were decreased by 25% in α1b−/− mice. The α1b-AR knockout mouse model provides a potentially useful tool to elucidate the functional specificity of different α1-AR subtypes, to better understand the effects of adrenergic drugs, and to investigate the multiple mechanisms involved in the control of blood pressure.

Nitric oxide in the contractile action of bradykinin, oxytocin, and prostaglandin F2 α in the estrogenized rat uterus

Experiments were performed on uteri from estrogen-primed female rats. Bradykinin (BK) (10−8 M) significantly augmented biosynthesis of prostaglandin F2 α (PGF2α) and prostaglandin E2 (PGE2), and this synthesis was completely blocked by NG-monomethyl l-arginine (NMMA) (300 μM), a competitive inhibitor of nitric oxide synthase (NOS). Blockade of prostaglandin synthesis by indomethacin caused rapid dissipation of isometric developed tension (IDT) induced by BK. Blockade of NOS with NMMA had similar but less marked effects. Combining the two inhibitors produced an even more rapid decay in IDT, suggesting that BK-induced NO release maintains IDT by release of prostanoids. The decline of frequency of contraction (FC) was not significantly altered by either indomethacin or NMMA but was markedly accelerated by combination of the inhibitors, which suggests that PGs maintain FC and therefore FC decline is accelerated only when PG production is blocked completely by combination of the two inhibitors of PG synthesis. The increase in IDT induced by oxytocin was unaltered by indomethacin, NMMA or their combination indicating that neither NO nor PGs are involved in the contractions induced by oxytocin. However, the decline in FC with time was significantly reduced by the inhibitor of NOS, NMMA, suggesting that FC decay following oxytocin is caused by NO released by the contractile process. In the case of PGF2α, NMMA resulted in increased initial IDT and FC. The decline in FC was rapid and dramatically inhibited by NMMA. Receptor-mediated contraction by BK, oxytocin, and PGF2α is modulated by NO that maintains IDT by releasing PGs but reduces IDT and FC via cyclic GMP.