Fission track analyses of ODP Hole 129-800A samples

Four models of fission track annealing in apatite are compared with measured fission track lengths in samples from Site 800 in the East Mariana Basin, Ocean Drilling Program Leg 129, given an independently determined temperature history. The temperature history of Site 800 was calculated using a one-dimensional, compactive, conductive heat flow model assuming two end-member thermal cases: one for cooling of Jurassic ocean crust that has experienced no subsequent heating, and one for cooling of Cretaceous ocean crust. Because the samples analyzed were only shallowly buried and because the tectonic history of the area since sample deposition is simple, resolution of the temperature history is high. The maximum temperature experienced by the sampled bed is between 16°-21°C and occurs at 96 Ma; temperatures since the Cretaceous have dropped in spite of continued pelagic sediment deposition because heat flow has continued to decay exponentially and bottom-water temperatures have dropped. Fission tracks observed within apatite grains from the sampled bed are 14.6 +/- 0.1 µm (1 sigma) long. Given the proposed temperature history of the samples, one unpublished and three published models of fission track annealing predict mean track lengths from 14.8 to 15.9 µm. These models require temperatures as much as 40°C higher than the calculated paleotemperature maximum of the sampled bed to produce the same degree of track annealing. Measured and predicted values are different because annealing models are based on extrapolation of high temperature laboratory data to geologic times. The model that makes the closest prediction is based on the greatest number of experiments performed at low temperature and on an apatite having composition closest to that of the core samples.

Temperaturas óptimas para resembrar especies mesotérmicas sobre céspedes de Cynodon dactylon en el centro-sur de la provincia de Córdoba, Argentina

Los objetivos fueron determinar temperaturas medias de suelo (TMS) y mínimas de aire (TMA) adecuadas para realizar resiembras otoñales; evaluar la tasa de crecimiento (TCC) de Cynodon dactylon (Bermuda) que minimice la competencia con la especie resembrada y el comportamiento de distintas especies mesotérmicas en el centro-sur de la provincia de Córdoba. Se resembró durante 2010 y 2011, en un diseño de parcelas divididas con cinco fechas de siembra (FS) quincenalmente desde principios de marzo, con tres genotipos: Lolium multiflorum cv Axcella, L. perenne y L. perenne cv Excel I. Las temperaturas se midieron entre principios de marzo y hasta que la bermuda entró en dormición, calculando TMA y TMS. En las subparcelas resembradas se registraron calidad visual y cobertura total; además, en la bermuda se calculó la TCC. Las resiembras que lograron valores más altos de calidad visual, cobertura y bajas TCC de la Bermuda, se dieron con TMS entre 18 - 21°C y TMA entre 11,5 - 15,5°C. De acuerdo con los valores medios normales de la región centro-sur de Córdoba, las temperaturas óptimas se observan entre la segunda década de marzo y primera de abril. Los tres genotipos tuvieron comportamientos similares independientemente de la FS utilizada.

Zeolite and silica diagenesis and sandstone petrography at DSDP Sites 57-438 and 57-439

We detected authigenic clinoptilolites in two core samples of tuffaceous, siliceous mudstone in the lower Miocene section of Hole 439. They occur as prismatic and tabular crystals as long as 0.03 mm in various voids of dissolved glass shards, radiolarian shells, calcareous foraminifers, and calcareous algae. They are high in alkalies, especially Na, and in silica varieties. There is a slight difference in composition among them. The Si : (Al+ Fe3+) ratio is highest (4.65) in radiolarian voids, intermediate (4.34) in dissolved glass voids, and lowest (4.26) in voids of calcareous organisms. This difference corresponds to the association of authigenic silica minerals revealed by the scanning electron microscope: There are abundant opal-CT lepispheres in radiolarian voids, low cristobalite and some lepispheres in dissolved glass voids, and a lack of silica minerals in the voids of calcareous organisms. Although it contains some silica from biogenic opal and alkalies from trapped sea water, clinoptilolite derives principally from dissolved glass. Although they are scattered in core samples of Quaternary through lower Miocene diatomaceous and siliceous deposits, acidic glass fragments react with interstitial water to form clinoptilolite only at a sub-bottom depth of 935 meters at approximately 25°C. Analcimes occur in sand-sized clasts of altered acidic vitric tuff in the uppermost Oligocene sandstones. The analcimic tuff clasts were probably reworked from the Upper Cretaceous terrain adjacent to Site 439. Low cristobalite and opal-CT are found in tuffaceous, siliceous mudstone of the middle and lower Miocene sections at Sites 438 and 439. Low cristobalite derives from acidic volcanic glass and opal-CT from biogenic silica. Both siliceous organic remains and acidic glass fragments occur in sediments from the Quaternary through lower Miocene sections. However, the shallowest occurrence is at 700 meters subbottom in Hole 438A, where temperature is estimated to be 21°C. The d(101) spacing of opal-CT varies from 4.09 to 4.11 Å and that of low cristobalite from 4.04 to 4.06 Å. Some opal-CT lepispheres are precipitated onto clinoptilolites in the voids of radiolarian shells at a sub-bottom depth of 950 meters in Hole 439. Sandstone interlaminated with Upper Cretaceous shale is chlorite- calcite cemented and feldspathic. Sandstones in the uppermost Oligocene section are lithic graywacke and consist of large amounts of lithic clasts grouped into older sedimentary and weakly metamorphosed rocks, younger sedimentary rocks, and acidic volcanic rocks. The acidic volcanic clasts probably originated from the volcanic high, which supplied the basal conglomerate with dacite gravels. The older sedimentary and weakly metamorphosed rocks and green rock correspond to the lithologies of the lower Mesozoic to upper Paleozoic Sorachi Group, including the chert, limestone, and slate in south-central Hokkaido. However, the angular shape and coarseness of the clasts and the abundance of carbonate rock fragments indicate a nearby provenance, which is probably the southern offshore extension of the Sorachi Group. The younger sedimentary rocks, including mudstone, carbonaceous shale, and analcime-bearing tuff, correspond to the lithologies of the Upper Cretaceous strata in south-central Hokkaido. Their clasts were reworked from the southern offshore extension of the strata. Because of the discontinuity of the zeolite zoning due to burial diagenesis, an overburden several kilometers thick must have been denuded before the deposition of sediments in the early Oligocene.

Growth rates of late Miocene corals from Crete (Greece)

Modern scleractinian corals are classical components of marine shallow warm water ecosystems. Their occurrence and diversity patterns in the geological record have been widely used to infer past climates and environmental conditions. Coral skeletal composition data reflecting the nature of the coral environment are often affected by diagenetic alteration. Ghost structures of annual growth rhythms are, however, often well preserved in the transformed skeleton. We show that these relicts represent a valuable source of information on growth conditions of fossil corals. Annual growth bands were measured in massive hemispherical Porites of late Miocene age from the island of Crete (Greece) that were found in patch reefs and level bottom associations of attached mixed clastic environments as well as isolated carbonate environments. The Miocene corals grew slowly, about 2-4 mm/yr, compatible with present-day Porites from high-latitude reefs. Slow annual growth of the Miocene corals is in good agreement with the position of Crete at the margin of the Miocene reef belt. Within a given time slice, extension rates were lowest in level bottom environments and highest in attached inshore reef systems. Because sea surface temperatures (SSTs) can be expected to be uniform within a time slice, spatial variations in extension rates must reflect local variations in light levels (low in the level bottom communities) and nutrients (high in the attached reef systems). During the late Miocene (Tortonian-early Messinian), maximum linear extension rates remained remarkably constant within seven chronostratigraphic units, and if the relationship of SSTs and annual growth rates observed for modern massive Indo-Pacific Porites spp. applies to the Neogene, minimum (winter) SSTs were 20°-21°C. Although our paleoclimatic record has a low resolution, it fits the trends revealed by global data sets. In the near future we expect this new and easy to use Porites thermometer to add important new information to our understanding of Neogene climate.

Enzyme activity, body measures and heart mass of Sepia officinalis sampled in the English Channel and Adriatic Sea

In the eurythermal cuttlefish Sepia officinalis, performance depends on hearts that ensure systemic oxygen supply over a broad range of temperatures. We therefore aimed to identify adjustments in energetic cardiac capacity and underlying mitochondrial function supporting thermal acclimation and adaptation that could be crucial for the cuttlefish's competitive success in variable environments. Two genetically distinct cuttlefish populations were acclimated to 11, 16 and 21°C. Subsequently, skinned and permeabilised heart fibres were used to assess mitochondrial functioning by means of high-resolution respirometry and a substrate-inhibitor protocol, followed by measurements of cardiac citrate synthase and cytosolic enzyme activities. Temperate English Channel cuttlefish had lower mitochondrial capacities but larger hearts than subtropical Adriatic cuttlefish. Warm acclimation to 21°C decreased mitochondrial complex I activity in Adriatic cuttlefish and increased complex IV activity in English Channel cuttlefish. However, compensation of mitochondrial capacities did not occur during cold acclimation to 11°C. In systemic hearts, the thermal sensitivity of mitochondrial substrate oxidation was high for proline and pyruvate but low for succinate. Oxygen efficiency of catabolism rose as temperature changed from 11 to 21°C via shifts to oxygen-conserving oxidation of proline and pyruvate and via reduced relative proton leak. The changes observed for substrate oxidation, mitochondrial complexes, relative proton leak and heart mass improve energetic efficiency and essentially seem to extend tolerance to high temperatures and reduce associated tissue hypoxia. We conclude that cuttlefish sustain cardiac performance and, thus, systemic oxygen delivery over short- and long-term changes of temperature and environmental conditions by multiple adjustments in cellular and mitochondrial energetics.

Abundance and biomass of phytoplankton in the Black Sea near Gelendzhik in 2002-2005

It is shown that in 2002-2005 mass development of coccolithofore Emiliania huxleyi on the Gelendzhik shelf (northeast Black Sea) occurred annually and in May-June its abundance reached 1500000 cells/l. In 2004-2005 bloom of E. huxleyi was accompanied by mass development of diatom alga Chaetoceros subtilis var. abnormis f. simplex (600000-900000 cells/l). For the first time it was registered as a dominating form of Black Sea phytoplankton. Small flagellates and picoplankton algae played a noticeable role in phytoplankton throughout the entire period of the studies. Meanwhile in the early summer period the bulk of biomass consisted of coccolithophores (50-60%), while in the late summer period diatomaceous algae dominated (50-70%). Among ecological factors that favor coccolithophore development one may note microstratification of the upper mixed layer at a high illumination level and high temperature in surface waters (18-21°C). Terrigenous runoff during the rainy period had a negative effect on E. huxleyi development, while storms dispersed the population over the upper mixed layer. A wind-induced near-shore upwelling stimulated development of diatoms.

Limited effects of increased CO2 and temperature on metal and radionuclide bioaccumulation in a sessile invertebrate, the oyster Crassostrea gigas

This study investigated the combined effects of reduced pH and increased temperature on the capacities of the Pacific cupped oyster Crassostrea gigas to bioconcentrate radionuclide and metals. Oysters were exposed to dissolved radiotracers (110mAg, 241Am, 109Cd,57Co,54Mn, and 65Zn) at three pH (7.5, 7.8, 8.1) and two temperatures (21 and 24°C) under controlled laboratory conditions. Although calcifying organisms are recognized as particularly vulnerable to ocean acidification, the oyster did not accumulate differently the studied metals when exposed under the different pH conditions. However, temperature alone or in combination with pH somewhat altered the bioaccumulation of the studied elements. At pH 7.5, Cd was accumulated with an uptake rate constant twofold higher at 24°C than 21°C. Bioaccumulation of Mn was significantly affected by an interactive effect between seawater pH and temperature, with a decreased uptake rate at pH 7.5 when temperature increased (27 ± 1 vs. 17 ± 1 /day at 21 and 24°C, respectively). Retention of Co and Mn tended also to decrease at the same pH with decreasing temperature. Neither pH nor temperature affected strongly the elements distribution between shell and soft tissues. Significant effects of pH were found on the bioaccessibility of Mn, Zn, and 241Am during experimental in vitro simulation of human digestion.

Influencia de la información termográfica infrarroja en el protocolo de prevención de lesiones de un equipo de fútbol profesional español

El fútbol es un deporte en cuya práctica existe una alta incidencia de lesión. Además, en el ámbito profesional las lesiones suponen un duro proceso de recuperación para el futbolista, una reducción del rendimiento deportivo para éste y para el equipo, y unos grandes costes económicos para el club. Dentro de esta problemática, la bibliografía consultada concluye que en las pretemporadas se produce una mayor incidencia de lesión por sobrecarga, es decir, sin contacto; un tipo de lesiones que está a nuestro alcance poder prevenir. Por ello, consideramos importante el conocer y desarrollar métodos, herramientas y principios para obtener programas preventivos efectivos, que reduzcan las elevadas cifras de incidencia de lesión mostradas por la literatura. El presente estudio observa y registra las lesiones, a través del cuestionario F-MARC, de un equipo profesional de fútbol de la Liga Española durante las pretemporadas 2008 (n=24) y 2009 (n=24). Además, durante la pretemporada 2009 se aplicó la termografía infrarroja para adquirir información sobre la asimilación de la carga de entrenamiento por parte de los jugadores, y dicha información se utilizarón para mejorar las tomas de decisiones de protocolos post-ejercicio específicos en prevención de lesiones, los cuales fueron los mismos que se utilizaron previamente en la pretemporada 2008. El estudio tiene un diseño con características pre-post sin grupo de control. Es un estudio longitudinal donde, tras un registro inicial de lesiones en la pretemporada 2008, los sujetos fueron expuestos a la variable independiente, utilización de la termografía infrarroja, en el protocolo de prevención de lesiones durante la pretemporada 2009. Los resultados de este trabajo muestran una reducción significativa de hasta el 60% en la frecuencia de lesión durante la pretemporada 2009, y un descenso de la incidencia de lesión total que pasa de 8,3 lesiones por cada 1000 horas de exposición en 2008 a 3,4 en 2009. Con ello, la probabilidad de lesión se redujo considerablemente pasando de un 85% de los jugadores lesionados en 2008 a un 26% en 2009; además, las lesiones de carácter muscular descendieron en 2009 un 70% con respecto al 2008, y los días de baja que causaron todas las lesiones pasó a reducirse un 91,8% en la pretemporada 2009. Por otro lado, el perfil térmico de los jugadores en función de su lateralidad y dominancia, guarda una gran similitud en sus temperaturas, tanto medias como máximas, con temperaturas más elevadas en la zona corporal lumbar y poplítea, y con temperaturas más bajas en tobillos y rodillas. Todas las zonas corporales estudiadas, exceptuando el tobillo (p<0,05), no presentan diferencias significativas entre ambos hemicuerpos, estableciendo un promedio de diferencia entre ambos lados de 0,06±0,16 ºC. Teniendo en cuenta estos resultados, consideramos el límite superior de normalidad de asimetría térmica bilateral en 0,3ºC para todas las zonas corporales estudiadas del miembro inferior exceptuando los tobillos. El parámetro ambiental que más relación tiene con la temperatura registrada por la cámara termográfica es la temperatura de la sala con un coeficiente de correlación cercano a r=1,00, seguido de la presión atmosférica con un coeficiente de correlación cercano r=0,50, y, por último, la humedad que no guarda ningún tipo de relación con la temperatura registrada en cada zona corporal en el rango de valores considerados en el estudio. Por otro lado, los resultados del ANOVA de un factor nos indican que existen diferencias de medias entre los tres grupos formados de temperatura ambiente de sala (1º=18º-21ºC, 2º=22º-24ºC y 3º=25º-31ºC). Además, los resultados de la prueba HSD de Tukey nos indican que existen diferencias entre cada uno de los grupos en todas las zonas corporales estudiadas exceptuando los tobillos. Por último, se propone la ecuación; TC-estándar = TC-real – [0,184 * (TS – 21ºC)] para predecir la influencia de la temperatura ambiente sobre la temperatura registrada por la cámara termográfica. Para concluir, tras los resultados obtenidos, podemos afirmar que la aplicación de un protocolo post-ejercicio de prevención de lesiones basado en la información adquirida a través de valoraciones con termografía infrarroja reduce la incidencia de lesión en el grupo de futbolistas profesionales estudiado. Tenemos que ser conscientes que nos encontramos ante un estudio de campo, donde existen muchos factores que han podido influenciar en los resultados y que son difíciles de controlar. Por lo tanto, debemos ser cautos y concluir que la información adquirida de las evaluaciones termográficas ha sido uno de los aspectos que ayudó a la reducción significativa de la incidencia de lesión en la pretemporada 2009 en el equipo de fútbol profesional español de este estudio, pero que seguramente hayan podido existir otros factores que también hayan favorecido este hecho. ABSTRACT Soccer is a sport with a high incidence of injury. Moreover, in professional soccer injuries lead to a tough recovery process for the players, a reduction athletic performance for them and for their teams, and large economic costs for the club. In this issue, the literature concludes that in the preseason a greater incidence of overuse injury occurs (ie, without contact), and this is a type of injury that we can prevent. Therefore, we consider that it is important to know and develop methods, tools and principles to obtain effective preventive programs that reduce the high injury incidence figures shown in the literature. This study observed and recorded injuries, through the questionnaire F-MARC, from a professional soccer team in the Spanish league during the preseason 2008 (n = 24) and 2009 (n = 24). Moreover, during the 2009 preseason infrared thermography was applied to acquire information about the assimilation of the training load by the players, and this information was used to improve the decision making in the specific post-exercise injury prevention protocols, which were the same used in the previous season 2008. The study had a pre-post design without control group. Is a longitudinal study where, after an initial registration of injuries in the 2008 preseason, subjects were exposed to the independent variable, using infrared thermography, included in the protocol for injury prevention during the 2009 preseason. The results of this study show a significant reduction of up to 60% in the frequency of injury during the 2009 preseason, and a decrease in total injury incidence passing from 8.3 injuries per 1000 hours of exposure in 2008 to 3.4 in 2008. With this, the likelihood of injury decreased significantly from 85% of the players injuried in 2008 to 26% in 2009, also muscle injuries in 2009 fell 70% compared to 2008, and sick leave days that caused by all the injuries happened were reduced a 91.8% in the 2009 preseason. On the other hand, the thermal profile of the players according to their laterality and dominance, is quiet similar in their temperatures, both average and maximum values, with an estimated average of the highest temperatures in the lower back and popliteal areas in the back areas, and lower temperatures in the ankles and knees. All body areas studied, except for the ankle (p <0.05), had no significant differences between both sides of the body, establishing an average difference between both sides of 0.06 ± 0.16 °C. Given these results, we consider the upper limit of normal bilateral thermal asymmetry 0.3 °C for all body areas studied in the lower limb except for ankles. The environmental parameter higher related with temperature recorded by the camera is the temperature of the room with a correlation coefficient close to r = 1.00, followed by atmospheric pressure with a correlation coefficient near r = 0.50, and finally, the humidity that, in the range of values considered in the study, it is not related with temperature in each body area. On the other hand, the results of one-way ANOVA indicate that there are differences between the three temperature of the room groups (1 ° = 18-21 °C, 2 º = 22-24 ºC and 3 º = 25-31 ºC). Moreover, the results of the Tukey HSD test indicate that there are differences between each of the groups for all body areas studied except the ankles. Finally, we propose the equation TC-standard = TC-real – [0,184 * (TS – 21ºC)] to predict the influence of temperature on the temperature recorded by the thermographic camera. In conclusion, we can say from our results that the implementation of a post-exercise injury prevention protocol based on information from assessments with infrared thermography reduces the incidence of injury in professional soccer players. We must be aware that we are facing a field study, where there are many factors that could influence the results and they are difficult to control. Therefore, we must be cautious and conclude that the information acquired from the thermographic evaluation has been one of the aspects that helped to significantly reduce the incidence of injury in the preseason 2009 in the Spanish professional football team, but probably they could exist other factors with a positive effect on the reduction of the injury rates.

Influence of climate change on the flowering of temperate fruit trees

It is well known that winter chilling is necessary for the flowering of temperate trees. The chilling requirement is a criterion for choosing a species or variety at a given location. Also chemistry products can be used for reducing the chilling-hours needs but make our production more expensive. This study first analysed the observed values of chilling hours for some representative agricultural locations in Spain for the last three decades and their projected changes under climate change scenarios. Usually the chilling is measured and calculated as chilling-hours, and different methods have been used to calculate them (e.g. Richarson et al., 1974 among others) according to the species considered. For our objective North Carolina method (Shaltout and Unrath, 1983) was applied for apples, Utah method (Richardson et al. 1974) for peach and grapevine and the approach used by De Melo-Abreu et al. (2004) for olive trees. The influence of climate change in temperate trees was studied by calculating projections of chilling-hours with climate data from Regional Climate Models (RCMs) at high resolution (25 km) from the European Project ENSEMBLES (http://www.ensembles-eu.org/). These projections will allow for analysing the modelled variations of chill-hours between 2nd half of 20C and 1st half of 21C at the study locations.