Electrocatalytic evaluation of DNA damage by superoxide radical for antioxidant capacity assessment

The integrity of DNA purine bases was herein used to evaluate the antioxidant capacity. Unlike other DNA-based antioxidant sensors reported so far, the damaging agent chosen was the O 2 radical enzymatically generated by the xanthine/xanthine oxidase system. An adenine-rich oligonucleotide was adsorbed on carbon paste electrodes and subjected to radical damage in the presence/absence of several antioxidant compounds. As a result, partial damage on DNA was observed. A minor product of the radical oxidation was identified by cyclic voltammetry as a diimine adenine derivative also formed during the electrochemical oxidation of adenine/guanine bases. The protective efficiency of several antioxidant compounds was evaluated after electrochemical oxidation of the remaining unoxidized adenine bases, by measuring the electrocatalytic current of NADH mediated by the adsorbed catalyst species generated. A comparison between O 2 and OH radicals as a source of DNA lesions and the scavenging efficiency of various antioxidant compounds against both of them is discussed. Finally, the antioxidant capacity of beverages was evaluated and compared with the results obtained with an optical method.

Divergent and convergent margins in the north-western Alps - Confrontation to actualistic models

Divergent and convergent margins actualistic models are reviewed and applied to the history of the western Alps. Tethyan rifting history and geometry are analyzed: the northern European margin is considered as an upper plate whereas the southern Apulian margin is a lower plate; the Breche basin is regarded as the former break-away trough; the internal Brianconnais domain represents the northern rift shoulder whilst the more external domains are regarded as the infill of a complex rim basin locally affected by important extension (Valaisan and Vocontain trough). The Schistes lustres and ophiolites of the Tsate nappe are compared to an accretionary prism: the imbrication of this nappe elements is regarded as a direct consequence of the accretionary phenomena already active in early Cretaceous; the Gets/Simme complex could orginate from a more internal part of the accretionary prism. Some eclogitic basements represent the former Apulian margin substratum (Sesia) others (Mont-Rose) are interpreted as the former edge of the European margin. The history of the closing Tethyan domain is analyzed and the remaining problems concerning the cinematics, the presence/absence of a volcanic arc and the eoalpine metamorphism are discussed.

Espace urbain et identité : l’imaginaire de la ville comme symptôme de la crise identitaire dans l’oeuvre d’Orhan Pamuk

Istanbul est pour Pamuk ce que Paris est pour Baudelaire : une source inépuisable d’inspiration et de spleen. Or, si le poète est davantage conscient de ses états d’âme, le romancier turc le plus lu des deux côtés du Bosphore ne sait pas toujours que tout discours sur le monde extérieur est un discours sur lui-même. Dans un premier temps, il se complait dans l’hüzün, ce sentiment collectif et généralisé de mélancolie, apparemment intrinsèque à la ville et ses ruines, traces tangibles de la décadence d’un grand empire dont les héritiers peinent à se relever. Il n’en est pourtant rien, car, au fur à mesure que Pamuk suit les traces des écrivains et artistes étrangers de passage à Istanbul, il s’aperçoit que l’apparente mélancolie des ruines n’est qu’une strate parmi d’autres, c’est-à-dire glissante, malléable et fluide, tout dépend de l’emplacement et du point de vue de l’observateur, dans une ville palimpseste qui cache dans ses entrailles toutes les altérités. En suivant les traces de l’altérité, Pamuk découvre la nature hétérogène de sa ville et de lui-même et s’aperçoit que la mélancolie collective est fabriquée de toutes pièces par un certain récit socio-politique et une certaine classe sociale. En effet, c’est en traquant les reflets de son double que le romancier prend soudainement conscience du caractère fuyant de sa propre subjectivité, mais aussi de celui du monde et des autres. Si tel est le cas, l’espace urbain qui préoccupe et obsède Pamuk n’est qu’un reflet de son esprit et l’accès à la présence pleine s’avère une illusion. Comme si, l’inquiétante étrangeté de son inconscient, en lui dévoilant le côté insaisissable du monde et du soi, l’encourageait à remettre en cause un certain nombre d’opinions acquises, non seulement à l’intérieur de sa propre culture, mais aussi dans la culture de son double européen. Car si tout est fluide et malléable, il n’y a pas raison de ne pas tout questionner, incluant la tradition et la politique, cette dernière faisant de lui, « une personne bien plus politique, sérieuse et responsable que je ne le suis et ne souhaitais l’être ». Ainsi, Istanbul, souvenir d’une ville questionne le rapport entre la subjectivité et les strates hétérogènes d’Istanbul, pour aboutir à un constat déconstructiviste : tout n’est que bricolage et substitut du sens là où il brille par son absence. S’il brille par son absence, il en est de même loin d’Istanbul, dans une maison périphérique appelée La Maison du Silence à l’intérieur de laquelle les personnages soliloques et par moments muets, se questionnent sur le rapport entre la tradition et la modernité, le centre et la périphérie, l’Occident et l’Orient, sans oublier le caractère destructeur et éphémère du temps, mais aussi de l’espace. Et enfin, Le Musée de l’Innoncence, cette oeuvre magistrale où l’amour joue (en apparence seulement) le rôle principal, n’est en fait que l’étrange aboutissement de la quête obsessessive et narcissique du personnage principal vers un autre espace-temps, quelque part entre la réalité et la fiction, entre l’Est et l’Ouest, entre la tradition et la modernité, cet entre-deux qui campe indéniablement Pamuk parmi les meilleurs romanciers postmodernes de notre époque. Or, pour y parvenir, il faut au préalable un bouc-émissaire qui, dans le cas de Pamuk, représente presque toujours la figure du féminin.

Étude pangénomique de la variabilité dans le nombre de copies liée à l’hypertension artérielle et ses anomalies métaboliques associées

L’hypertension artérielle essentielle (HTA) est une pathologie complexe, multifactorielle et à forte composante génétique. L’impact de la variabilité dans le nombre de copies sur l’HTA est encore peu connu. Nous envisagions que des variants dans le nombre de copies (CNVs) communs pourraient augmenter ou diminuer le risque pour l’HTA. Nous avons exploré cette hypothèse en réalisant des associations pangénomiques de CNVs avec l’HTA et avec l’HTA et le diabète de type 2 (DT2), chez 21 familles du Saguenay-Lac-St-Jean (SLSJ) caractérisées par un développement précoce de l’HTA et de la dyslipidémie. Pour la réplication, nous disposions, d’une part, de 3349 sujets diabétiques de la cohorte ADVANCE sélectionnés pour des complications vasculaires. D’autre part, de 187 sujets de la cohorte Tchèque Post-MONICA (CTPM), choisis selon la présence/absence d’albuminurie et/ou de syndrome métabolique. Finalement, 134 sujets de la cohorte CARTaGENE ont été analysés pour la validation fonctionnelle. Nous avons détecté deux nouveaux loci, régions de CNVs (CNVRs) à effets quantitatifs sur 17q21.31, associés à l’hypertension et au DT2 chez les sujets SLSJ et associés à l’hypertension chez les diabétiques ADVANCE. Un modèle statistique incluant les deux variants a permis de souligner le rôle essentiel du locus CNVR1 sur l’insulino-résistance, la précocité et la durée du diabète, ainsi que sur le risque cardiovasculaire. CNVR1 régule l’expression du pseudogène LOC644172 dont le dosage est associé à la prévalence de l’HTA, du DT2 et plus particulièrement au risque cardiovasculaire et à l’âge vasculaire (P<2×10-16). Nos résultats suggèrent que les porteurs de la duplication au locus CNVR1 développent précocement une anomalie de la fonction bêta pancréatique et de l’insulino-résistance, dues à un dosage élevé de LOC644172 qui perturberait, en retour, la régulation du gène paralogue fonctionnel, MAPK8IP1. Nous avons également avons identifié six CNVRs hautement hérités et associés à l'HTA chez les sujets SLSJ. Le score des effets combinés de ces CNVRs est apparu positivement et étroitement relié à la prévalence de l’HTA (P=2×10-10) et à l’âge de diagnostic de l’HTA. Dans la population SLSJ, le score des effets combinés présente une statistique C, pour l’HTA, de 0.71 et apparaît aussi performant que le score de risque Framingham pour la prédiction de l’HTA chez les moins de 25 ans. Un seul nouveau locus de CNVR sur 19q13.12, où la délétion est associée à un risque pour l’HTA, a été confirmé chez les Caucasiens CTPM. Ce CNVR englobe le gène FFAR3. Chez la souris, il a été démontré que l’action hypotensive du propionate est en partie médiée par Ffar3, à travers une interférence entre la flore intestinale et les systèmes cardiovasculaire et rénal. Les CNVRs identifiées dans cette étude, affectent des gènes ou sont localisées dans des QTLs reliés majoritairement aux réponses inflammatoires et immunitaires, au système rénal ainsi qu’aux lésions/réparations rénales ou à la spéciation. Cette étude suggère que l’étiologie de l’HTA ou de l’HTA associée au DT2 est affectée par des effets additifs ou interactifs de CNVRs.

''L'intervallo perduto'' nella Metropoli Modern

The city is not only a visual environment, but it is also sonorous and therefore the “unintentional hearing which is much more influencing” is involved in an urban space experience just as sight is. Beginning with Assunto’s consideration in Il paesaggio e l’estetica, the analysis we provide cannot avoid outlining the peculiarities of aestetic fruition of the city seen as a space we cross, in which we live and in which we, as a matter of fact, are agent actors. And it is as a consequence of this peculiarity that silence has a leading role in our urban experience. Seen as a presence of itself, it is a positive value especially if we consider that nowadays modernity is expressed through its absence. It is an absence that reaches its climax in the experience of the metropolis. Besides Assunto, there is another witness of this in Simmel’s The Metropolis and Mental Life from which our analysis cannot leave out of consideration. Given that this analysis is a sort of analytic excursus it develops around a well defined barycentre represented by the acoustic experience of the city that focuses on the presence/absence of silence as a result of modernity. Taking the first steps from Assunto and Simmel’s assumptions, this work takes into account the theme of silence in the metropolis and introduces it as a loss of interval and thus uses the analysis carried out by Dorfles in L’intervallo perduto and in Horror Pleni. The metropolitan experience is highly characterized by a sensory disorientation for which we can detect a “strong” starting, the Great War, which shows a caesura that outlines the edges of a new mental world. It shows the systematic use of modern technique, of its sonorous universe and urbanization which appears as a corollary of this picture.

Spatangoid-produced ichnofabrics (Bateig Limestone, Miocene, Spain) and the preservation of spatangoid trace fossils

A spatangoid-produced ichnofabric is described from the Miocene Bateig Limestone, SE Spain. This ichnofabric is characterized by the dominant presence of large meniscate burrows (Bichordites) produced by irregular echinoids. This constitutes an unusual mode of occurrence for spatangoid bioturbation, as their traces are most typically preserved in bases and tops of sandstone event beds. In fact, despite their important role as burrowers in modern settings (that can be extended back to the Early Cretaceous based on their body fossil record), spatangoid trace fossils (Scolicia and Bichordites) are comparatively rare. Several factors play an important role in their preservation: mechanism of burrowing, sediment characteristics, early diagenesis and presence/absence of deep-tier burrowers. Spatangoid-produced ichnofabrics, such as those from the Bateig Limestone, characterize depositional settings with intermittent deposition of event beds where there is an absence of deeper-tier bioturbation. (C) 2008 Elsevier B.V. All rights reserved

Iron Uptake and Homeostasis in Microorganisms

Preface. Iron is considered to be a minor element employed, in a variety of forms, by nearly all living organisms. In some cases, it is utilised in large quantities, for instance for the formation of magnetosomes within magnetotactic bacteria or during use of iron as a respiratory donor or acceptor by iron oxidising or reducing bacteria. However, in most cases the role of iron is restricted to its use as a cofactor or prosthetic group assisting the biological activity of many different types of protein. The key metabolic processes that are dependent on iron as a cofactor are numerous; they include respiration, light harvesting, nitrogen fixation, the Krebs cycle, redox stress resistance, amino acid synthesis and oxygen transport. Indeed, it is clear that Life in its current form would be impossible in the absence of iron. One of the main reasons for the reliance of Life upon this metal is the ability of iron to exist in multiple redox states, in particular the relatively stable ferrous (Fe2+) and ferric (Fe3+) forms. The availability of these stable oxidation states allows iron to engage in redox reactions over a wide range of midpoint potentials, depending on the coordination environment, making it an extremely adaptable mediator of electron exchange processes. Iron is also one of the most common elements within the Earth’s crust (5% abundance) and thus is considered to have been readily available when Life evolved on our early, anaerobic planet. However, as oxygen accumulated (the ‘Great oxidation event’) within the atmosphere some 2.4 billion years ago, and as the oceans became less acidic, the iron within primordial oceans was converted from its soluble reduced form to its weakly-soluble oxidised ferric form, which precipitated (~1.8 billion years ago) to form the ‘banded iron formations’ (BIFs) observed today in Precambrian sedimentary rocks around the world. These BIFs provide a geological record marking a transition point away from the ancient anaerobic world towards modern aerobic Earth. They also indicate a period over which the bio-availability of iron shifted from abundance to limitation, a condition that extends to the modern day. Thus, it is considered likely that the vast majority of extant organisms face the common problem of securing sufficient iron from their environment – a problem that Life on Earth has had to cope with for some 2 billion years. This struggle for iron is exemplified by the competition for this metal amongst co-habiting microorganisms who resort to stealing (pirating) each others iron supplies! The reliance of micro-organisms upon iron can be disadvantageous to them, and to our innate immune system it represents a chink in the microbial armour, offering an opportunity that can be exploited to ward off pathogenic invaders. In order to infect body tissues and cause disease, pathogens must secure all their iron from the host. To fight such infections, the host specifically withdraws available iron through the action of various iron depleting processes (e.g. the release of lactoferrin and lipocalin-2) – this represents an important strategy in our defence against disease. However, pathogens are frequently able to deploy iron acquisition systems that target host iron sources such as transferrin, lactoferrin and hemoproteins, and thus counteract the iron-withdrawal approaches of the host. Inactivation of such host-targeting iron-uptake systems often attenuates the pathogenicity of the invading microbe, illustrating the importance of ‘the battle for iron’ in the infection process. The role of iron sequestration systems in facilitating microbial infections has been a major driving force in research aimed at unravelling the complexities of microbial iron transport processes. But also, the intricacy of such systems offers a challenge that stimulates the curiosity. One such challenge is to understand how balanced levels of free iron within the cytosol are achieved in a way that avoids toxicity whilst providing sufficient levels for metabolic purposes – this is a requirement that all organisms have to meet. Although the systems involved in achieving this balance can be highly variable amongst different microorganisms, the overall strategy is common. On a coarse level, the homeostatic control of cellular iron is maintained through strict control of the uptake, storage and utilisation of available iron, and is co-ordinated by integrated iron-regulatory networks. However, much yet remains to be discovered concerning the fine details of these different iron regulatory processes. As already indicated, perhaps the most difficult task in maintaining iron homeostasis is simply the procurement of sufficient iron from external sources. The importance of this problem is demonstrated by the plethora of distinct iron transporters often found within a single bacterium, each targeting different forms (complex or redox state) of iron or a different environmental condition. Thus, microbes devote considerable cellular resource to securing iron from their surroundings, reflecting how successful acquisition of iron can be crucial in the competition for survival. The aim of this book is provide the reader with an overview of iron transport processes within a range of microorganisms and to provide an indication of how microbial iron levels are controlled. This aim is promoted through the inclusion of expert reviews on several well studied examples that illustrate the current state of play concerning our comprehension of how iron is translocated into the bacterial (or fungal) cell and how iron homeostasis is controlled within microbes. The first two chapters (1-2) consider the general properties of microbial iron-chelating compounds (known as ‘siderophores’), and the mechanisms used by bacteria to acquire haem and utilise it as an iron source. The following twelve chapters (3-14) focus on specific types of microorganism that are of key interest, covering both an array of pathogens for humans, animals and plants (e.g. species of Bordetella, Shigella, , Erwinia, Vibrio, Aeromonas, Francisella, Campylobacter and Staphylococci, and EHEC) as well as a number of prominent non-pathogens (e.g. the rhizobia, E. coli K-12, Bacteroides spp., cyanobacteria, Bacillus spp. and yeasts). The chapters relay the common themes in microbial iron uptake approaches (e.g. the use of siderophores, TonB-dependent transporters, and ABC transport systems), but also highlight many distinctions (such as use of different types iron regulator and the impact of the presence/absence of a cell wall) in the strategies employed. We hope that those both within and outside the field will find this book useful, stimulating and interesting. We intend that it will provide a source for reference that will assist relevant researchers and provide an entry point for those initiating their studies within this subject. Finally, it is important that we acknowledge and thank wholeheartedly the many contributors who have provided the 14 excellent chapters from which this book is composed. Without their considerable efforts, this book, and the understanding that it relays, would not have been possible. Simon C Andrews and Pierre Cornelis

Bone morphogenetic protein-6 enhances gonadotrophin-dependent progesterone and inhibin secretion and expression of rnRNA transcripts encoding gonadotrophin receptors and inhibin/activin subunits in chicken granulosa cells

The aims were to examine ovarian expression of bone morphogenetic protein (BMP) ligands/receptor mRNAs in the chicken and to test the hypothesis that theca-derived BMP(s) modulates granulosa cell function in a paracrine manner. RT-PCR revealed expression of multiple BMPs in granulosa and theca cells from prehierarchical and preovulatory follicles with greater expression in theca cells; both cell types expressed BMP receptors-1A, -1B and -II consistent with tissue responsiveness. Preovulatory granulosa cells F1, F2 and F3/4) were cultured with BMP-6 (expressed by theca but not granulosa) in the presence/absence of LH, FSH or 8-Br-cAMP. RMP-6 increased 'basal' and gonadotrophin-induced inhibin-A and progesterone secretion by each cell type but did not enhance the effect of 8-Br-cAMP. This indicates that the observed synergism between BMP-6 and gonadotrophin might involve BMP-induced up-regulation of gonadotrophin receptors. In support of this, BMP-6 alone increased LH-receptor (LHR) mRNA in F1 cells and FSH-receptor (FSHR) mRNA in F1, F2 and F3/4 cells. RMP-6 also enhanced LH/FSH-induced LHR transcript amount in each cell type but did not raise FSHR transcript amounts above those induced by BMP-6 alone. To further explore BMP6 action on inhibin-A secretion, we quantified inhibin/activin subunits (alpha, beta(A), beta(B)) mRNAs. Consistent with its effect on inhibin-A secretion, BMP-6 enhanced 'basal' expression of alpha- and beta(A)-Subunit mRNA in F1, F2 and F3/4 cells, and beta(B)-subunit mRNA in F3/4 cells. BMP-6 markedly enhanced FSH/LH-induced expression of alpha-subunit in all follicles and FSH-induced beta(A)-subunit in F2 and F3/4 follicles but not in F1 follicles. Neither BMP-6 alone, nor FSH/LH alone, affected 'basal' OB mRNA abundance. However, co-treatment with gonadotrophin and BMP-6 greatly increased beta(B)-subunit expression, the response being lowest in F1 follicles and greatest in F3/4 follicles. Collectively, these results support the hypothesis that intra-ovarian OMPs of thecal origin have a paracrine role in modulating granulosa cell function in the chicken in a preovulatory stage-dependent manner.

The impact of sarcoptic mange Sarcoptes scabiei on the British fox Vulpes vulpes population

1. Disease epizootics can significantly influence host population dynamics and the structure and functioning of ecological communities. Sarcoptic mange Sarcoptes scabiei has dramatically reduced red fox populations Vulpes vulpes in several countries, including Britain, although impacts on demographic processes are poorly understood. We review the literature on the impact of mange on red fox populations, assess its current distribution in Britain through a questionnaire survey and present new data on resultant demographic changes in foxes in Bristol, UK. 2. A mange epizootic in Sweden spread across the entire country in < 10 years resulting in a decline in fox density of up to 95%; density remained lowered for 15–20 years. In Spain, mange has been enzootic for > 75 years and is widely distributed; mange presence was negatively correlated with habitat quality. 3. Localized outbreaks have occurred sporadically in Britain during the last 100 years. The most recent large-scale outbreak arose in the 1990s, although mange has been present in south London and surrounding environs since the 1940s. The questionnaire survey indicated that mange was broadly distributed across Britain, but areas of perceived high prevalence (> 50% affected) were mainly in central and southern England. Habitat type did not significantly affect the presence/absence of mange or perceived prevalence rates. Subjective assessments suggested that populations take 15–20 years to recover. 4. Mange appeared in Bristol's foxes in 1994. During the epizootic phase (1994–95), mange spread through the city at a rate of 0.6–0.9 km/month, with a rise in infection in domestic dogs Canis familiaris c. 1–2 months later. Juvenile and adult fox mortality increased and the proportion of females that reproduced declined but litter size was unaffected. Population density declined by > 95%. 5. In the enzootic phase (1996–present), mange was the most significant mortality factor. Juvenile mortality was significantly higher than in the pre-mange period, and the number of juveniles classified as dispersers declined. Mange infection reduced the reproductive potential of males and females: females with advanced mange did not breed; severely infected males failed to undergo spermatogenesis. In 2004, Bristol fox population density was only 15% of that in 1994.

Influence of gut morphology on passive transport of freshwater bryozoans by waterfowl in Donana (southwestern Spain)

Waterbirds have been proposed as important vectors for the passive dispersal of those aquatic invertebrates and plants that lack a capacity for active dispersal between isolated water bodies. We analysed the frequency of internal transport of bryozoan propagules (statoblasts) by waterbirds in Donana, Spain, by examining their presence in the intestines and ceca of dead birds and analysing the role of different aspects of gut characteristics in explaining variation in the presence/absence and abundance of statoblasts. Of the 228 samples examined, 7.9% presented intact statoblasts of Plumatella fungosa (Pallas, 1768), Plumatella emarginata Allman, 1844, and two unidentified Plumatella species. For a given bird species, individuals with heavier gizzards and shorter ceca had a lower incidence and abundance of statoblasts in the lower gut. Grit mass and intestine length were unrelated to the presence or abundance of statoblasts. Our results suggest that waterbirds frequently transport bryozoans on a local scale, with lighter gizzards and longer ceca favouring such transport. Lighter gizzards are likely to destroy fewer propagules before they reach the lower gut. Species and individuals with longer ceca are particularly good candidates for long-distance dispersal of bryozoans, given the longer passage time of propagules that enter the ceca.

Model inter-comparison between statistical and dynamic model assessments of the long-term stability of blanket peat in Great Britain (1940-2099)

We compared output from 3 dynamic process-based models (DMs: ECOSSE, MILLENNIA and the Durham Carbon Model) and 9 bioclimatic envelope models (BCEMs; including BBOG ensemble and PEATSTASH) ranging from simple threshold to semi-process-based models. Model simulations were run at 4 British peatland sites using historical climate data and climate projections under a medium (A1B) emissions scenario from the 11-RCM (regional climate model) ensemble underpinning UKCP09. The models showed that blanket peatlands are vulnerable to projected climate change; however, predictions varied between models as well as between sites. All BCEMs predicted a shift from presence to absence of a climate associated with blanket peat, where the sites with the lowest total annual precipitation were closest to the presence/absence threshold. DMs showed a more variable response. ECOSSE predicted a decline in net C sink and shift to net C source by the end of this century. The Durham Carbon Model predicted a smaller decline in the net C sink strength, but no shift to net C source. MILLENNIA predicted a slight overall increase in the net C sink. In contrast to the BCEM projections, the DMs predicted that the sites with coolest temperatures and greatest total annual precipitation showed the largest change in carbon sinks. In this model inter-comparison, the greatest variation in model output in response to climate change projections was not between the BCEMs and DMs but between the DMs themselves, because of different approaches to modelling soil organic matter pools and decomposition amongst other processes. The difference in the sign of the response has major implications for future climate feedbacks, climate policy and peatland management. Enhanced data collection, in particular monitoring peatland response to current change, would significantly improve model development and projections of future change.

Solar signal propagation: the role of gravity waves and stratospheric sudden warmings

We use a troposphere‐stratosphere model of intermediate complexity to study the atmospheric response to an idealized solar forcing in the subtropical upper stratosphere during Northern Hemisphere (NH) early winter. We investigate two conditions that could influence poleward and downward propagation of the response: (1) the representation of gravity wave effects and (2) the presence/absence of stratospheric sudden warmings (SSWs). We also investigate how the perturbation influences the timing and frequency of SSWs. Differences in the poleward and downward propagation of the response within the stratosphere are found depending on whether Rayleigh friction (RF) or a gravity wave scheme (GWS) is used to represent gravity wave effects. These differences are likely related to differences in planetary wave activity in the GWS and RF versions, as planetary wave redistribution plays an important role in the downward and poleward propagation of stratospheric signals. There is also remarkable sensitivity in the tropospheric response to the representation of the gravity wave effects. It is most realistic for GWS. Further, tropospheric responses are systematically different dependent on the absence/presence of SSWs. When only years with SSWs are examined, the tropospheric signal appears to have descended from the stratosphere, while the signal in the troposphere appears disconnected from the stratosphere when years with SSWs are excluded. Different troposphere‐stratosphere coupling mechanisms therefore appear to be dominant for years with and without SSWs. The forcing does not affect the timing of SSWs, but does result in a higher occurrence frequency throughout NH winter. Quasi‐Biennial Oscillation effects were not included.

An eight-parent multiparent advanced generation inter-cross population for winter-sown wheat: creation, properties, and validation

MAGIC populations represent one of a new generation of crop genetic mapping resources combining high genetic recombination and diversity. We describe the creation and validation of an eight-parent MAGIC population consisting of 1091 F7 lines of winter-sown wheat (Triticum aestivum L.). Analyses based on genotypes from a 90,000-single nucleotide polymorphism (SNP) array find the population to be well-suited as a platform for fine-mapping quantitative trait loci (QTL) and gene isolation. Patterns of linkage disequilibrium (LD) show the population to be highly recombined; genetic marker diversity among the founders was 74% of that captured in a larger set of 64 wheat varieties, and 54% of SNPs segregating among the 64 lines also segregated among the eight founder lines. In contrast, a commonly used reference bi-parental population had only 54% of the diversity of the 64 varieties with 27% of SNPs segregating. We demonstrate the potential of this MAGIC resource by identifying a highly diagnostic marker for the morphological character "awn presence/absence" and independently validate it in an association-mapping panel. These analyses show this large, diverse, and highly recombined MAGIC population to be a powerful resource for the genetic dissection of target traits in wheat, and it is well-placed to efficiently exploit ongoing advances in phenomics and genomics. Genetic marker and trait data, together with instructions for access to seed, are available at http://www.niab.com/MAGIC/.

Evaluation of the realism of climate reconstruction using the Coexistence Approach with modern pollen samples from the Tibetan Plateau

We apply the Coexistence Approach (CoA) to reconstruct mean annual precipitation (MAP), mean annual temperature (MAT), mean temperature of thewarmestmonth (MTWA) and mean temperature of the coldest month (MTCO) at 44 pollen sites on the Qinghai–Tibetan Plateau. The modern climate ranges of the taxa are obtained (1) from county-level presence/absence data and (2) from data on the optimum and range of each taxon from Lu et al. (2011). The CoA based on the optimumand range data yields better predictions of observed climate parameters at the pollen sites than that based on the county-level data. The presence of arboreal pollen, most of which is derived fromoutside the region, distorts the reconstructions. More reliable reconstructions are obtained using only the non-arboreal component of the pollen assemblages. The root mean-squared error (RMSE) of the MAP reconstructions are smaller than the RMSE of MAT, MTWA and MTCO, suggesting that precipitation gradients are the most important control of vegetation distribution on the Qinghai–Tibetan Plateau. Our results show that CoA could be used to reconstruct past climates in this region, although in areas characterized by open vegetation the most reliable estimates will be obtained by excluding possible arboreal contaminants.

Fine-scale temporal characterization of trends in soil water dissolved organic carbon and potential drivers

Long-term monitoring of surface water quality has shown increasing concentrations of Dissolved Organic Carbon (DOC) across a large part of the Northern Hemisphere. Several drivers have been implicated including climate change, land management change, nitrogen and sulphur deposition and CO2 enrichment. Analysis of stream water data, supported by evidence from laboratory studies, indicates that an effect of declining sulphur deposition on catchment soil chemistry is likely to be the primary mechanism, but there are relatively few long term soil water chemistry records in the UK with which to investigate this, and other, hypotheses directly. In this paper, we assess temporal relationships between soil solution chemistry and parameters that have been argued to regulate DOC production and, using a unique set of co-located measurements of weather and bulk deposition and soil solution chemistry provided by the UK Environmental Change Network and the Intensive Forest Monitoring Level II Network . We used statistical non-linear trend analysis to investigate these relationships at 5 forested and 4 non-forested sites from 1993 to 2011. Most trends in soil solution DOC concentration were found to be non-linear. Significant increases in DOC occurred mostly prior to 2005. The magnitude and sign of the trends was associated qualitatively with changes in acid deposition, the presence/absence of a forest canopy, soil depth and soil properties. The strongest increases in DOC were seen in acidic forest soils and were most clearly linked to declining anthropogenic acid deposition, while DOC trends at some sites with westerly locations appeared to have been influenced by shorter-term hydrological variation. The results indicate that widespread DOC increases in surface waters observed elsewhere, are most likely dominated by enhanced mobilization of DOC in surficial organic horizons, rather than changes in the soil water chemistry of deeper horizons. While trends in DOC concentrations in surface horizons have flattened out in recent years, further increases may be expected as soil chemistry continues to adjust to declining inputs of acidity.