A toxicokinetic model for thiamethoxam in rats: implications for higher-tier risk assessment

Risk assessment for mammals is currently based on external exposure measurements, but effects of toxicants are better correlated with the systemically available dose than with the external administered dose. So for risk assessment of pesticides, toxicokinetics should be interpreted in the context of potential exposure in the field taking account of the timescale of exposure and individual patterns of feeding. Internal concentration is the net result of absorption, distribution, metabolism and excretion (ADME). We present a case study for thiamethoxam to show how data from ADME study on rats can be used to parameterize a body burden model which predicts body residue levels after exposures to LD50 dose either as a bolus or eaten at different feeding rates. Kinetic parameters were determined in male and female rats after an intravenous and oral administration of 14C labelled by fitting one-compartment models to measured pesticide concentrations in blood for each individual separately. The concentration of thiamethoxam in blood over time correlated closely with concentrations in other tissues and so was considered representative of pesticide concentration in the whole body. Body burden model simulations showed that maximum body weight-normalized doses of thiamethoxam were lower if the same external dose was ingested normally than if it was force fed in a single bolus dose. This indicates lower risk to rats through dietary exposure than would be estimated from the bolus LD50. The importance of key questions that should be answered before using the body burden approach in risk assessment, data requirements and assumptions made in this study are discussed in detail.

Middle and Late Pleistocene humid periods recorded in palaeolake deposits of the Nafud desert, Saudi Arabia

Present climate in the Nafud desert of northern Saudi Arabia is hyper-arid and moisture brought by north-westerly winds scarcely reaches the region. The existence of abundant palaeolake sediments provides evidence for a considerably wetter climate in the past. However, the existing chronological framework of these deposits is solely based on radiocarbon dating of questionable reliability, due to potential post-depositional contamination with younger 14C. By using luminescence dating, we show that the lake deposits were not formed between 40 and 20 ka as suggested previously, but approximately ca 410 ka, 320 ka, 200 ka, 125 ka, and 100 ka ago. All of these humid phases are in good agreement with those recorded in lake sediments and speleothems from southern Arabia. Surprisingly, no Holocene lake deposits were identified. Geological characteristics of the deposits and diatom analysis suggest that a single, perennial lake covered the entire south-western Nafud ca 320 ka ago. In contrast, lakes of the 200 ka, 125 ka, and 100 ka humid intervals were smaller and restricted to interdune depressions of a pre-existing dune relief. The concurrent occurrence of humid phases in the Nafud, southern Arabia and the eastern Mediterranean suggests that moisture in northern Arabia originated either from the Mediterranean due to more frequent frontal depression systems or from stronger Indian monsoon circulation, respectively. However, based on previously published climate model simulations and palaecolimate evidence from central Arabia and the Negev desert, we argue that humid climate conditions in the Nafud were probably caused by a stronger African monsoon and a distinct change in zonal atmospheric circulation.

Evidence of resilience to past climate change in Southwest Asia: early farming communities and the 9.2 and 8.2 ka events

Climate change is often cited as a major factor in social change. The so-called 8.2 ka event was one of the most pronounced and abrupt Holocene cold and arid events. The 9.2 ka event was similar, albeit of a smaller magnitude. Both events affected the Northern Hemisphere climate and caused cooling and aridification in Southwest Asia. Yet, the impacts of the 8.2 and 9.2 ka events on early farming communities in this region are not well understood. Current hypotheses for an effect of the 8.2 ka event vary from large-scale site abandonment and migration (including the Neolithisation of Europe) to continuation of occupation and local adaptation, while impacts of the 9.2 ka have not previously been systematically studied. In this paper, we present a thorough assessment of available, quality-checked radiocarbon (14C) dates for sites from Southwest Asia covering the time interval between 9500 and 7500 cal BP, which we interpret in combination with archaeological evidence. In this way, the synchronicity between changes observed in the archaeological record and the rapid climate events is tested. It is shown that there is no evidence for a simultaneous and widespread collapse, large-scale site abandonment, or migration at the time of the events. However, there are indications for local adaptation. We conclude that early farming communities were resilient to the abrupt, severe climate changes at 9250 and 8200 cal BP.

Including an ocean carbon cycle model into iLOVECLIM (v1.0)

The atmospheric carbon dioxide concentration plays a crucial role in the radiative balance and as such has a strong influence on the evolution of climate. Because of the numerous interactions between climate and the carbon cycle, it is necessary to include a model of the carbon cycle within a climate model to understand and simulate past and future changes of the carbon cycle. In particular, natural variations of atmospheric CO2 have happened in the past, while anthropogenic carbon emissions are likely to continue in the future. To study changes of the carbon cycle and climate on timescales of a few hundred to a few thousand years, we have included a simple carbon cycle model into the iLOVECLIM Earth System Model. In this study, we describe the ocean and terrestrial biosphere carbon cycle models and their performance relative to observational data. We focus on the main carbon cycle variables including the carbon isotope ratios δ13C and the Δ14C. We show that the model results are in good agreement with modern observations both at the surface and in the deep ocean for the main variables, in particular phosphates, dissolved inorganic carbon and the carbon isotopes.

Dating WF16: exploring the chronology of a Pre-Pottery Neolithic A settlement in the Southern Levant

A pre-requisite for understanding the transition to the Neolithic in the Levant is the establishment of a robust chronology, most notably for the late Epi-Palaeolithic and Pre-Pottery Neolithic A (PPNA) periods. In this contribution we undertake a dating analysis of the Pre-Pottery Neolithic site of WF16, southern Jordan, drawing on a sample of 46 AMS 14C dates. We utilise Bayesian methods to quantify an old wood effect to provide an offset that we factor into chronological models for a number of individual structures at WF16 and for the settlement as a whole. In doing so we address the influence of slope variations in the calibration curve and expose the significance of sediment and sample redeposition within sites of this nature. We conclude that for the excavated deposits at WF16 human activity is likely to have started by c. 11.84 ka cal bp and lasted for at least c. 1590 years, ceasing by c. 10.24 ka cal bp. This is marked by a particularly intensive period of activity lasting for c. 350 years centred on 11.25 ka cal bp followed by less intensive activity lasting a further c. 880 years. The study reveals the potential of WF16 as a laboratory to explore methodological issues concerning 14C dating of early Neolithic sites in arid, erosional environments.

Strangely dual orbifold equivalence I

In this brief note we prove orbifold equivalence between two potentials described by strangely dual exceptional unimodular singularities of type K14 and Q10 in two different ways. The matrix factorizations proving the orbifold equivalence give rise to equations whose solutions are permuted by Galois groups which differ for different expressions of the same singularity.

CztR, a LysR-Type Transcriptional Regulator Involved in Zinc Homeostasis and Oxidative Stress Defense in Caulobacter crescentus

Caulobacter crescentus is a free-living alphaproteobacterium that has 11 predicted LysR-type transcriptional regulators (LTTRs). Previously, a C. crescentus mutant strain with a mini-Tn5lacZ transposon inserted into a gene encoding an LTTR was isolated; this mutant was sensitive to cadmium. In this work, a mutant strain with a deletion was obtained, and the role of this LTTR (called CztR here) was evaluated. The transcriptional start site of this gene was determined by primer extension analysis, and its promoter was cloned in front of a lacZ reporter gene. beta-Galactosidase activity assays, performed with the wild-type and mutant strains, indicated that this gene is 2-fold induced when cells enter stationary phase and that it is negatively autoregulated. Moreover, this regulator is essential for the expression of the divergent cztA gene at stationary phase, in minimal medium, and in response to zinc depletion. This gene encodes a hypothetical protein containing 10 predicted transmembrane segments, and its expression pattern suggests that it encodes a putative zinc transporter. The cztR strain was also shown to be sensitive to superoxide (generated by paraquat) and to hydrogen peroxide but not to tert-butyl hydroperoxide. The expression of katG and ahpC, but not that of the superoxide dismutase genes, was increased in the cztR mutant. A model is proposed to explain how CztR binding to the divergent regulatory regions could activate cztA expression and repress its own transcription.

Catalase-peroxidase activity is decreased in a Caulobacter crescentus rho mutant

A Caulobacter crescentus rho:Tn5 mutant strain presenting a partially functional transcription termination factor Rho is highly sensitive to hydrogen peroxide in both exponential and stationary phases. The mutant was shown to be permanently under oxidative stress, based on fluorophore oxidation, and also to be sensitive to tert-butyl hydroperoxide and paraquat. However, the results showed that the activities of superoxide dismutases CuZnSOD and FeSOD and the alkylhydroperoxide reductase ahpC mRNA levels in the rho mutant were comparable to the wild-type control in the exponential and stationary phases. In contrast, the KatG catalase activity of the rho mutant strain was drastically decreased and did not show the expected increase in the stationary phase compared with the exponential phase. Transcription of the katG gene was increased in the rho mutant and the levels of the immunoreactive KatG protein do not differ considerably compared with the wild type in the stationary phase, suggesting that KatG activity is affected in a translational or a post-translational step.

A simple and sensitive detection of diquat herbicide using a dental amalgam electrode A comparison using the chromatographic technique

This paper describes the use of a dental amalgam electrode (DAE) to evaluate the electrochemical behaviour and to develop an electroanalytical procedure for determination of diquat herbicide in natural water and potato samples. The work was based on the square wave voltammetry responses of diquat, which presented two well-defined and reversible reduction peaks, at -0.56 V (peak 1) and -1.00V (peak 2). The experimental and voltammetric parameters were optimised, and the analytical curves were constructed and compared to similar curves performed by high performance liquid chromatography coupled to ultraviolet-visible spectrophotometric detector (HPLC/UV-vis). The responses were directly proportional to diquat concentration in a large interval of concentration, and the calculated detection limits were very similar, around 10 mu g L(-1) (10 ppb) for voltammetric and chromatographic experiments. These values were lower than the maximum residue limit established for natural water by the Brazilian Environmental Agency. The recovery percentages in pure electrolyte, natural water and potato samples showed values from 70% to 130%, demonstrating that the voltammetric methodology proposed is suitable for determining any contamination by diquat in different samples, minimising the toxic residues due to the use of liquid mercury or the adsorptive process relative to use of other solid surfaces. (C) 2009 Published by Elsevier B.V.

"Falun ovan från Falun under", ny kunskap om Falu gruva. Projektrapport 2 : Jordartskartering och sedimentborrningar runt Falu gruva

This report is the second presentation of the project ‘Falun above from Falun under’ and comprises one report on ongoing work within the project. The main aims of this particular project are to reconstruct the landscape surrounding Falu Copper mine before mining activity started and to determine how increasing activity in the area affected the environment, and whether this could be measured as an indicator of increasing human impact in the area. This report presents the mapping and investigation of quaternary deposits and landscape analysis, the results from cores taken at two lake sites, Önsbacksdammen and Stora Vällan, 14C dating on selected seeds, and planning of continued research within the project.

Paleoenvironmental analysis of a late-holocene subfossil Coleopteran fauna from Starks, Maine

The Sandy River in central Maine Is flanked along much of its length by low terraces. Approximately 100 kg of sediment from one terrace in Starks, Somerset County, Maine was wet-sieved in the field. Over 1100 subfossil Coleoptera were recovered representing 53 individual species of a total of 99 taxa. Wood associated with the fauna is 2000 +/-80 14C Yr in age (1-16,038). The fauna is dominated by species characteristic of habitats apparent in modern central Maine. The subfossil assemblage is indicative of a wide vartety of environments including open ground (e.g., Harpalus pensylvanicus), dense forest (e.g., pterostichus honestus), aquatic environments (e.g., Gyrinus, Helophorus), riparian environments with sand and gravel substrates (e.g., Bembidion inaequale, Schizogenius lineolatus), and moist, organic-rich terrestrial environments (e.g., Micropeplus sculptus). The ecological requirements for each taxon permit an environmental reconstruction suggesting an area vegetationally, climatically, and ecologically similar to that of the Sandy River today. The lowest terraces apparently represent the modern-day floodplain of the Sandy River. An average sedimentation rate of l.00 to 1.04 mm per year has been inferred based on radiocarbon dates here and elsewhere on the Sandy River. The Coleopteran fauna suggests that sand and gravel were distinctly abundant, and that the aggradation of point bars, as seen today, contributed to the flood history. Lateral bank erosion of the modern Sandy River accelerated after the State of Maine mandated cessation of bar removal in 1975: flood severity has dramatically increased since that time. Implications suggest that mining of the bars may be necessary to minimize future flooding problems.

Efeitos da mal nutrição protéica sobre o metabolismo da glicina em cerebelo de ratos durante o seu desenvolvimento

Malnutrition is a worldwide problem affecting millions of unborn and young children during the most vulnerable stages of brain development (1). All restriction of protein during the perinatal period of life can alter the development of mammalian fetus and have marked repercussions on development of the Central Nervous System (CNS). The brain is vulnerable to protein malnutrition with altered morphologic and biochemical maturation, leading to impaired functions. The focus of this study is to investigate [U-14C]glycine metabolism in malnourished rats submitted to pre- and postnatal protein deprivation (diet: 8% protein with addition and without addition of L-methionine) on glycine metabolism of rats (normonourished group: 25% protein). It was observed that protein malnutrition alters oxidation to CO2, conversion to lipids and protein synthesis from [U-14C]glycine in cerebellum of malnourished rats without addition of L-methionine on a diet at 7 and 21 days of postnatal life. Our results also indicate that protein malnutrition causes a retardation in the normally ordered progression of brain development, and the malnourished groups have smaller cells, reduction in cell numbers and smaller cerebellar weight comparing to the control group.

A relação do espaço na evolução morfodinâmica do Manguezal do Itacorubi, Florianópolis,SC.

Este trabalho aborda o estudo de gerenciamento costeiro feito na área do Manguezal do Itacorubi, na Ilha de Santa Catarina, Estado de Santa Catarina, sul do Brasil. São apresentados dois enfoques, o primeiro discute o comportamento do ecossistema ao longo do século XX diante de diferentes fatores de estresse, concluindo que o manguezal, em 1998, havia perdido 13,32% de área em relação a 1938, porém, nesse mesmo período, progradou aproximadamente 80 m sobre a plataforma continental adjacente, o que indica que o manguezal, apesar de sitiado por uma vizinhança densamente povoada, tem capacidade regenerativa e de avançar em direção do oceano. O segundo enfoque aborda os aspectos geológicos, relacionando os depósitos sedimentares encontrados nesse embaiamento costeiro e as variações holocênicas do nível do mar, constatando que o mar já cobriu essa área em tempos recentes, deixando como testemunho espessos pacotes sedimentares que se apóiam diretamente sobre o embasamento cristalino da região. Dados de testemunhos de sondagem auxiliaram no mapeamento de subsuperfície, indicando a ocorrência de um vale inciso no embasamento, o qual teria servido de acesso preferencial durante o evento transgressivo, guardando os sedimentos de maior granulometria, associados a uma região de maior dinâmica, enquanto nas áreas adjacentes, mais rasas, as granulometrias tendem para as frações mais finas. Sobre esse pacote essencialmente clástico estabeleceu-se a sedimentação carbonosa do manguezal. As variações sedimentares laterais são muito notáveis mesmo naqueles furos relativamente próximos (menos de 20 m), evidenciando a dificuldade que seria a construção de um mapa defácies de uma área de pântano parálico. O bosque de mangue existe nessa área há pelo menos 4,5 Ka, afirmação apoiada sobre os resultados obtidos com a datação de 14C sobre amostra de sedimentos carbonosos.

Efeitos do estresse hipo e hiperosmótico sobre as características do receptor à insulina e sobre a captação de glicose em branquias do caranguejo Chasmagnathus granulata

Neste trabalho investigou-se as características do receptor à insulina e a capacidade de captação de glicose nas brânquias do caranguejo Chasmagnathus granulata aclimatado a diferentes tempos (24, 72 e 144 horas) de estresse hiper e hiposmótico. Primeiramente, o cDNA do receptor para insulina foi parcialmente clonado e seqüenciado em brânquias posteriores de Chasmagnathus granulata. A seqüência peptídica mostrou a presença de 39 aminoácidos e foi designada CGIRLTK (C. granulata insulina receptor-like tyrosine kinase). Esta seqüência apresentou significativa homologia com o domínio tirosina quinase da subunidade b dos receptores para insulina de mamíferos (69%) e de Drosophila (74%). Sítios de ligação à insulina foram caracterizados nas membranas plasmáticas das brânquias através do estudo de ligação com 125I-insulina. A atividade tirosina quinase foi determinada pela capacidade do CGIRLTK de fosforilar o substrato sintético poly (Glu; Tyr 4:1). A captação de glicose foi avaliada pela captação de [14C] 2-deoxi-D-glicose pelo tecido branquial. Nas brânquias posteriores a insulina bovina estimulou significativamente a fosforilação do CGIRLTK nos animais aclimatados a 20‰ de salinidade (controle), já nas brânquias anteriores este estímulo não foi observado. O estresse hiperosmótico (34 ‰ de salinidade) levou a uma diminuição do número e da afinidade dos receptores à insulina nas brânquias posteriores, bem como a uma redução na atividade tirosina quinase. A captação de glicose não mudou durante os tempos de estresse osmótico estudados Esses resultados mostram que o estresse hiperosmótico modifica a sinalização da insulina, causando um estado de resistência à insulina nas brânquias posteriores. Nenhuma mudança foi observada na concentração dos receptores à insulina nas brânquias posteriores de caranguejos aclimatados durante 24 horas ao estresse hiposmótico (0‰). Contudo, foi observada uma redução na afinidade dos receptores pela insulina bovina. A fosforilação do CGIRLTK diminui às 24 horas de estresse e retornou aos valores basais às 144horas. A captação de glicose não foi alterada significativamente. Os resultados sugerem que o estresse hiposmótico modifica as características do CGIRLTK nas brânquias posteriores de C. granulata de forma tempo-dependente. Essas mudanças são parte dos ajustes necessários à sobrevivência à baixa salinidade. Nas brânquias anteriores, durante aclimatação ao estresse hiperosmótico, foi observada redução da concentração e da capacidade de fosforilação dos receptores insulínicos. Contudo, a insulina bovina não estimulou a fosforilação nas brânquias anteriores durante o estresse Nenhuma alteração foi observada na concentração e na afinidade de receptores à insulina nas brânquias anteriores após 24 horas de estresse hiposmótico. A fosforilação do receptor à insulina diminuiu após 24 horas de estresse e voltou aos valores basais após 72 horas. A capacidade de captação de glicose, por sua vez, não foi modificada em função de mudanças na osmoliridade do ambiente. Assim como no estresse hiperosmótico, a insulina bovina não estimulou a fosforilação nas brânquias anteriores no estresse hiposmótico. Os resultados deste trabalho demonstram que o estresse osmótico modifica as características do CGILRTK e conseqüentemente a transdução do sinal insulínico nas brânquias. As respostas às alterações de salinidade dependem do tipo de estresse ao qual o animal é submetido e da brânquia estudada (anterior ou posterior). As mudanças observadas no sinal insulínico fazem parte dos ajustes necessários para a regulação osmótica frente às mudanças ambientais de salinidade.

Estudo do metabolismo de carboidratos e de lipídios em tecidos de caranguejos Chasmagnathus granulatus (Dana, 1851) submetidos ao estresse osmótico : inverno e verão

Este estudo teve como objetivo verificar o efeito do estresse osmótico sobre a via gliconeogênica a partir de glicerol em brânquias e sobre a concentração de lipídios totais em diferentes tecidos de Chasmagnathus granulatus, no inverno e no verão, bem como a atividade das enzimas gliconeogênicas glicose-6-fosfatase (G6Fase) e frutose 1,6-bifosfatase (FBFase). Foram determinadas as concentrações de lipídios totais em brânquias anteriores (BA) e posteriores (BP), hepatopâncreas, músculo da quela e hemolinfa de animais do grupo controle (20‰) ou submetidos a 1, 3 e 6 dias de estresse hipo (0‰) ou hiperosmótico (34‰) no inverno e no verão. Em BPs a concentração de lipídios totais foi maior do que nas BAs de inverno e verão. No hepatopâncreas, durante o estresse hiperosmótico, a concentração de lipídios foi maior no inverno do que no verão. No verão, a concentração de lipídios totais diminuiu nas BPs, no hepatopâncreas e no músculo durante o estresse hiperosmótico, sugerindo que os lipídios estão sendo utilizados como substrato energético durante a aclimatação ao estresse. O aumento da concentração de lipídios totais nas brânquias e no hepatopâncreas sugere a participação da lipogênese no ajuste metabólico ao estresse hiposmótico no inverno. A formação de glicose foi determinada a partir de [14C] - glicerol-, in vitro, em BAs e BPs de animais do grupo controle ou submetidos ao estresse hipo ou hiperosmótico de 1, 3 e 6 dias no inverno e no verão. A gliconeogênese em BAs e BPs do grupo controle foi maior no verão do que no inverno. No verão, no grupo controle, a gliconeogênese das BPs foi maior do que aquela das BAs. A diminuição da capacidade gliconeogênica das brânquias durante diferentes tempos de estresse hiperosmótico sugere a participação desses tecidos no ajuste metabólico ao estresse. Durante o estresse hiposmótico, o glicerol parece não ser o substrato preferencial utilizado por essa dessa via tanto no verão como no inverno. A atividade das enzimas G6Fase e FBFase foi determinada em BAs e BPs, hepatopâncreas e músculo da mandíbula de animais do grupo controle ou submetidos a 3 dias de estresse hipo ou hiperosmótico nos meses de verão. A atividade da G6Fase e da FBFase no grupo controle foi mais elevada no hepatopâncreas do que nos outros tecidos. As atividades dessas enzimas confirmam que a via gliconeogênica é completa nos tecidos estudados. O efeito do estresse hipo ou hiperosmótico, in vivo, sobre a atividade das enzimas varia conforme o tecido do caranguejo.