Uso dos fenóis da lignina no estudo da matéria orgânica na várzea do Lago Grande Curuái, Pará e no Lago do Caçó, Maranhão, Brasil

Este estudo tem por objetivo caracterizar os sedimentos superficiais, quanto ao seu teor e qualidade dos fenóis da lignina, em dois sistemas lacustres distintos: a Várzea do Lago Grande Curuái (PA) e o Lago do Caçó (MA). A Várzea do Lago Grande Curuái é localizada na margem direita do Rio Amazonas, aproximadamente 850 km da foz e é caracterizada pela presença de lagos de águas brancas e pretas. O Lago do Caçó está localizado no Maranhão, na borda do ecossistema amazônico. Foram realizadas análises da concentração de lignina (λ), carbono orgânico total (COT), nitrogênio e isótopos do carbono (δ13C). Os resultados indicam que os sedimentos superficias de lagos de águas brancas apresentam baixos valores de COT (1,5 a 3,6%), baixa concentração de λ (0,73 a 1,28 mg.100mg CO-1) e alto índice de degradação (0,29 a 2,01). Os sedimentos superficiais de lagos de águas pretas apresentam maiores valores de COT (6,0 a 12,1%) e de λ (1,44 a 1,93 mg.100mg CO-1) em relação aos sedimentos de lagos de águas brancas, porém baixos em comparação com os sedimentos do Lago do Caçó (7,2 ~ 15,3% e 1,83 ~ 4,64 mg .100mg CO-1, respectivamente). Através das análises realizadas foi possível identificar diferentes contribuições de fontes assim como diferentes estados de preservação da matéria orgânica sedimentada nos dois sistemas apresentados.

Prevalencia de factores de riesgo cardiovascular en niños de 3 a 17 años

Introducción: Los factores de riesgo de la enfermedad cardiovascular (FRECV) pueden estar presentes desde la infancia y predicen la enfermedad cardiovascular del adulto. Objetivo: Evaluar la prevalencia de FRECV en niños de 3 a 17 años hijos de Enfermeras de la Fundación CardioInfantil - Instituto de cardiología (FCI). Métodos: Estudio de corte transversal analítico. Resultados: 118 niños, edad promedio 7,4 años, desviación estándar 3,86, la mayoría eutróficos 72,0%. Presentaron FRECV como malos hábitos alimenticios 89,0%, sedentarismo 78,8%, exposición a tabaco 19,5%, historia familiar de riesgo cardiovascular 16,1%, sobrepeso 15,3% y obesidad 12,7%. No se encontraron diferencias entre factores de riesgo entre niños y niñas.El sedentarismo en niños con sobrepeso u obesidad fue del 90,9% y en niños eutróficos del 36,5%. Los malos hábitos alimentarios en niños con sobrepeso u obesidad fueron 84,8% y en niños eutróficos 42,4%. Los adolescentes presentaron una mayor exposición a tabaco en comparación con los preescolares y escolares, al igual que una mayor proporción de malos hábitos alimenticios en comparación con ambos grupos. De la totalidad de la población de estudio, el 97,5% presentó al menos un FRECV, y el 42,4% 3 o más FRECV. La presencia de ≥3 FRECV fue mayor en obesos al compararlos con los niños en sobrepeso y eutróficos. Conclusiones: Los resultados del estudio indican que los niños de 3 a 17 años evaluados presentan una alta carga de FRECV, en especial en aquellos con sobrepeso y obesidad.

(Table S3) Benthic foraminiferal Mg/Ca, Li/Ca and stable isotope ratios of ODP Site 122-761

The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate saturation state have recently been assessed. Here we present a new approach that uses paired Mg/Ca and Li/Ca records to calculate simultaneous changes in temperature and saturation state. Using previously published records, we first use this approach to document a cooling of deep ocean waters associated with the establishment of the Antarctic ice sheet at the Eocene-Oligocene climate transition. We then apply this approach to new records of the Middle Miocene Climate Transition from ODP Site 761 to estimate variations in bottom water temperature and the oxygen isotopic composition of seawater. We estimate that the oxygen isotopic composition of seawater varied by ~1 per mil between the deglacial extreme of the Miocene Climatic Optimum and the glacial maximum following the Middle Miocene Climate Transition, indicating large amplitude variations in ice volume. However, the longer-term change between 15.3 and 12.5 Ma is marked by a ~1°C cooling of deep waters, and an increase in the oxygen isotopic composition of seawater of ~0.6 per mil. We find that bottom water saturation state increased in the lead up to the Middle Miocene Climate Transition and decreased shortly after. This supports decreasing pCO2 as a driver for global cooling and ice sheet expansion, in agreement with existing boron isotope and leaf stomatal index CO2 records but in contrast to the published alkenone CO2 records.

Age model, lipids, and iron/calcium-ratios of sediment core GeoB9307-3

Hide Intense debate persists about the climatic mechanisms governing hydrologic changes in tropical and subtropical southeast Africa since the Last Glacial Maximum, about 20,000 years ago. In particular, the relative importance of atmospheric and oceanic processes is not firmly established. Southward shifts of the intertropical convergence zone (ITCZ) driven by high-latitude climate changes have been suggested as a primary forcing, whereas other studies infer a predominant influence of Indian Ocean sea surface temperatures on regional rainfall changes. To address this question, a continuous record representing an integrated signal of regional climate variability is required, but has until now been missing. Here we show that remote atmospheric forcing by cold events in the northern high latitudes appears to have been the main driver of hydro-climatology in southeast Africa during rapid climate changes over the past 17,000 years. Our results are based on a reconstruction of precipitation and river discharge changes, as recorded in a marine sediment core off the mouth of the Zambezi River, near the southern boundary of the modern seasonal ITCZ migration. Indian Ocean sea surface temperatures did not exert a primary control over southeast African hydrologic variability. Instead, phases of high precipitation and terrestrial discharge occurred when the ITCZ was forced southwards during Northern Hemisphere cold events, such as Heinrich stadial 1 (around 16,000 years ago) and the Younger Dryas (around 12,000 years ago), or when local summer insolation was high in the late Holocene, i.e., during the last 4,000 years.

The report of the committee about Harvard Coledge: presented to the Generall Court held the 3 of (3) month, 1654

Two folio-sized leaves with a handwritten draft of the May 3, 1654 report of a General Court Committee authorized to investigate the financial state of Harvard College. The report responds directly to eight questions raised in the September 10, 1653 Order of the General Court that established the Committee. The report provides summaries of Harvard's income sources and disbursements, offers recommendations regarding the President's salary and the allowances for the academic Fellows, steward, butler, and cook, and indicates specific contributions from local towns.

Water temperature reconstructions based on paired Uk'37 and Tex86 records, and paired surface and subsurface Mg/Ca records

This dataset contains the collection of available published paired Uk'37 and Tex86 records spanning multi-millennial to multi-million year time scales, as well as a collection of Mg/Ca-derived temperatures measured in parallel on surface and subsurface dwelling foraminifera, both used in the analyses of Ho and Laepple, Nature Geoscience 2016. As the signal-to-noise ratios of proxy-derived Holocene temperatures are relatively low, we selected records that contain at least the last deglaciation (oldest sample >18kyr BP).

Foraminifera Mg/Ca, test weight and XDX for sediment core WIND28K

A record of deep-sea calcite saturation (D[CO3**-2]), derived from X-ray computed tomography-based foraminifer dissolution index, XDX, was constructed for the past 150 ka for a core from the deep (4157 m) tropical western Indian Ocean. G. sacculifer and N. dutertrei recorded a similar dissolution history, consistent with the process of calcite compensation. Peaks in calcite saturation (~15 µmol/kg higher than the present-day value) occurred during deglaciations and early in MIS 3. Dissolution maxima coincided with transitions to colder stages. The mass record of G. sacculifer better indicated preservation than did that of N. dutertrei or G. ruber. Dissolution-corrected Mg/Ca-derived SST records, like other SST records from marginal Indian Ocean sites, showed coolest temperatures of the last 150 ka in early MIS 3, when mixed layer temperatures were ~4°C lower than present SST. Temperatures recorded by N. dutertrei showed the thermocline to be ~4°C colder in MIS 3 compared to the Holocene (8 ka B.P.).

Gellan gum-Ionic liquid membranes for electrochromic device application

Biopolymer-based materials have been of particular interest and they are alternatives to synthetic polymers based on the decreasing oil resources. The polymer electrolytes were doped with choline-based IL N,N,Ntrimethyl- N-(2-hydroxyethyl)ammonium bis(trifluoromethylsulfonyl)imide ([N1 1 1 2(OH)][NTf2]), or Er (CF3SO3)3 or both. The polymer electrolytes were employed in the production of glass/ITO/WO3/electrolyte/ CeO2–TiO2/ITO/glass electrochromic devices (ECDs). The lowest onset temperature for the degradation of all the SPEs is at ~130 °C for the Gellan Er (CF3SO3)3 (10:1) this temperature range of stability is wide enough for a material to be applied as an electrolyte/separator component in electrochemical devices. The three ECDs displayed fast switching speed (ca. 15 s). Gellan [N1 1 1 2(OH)][NTf2] Er (CF3SO3)3 (5:1:10) exhibited an electrochromic contrast of 4.2% in the visible region, the coloration efficiency attained at 555 nm was 3.5 and 0.90 cm-2 C-1 in the “colored” and “bleached” states, respectively, and the open circuit memorywas 48 h. Preliminary tests performed with a prototype electrochromic device (ECD) incorporating WO3 as cathodic electrochromic layer, are extremely encouraging.

Glomevella cingulata (Stonem.) spauld. et v. schrenk. F. SP. phaseoli N.F., fase ascógena do agente causal da antracnose do feijoeiro

O presente trabalho versa sobre a obtenção da fase perfeita de Colletotriohum lindemuthianum (Sacc. et Magn.) Scrib., dirimindo duvidas quanto a sua existência, suscitada pelo primeiro relato feito por SHEAR e WOOD (1913). Após ter encontrado duas linhagens heterotálicas que formaram ascosporos em acasalamentos, os autores estudaram alguns fatores ambientais que favorecem a reprodução sexuada, chegando-se as seguintes conclusões: peritecios se formaram sobre varios meios de cultura semi-sintéticos em cuja composição entram glucose, Ca(N0(3))2.4H(2)0(, MgSO4.7H2O e KH2PO4, agar e água; a quantidade de glucose deve ser igual ou maior do que 4g/l, a de Ca(NO3)2.4H2O de 0,15 a 0,60 g/l e a relação C/N deve estar entre 29,8 a 89,6:1; a adição de vitaminas alterou levemente o nível de aproveitamento de Ca(NO3)2.4H2O, nao havendo boa produção de peritécio ao nível de 0,15 g/l mas permitindo-se ate o nível de 1 g/l, mantendo-se as relações C/N mais ou menos no mesmo nivel; a luz, nos estágios final ou inicial ou em períodos alternados acima de 8 horas, inibiu a formação de ascosporos, sendo, portanto, essencial a escuridão contínua; peritécios se formaram sob condições de pH variável de 4,0 a 6,0; peritécios ejetam ascosporos em condições de alta umidade; a temperatura em que foram obtidos os peritécios foi sempre de 209C. Do acasalamento de linhagens conidiais de C.lindemuthianum o autor obteve resultados a priori comparáveis aos de trabalhos genéticos feitos com G.cingulata, chegando-se a conclusão de que as linhagens usadas sao heterotãlicas possivelmente condicionadas por varios fatores genéticos. Isolamentos ascospóricos foram inoculados, sendo todos patogênicos ao feijoeiro, pelo menos para a variedade Michelite. Comparando morfológicamente a fase ascogena de C.lindemuthvanwn com G.cvngulata, o autor propõe o nome de Glomerelia cingulata (Stonem.) Spauld et v. Schrenk f.phaseoli n.f.

Deficiências de macronutrientes e de boro em Nicotiana tabacum L. var. goianinho

Com os objetivos de determinar: 1) O quadro sintomatológico das carências dos macronutrientes e de boro; 2) Concentração dos macronutrientes e de boro nas folhas novas, velhas e no caule na presença e ausência dos nutrientes. Foi instalado em ensaio em solução nutritiva tendo como sílica o substrato. Os tratamentos constaram da omissão de N, P, K, Ca, Mg, S, B, e presença de todos os nutrientes. Acompanhou-se o desenvolvimento dos sintomas e uma vez evidenciados coletou-se as plantas que foram analisadas para os elementos em estudo. Verificou-se que: 1) Houve efeito na produção de matéria seca influência pela omissão de N, P, K, Ca e Mg; 2) Os sintomas visuais de deficiência são bem definidos e de fácil caracterização para todos os nutrientes; 3) Os níveis de deficiência adequado, obtidos nas folhas foram: N% 1,23-3,06; P% 0,04-0,11; K% 1,15-3,25; Ca% 0,20-0,59; Mg% 1,13-1,25, S% 0,16-0,20; B ppm 34-59.

Acúmulo de massa seca e extração de macro e micronutrientes por uma cultura de gengibre

De uma plantação bem conduzida no Município de Caraguatatuba, litoral do Estado de São Paulo, foram coletadas plantas (Zingeber officinalis, Rosae, var. Brasil) em número nunca inferior a quatro por amostragem a partir de dois meses da brotação até a época da colheita com intervalos de trinta dias. As plantas após a coleta foram divididas em folhas, "caule", flores e rizomas, tratadas e analisadas para macro e micronutrientes de acordo com os métodos tradicionais de laboratório. Os autores concluíram que o gengibre tem um crescimento contínuo e a extração de macronutrientes obedece a seguinte ordem decrescente: N, K, Ca, Mg, S e P. Para os micronutrientes a ordem decrescente é: Fe, Mn, Zn, B e Cu. Os rizomas exportam 15,3% do total de nutrientes contidos na plantação. A cultura do gengibre pode ser considerada como exigente em nutrientes.

Sustaining sleep spindles through enhanced SK2-channel activity consolidates sleep and elevates arousal threshold.

Sleep spindles are synchronized 11-15 Hz electroencephalographic (EEG) oscillations predominant during nonrapid-eye-movement sleep (NREMS). Rhythmic bursting in the reticular thalamic nucleus (nRt), arising from interplay between Ca(v)3.3-type Ca(2+) channels and Ca(2+)-dependent small-conductance-type 2 (SK2) K(+) channels, underlies spindle generation. Correlative evidence indicates that spindles contribute to memory consolidation and protection against environmental noise in human NREMS. Here, we describe a molecular mechanism through which spindle power is selectively extended and we probed the actions of intensified spindling in the naturally sleeping mouse. Using electrophysiological recordings in acute brain slices from SK2 channel-overexpressing (SK2-OE) mice, we found that nRt bursting was potentiated and thalamic circuit oscillations were prolonged. Moreover, nRt cells showed greater resilience to transit from burst to tonic discharge in response to gradual depolarization, mimicking transitions out of NREMS. Compared with wild-type littermates, chronic EEG recordings of SK2-OE mice contained less fragmented NREMS, while the NREMS EEG power spectrum was conserved. Furthermore, EEG spindle activity was prolonged at NREMS exit. Finally, when exposed to white noise, SK2-OE mice needed stronger stimuli to arouse. Increased nRt bursting thus strengthens spindles and improves sleep quality through mechanisms independent of EEG slow waves (<4 Hz), suggesting SK2 signaling as a new potential therapeutic target for sleep disorders and for neuropsychiatric diseases accompanied by weakened sleep spindles.

Ca(2+) signaling by T-type Ca(2+) channels in neurons.

Among the major families of voltage-gated Ca(2+) channels, the low-voltage-activated channels formed by the Ca(v)3 subunits, referred to as T-type Ca(2+) channels, have recently gained increased interest in terms of the intracellular Ca(2+) signals generated upon their activation. Here, we provide an overview of recent reports documenting that T-type Ca(2+) channels act as an important Ca(2+) source in a wide range of neuronal cell types. The work is focused on T-type Ca(2+) channels in neurons, but refers to non-neuronal cells in cases where exemplary functions for Ca(2+) entering through T-type Ca(2+) channels have been described. Notably, Ca(2+) influx through T-type Ca(2+) channels is the predominant Ca(2+) source in several neuronal cell types and carries out specific signaling roles. We also emphasize that Ca(2+) signaling through T-type Ca(2+) channels occurs often in select subcellular compartments, is mediated through strategically co-localized targets, and is exploited for unique physiological functions.

Plan d'El-Arych : Pour servir à la relation de la campagne de Syrie / J. F. S. Bailly del.

Échelle(s) : [ca 1:3 300], 100 mètres [= 3 cm]

Synaptic Plasticity at Intrathalamic Connections via CaV3.3 T-type Ca2+ Channels and GluN2B-Containing NMDA Receptors.

The T-type Ca(2+) channels encoded by the Ca(V)3 genes are well established electrogenic drivers for burst discharge. Here, using Ca(V)3.3(-/-) mice we found that Ca(V)3.3 channels trigger synaptic plasticity in reticular thalamic neurons. Burst discharge via Ca(V)3.3 channels induced long-term potentiation at thalamoreticular inputs when coactivated with GluN2B-containing NMDA receptors, which are the dominant subtype at these synapses. Notably, oscillatory burst discharge of reticular neurons is typical for sleep-related rhythms, suggesting that sleep contributes to strengthening intrathalamic circuits.