Pain pressure threshold algometry of the abdominal wall in healthy women

The objective of this study was to determine the inter- and intra-examiner reliability of pain pressure threshold algometry at various points of the abdominal wall of healthy women. Twenty-one healthy women in menacme with a mean age of 28 +/- 5.4 years (range: 19-39 years) were included. All volunteers had regular menstrual cycles (27-33 days) and were right-handed and, to the best of our knowledge, none were taking medications at the time of testing. Women with a diagnosis of depression, anxiety or other mood disturbances were excluded. Women with previous abdominal surgery, any pain condition or any evidence of inflammation, hypertension, smoking, alcoholism, or inflammatory disease were also excluded. Pain perception thresholds were assessed with a pressure algometer with digital traction and compression and a measuring capacity for 5 kg. All points were localized by palpation and marked with a felt-tipped pen and each individual was evaluated over a period of 2 days in two consecutive sessions, each session consisting of a set of 14 point measurements repeated twice by two examiners in random sequence. There was no statistically significant difference in the mean pain threshold obtained by the two examiners on 2 diferent days (examiner A: P = 1.00; examiner B: P = 0.75; Wilcoxon matched pairs test). There was excellent/good agreement between examiners for all days and all points. Our results have established baseline values to which future researchers will be able to refer. They show that pressure algometry is a reliable measure for pain perception in the abdominal wall of healthy women.

Quartz OSL sensitivity as a proxy for storm activity on the southern Brazilian coast during the Late Holocene

Natural cycles of irradiation during burial and bleaching due to solar exposure during transport increase the Optically Stimulated Luminescence (OSL) sensitivity of quartz sand grains. The relationship between the OSL sensitivity and sediment transport allows to discriminate quartz sand grains with different depositional histories. In this paper, we evaluate the variation of OSL sensitivity in quartz grains deposited during the progradation of the Ilha Comprida barrier on the southern Brazilian, coast. Changes in sand sensitivity recorded by barrier growth since 6 ka ago are controlled by the variation in the proportion of low versus high sensitivity quartz grains. Low sensitivity grains with short sedimentary history are supplied by the Ribeira de Iguape River and reach the barrier through southward alongshore currents during fair weather conditions. Storm conditions shift the alongshore currents to northeast and permit the transport of high sensitivity grains with long sedimentary history from distal southern coastal sectors to the barrier. Therefore, the input of distal sediments for the Ilha Comprida barrier depends on the frequency and intensity of storms. Thus, the OSL sensitivity can be used as proxy for storm activity. The variation of OSL sensitivity through time indicates that the Ilha Comprida barrier changed from a relatively stable to an unstable storm pattern around 2 ka ago. Periods with increased storm activity peaked around AD 500, AD 1500 and AD 1850, approximately on the boundaries of the Medieval Climate Anomaly and the Little Ice Age. (C) 2012 Elsevier B.V. All rights reserved.

Molting dynamics and juvenile hormone titer profiles in the nymphal stages of a lower termite, Cryptotermes secundus (Kalotermitidae) - signatures of developmental plasticity

Termites are social cockroaches and this sociality is founded on a high plasticity during development. Three molting types (progressive, stationary and regressive molts) are fundamental to achieve plasticity during alate/sexual development, and they make termites a major challenge to any model on endocrine regulation in insect development. As the endocrine signatures underpinning this plasticity are barely understood, we studied the developmental dynamics and their underlying juvenile hormone OH) titers in a wood-dwelling termite. Cryptotermes secundus, which is characterized by an ancestral life style of living in dead wood and individuals being totipotent in development. The following general pattern elements could be identified during winged sexual development (i) regressive molts were accompanied by longer intermolt periods than other molting types, (ii) JH titers decreased gradually during the developmental transition from larva (immatures without wing buds), to nymph (immatures with wing buds), to winged adult, (iii) in all nymphal stages, the JH titer rose before the next molt and dropped thereafter within the first week, (iv) considerable variation in JH titers occurred in the midphase of the molting cycle of the 2nd and 3rd nymphal instar, inferring that this variation may reflect the underlying endocrine signature of each of the three molting types, (v) the 4th nymphal instar, the shortest of all, seems to be a switch point in development, as nymphs in this stage mainly developed progressively. When comparing these patterns with endocrine signatures seen in cockroaches, the developmental program of Cryprotermes can be interpreted as a co-option and repetitive use of hormonal dynamics of the post dorsal-closure phase of cockroach embryonic development. (C) 2012 Elsevier Ltd. All tights reserved.

Influence of myofascial pain on the pressure pain threshold of masticatory muscles in women with migraine

Objective: To evaluate the influence of myofascial pain on the Pressure Pain Threshold (PPT) of masticatory muscles in women with migraine. Methods: The sample comprised 101 women, ages ranging from 18 to 60 years, with an episodic migraine diagnosis previously confirmed by a neurologist. All patients were evaluated using Research Diagnostic Criteria for Temporomandibular Disorders to determine the presence of myofascial pain and were divided into 2 groups: group I (n=56), comprising women with a migraine, and group II (n=45), comprising women with a migraine and myofascial pain. Two more groups (49 asymptomatic women and 50 women with myofascial pain), matched for sex and race, obtained from a previous study, were added to this study. The PPT values of masseter and temporalis (anterior, middle, and posterior regions) muscles were recorded bilaterally using a pressure algometer. One-way analysis of variance and the Tukey test for pairwise comparisons were used in statistical analysis with a 5% significance level. Results: We found that all groups had significantly lower PPT values compared with asymptomatic women, with lower values seen in group II (women with migraine and myofascial pain). Women with a migraine and myofascial pain showed significantly lower PPT values compared with women with a migraine only, and also when compared with women with myofascial pain only. Discussion: Migraine, especially when accompanied by myofascial pain, reduces the PPT of masticatory muscles, suggesting the importance of masticatory muscle palpation during examination of patients with migraine.

Comparison of child self-reports and parent proxy-reports on quality of life of children with attention deficit hyperactivity disorder

Abstract Background Attention deficit hyperactivity disorder (ADHD) is a neurobiological condition that affects 3%–7% of the pediatric population and significantly compromises the quality of life (QoL) of these individuals. The aim of the current study was to compare child self-reports and parent proxy reports on the QoL of children with ADHD. Methods Forty-five children with ADHD, combined type, aged 8–12 years without comorbidities, were compared with 43 typically developing children. PedsQL™ 4.0 (Pediatric QoL Inventory™) Generic Core Scales (physical, emotional, social, and school functioning) were completed by families and children self-reporting their health-related QoL. Results Children with ADHD reported themselves significantly lowered their PedsQL™ scores on all dimensions in comparison to typically developing children. Statistically significant differences were observed in social functioning (p = 0.010), school functioning (p <0.001), psychosocial health (p <0.001), and total score (p = 0.002). The physical functioning and emotional functioning dimensions did not differ significantly between groups, with p = 0.841 and p = 0.070, respectively. Parents of children with ADHD also reported lower PedsQL™ scores, with statistically significant differences in all dimensions. The relationship between child self-reports and parent proxy reports indicated that there is greater agreement among children with ADHD, except for the school functioning. Conclusions This suggests that children with the disorder and their parents have a perception of the functional limitations the disorder brings. It is therefore important to undertake studies to verify the QoL in children with ADHD that aim to provide and measure the scope of the well-being of these children.

Estudios tafonómicos en foraminíferos bentónicos como proxy de hidrodinámica y sedimentología en el gradiente Río de La Plata – Océano Atlántico Sur Occidental

Los foraminíferos bentónicos representan un excelente proxy geológico, ya que sus caparazones son incorporados en el sedimento y pasan a comportarse como granos sedimentares durante los eventos de transporte y erosión, permitiendo así, el registro de condiciones y eventos que ocurren en los océanos. De este modo, son usados para describir patrones de hidrodinámica y evaluar índices de deposición, erosión y retrabajamiento del sedimento en los ambientes marinos. Concretamente, las regiones costeras representan zonas de alta complejidad ambiental, debido a que en ellas se da la mezcla de agua tanto de origen continental como marino, y a su vez, al efecto de la descarga fluvial que aporta material particulado del continente para el océano. El Río de la Plata (RdLP) representa el cuarto mayor estuario del mundo y el segundo del continente americano, lo cual convierte al sistema RdLP-Océano Atlántico en un complejo gradiente estuarino de interés en estudios sedimentológicos con posteriores aplicaciones paleo-climáticas y paleo-ecológicas del Cuaternario Superior. En el presente estudio, se registra a partir de las asociaciones muertas, para la región del estuario entrada de agua marina hasta la zona del frente termohalino. Dichas asociaciones se caracterizaron por especies típicas de plataforma y aguas frías. La región marina del RdlP registró los mayores porcentajes de abrasión y fragmentación de caparazones, indicando una zona de alta energía. Por otro lado, en la región más oceánica las asociaciones muertas reflejaron un transporte en dirección norte, influenciado por la pluma del RdlP. Cabe resaltar la presencia en esta región de una isla barrera, vestigio de una paleo-costa producto de una regresión Holocénica. Este local se caracterizó por un aumento de la abrasión y fragmentación mostrando la gran hidrodinámica presente. En todos los casos existió correlación entre las señales tafonómicas y los datos geo-químicos (sedimentología, pH, oxígeno disuelto, carbono orgánico y nitrógeno total)

Estudios tafonómicos en foraminíferos bentónicos como proxy de hidrodinámica y sedimentología en el gradiente Río de La Plata – Océano Atlántico Sur Occidental

Los foraminíferos bentónicos representan un excelente proxy geológico, ya que sus caparazones son incorporados en el sedimento y pasan a comportarse como granos sedimentares durante los eventos de transporte y erosión, permitiendo así, el registro de condiciones y eventos que ocurren en los océanos. De este modo, son usados para describir patrones de hidrodinámica y evaluar índices de deposición, erosión y retrabajamiento del sedimento en los ambientes marinos. Concretamente, las regiones costeras representan zonas de alta complejidad ambiental, debido a que en ellas se da la mezcla de agua tanto de origen continental como marino, y a su vez, al efecto de la descarga fluvial que aporta material particulado del continente para el océano. El Río de la Plata (RdLP) representa el cuarto mayor estuario del mundo y el segundo del continente americano, lo cual convierte al sistema RdLP-Océano Atlántico en un complejo gradiente estuarino de interés en estudios sedimentológicos con posteriores aplicaciones paleo-climáticas y paleo-ecológicas del Cuaternario Superior. En el presente estudio, se registra a partir de las asociaciones muertas, para la región del estuario entrada de agua marina hasta la zona del frente termohalino. Dichas asociaciones se caracterizaron por especies típicas de plataforma y aguas frías. La región marina del RdlP registró los mayores porcentajes de abrasión y fragmentación de caparazones, indicando una zona de alta energía. Por otro lado, en la región más oceánica las asociaciones muertas reflejaron un transporte en dirección norte, influenciado por la pluma del RdlP. Cabe resaltar la presencia en esta región de una isla barrera, vestigio de una paleo-costa producto de una regresión Holocénica. Este local se caracterizó por un aumento de la abrasión y fragmentación mostrando la gran hidrodinámica presente. En todos los casos existió correlación entre las señales tafonómicas y los datos geo-químicos (sedimentología, pH, oxígeno disuelto, carbono orgánico y nitrógeno total).