The interplay of localization and interactions in quantum many-body systems

Disorder and interactions both play crucial roles in quantum transport. Decades ago, Mott showed that electron-electron interactions can lead to insulating behavior in materials that conventional band theory predicts to be conducting. Soon thereafter, Anderson demonstrated that disorder can localize a quantum particle through the wave interference phenomenon of Anderson localization. Although interactions and disorder both separately induce insulating behavior, the interplay of these two ingredients is subtle and often leads to surprising behavior at the periphery of our current understanding. Modern experiments probe these phenomena in a variety of contexts (e.g. disordered superconductors, cold atoms, photonic waveguides, etc.); thus, theoretical and numerical advancements are urgently needed. In this thesis, we report progress on understanding two contexts in which the interplay of disorder and interactions is especially important.

The first is the so-called “dirty” or random boson problem. In the past decade, a strong-disorder renormalization group (SDRG) treatment by Altman, Kafri, Polkovnikov, and Refael has raised the possibility of a new unstable fixed point governing the superfluid-insulator transition in the one-dimensional dirty boson problem. This new critical behavior may take over from the weak-disorder criticality of Giamarchi and Schulz when disorder is sufficiently strong. We analytically determine the scaling of the superfluid susceptibility at the strong-disorder fixed point and connect our analysis to recent Monte Carlo simulations by Hrahsheh and Vojta. We then shift our attention to two dimensions and use a numerical implementation of the SDRG to locate the fixed point governing the superfluid-insulator transition there. We identify several universal properties of this transition, which are fully independent of the microscopic features of the disorder.

The second focus of this thesis is the interplay of localization and interactions in systems with high energy density (i.e., far from the usual low energy limit of condensed matter physics). Recent theoretical and numerical work indicates that localization can survive in this regime, provided that interactions are sufficiently weak. Stronger interactions can destroy localization, leading to a so-called many-body localization transition. This dynamical phase transition is relevant to questions of thermalization in isolated quantum systems: it separates a many-body localized phase, in which localization prevents transport and thermalization, from a conducting (“ergodic”) phase in which the usual assumptions of quantum statistical mechanics hold. Here, we present evidence that many-body localization also occurs in quasiperiodic systems that lack true disorder.

Slender-body hypervelocity boundary-layer instability

With novel application of optical techniques, the slender-body hypervelocity boundary-layer instability is characterized in the previously unexplored regime where thermo-chemical effects are important. Narrowband disturbances (500-3000~kHz) are measured in boundary layers with edge velocities of up to 5~km/s at two points along the generator of a 5 degree half angle cone. Experimental amplification factor spectra are presented. Linear stability and PSE analysis is performed, with fair prediction of the frequency content of the disturbances; however, the analysis over-predicts the amplification of disturbances. The results of this work have two key implications: 1) the acoustic instability is present and may be studied in a large-scale hypervelocity reflected-shock tunnel, and 2) the new data set provides a new basis on which the instability can be studied.

Constraints on the carbon cycle and climate during the early evolution of animals

One of the greatest challenges in science lies in disentangling causality in complex, coupled systems. This is illustrated no better than in the dynamic interplay between the Earth and life. The early evolution and diversification of animals occurred within a backdrop of global change, yet reconstructing the potential role of the environment in this evolutionary transition is challenging. In the 200 million years from the end-Cryogenian to the Ordovician, enigmatic Ediacaran fauna explored body plans, animals diversified and began to biomineralize, forever changing the ocean's chemical cycles, and the biological community in shallow marine ecosystems transitioned from a microbial one to an animal one.

In the following dissertation, a multi-faceted approach combining macro- and micro-scale analyses is presented that draws on the sedimentology, geochemistry and paleontology of the rocks that span this transition to better constrain the potential environmental changes during this interval.

In Chapter 1, the potential of clumped isotope thermometry in deep time is explored by assessing the importance of burial and diagenesis on the thermometer. Eocene- to Precambrian-aged carbonates from the Sultanate of Oman were analyzed from current burial depths of 350-5850 meters. Two end-member styles of diagenesis independent of burial depth were observed.

Chapters 2, 3 and 4 explore the fallibility of the Ediacaran carbon isotope record and aspects of the sedimentology and geochemistry of the rocks preserving the largest negative carbon isotope excursion on record---the Shuram Excursion. Chapter 2 documents the importance of temperature, fluid composition and mineralogy on the delta 18-O min record and interrogates the bulk trace metal signal. Chapter 3 explores the spatial variability in delta 13-C recorded in the transgressive Johnnie Oolite and finds a north-to-south trend recording the onset of the excursion. Chapter 4 investigates the nature of seafloor precipitation during this excursion and more broadly. We document the potential importance of microbial respiratory reactions on the carbonate chemistry of the sediment-water interface through time.

Chapter 5 investigates the latest Precambrian sedimentary record in carbonates from the Sultanate of Oman, including how delta 13-C and delta 34-S CAS vary across depositional and depth gradients. A new model for the correlation of the Buah and Ara formations across Oman is presented. Isotopic results indicate delta 13-C varies with relative eustatic change and delta 34-S CAS may vary in absolute magnitude across Oman.

Chapter 6 investigates the secular rise in delta 18-Omin in the early Paleozoic by using clumped isotope geochemistry on calcitic and phosphatic fossils from the Cambrian and Ordovician. Results do not indicate extreme delta 18-O seawater depletion and instead suggest warmer equatorial temperatures across the early Paleozoic.

Two-color two-photon excitation of indole using a femtosecond laser regenerative amplifier

The fluorescence emission from indole resulting from two-color two-photon (2C2P) excitation with 400 and 800 nm wavelengths is observed, using the second harmonic and fundamental wavelength of a 800 nm 40 fs pulsed Ti:Sapphire femtosecond (fs) regenerative amplifier operating at a repetition rate of 1 kHz. By delaying one fs laser pulse relative to the other, the cross correlation of fluorescence is observed, which indicates the generation of 2C2P fluorescence signal in the experiment. The strongest 2C2P fluorescence emission characterized by the peak of cross correlation curve suggests optimal temporal overlap of the two fs laser pulses. The 2C2P fluorescence signal is linearly dependent on the total excitation intensity. The fluorescence signals with 400 nm and 800 nm irradiation alone are also demonstrated and discussed in this paper. (C) 2008 Elsevier B.V. All rights reserved.

Geological evolution of two crustal scale shear zones. Part I. The Rand thrust complex, northwestern Mojave Desert, California. Part II. The Magdalena metamorphic core complex, north central Sonora, Mexico

The geology and structure of two crustal scale shear zones were studied to understand the partitioning of strain within intracontinental orogenic belts. Movement histories and regional tectonic implications are deduced from observational data. The two widely separated study areas bear the imprint of intense Late Mesozoic through Middle Cenozoic tectonic activity. A regional transition from Late Cretaceous-Early Tertiary plutonism, metamorphism, and shortening strain to Middle Tertiary extension and magmatism is preserved in each area, with contrasting environments and mechanisms. Compressional phases of this tectonic history are better displayed in the Rand Mountains, whereas younger extensional structures dominate rock fabrics in the Magdalena area.

In the northwestern Mojave desert, the Rand Thrust Complex reveals a stack of four distinctive tectonic plates offset along the Garlock Fault. The lowermost plate, Rand Schist, is composed of greenschist facies metagraywacke, metachert, and metabasalt. Rand Schist is structurally overlain by Johannesburg Gneiss (= garnet-amphibolite grade orthogneisses, marbles and quartzites), which in turn is overlain by a Late Cretaceous hornblende-biotite granodiorite. Biotite granite forms the fourth and highest plate. Initial assembly of the tectonic stack involved a Late Cretaceous? south or southwest vergent overthrusting event in which Johannesburg Gneiss was imbricated and attenuated between Rand Schist and hornblende-biotite granodiorite. Thrusting postdated metamorphism and deformation of the lower two plates in separate environments. A post-kinematic stock, the Late Cretaceous Randsburg Granodiorite, intrudes deep levels of the complex and contains xenoliths of both Rand Schist and mylonitized Johannesburg? gneiss. Minimum shortening implied by the map patterns is 20 kilometers.

Some low angle faults of the Rand Thrust Complex formed or were reactivated between Late Cretaceous and Early Miocene time. South-southwest directed mylonites derived from Johannesburg Gneiss are commonly overprinted by less penetrative north-northeast vergent structures. Available kinematic information at shallower structural levels indicates that late disturbance(s) culminated in northward transport of the uppermost plate. Persistence of brittle fabrics along certain structural horizons suggests a possible association of late movement(s) with regionally known detachment faults. The four plates were juxtaposed and significant intraplate movements had ceased prior to Early Miocene emplacement of rhyolite porphyry dikes.

In the Magdalena region of north central Sonora, components of a pre-Middle Cretaceous stratigraphy are used as strain markers in tracking the evolution of a long lived orogenic belt. Important elements of the tectonic history include: (1) Compression during the Late Cretaceous and Early Tertiary, accompanied by plutonism, metamorphism, and ductile strain at depth, and thrust driven? syntectonic sedimentation at the surface. (2) Middle Tertiary transition to crustal extension, initially recorded by intrusion of leucogranites, inflation of the previously shortened middle and upper crustal section, and surface volcanism. (3) Gravity induced development of a normal sense ductile shear zone at mid crustal levels, with eventual detachment and southwestward displacement of the upper crustal stratigraphy by Early Miocene time.

Elucidation of the metamorphic core complex evolution just described was facilitated by fortuitous preservation of a unique assemblage of rocks and structures. The "type" stratigraphy utilized for regional correlation and strain analysis includes a Jurassic volcanic arc assemblage overlain by an Upper Jurassic-Lower Cretaceous quartz pebble conglomerate, in turn overlain by marine strata with fossiliferous Aptian-Albian limestones. The Jurassic strata, comprised of (a) rhyolite porphyries interstratified with quartz arenites, (b) rhyolite cobble conglomerate, and (c) intrusive granite porphyries, are known to rest on Precambrian basement north and east of the study area. The quartz pebble conglomerate is correlated with the Glance Conglomerate of southeastern Arizona and northeastern Sonora. The marine sequence represents part of an isolated arm? of the Bisbee Basin.

Crosscutting structural relationships between the pre-Middle Cretaceous supracrustal section, younger plutons, and deformational fabrics allow the tectonic sequence to be determined. Earliest phases of a Late Cretaceous-Early Tertiary orogeny are marked by emplacement of the 78 ± 3 Ma Guacomea Granodiorite (U/Pb zircon, Anderson et al., 1980) as a sill into deep levels of the layered Jurassic series. Subsequent regional metamorphism and ductile strain is recorded by a penetrative schistosity and lineation, and east-west trending folds. These fabrics are intruded by post-kinematic Early Tertiary? two mica granites. At shallower crustal levels, the orogeny is represented by north directed thrust faulting, formation of a large intermontane basin, and development of a pronounced unconformity. A second important phase of ductile strain followed Middle Tertiary? emplacement of leucogranites as sills and northwest trending dikes into intermediate levels of the deformed section (surficial volcanism was also active during this transitional period to regional extension). Gravitational instabilities resulting from crustal swelling via intrusion and thermal expansion led to development of a ductile shear zone within the stratigraphic horizon occupied by a laterally extensive leucogranite sill. With continued extension, upper crustal brittle normal faults (detachment faults) enhanced the uplift and tectonic denudation of this mylonite zone, ultimately resulting in southwestward displacement of the upper crustal stratigraphy.

Strains associated with the two ductile deformation events have been successfully partitioned through a multifaceted analysis. R_f/Ø measurements on various markers from the "type" stratigraphy allow a gradient representing cumulative strain since Middle Cretaceous time to be determined. From this gradient, noncoaxial strains accrued since emplacement of the leucogranites may be removed. Irrotational components of the postleucogranite strain are measured from quartz grain shapes in deformed granites; rotational components (shear strains) are determined from S-C fabrics and from restoration of rotated dike and vein networks. Structural observations and strain data are compatable with a deformation path of: (1) coaxial strain (pure shear?), followed by (2) injection of leucogranites as dikes (perpendicular to the minimum principle stress) and sills (parallel to the minimum principle stress), then (3) southwest directed simple shear. Modeling the late strain gradient as a simple shear zone permits a minimum displacement of 10 kilometers on the Magdalena mylonite zone/detachment fault system. Removal of the Middle Tertiary noncoaxial strains yields a residual (or pre-existing) strain gradient representative of the Late Cretaceous-Early Tertiary deformation. Several partially destrained cross sections, restored to the time of leucogranite emplacement, illustrate the idea that the upper plate of the core complex bas been detached from a region of significant topographic relief. 50% to 100% bulk extension across a 50 kilometer wide corridor is demonstrated.

Late Cenozoic tectonics of the Magdalena region are dominated by Basin and Range style faulting. Northeast and north-northwest trending high angle normal faults have interacted to extend the crust in an east-west direction. Net extension for this period is minor (10% to 15%) in comparison to the Middle Tertiary detachment related extensional episode.

The structure of liquid argon as determined by x-ray diffraction

X-ray diffraction measurements and subsequent data analyses have been carried out on liquid argon at five states in the density range of 0.91 to 1.135 gm/cc and temperature range of 127 to 143°K. Duplicate measurements were made on all states. These data yielded radial distribution and direct correlation functions which were then used to compute the pair potential using the Percus-Yevick equation. The potential minima are in the range of -105 to -120°K and appear to substantiate current theoretical estimates of the effective pair potential in the presence of a weak three-body force.

The data analysis procedure used was new and does not distinguish between the coherent and incoherent absorption factors for the cell scattering which were essentially equal. With this simplification, the argon scattering estimate was compared to the gas scattering estimate on the laboratory frame of reference and the two estimates coincided, indicating the data normalized. The argon scattering on the laboratory frame of reference was examined for the existence of the peaks in the structure factor and the existence of an observable third peak was considered doubtful.

Numerical studies of the effect of truncation, normalization, the subsidiary peak phenomenon in the radial distribution function, uncertainties in the low angle data relative to errors in the direct correlation function and the distortion phenomenon are presented.

The distortion phenomenon for this experiment explains why the Mikolaj-Pings argon data yielded pair potential well depths from the Percus-Yevick equation that were too shallow and an apparent slope with respect to density that was too steep compared to theoretical estimates.

The data presented for each measurement are: empty cell and cell plus argon intensity, absorption factors, argon intensity, smoothed argon intensity, smoothed argon intensity corrected for distortion, structure factor, radial distribution function, direct correlation function and the pair potential from the Percus-Yevick equation.

Spatiotemporal segmentation based on two-dimensional spatiotemporal entropic thresholding

A novel spatiotemporal segmentation technique is further developed for extracting uncovered background and moving objects from the image sequences, then the following motion estimation is performed only on the regions corresponding to moving objects. The frame difference contrast (FCON) and local variance contrast (LCON), which are related to the temporal and spatial homogeneity of the image sequence, are selected to form the 2-D spatiotemporal entropy. Then the spatial segmentation threshold is determined by maximizing the 2-D spatiotemporal entropy, and the temporal segmentation point is selected to minimize the complexity measure for image sequence coding. Since both temporal and spatial correlation of an image sequence are exploited, this proposed spatiotemporal segmentation technique can further be used to determine the positions of reference frames adaptively, hence resulting in a low bit rate. Experimental results show that this segmentation-based coding scheme is more efficient than usual fixed-size coding algorithms. (C) 1997 Society of Photo-Optical Instrumentation Engineers.

Two-photon excited red upconversion luminescence of thulium ions doped GeS2-In2S3-CsI glass

We report a novel phenomenon in GeS2-In2S3-CsI chalcohalide glass doped with Tm3+ ions. Under irradiation with an 808 nm laser diode, a bright red emission centered at 700 nm is observed for the first time in this glass. The log-log correlation between integrated emission intensity and pump power reveals that a two-photon absorption process is involved in the phenomenon, suggesting that the F-3(3,2) -> H-3(6) transition of Tm3+ ions is responsible for the appearance of the red emission. The results indicate that the indium (In) based chalcohalide glass containing Tm3+ ions is expected to find applications in visible lasers, high density optical storage and three-dimensional color displays. (C) 2009 Elsevier B.V. All rights reserved.

Velocidade da onda de pulso em adultos jovens acompanhados por 18 anos: impacto de variáveis pressóricas, antropométricas, metabólicas, inflamatórias e de função endotelial. Estudo do Rio de Janeiro.

Dados sobre a avaliação não invasiva da rigidez vascular e suas relações com variáveis de risco cardiovascular são escassos em jovens. Objetiva avaliar a relação entre a velocidade de onda de pulso (VOP) e a pressão arterial (PA), variáveis antropométricas, metabólicas, inflamatórias e de disfunção endotelial em indivíduos adultos jovens. Foram estudados 96 indivíduos (51 homens) do Estudo do Rio de Janeiro, em duas avaliações, A1 e A2, com intervalo de 17,691,58 anos (16 a 21 anos). Em A1 foram avaliados em suas escolas (10-15 anos - média 12,421,47 anos) e em A2 foram novamente avaliados em nível ambulatorial (26-35 anos - média 30,091,92 anos). Em A1 foram obtidos pressão arterial (PA) e índice de massa corporal (IMC). Em A2 foram obtidos a velocidade da onda de pulso (VOP)-método Complior, PA, IMC, circunferência abdominal (CA), glicose, perfil lipídico, leptina, insulina, adiponectina, o índice de resistência à insulina HOMA-IR, proteína C-Reativa ultrassensível (PCRus) e as moléculas de adesão E-selectina, Vascular Cell Adhesion Molecule-1(VCAM-1) e Intercellular Adhesion Molecule-1 (ICAM-1). Foram obtidos, ainda, a variação da PA e do IMC entre as 2 avaliações. Em A2 os indivíduos foram estratificados segundo o tercil da VOP para cada sexo. Como resultados temos: 1) Os grupos foram constituídos da seguinte forma: Tercil 1:homens com VOP < 8,69 m/s e mulheres com VOP < 7,66 m/s; Tercil 2: homens com VOP ≥ 8,69 m/s e < 9,65m/s e mulheres com VOP ≥ 7,66 m/s e < 8,31m/s;Tercil 3:homens com VOP ≥ 9,65 m/s e mulheres com VOP ≥ 8,31 m/s. 2) O grupo com maior tercil de VOP mostrou maiores médias de PA sistólica (PAS) (p=0,005), PA diastólica (PAD) (p=0,007), PA média (PAM) (p=0,004), variação da PAD (p=0,032), variação da PAM (p=0,003), IMC (p=0,046), variação do IMC (p=0,020), insulina (p=0,019), HOMA-IR (p=0,021), E-selectina (p=0,032) e menores médias de adiponectina (p=0,016), além de maiores prevalências de diabetes mellitus/intolerância à glicose (p=0,022) e hiperinsulinemia (p=0,038); 3) Houve correlação significativa e positiva da VOP com PAS (p<0,001), PAD (p<0,001), PP (p=0,048) e PAM (p<0,001) de A2, com a variação da pressão arterial (PAS, PAD e PAM) (p<0,001) entre as duas avaliações, com o IMC de A2 (p=0,005) e com a variação do IMC (p<0,001) entre as duas avaliações, com CA (p=0,001), LDLcolesterol (p=0,049) e E-selectina (p<0,001) e correlação negativa com HDLcolesterol (p<0,001) e adiponectina (p<0,001); 4)Em modelo de regressão múltipla, após ajuste do HDL-colesterol, LDLcolesterol e adiponectina para sexo, idade, IMC e PAM, apenas o sexo masculino e a PAM mantiveram correlação significativa com a VOP. A VOP em adultos jovens mostrou relação significativa com variáveis de risco cardiovascular, destacando-se o sexo masculino e a PAM como importantes variáveis no seu determinismo. Os achados sugerem que a medida da VOP pode ser útil para a identificação do acometimento vascular nessa faixa etária.

Validação da impedância bioelétrica para determinação da composição corporal em mulheres no período pós parto

O período pós-parto pode ser considerado a fase em que a mulher está exposta a retenção de massa corporal (MC) e desenvolvimento da obesidade. Na maioria das situações valorizam-se mais a perda de MC e pouco se conhece a respeito dos componentes que estão sendo mobilizados. Desta forma, há interesse de se validar técnicas acessíveis, como a impedância bioelétrica (BIA), que possam ser aplicadas no acompanhamento nutricional destas mulheres. O presente estudo teve como objetivo validar diferentes modelos de impedância bioelétrica (BIA) para a determinação da composição corporal em mulheres pós-parto tendo como ?padrão ouro? a técnica de absorciometria de dupla energia de raio X(DXA). A amostra foi composta por 46 mulheres no período pós-parto com idade acima de 18anos, inicialmente recrutadas e convidadas a participar da pesquisa, logo após o parto, para posteriormente serem avaliadas. A composição corporal (CC) foi mensurada através de três aparelhos distintos de BIA: RJL , BIO e Tanita e pela DXA. Os componentes101450BC 533corporais medidos foram: massa livre de gordura (MLG), massa gorda (MG) e percentual degordura corporal (%GC). Na análise estatística foram calculadas as médias e desvio-padrãodas variáveis contínuas. A concordância entre os componentes corporais determinados pelaDXA e cada BIA foi avaliada pelo método de Bland & Altman e pelo coeficiente decorrelação de concordância (CCC). Para comparação de médias das variáveis obtidas por BIAe DXA para cada faixa de índice de massa corporal (IMC), foi aplicada a ANOVA e oadotado o teste post-hoc de Tukey. O nível de significância adotado foi de 95% (p=0,05). Amédia ( desvio padrão) de idade foi de 25,5 4,6 anos, a MC de 73,6 12,2kg, o IMC de28,7 4,3kg/m, a MG de 29,87,4kg, a MLG de 43,25,7kg e o %GC de 41,84,3%,obtidos pelo DXA. Ao comparar-se os resultados dos diferentes equipamentos com o método padrão-ouro, verificou-se que houve diferença significativa entre a DXA e as BIA para todos componentes corporais, com exceção da MG fornecida pelo RJL (27,1Kg) e TAN (27,1Kg)em relação à DXA (29,8Kg). Os resultados mostraram haver uma boa reprodutibilidade emrelação aos aparelhos de BIA TAN (r=0,74; r=0,90) e RJL (r=0,78; r=0,89) para MLG e MG.Verificou-se que os equipamentos de BIA TAN e RJL forneceram estimativas semelhantes em relação à MLG, MG e %GC. Em relação aos valores da DXA o equipamento que mais se aproximou foi a TAN e o RJL quando avaliada a MG considerando todas as mulheres, mas quando estratificadas segundo o IMC, a análise foi mais acurada em mulheres obesas.Entretanto, a concordância não foi satisfatória entre os componentes corporais fornecidos pelas BIA em relação à DXA. As BIAs avaliadas no presente estudo subestimaram o %GC e superestimaram a MLG para esse grupo de mulheres no período pós-parto. Conclui-se que as BIA avaliadas não são recomendadas para avaliação da CC neste grupo de mulheres no período pós-parto.

Níveis circulantes de Grelina, índices de adiposidade e fatores de risco cardiovascular e metabólico relacionados, em população multiétnica do Estado do Rio de Janeiro

O objetivo deste estudo foi analisar o comportamento dos níveis plasmáticos de grelina, em relação aos fatores de risco cardiometabólico, em uma população multiétnica de eutróficos e de obesos..A grelina é um peptídeo produzido predominantemente pelas células oxínticas gástricas, que desempenha importante papel na homeostase energética, promovendo estímulo do apetite e aumento do peso corporal, além de participar do controle do metabolismo lipídico e glicídico, interagindo diretamente com os fatores de risco cardiometabólico. Este é um estudo transversal. Duzentos indivíduos entre 18 e 60 anos com diferentes graus de índice de massa corporal (IMC) compuseram a amostra, assim dividida: cem eutróficos (IMC < 25 kg/m2) e 100 obesos (IMC ≥ 30 kg/m2). Todos foram avaliados para parâmetros antropométricos, determinação da pressão arterial (aferida por método oscilométrico através de monitor automático) e variáveis metabólicas (métodos usuais certificados). A grelina acilada foi mensurada pela técnica de sanduíche ELISA; a leptina, pelo método Milliplex MAP. O marcador inflamatório proteína C reativa ultrassensível(PCRUS)foi estimado por nefelometria ultrassensível. A insulina foi determinada por quimioluminescência e o HOMA-IR calculado pelo produto insulinemia (U/ml) X níveis de glicemia de jejum (mmol/L) / 22.5. Foram excluídos do estudo aqueles com história de comorbidades crônicas, doenças inflamatórias agudas, dependência de drogas e em uso de medicação nos dez dias anteriores à entrada no estudo. As concentrações de grelina acilada mostraram tendência de redução ao longo dos graus de adiposidade (P<0,001); a leptina se comportou de maneira oposta (P<0,001). Os níveis de grelina se correlacionaram negativamente com IMC (r = -.36; P<0,001), circunferência da cintura (CC) (r=-.34; P<0,001), relação cintura/quadril (RCQ) (r=-.22; P=0,001), diâmetro abdominal sagital (DAS) (r=-.28; P<0,001), pressão arterial sistólica (PAS) (r=-.21; P=0,001), insulina (r=-.27; P<0,001), HOMA-IR (r=-.24; P=0,001) e PCRUS (r=-.29; P<0,001); e positivamente com o HDL-colesterol (r=.30; P<0,001).A PCRUS acompanhou o grau de resistência insulínica e os níveis de grelina também mostraram tendência de redução ao longo dos tercis de resistência insulínica (P=0,001). Em modelo de regressão linear múltipla as principais associações independentes da grelina acilada foram sexo feminino (P=0,005) e HDL-colesterol (P=0,008), ambos com associação positiva e IMC (P<0,001) (associação negativa). Esses achados apontam para uma associação da grelina acilada com melhor perfil metabólico, já que seus níveis se correlacionaram positivamente com HDL-colesterol e negativamente com indicadores de resistência insulínica e atividade inflamatória.

Offshore Migratory Corridors and Aerial Photogrammetric Body Length Comparisons of Southbound Gray Whales, Eschrichtius robustus, in the Southern California Bight, 1988–1990

Through most of their annual migration, gray whales, Eschrichtius robustus, remain within 10 km of shore, but in the Southern California Bight many individuals migrate much farther from shore. This paper summarizes aerial survey and photogrammetric efforts to determine body lengths and temporal and spatial distributions of migratory gray whales in the southern portion of the Southern California Bight. Aerial surveys were flown along 13 east–west transects between lat. 32°35′N and 33°30′N during the southbound gray whale migratory seasons of 1988–90 in the Southern California Bight. Photogrammetry was used to obtain body length estimates of animals during some of the surveys. A total of 1,878 whales in 675 groups were sighted along 25,440 km of transect distance flown and 217 body lengths were measured. Using position and heading data, three major migratory pathways or corridors in the southern portion of the bight are defined. Those migrating offshore were split almost evenly between two corridors along the west sides of Santa Catalina and San Clemente Islands. These corridors converge on the mainland coast between San Diego and the United States–Mexico border. No whales larger than 11.5 m were photographed within 30 km of the mainland coast, suggesting that smaller, and presumably younger, whales use the coastal migratory corridor through the California Bight.

Avaliação da técnica de impedância bioelétrica na identificação das alterações da composição corporal em mulheres no período pós-parto

Este trabalho teve como objetivo verificar se a técnica de impedância bioelétrica (IB) identifica as modificações da composição corporal em mulheres no período pós-parto. Participaram do estudo 47 mulheres (≥ 18 anos), nas quais foram avaliadas massa livre de gordura (MLG), massa gorda (MG) e percentual de gordura corporal (%GC) pelos equipamentos IB_Tanita BC 533; IB_RJL 101 e por absorciometria de raio X de dupla energia (DXA). Todas as avaliações foram feitas no mesmo dia. Posteriormente, as mulheres foram categorizadas em dois grupos: com perda ponderal (n= 24) e com ganho ponderal (n= 22). Os valores médios das alterações da composição corporal (CC), foram comparados intra-métodos e em relação ao método padrão-ouro (DXA) através de teste T-pareado. A concordância entre as diferenças das alterações da CC obtidas pelas IB e DXA foi avaliada pelo método de Bland & Altman e pelo coeficiente de correlação intraclasse (CCI). A média  desvio padrão de idade foi de 26,7  5,2 anos e o tempo médio da captação no pós-parto para a primeira avaliação foi de 2,6  2,0 meses e 8,0  2,7 meses para a segunda avaliação. A média de massa corporal (MC) foi de 74,6  11,4 kg na primeira avaliação e 75,1  12,6 kg na segunda avaliação, correspondendo a um valor de índice de massa corporal (IMC) de 28,8  4,0 kg/m2 e 29,0  4,6 kg/m2, respectivamente. O %GC medido pela DXA foi de 40,1  4,9 % para a primeira avaliação e de 41,0  5,2 %, para a segunda avaliação, representando uma MG de 30,2  6,6 kg e de 30,9  8,0 kg, respectivamente. Ambas as IB subestimaram a alteração do % GC (-0,7 % para IB_Tanita e -1,1% para IB_RJL) e MG (-0,6 kg para IB_Tanita e -1,0 kg IB_RJL) em relação ao DXA. Por sua vez, as alterações de MLG foram superestimadas 0,8 kg pela IB_Tanita e 1,0 kg IB_RJL. Houve boa concordância (CCI ≥ 0,75) entre as alterações identificadas para MG pela IB_Tanita e por DXA e satisfatória pela IB_RJL. Dessa forma o presente estudo verificou um desempenho satisfatório da técnica de IB em identificar as alterações da MG gorda e que a IB_Tanita mostrou-se melhor que a IB_RJL na estimativa da alteração desse componente corporal nesse grupo de mulheres pós-parto.

Estudo do perfil clínico, metabólico, hormonal e inflamatório de crianças pré-púberes nascidas com baixo peso e sua relação com a prematuridade, retardo do crescimento intrauterino e ganho ponderal pós-natal

O baixo peso ao nascer (BPN) possui grande impacto na mortalidade neonatal, assim como no desenvolvimento de complicações futuras, como obesidade, hipertensão arterial sistêmica e resistência insulínica, condições relacionadas à doença cardiovascular aterosclerótica, principal causa de morbimortalidade no mundo. O objetivo desta pesquisa foi estudar o perfil clínico, metabólico, hormonal e inflamatório relacionado à doença cardiovascular em crianças pré-púberes de BPN, bem como avaliar a influência do BPN, prematuridade e restrição do crescimento intrauterino nas variáveis de interesse. Realizou-se estudo transversal com 58 crianças de dois a sete anos de BPN, sendo 32 prematuros adequados para idade gestacional (AIG), 17 prematuros pequenos para idade gestacional (PIG), 9 a termo PIG e 38 crianças de peso ao nascer adequado, nascidas no Hospital Universitário Pedro Ernesto da Universidade do Estado do Rio de janeiro, oriundas do Ambulatório de Pediatria Geral deste mesmo hospital. Frequências de perfil lipídico alterado, assim como medianas das variações no Z escore de peso e estatura do nascimento até o momento do estudo, do Z escore de índice de massa corporal (ZIMC), da circunferência da cintura, da pressão arterial sistólica e diastólica, do colesterol total, da lipoproteína de baixa densidade, da lipoproteína de baixa densidade, do triglicerídeo, da glicose, insulina, do Homeostasis Assessment for Insulin Resistance (HOMA-IR), da leptina, da adiponectina, da interleucina 6 e da proteína C reativa foram comparadas entre os dois grupos. No grupo de BPN, avaliou-se a correlação entre estas mesmas variáveis e peso de nascimento, idade gestacional, Z escores de peso e comprimento de nascimento e variações no Z escore de peso e comprimento até o primeiro ano, e até o momento do estudo, com ajuste para idade e sexo. O grupo de BPN apresentou maiores variações nos Z escore de peso (p-valor 0,0002) e estatura (p-valor 0,003) até o momento do estudo e menores níveis de adiponectina (p-valor 0,027). Não houve correlação entre as variáveis associadas ao risco cardiovascular e o grau de baixo peso, prematuridade ou crescimento intrauterino retardado. Os níveis de ZIMC (p-valor 0,0001), circunferência da cintura (p-valor 0,0008), pressão arterial diastólica (p-valor 0,046), insulina (p-valor 0,02), HOMA-IR (p-valor 0,016) e leptina (p-valor= 0,0008) se correlacionaram com a variação no Z escore de peso no primeiro ano. O ZIMC (p-valor 0,042) também se correlacionou com a variação do Z escore de comprimento no primeiro ano. Houve ainda correlação entre o ZIMC (p-valor 0,0001), circunferência da cintura (p-valor 0,0001), pressão arterial sistólica (p-valor 0,022), pressão arterial diastólica (p-valor 0,003), insulina (p-valor 0,007), HOMA-IR (p-valor 0,005) e leptina (p-valor 0,0001) com a variação no Z escore de peso até o momento do estudo. Os achados mostram que este grupo de crianças pré-púberes com BPN ainda não diferem do grupo de crianças nascidas com peso adequado exceto pelos níveis de adiponectina, sabidamente um protetor cardiovascular. Em relação às análises de correlação, nem o peso ao nascer, tampouco a prematuridade ou CIUR, influenciaram as variáveis de interesse. No entanto, fatores pós-natais como o ganho pondero-estatural se correlacionaram com o ZIMC, circunferência da cintura, pressão arterial sistólica e diastólica, insulina, HOMA-IR e leptina. Mais estudos são necessários para avaliar se os achados configuram risco cardiovascular aumentado neste grupo de pacientes.

Geographical and morphological variation within and between colour phases inCoris julis(L. 1758), a protogynous marine fish

The possible differences between sexes in patterns of morphological variation in geographical space have been explored only in gonochorist freshwater species. We explored patterns of body shape variation in geographical space in a marine sequential hermaphrodite species, Coris julis (L. 1758), analyzing variation both within and between colour phases, through the use of geometric morphometrics and spatially-explicit statistical analyses. We also tested for the association of body shape with two environmental variables: temperature and chlorophyll a concentration, as obtained from time-series of satellite-derived data. Both colour phases showed a significant morphological variation in geographical space and patterns of variation divergent between phases. Although the morphological variation was qualitatively similar, individuals in the initial colour phase showed a more marked variation than individuals in the terminal phase. Body shape showed a weak but significant correlation with environmental variables, which was more pronounced in primary specimens.