Mid- to late Holocene landscape change and anthropogenic transformations on Mo‘orea, Society Islands: a multi-proxy approach

Archaeology’s ability to generate long-term datasets of natural and human landscape change positions the discipline as an inter-disciplinary bridge between the social and natural sciences. Using a multi-proxy approach combining archaeological data with palaeoenvironmental indicators embedded in coastal sediments, we outline millennial timescales of lowland landscape evolution in the Society Islands. Geomorphic and cultural histories for four coastal zones on Mo‘orea are reconstructed based on stratigraphic records, sedimentology, pollen analysis, and radiocarbon determinations from mid- to late Holocene contexts. Prehuman records of the island’s flora and fauna are described utilizing landsnail, insect, and botanical data, providing a palaeo-backdrop for later anthropogenic change. Several environmental processes, including sea level change, island subsidence, and anthropogenic alterations, leading to changes in sedimentary budget have operated on Mo‘orea coastlines from c. 4600 to 200 BP. We document significant transformation of littoral and lowland zones which obscured earlier human activities and created significant changes in vegetation and other biota. Beginning as early as 440 BP (1416–1490 cal. ad), a major phase of sedimentary deposition commenced which can only be attributed to anthropogenic effects. At several sites, between 1.8 and 3.0 m of terrigenous sediments accumulated within a span of two to three centuries due to active slope erosion and deposition on the coastal flats. This phase correlates with the period of major inland expansion of Polynesian occupation and intensive agriculture on the island, indicated by the presence of charcoal throughout the sediments, including wood charcoal from several economically important tree species.

Relação dos salários como proxy de corrupção: os efeitos sobre as despesas de governos subnacionais no Brasil ( 1992 - 1998)

O objetivo desta dissertação foi verificar a influência da corrupção na taxa de crescimento do produto, investimentos públicos, gastos totais e gastos específicos dos governos estaduais do Brasil. Como não tínhamos um índice de percepção da corrupção como Mauro (1996) possuía para captar esta influência entre países, e Mauro (1998) e Van Rijckeghem e Weder (1997) já haviam demonstrado que a variável que melhor explicava este índice era a relação de salários entre o setor público e privado, utilizamos esta relação como variável para a proxy de corrupção por estado. Este tipo de variável nos possibilitou enxergar a corrupção em diferentes níveis: diferença na média, mediana, 25% piores (menos qualificados) e 25% melhores (mais qualificados). Não obtivemos qualquer evidência forte da influência da corrupção sobre a taxa de crescimento do produto ou sobre o nível de investimento público, mas a encontramos em alguns gastos específicos. Nossos resultados mais contundentes foram encontrados quando houve uma redução dos salários, o que indicaria um aumento na corrupção, levou a uma expansão dos gastos com assistência e previdência e a uma redução nos gastos com Administração e planejamento.

Proxy-reported health-related quality of life of patients with juvenile idiopathic arthritis: Pediatric rheumatology international trials organization multinational quality of life cohort study

Objective. To investigate the proxy-reported health-related quality of life (HRQOL) and its determinants in patients with juvenile idiopathic arthritis (JIA).Methods. In this multinational, multicenter, cross-sectional study, HRQOL of patients with JIA was assessed through the Child Health Questionnaire (CHQ) and was compared with that of healthy children of similar age from the same geographic area. of joint inflammation, Childhood Health Assessment Questionnaire (CHAQ), and erythrocyte sedimentation rate.Results. A total of 6,639 participants (3,324 with JIA and 3,315 healthy) were enrolled from 32 countries. The mean SD physical and psychosocial summary scores of the CHQ were significantly lower in patients with JIA than in healthy children (physical: 44.5 +/- 10.6 versus 54.6 +/- 4.0, P < 0.0001; psychosocial: 47.6 +/- 8.7 versus 51.9 +/- 7.59 P < 0.0001), with the physical well-being domain being most impaired. Patients with persistent oligoarthritis had better HRQOL compared with other subtypes, whereas HRQOL was similar across patients with systemic arthritis, polyarthritis, and extended oligoarthritis. A CHAQ score > 1 and a pain intensity rating > 3.4 cm on a 10-cm visual analog scale were the strongest determinants of poorer HRQOL in the physical and psychosocial domains, respectively.Conclusion. We found that patients with JIA have a significant impairment of their HRQOL compared with healthy peers, particularly in the physical domain. Physical well-being was mostly affected by the level of functional impairment, whereas the intensity of pain had the greatest influence on psychosocial health.

Strontium isotopes measurement from bunker cave system: a contribution for the multi-proxy paleoclimate research of Central Europe

In recent years speleothem has been intensely studied due to its great potential of registering paleoclimate proxies but some considerably uncertaintiesregarding speleothem proxy interpretation still exist. In order to minimize these uncertainties, multi-proxy approach has been used. Here is presented the strontium isotope record from Bunker cave, northwest Germany. This cave was previously studied and has proved well record paleoclimate changes during Holocene for central Europe.87Sr/86Sr ratio is presented for rain water, A-horizon soil (water and leachate), C-horizon soil (water and leachate), host rock and host rock leachate, drip water and from a stalagmite (Bu4) previously dated covering the Holocene. Upper soil presented the higher values in contrast with host rock (lower values). Drip water and C-horizon presented intermediated ratios. Sr isotopesare used to track the source of 87Sr/86Sr in the Bunker system, resulting in a mixture between A-horizon soil, C-horizon soil and host rock. A decreasing trend in Bu4 indicates change in the Sr source in the system

Validating NCAR-CCSM last glacial maximum sea surface temperature in the tropical and South Atlantic with proxy-data

Last Glacial Maximum simulated sea surface temperature from the Paleo-Climate version of the National Center for Atmospheric Research Coupled Climate Model (NCAR-CCSM) are compared with available reconstructions and data-based products in the tropical and south Atlantic region. Model results are compared to data proxies based on the Multiproxy Approach for the Reconstruction of the Glacial Ocean surface product (MARGO). Results show that the model sea surface temperature is not consistent with the proxy-data in all of the region of interest. Discrepancies are found in the eastern, equatorial and in the high-latitude South Atlantic. The model overestimates the cooling in the southern South Atlantic (near 50 degrees S) shown by the proxy-data. Near the equator, model and proxies are in better agreement. In the eastern part of the equatorial basin the model underestimates the cooling shown by all proxies. A northward shift in the position of the subtropical convergence zone in the simulation suggests a compression or/and an equatorward shift of the subtropical gyre at the surface, consistent with what is observed in the proxy reconstruction. (C) 2008 Elsevier B.V. All rights reserved

Paleoenvironmental reconstruction of a Late Quaternary lagoon system in southern Brazil (Jaguaruna region, Santa Catarina state) based on multi-proxy analysis

This paper provides a paleoenvironmental reconstruction of a Late Quaternary lagoon system in the Jaguaruna region of Santa Catarina state, southern Brazil. Integrated results of bulk sedimentary organic matter characterization (delta C-13, delta N-15 and C/N), microfossil (pollen and diatom) and grain-size analysis from three shallow cores (similar to 2.5m depth) allowed us to propose an evolving paleogeographic scenario in this coastal region for the last ca. 5500 cal a BP. The lagoonal system in this area was more extensive during the mid-Holocene than today, with a gradual and continuous lagoon-sea disconnection until the present. We add to the debate regarding relative sea-level (RSL) variations for the Brazilian coast during the Holocene and discuss the importance of sedimentary dynamics for interpreting changes in coastal ecosystems. The multi-proxy analysis suggests that changes in coastal ecosystems could be directly related to local sedimentary processes, which are not necessarily linked to RSL fluctuations and/or to climatic variations. Copyright (c) 2011 John Wiley & Sons, Ltd.

Stable water isotopes of precipitation and firn cores from the northern Antarctic Peninsula region as a proxy for climate reconstruction

In order to investigate the climate variability in the northern Antarctic Peninsula region, this paper focuses on the relationship between stable isotope content of precipitation and firn, and main meteorological variables (air temperature, relative humidity, sea surface temperature, and sea ice extent). Between 2008 and 2010, we collected precipitation samples and retrieved firn cores from several key sites in this region. We conclude that the deuterium excess oscillation represents a robust indicator of the meteorological variability on a seasonal to sub-seasonal scale. Low absolute deuterium excess values and the synchronous variation of both deuterium excess and air temperature imply that the evaporation of moisture occurs in the adjacent Southern Ocean. The delta O-18-air temperature relationship is complicated and significant only at a (multi)seasonal scale. Backward trajectory calculations show that air-parcels arriving at the region during precipitation events predominantly originate at the South Pacific Ocean and Bellingshausen Sea. These investigations will be used as a calibration for ongoing and future research in the area, suggesting that appropriate locations for future ice core research are located above 600 m a.s.l. We selected the Plateau Laclavere, Antarctic Peninsula as the most promising site for a deeper drilling campaign.

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.

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).

Methodology to create a proxy climate index for environmental and Octopus vulgaris fishery studies at the Northwest Africa: analytical and mathematical analyses

Diploma de Estudios Avanzados y Tesis de Máster

The use of AARS activity as a proxy for zooplankton and ichthyoplankton growth rates

Programa de doctorado en Oceanografía