Residential mobility and neighborhood inequality during the transition to adulthood

There is ongoing interest on the outcomes of residential mobility during the young adulthood. In this paper, we examine movement in and out of disadvantaged and advantaged neighborhoods as individuals move out of the family home and experience significant life course events. Using longitudinal data on young adults in the United States from the National Longitudinal Study of Adolescent to Adult Health, we find that while the point-in-time measure of the neighborhood poverty gap (the difference between the most and least advantaged neighborhoods) remained nearly identical from adolescence to young adulthood. But the neighborhood poverty gap between individuals starting out in the least and most disadvantaged residential settings decreased by 18.2 percentage points. In other words, cross sectional estimates of the poverty gap do not capture the dynamism of changes in poverty with young adult transitions. Partner formation, home ownership, and educational attainment are important life course transitions associated with significant moves up and down the neighborhood poverty distribution.     

Evidences of Holocene transgression on Domingos Petrolini Swamp, southern coastal plain, Rio Grande do Sul, Brazil

The Domingos Petrolini Swamp, located on the Southern Coastal Plain of Rio Grande do Sul, near the town of Rio Grande, constitutes an ample holocene lagoonal deposit. Events related to the holocene transgression and their diverse phases of glacial-eustatic ocillations were found through palynological analysis. Bases on these palynological data, four distinct phases to the paleoenvironmental evolution of the ecosystem were identified. It has also shown a transgressive restricted marine sequence on the base , which suggests the existence of a coastal brackish lagoon or a marisme type of environment. Later, there was a gradation for continentality conditions along with a scarce pollinical record. The third phase is characterized by the presence of marine components and halophyte vegetation, showing another transgressive event in that place. Lastly, the end of direct marine influence over the swamp was recorded and also the vegetation development as it appears these days.