Fast changes in seasonal forest communities due to soil moisture increase after damming.

Local changes caused by dams can have drastic consequences for ecosystems, not only because they change the water regime but also the modification on lakeshore areas. Thus, this work aimed to determine the changes in soil moisture after damming, to understand the consequences of this modification on the arboreal community of dry forests, some of the most endangered systems on the planet. We studied these changes in soil moisture and the arboreal community in three dry forests in the Araguari River Basin, after two dams construction in 2005 and 2006, and the potential effects on these forests. For this, plots of 20 m x 10 m were distributed close to the impoundment margin and perpendicular to the dam margin in two deciduous dry forests and one semi-deciduous dry forest located in Southeastern Brazil, totaling 3.6 ha sampled. Besides, soil analysis were undertaken before and after impoundment at three different depths (0-10, 20-30 and 40-50 cm). A tree (minimum DBH of 4.77 cm) community inventory was made before (TO) and at two (T2) and four (T4) years after damming. Annual dynamic rates of all communities were calculated, and statistical tests were used to determine changes in soil moisture and tree communities. The analyses confirmed soil moisture increases in all forests, especially during the dry season and at sites closer to the reservoir; besides, an increase in basal area due to the fast growth of many trees was observed. The highest turnover occurred in the first two years after impoundment, mainly due to the higher tree mortality especially of those closer to the dam margin. All forests showed reductions in dynamic rates for subsequent years (T2-T4), indicating that these forests tended to stabilize after a strong initial impact. The modifications were more extensive in the deciduous forests, probably because the dry period resulted more rigorous in these forests when compared to semideciduous forest. The new shorelines created by damming increased soil moisture in the dry season, making plant growth easier. We concluded that several changes occurred in the T0-T2 period and at 0-30 m to the impoundment, mainly for the deciduous forests, where this community turned into a "riparian-deciduous forest" with large basal area in these patches. However, unlike other transitory disturbances, damming is a permanent alteration and transforms the landscape to a different scenario, probably with major long-term consequences for the environment.

Heterogeneity of Cerebrospinal Fluid Biomarkers Profiles in Individuals with Distinct Levels of Cognitive Decline: A Cross-Sectional Study.

BACKGROUND: Decreased cerebrospinal fluid (CSF) concentrations of the amyloid-ß (Aß), along with increased total (T-tau) and phosphorylated tau protein (P-tau), are widely accepted as core biomarkers of Alzheimer's disease (AD) pathology. Nonetheless, there are a few remaining caveats that still preclude the full incorporation of AD biomarkers into clinical practice. OBJECTIVE: To determine the frequency of clinical-biological mismatches in a clinical sample of older adults with varying degrees of cognitive impairment. METHODS: 204 participants were enrolled for a cross-sectional assessment and allocated into diagnostic groups: probable AD (n = 60, 29.4%); MCI (n = 84, 41.2%); or normal cognition (NC, n = 60, 29.4%). CSF concentrations of Aß42, T-tau, and 181Thr-P-tau were determined, and Aß42/P-tau ratio below 9.53 was used as a proxy of AD pathology. The AT(N) classification was further used as a framework to ascertain the biological evidence of AD. RESULTS: The majority (73.7%) of patients in the AD group had the Aß42/P-tau ratio below the cut-off score for AD, as opposed to a smaller proportion in the MCI (42.9%) and NC (23.3%) groups. In the latter, 21 subjects (35%) were classified as A+, 28 (46.7%) as T+, and 23 (38.3%) as N + . In the AD group, 66.7%of the cases were classified as A+, 78.3%as T+, and 80%as N+. CONCLUSION: Analysis of CSF biomarkers was able to discriminate between AD, MCI, and NC. However, clinical-biological mismatches were observed in a non-negligible proportion of cases.

Persistence of Coffea arabica and its relationship with the structure, species diversity and composition of a secondary forest in Brazil.

Understanding the relationships between Coffea arabica L. and the native tree community of secondary forests regrowing after the abandonment of coffee plantations is important because, as a non-native species in the Neotropics, coffee can outcompete native species, reducing diversity and forests ecosystem services. We aimed to answer three questions: 1) Does coffee regeneration in secondary forests differ between shaded and unshaded abandoned plantations?; 2) How is coffee basal area related to structural attributes, species diversity and composition of the native community?; and 3) Do the relationships between coffee and native community differ between tree and sapling components? We sampled the tree and sapling components in a seasonal tropical dry forest that were previously used as shaded and unshaded coffee plantations. Coffee was the most important species in the sapling component of shaded systems, but was almost absent in unshaded ones. Coffee basal area was negatively related with the native density and absolute species richness of the sapling component; and was negatively related with tree density, and positively related with the percentage of pioneer individuals of the native tree component. Our results indicate that coffee persists in secondary forest communities even after more than 70 years of shaded-coffee plantations were abandoned, potentially reducing density and diversity of native species. Despite limitations, which hinder more general conclusions on coffee invasiveness in Brazilian secondary tropical forests, our results indicate that coffee is a strong competitor in the studied secondary forests and provide important insights for future research on this topic.

Fast changes in seasonal forest communities due to soil moisture increase after damming / Cambios estacionales acelerados en comunidades boscosas debidos al aumento en la humedad del suelo después de la construcción de una represa

Local changes caused by dams can have drastic consequences for ecosystems, not only because they change the water regime but also the modification on lakeshore areas. Thus, this work aimed to determine the changes in soil moisture after damming, to understand the consequences of this modification on the arboreal community of dry forests, some of the most endangered systems on the planet. We studied these changes in soil moisture and the arboreal community in three dry forests in the Araguari River Basin, after two dams construction in 2005 and 2006, and the potential effects on these forests. For this, plots of 20m x10m were distributed close to the impoundment margin and perpendicular to the dam margin in two deciduous dry forests and one semi-deciduous dry forest located in Southeastern Brazil, totaling 3.6ha sampled. Besides, soil analysis were undertaken before and after impoundment at three different depths 0-10, 20-30 and 40-50cm. A tree minimum DBH of 4.77cm community inventory was made before T0 and at two T2 and four T4 years after damming. Annual dynamic rates of all communities were calculated, and statistical tests were used to determine changes in soil moisture and tree communities. The analyses confirmed soil moisture increases in all forests, especially during the dry season and at sites closer to the reservoir; besides, an increase in basal area due to the fast growth of many trees was observed. The highest turnover occurred in the first two years after impoundment, mainly due to the higher tree mortality especially of those closer to the dam margin. All forests showed reductions in dynamic rates for subsequent years T2-T4, indicating that these forests tended to stabilize after a strong initial impact. The modifications were more extensive in the deciduous forests, probably because the dry period resulted more rigorous in these forests when compared to semideciduous forest. The new shorelines created by damming increased soil moisture in the dry season, making plant growth easier. We concluded that several changes occurred in the T0-T2 period and at 0-30m to the impoundment, mainly for the deciduous forests, where this community turned into a riparian-deciduous forest with large basal area in these patches. However, unlike other transitory disturbances, damming is a permanent alteration and transforms the landscape to a different scenario, probably with major long-term consequences for the environment.

Los cambios locales provocados por las represas pueden tener consecuencias para un ecosistema, ya que no solo cambian el régimen de las aguas, sino que también modifican las áreas a la orilla de los lagos. Por lo tanto, este trabajo tuvo como objetivo observar los cambios en la humedad del suelo después de la construcción de represas, para entender las consecuencias de esta modificación a la comunidad arbórea de los bosques secos, que son uno de los sistemas más amenazados del planeta. Después de la construcción de tres represas, se estudiaron los cambios en la humedad del suelo y la comunidad arbórea en 3 bosques secos de la cuenca del río Araguari, en donde se construyeron dos represas en 2005 y 2006. Se demarcaron parcelas de 20x10m que se distribuyeron cerca y perpendicular al margen de la represa en dos bosques secos caducifolios y un bosque seco semideciduo ubicado en el sureste de Brasil, en total se muestrearon 3.6 hectáreas. Se realizó un análisis de la humedad del suelo antes y después de la construcción del embalse en tres profundidades 0-10, 20-30, 40-50cm. El inventario de la comunidad arbórea DAP de 4.77cm se realizó antes T0, dos T2 y cuatro T4 años a partir de la retención del agua. Además se calcularon las tasas anuales dinámicas de todas las comunidades, y se utilizaron pruebas estadísticas para confirmar los cambios en la humedad del suelo y las comunidades de árboles. Los análisis confirmaron aumento de humedad del suelo en todos los bosques, especialmente durante la estación seca y en los lugares más cercanos al embalse, con un aumento del área basal debido al rápido crecimiento de muchos árboles. El mayor volumen de modificaciones se produjo en los primeros dos años después de La construcción del embalse, principalmente debido a la mayor mortalidad de los árboles más cerca del margen de la represa. Sin embargo, todos los bosques mostraron reducción de las tasas dinámicas en los años siguientes T2-T4, lo que indica que estos bosques tienden a estabilizarse después de un fuerte primer impacto. Las modificaciones fueron más severas en los bosques caducifolios, probablemente debido a una estación seca más severa en estos bosques en comparación con el semideciduo. Las nuevas márgenes creadas por el embalse aumentaron la humedad del suelo en la época seca facilitando el crecimiento de muchas plantas. Se concluye que los cambios que se produjeron en el período de T0-T2 y de 0-30m del embalse, principalmente en los bosques caducifolios estan transformando estas comunidades en bosque de ribera-caducifolia con gran área basal en estos parches. Sin embargo, este impacto es diferente a otras alteraciones transitorias, así la construcción del embalse es un cambio permanente y transforma el paisaje en otro escenario, probablemente con importantes consecuencias a largo plazo para el ambiente.