Immunohistochemical changes in vulnerable rat brain regions after reversible global brain ischaemia

Human global ischaemia was simulated in adult rats by inducing 20 min brain ischaemia and 60 min post-ischaemic recirculation. Immunohistochemical expression of MMP-9, TIMP-3, Bax and Bcl-2, and DNA fragmentation (with the TUNEL reaction) were investigated. The morphological data showed different neuronal responses in the hippocampus compared with the cerebral and cerebellar cortices. MMP-9 immunoreactivity was different in the hippocampus, particularly in dentate gyrus and the CA1 region, compared with these cortices. Negative TIMP-3 staining in ischaemic hippocampal neurons may indicate a loss of its inhibitory activity on MMP-9 that could enhance cell death. Bcl-2 down regulation, Bax positivity and TUNEL+ type II cells in the dentate gyrus granular layer could be responsible for induction of apoptotic death in CA1 hippocampal pyramidal cells via loss of fibre input. Results suggest differential behaviours of neural cells after 60 min reperfusion.     

Rapid leaf development drives the seasonal pattern of volatile organic compound (VOC) fluxes in a ‘coppiced’ bioenergy poplar plantation

Leaves of fast‐growing, woody bioenergy crops often emit volatile organic compounds (VOC). Some reactive VOC (especially isoprene) play a key role in climate forcing and may negatively affect local air quality. We monitored the seasonal exchange of VOC using the eddy covariance technique in a ‘coppiced’ poplar plantation. The complex interactions of VOC fluxes with climatic and physiological variables were also explored by using an artificial neural network (Self Organizing Map). Isoprene and methanol were the most abundant VOC emitted by the plantation. Rapid development of the canopy (and thus of the leaf area index, LAI) was associated with high methanol emissions and high rates of gross primary production (GPP) since the beginning of the growing season, while the onset of isoprene emission was delayed. The highest emissions of isoprene, and of isoprene photo‐oxidation products (Methyl Vinyl Ketone and Methacrolein, i_ox), occurred on the hottest and sunniest days, when GPP and evapotranspiration were highest, and formaldehyde was significantly deposited. Canopy senescence enhanced the exchange of oxygenated VOC. The accuracy of methanol and isoprene emission simulations with the Model of Emissions of Gases and Aerosols from Nature increased by applying a function to modify their basal emission factors, accounting for seasonality of GPP or LAI.     

Leaf carbon assimilation in a water-limited world

Abstract

Over the past 150 years the amount of CO₂ in the atmosphere has been increasing, largely as a result of land-use change and anthropogenic emissions from the burning of fossil fuels. It is estimated that the atmospheric [CO₂] will reach 70 Pa by the end of the 21st Century. The most important consequence of this rise in [CO₂] is warming the surface temperature of the Earth by 0.4 – 0.6°C per decade throughout the 21st Century. Increasing [CO₂] along with associated changes in temperature will most likely alter the structure and function of agro-ecosystems, affecting their productivity and their role as stable sinks to CO₂ sequestration. Both CO₂ and temperature are key variables affecting plant growth, development and functions. Moreover, because of the future scenario of higher temperature and evaporative demand, drought occurrences will be increased in frequency, intensity, and erratic pattern. The combination of elevated temperatures and the increased incidence of environmental stress will probably constitute the greatest risk caused by climate change to the agro-ecosystems in arid or semiarid areas of the world. The purpose of this paper is to review the exchange of carbon driving the main ecophysiological processes of plants in response to climate change and environmental stresses. Drought and salinity first affect the acquisition of CO₂ by increasing stomatal and mesophyll resistances, and only after cause irreversible damages to the biochemical apparatus. Heat stress denatures thylakoid membranes, but this action may be counteracted by the synthesis of many isoprenoids in the chloroplasts from carbon freshly fixed by photosynthesis. There is rising concern about the impact of environmental stress on tree growth with this future scenario of global climate change. The combination of elevated temperatures and the increased incidence of environmental stress (particularly drought and salinity) will probably constitute the greatest risk caused by global climate change to the forest ecosystems in arid or semiarid areas of the world.     

Modeling the Emergence of Contact Languages

Contact languages are born out of the non-trivial interaction of two (or more) parent languages. Nowadays, the enhanced possibility of mobility and communication allows for a strong mixing of languages and cultures, thus raising the issue of whether there are any pure languages or cultures that are unaffected by contact with others. As with bacteria or viruses in biological evolution, the evolution of languages is marked by horizontal transmission; but to date no reliable quantitative tools to investigate these phenomena have been available. An interesting and well documented example of contact language is the emergence of creole languages, which originated in the contacts of European colonists and slaves during the 17th and 18th centuries in exogenous plantation colonies of especially the Atlantic and Indian Ocean. Here, we focus on the emergence of creole languages to demonstrate a dynamical process that mimics the process of creole formation in American and Caribbean plantation ecologies. Inspired by the Naming Game (NG), our modeling scheme incorporates demographic information about the colonial population in the framework of a non-trivial interaction network including three populations: Europeans, Mulattos/Creoles, and Bozal slaves. We show how this sole information makes it possible to discriminate territories that produced modern creoles from those that did not, with a surprising accuracy. The generality of our approach provides valuable insights for further studies on the emergence of languages in contact ecologies as well as to test specific hypotheses about the peopling and the population structures of the relevant territories. We submit that these tools could be relevant to addressing problems related to contact phenomena in many cultural domains: e.g., emergence of dialects, language competition and hybridization, globalization phenomena.     

Urban influences on the nitrogen cycle in Puerto Rico

Anthropogenic actions are altering fluxes of nitrogen (N) in the biosphere at unprecedented rates. Efforts to study these impacts have concentrated in the Northern hemisphere, where experimental data are available. In tropical developing countries, however, experimental studies are lacking. This paper summarizes available data and assesses the impacts of human activities on N fluxes in Puerto Rico, a densely populated Caribbean island that has experienced drastic landscape transformations over the last century associated with rapid socioeconomic changes. N yield calculations conducted in several watersheds of different anthropogenic influences revealed that disturbed watersheds export more N per unit area than undisturbed forested watersheds. Export of N from urban watersheds ranged from 4.8 kg ha^?1 year^?1 in the Río Bayamón watershed to 32.9 kg ha^?1 year^?1 in the highly urbanized Río Piedras watershed and 33.3 kg ha^?1 year^?1 in the rural-agricultural Río Grande de Añasco watershed. Along with land use, mean annual runoff explained most of the variance in fluvial N yield. Wastewater generated in the San Juan Metropolitan Area receives primary treatment before it is discharged into the Atlantic Ocean. These discharges are N-rich and export large amounts of N to the ocean at a rate of about 140 kg ha^?1 year^?1. Data on wet deposition of inorganic N ( $\hbox{NH}_{4}^{+}+\hbox{NO}_{3}^{-}Anthropogenic actions are altering fluxes of nitrogen (N) in the biosphere at unprecedented rates. Efforts to study these impacts have concentrated in the Northern hemisphere, where experimental data are available. In tropical developing countries, however, experimental studies are lacking. This paper summarizes available data and assesses the impacts of human activities on N fluxes in Puerto Rico, a densely populated Caribbean island that has experienced drastic landscape transformations over the last century associated with rapid socioeconomic changes. N yield calculations conducted in several watersheds of different anthropogenic influences revealed that disturbed watersheds export more N per unit area than undisturbed forested watersheds. Export of N from urban watersheds ranged from 4.8 kg ha⁻¹ year⁻¹ in the Río Bayamón watershed to 32.9 kg ha⁻¹ year⁻¹ in the highly urbanized Río Piedras watershed and 33.3 kg ha⁻¹ year⁻¹ in the rural-agricultural Río Grande de A?asco watershed. Along with land use, mean annual runoff explained most of the variance in fluvial N yield. Wastewater generated in the San Juan Metropolitan Area receives primary treatment before it is discharged into the Atlantic Ocean. These discharges are N-rich and export large amounts of N to the ocean at a rate of about 140 kg ha⁻¹ year⁻¹. Data on wet deposition of inorganic N () suggest that rates of atmospheric N deposition are increasing in the pristine forests of Puerto Rico. Stationary and mobile sources of NO _x (NO+NO₂) and N₂O generated in the large urban centers may be responsible for this trend. Comprehensive measurements are required in Puerto Rico to quantitatively characterize the local N cycle. More research is required to assess rates of atmospheric N deposition, N fixation in natural and human-dominated landscapes, N-balance associated with food and feed trade, and denitrification.