Carbon dioxide assimilation rate, gas and ion composition in samples, and bacterial production of organic matter within and above the Broken Spur and TAG hydrothermal fields, Mid-Atlantic Ridge

Rate of CO2 assimilation was determined above the Broken Spur and TAG active hydrothermal fields for three main ecosystems: (1) hydrothermal vents; (2) 300 m near-bottom layer of plume water; and (3) bottom sediments. In water samples from warm (40-45°C) vents assimilation rates were maximal and reached 2.82-3.76 µg C/l/day. In plume waters CO2 assimilation rates ranged from 0.38 to 0.65 µg C/l/day. In bottom sediments CO2 assimilation rates varied from 0.8 to 28.0 µg C/l/day, rising up to 56 mg C/kg/day near shrimp swarms. In the most active plume zone of the long-living TAG field bacterial production of organic matter (OM) from carbonic is up to 170 mg C/m**2/day); production of autotrophic process of bacterial chemosynthesis reaches about 90% (156 mg C/m**2/day). Thus, chemosynthetic production of OM in September-October is almost equal to that of photosynthetic production in the oceanic region. Bacterial production of OM above the Broken Spur hydrothermal field is one order lower and reaches only 20 mg C/m**2/day.

Régression de la calcification artérielle médiale comme avenue thérapeutique potentielle pour l'hypertension systolique isolée

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Régression de la calcification artérielle médiale comme avenue thérapeutique potentielle pour l'hypertension systolique isolée

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Seawater carbonate chemistry and calcification rate of eastern oyster Crassostrea virginica, 2011

Anthropogenic carbon dioxide (CO2) emissions reduce pH of marine waters due to the absorption of atmospheric CO2 and formation of carbonic acid. Estuarine waters are more susceptible to acidification because they are subject to multiple acid sources and are less buffered than marine waters. Consequently, estuarine shell forming species may experience acidification sooner than marine species although the tolerance of estuarine calcifiers to pH changes is poorly understood. We analyzed 23 years of Chesapeake Bay water quality monitoring data and found that daytime average pH significantly decreased across polyhaline waters although pH has not significantly changed across mesohaline waters. In some tributaries that once supported large oyster populations, pH is increasing. Current average conditions within some tributaries however correspond to values that we found in laboratory studies to reduce oyster biocalcification rates or resulted in net shell dissolution. Calcification rates of juvenile eastern oysters, Crassostrea virginica, were measured in laboratory studies in a three-way factorial design with 3 pH levels, two salinities, and two temperatures. Biocalcification declined significantly with a reduction of ~0.5 pH units and higher temperature and salinity mitigated the decrease in biocalcification.

Seawater carbonate chemistry and Emiliania huxleyi mass and size, 2011

About one-third of the carbon dioxide (CO2) released into the atmosphere as a result of human activity has been absorbed by the oceans, where it partitions into the constituent ions of carbonic acid. This leads to ocean acidification, one of the major threats to marine ecosystems and particularly to calcifying organisms such as corals, foraminifera and coccolithophores. Coccolithophores are abundant phytoplankton that are responsible for a large part of modern oceanic carbonate production. Culture experiments investigating the physiological response of coccolithophore calcification to increased CO2 have yielded contradictory results between and even within species. Here we quantified the calcite mass of dominant coccolithophores in the present ocean and over the past forty thousand years, and found a marked pattern of decreasing calcification with increasing partial pressure of CO2 and concomitant decreasing concentrations of CO3. Our analyses revealed that differentially calcified species and morphotypes are distributed in the ocean according to carbonate chemistry. A substantial impact on the marine carbon cycle might be expected upon extrapolation of this correlation to predicted ocean acidification in the future. However, our discovery of a heavily calcified Emiliania huxleyi morphotype in modern waters with low pH highlights the complexity of assemblage-level responses to environmental forcing factors.

El climatismo

En la actualidad, el lenguaje dominante en que se expresa la conciencia ecológica o ambiental gira alrededor del cambio climático antropogénico. La política de la ecología hoy día es la política del climatismo. El climatismo refleja, en primer lugar, la evolución de los discursos ambientales desde su aparición hasta el cambio de siglo y la nueva constelación política. En segundo lugar, encarna una configuración específica de actores y discursos en forma de un sentido común dominante a la hora de pensar la relación sociedad-medio natural, que generan un efecto de maquillaje verde, de pánico, de homogeneización métrica carbónica, y de sujeción estatal bajo el régimen Kioto. Todos estos efectos ayudan a crear o enmascarar inequidades. Tomar en cuenta ciertas visiones alternativas del régimen climático global puede ayudar a corregir estos efectos.

Diseño conceptual para la elaboración y desalcoholización de cerveza artesanal

Este trabajo de grado consistió en la elaboración y desalcoholización de 3 recetas de cerveza artesanal basadas en recetas previamente diseñadas -- Las cervezas fueron desalcoholizadas mediante un proceso de sublimación bajo vacío y luego reconstituidas con agua carbonatada -- Usando espectrometría infrarroja y cromatografía de gases se determinó que más del 98% del alcohol presente en cada una de las muestras originales fue removido exitosamente -- El grado de aceptación de cada una de las 6 variedades de cerveza se determinó mediante un panel de consumidores -- Los resultados del panel mostraron un mayor grado de aceptación para las cervezas alcohólicas que para las cervezas no alcohólicas y permitieron determinar que existían diferencias significativas entre el sabor de las cervezas no alcohólicas y las cervezas originales -- Por último se elaboró un diseño conceptual de la planta para la elaboración de cerveza con y sin alcohol a partir del cual se realizó un análisis económico en el que se observa que el proyecto no es económicamente viable bajo las condiciones estudiadas, presentando una TIR del 7% y un VPN ($1,054’498,368) menor a la inversión inicial ($1,151’965,681)

Preenchimento sedimentar de duas zonas de dinâmica diferenciada no sapal de Castro Marim

Dissertação de mest. em Estudos Marinhos e Costeiros Ramo Gestão Costeira, Faculdade de Ciências do Mar e do Ambiente, Univ. do Algarve, 2002