Aurelio Fernández, La libertad en el pensamiento griego. Crisis, Revista Española de Filosofía, Nº 85, enero-marzo 1975; ps . 100-115.

Fil: Rego, Francisco.

Josep Maria Ruiz Simon, A arte de Raimundo Lúlio e a teoria escolástica da ciência, trad. Fernando Salles, Instituto Brasileiro de Filosofía e Ciência “Raimundo Lúlio" (Ramon Llull), Sâo Paulo, 2004. ISBN: 85 - 89294 - 05 - 6. 368 p.

Fil: Mendoza, José María Felipe.

(Table 1) Stable isotope data of chemoherm carbonates at Hydrate Ridge on the Cascadia continental margin

Two active chemoherm build-ups growing freely up into the oceanic water column, the Pinnacle and the South East-Knoll Chemoherms, have been discovered at Hydrate Ridge on the Cascadia continental margin. These microbially-mediated carbonate formations rise above the seafloor by several tens of meters and display a pinnacle-shaped morphology with steep flanks. The recovered rocks are pure carbonates dominated by aragonite. Based on fabric and mineralogic composition different varieties of authigenic aragonite can be distinguished. Detailed visual and petrographic investigations unambiguously reveal the involvement of microbes during the formation of the carbonates. The fabric of the cryptocrystalline and fibrous aragonite can be described as thrombolitic. Fossilized microbial filaments in the microcrystalline aragonite indicate the intimate relationship between microbes and carbonates. The strongly 13C-depleted carbon isotope values of the samples (as low as -48.1 per mill PDB) are characteristic of methane as the major carbon source for the carbonate formation. The methane-rich fluids from which the carbonates are precipitated originate most probably from a gas reservoir below the bottom-simulating reflector (BSR) and rise through fault systems. The d18O values of the aragonitic chemoherm carbonates are substantially higher (as high as 5.0 per mill PDB) than the expected equilibrium value for an aragonite forming from ambient seawater (3.5 per mill PDB). As a first approximation this indicates formation from glacial ocean water but other factors are considered as well. A conceptual model is presented for the precipitation of these chemoherm carbonates based on in situ observations and the detailed petrographic investigation of the carbonates. This model explains the function of the consortium of archaea and sulfate-reducing bacteria that grows on the carbonates performing anaerobic oxidation of methane (AOM) and enabling the precipitation of the chemoherms above the seafloor surrounded by oxic seawater. Beggiatoa mats growing on the surface of the chemoherms oxidize the sulfide provided by sulfate-dependent anaerobic oxidation of methane within an oxic environment. The contact between Beggiatoa and the underlying microbial consortium represents the interface between the overlying oxic water column and an anoxic micro-environment where carbonate formation takes place.

Caso Karen Llantoy v. Perú. Documento No. CCPR/C/85/D/1153/2003

http://www.cdh.uchile.cl/libros/dh-mujeres/21llantoy.pdf

Calcium carbonate, sedimentation and mass accumulation rates at DSDP Site 85-572

At Site 572, located at 1°N, 114° W (3903 m water depth), we recovered a continuous hydraulic piston cored section of upper Miocene to upper Pleistocene pelagic sediments. The sediment is composed of biogenic carbonate and silica with nonbiogenic material as a minor component. Detailed analysis of the calcium carbonate content shows that the degree of variability in carbonate deposition apparently changed markedly between the late Miocene and Pliocene at this equatorial Pacific site. During this interval carbonate mass accumulation rates decreased from 2.6 to 0.8 g/cm**2 per 10**3 yr. If we assume that variations in CaCO3 content reflect changes in the degree of dissolution, then the detailed carbonate analysis would suggest that the degree of variability in carbonate deposition decreases by a factor of 5 as the dominant wavelength of variations increases significantly. However, if the variability in carbonate concentration is described in terms of changes in mean mass accumulation, calculations then suggest that relatively small changes in noncarbonate rates may be important in controlling the observed carbonate records. In addition, the analysis suggests that the degree of variability observed in pelagic carbonate data may in part reflect total accumulation rates. Intervals with high sedimentation rates show lower amplitude variations in concentration than intervals with lower sedimentation rates for the same degree of change in the carbonate accumulation rate.

El discurso narrativizado y las normalizaciones citativas : Dos formas solapadas de caracterizar la palabra ajena

Este trabajo de investigación tiene por objeto demostrar que, dentro de un continuum que existe en la reformulación del discurso ajeno en el propio, donde se pasa de una forma a otra casi sin solución de continuidad, se puede hablar de una gradación entre un polo más objetivo (o con pretensión de mayor objetividad) a un polo más subjetivo, donde la interpretación tendría un papel más significativo. El polo más objetivo lo ubicaríamos en el extremo izquierdo y lo ejemplificaríamos con el discurso directo, mientras que el polo más subjetivo ocuparía el extremo derecho y estaría representado por el discurso narrativizado y las nominalizaciones citativas. En medio de estos dos polos se encontrarían todas las demás formas de discurso referido. En el campo del discurso periodístico, donde la investigación fue realizada, se pudo corroborar que existe, en la mayoría de los casos, una elección por parte del locutor (en este caso el periodista) de utilizar una forma u otra. Podría ser objetivo para posteriores estudios el de determinar el criterio que prevalece en esta elección.