<p>El presente trabajo tiene por fin mostrar cómo la hermenéutica nihilista de Gianni Vattimo mediante su crítica a la hermenéutica ontológica de Gadamer recupera la figura de Walter Benjamin y la asocia al proyecto de Heidegger. Esto lleva a que el presente trabajo, en primer lugar, describa cuáles son las críticas que Vattimo le realiza a Gadamer; y, en segundo lugar, muestre cómo es posible aunar la filosofía de Heidegger con el pensamiento crítico de Benjamin. Por último, se indica mediante la congruencia de estos autores cómo es posible la construcción de un sujeto post-metafísico</p

Beaulieu, Claudie

Gloor, Manuel

Gruber, Nicolas

Jacobson, Andrew R.

Mikaloff Fletcher, Sara E.

Pacala, Stephen W.

Rodgers, Keith B.

Sarmiento, Jorge L.

El presente trabajo tiene por fin mostrar cómo la hermenéutica nihilista de Gianni Vattimo mediante su crítica a la hermenéutica ontológica de Gadamer recupera la figura de Walter Benjamin y la asocia al proyecto de Heidegger. Esto lleva a que el presente trabajo, en primer lugar, describa cuáles son las críticas que Vattimo le realiza a Gadamer; y, en segundo lugar, muestre cómo es posible aunar la filosofía de Heidegger con el pensamiento crítico de Benjamin. Por último, se indica mediante la congruencia de estos autores cómo es posible la construcción de un sujeto post-metafísico.The present work aims to show how the hermeneutics of nihilistic Gianni Vattimo using his criticism of the ontological hermeneutic of Gadamer retrieves the figure of Walter Benjamin and the associated with the project of Heidegger. This leads to the present work, in the first place, describe which are the criticisms that Vattimo you performed to Gadamer; and, secondly, show how it is possible combine the philosophy of Heidegger with the critical thinking of Benjamin. Finally, it is indicated by the consistency of these authors as is possible the construction of a subject postmetaphysical.Fil: Catoggio, Leandro Martín. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Lanús; Argentin

Catoggio, Leandro Martín

CONICET Digital

Spanish

The historic disease of hermeneutics and its dialectical transformation. The weak thought between Gadamer and Benjamin

We show here an updated estimate of the net land carbon sink (NLS) as a function of time from 1960 to 2007 calculated from the difference between fossil fuel emissions, the observed atmospheric growth rate, and the ocean uptake obtained by recent ocean model simulations forced with reanalysis wind stress and heat and water fluxes. Except for interannual variability, the net land carbon sink appears to have been relatively constant at a mean value of −0.27 Pg C yr&lt;sup&gt;−1&lt;/sup&gt; between 1960 and 1988, at which time it increased abruptly by −0.88 (−0.77 to −1.04) Pg C yr&lt;sup&gt;−1&lt;/sup&gt; to a new relatively constant mean of −1.15 Pg C yr&lt;sup&gt;−1&lt;/sup&gt; between 1989 and 2003/7 (the sign convention is negative out of the atmosphere). This result is detectable at the 99% level using a t-test. The land use source (LU) is relatively constant over this entire time interval. While the LU estimate is highly uncertain, this does imply that most of the change in the net land carbon sink must be due to an abrupt increase in the land sink, LS = NLS – LU, in response to some as yet unknown combination of biogeochemical and climate forcing. A regional synthesis and assessment of the land carbon sources and sinks over the post 1988/1989 period reveals broad agreement that the Northern Hemisphere land is a major sink of atmospheric CO&lt;sub&gt;2&lt;/sub&gt;, but there remain major discrepancies with regard to the sign and magnitude of the net flux to and from tropical land

J. L. Sarmiento

M. Gloor

N. Gruber

C. Beaulieu

A. R. Jacobson

S. E. Mikaloff Fletcher

S. Pacala

K. Rodgers

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Biogeosciences

Trends and regional distributions of land and ocean carbon sinks

We show here an updated estimate of the net land carbon sink (NLS) as a function of time from 1960 to 2007 calculated from the difference between fossil fuel emissions, the observed atmospheric growth rate, and the ocean uptake obtained by recent ocean model simulations forced with reanalysis wind stress and heat and water fluxes. Except for interannual variability, the net land carbon sink appears to have been relatively constant at a mean value of −0.27 Pg C yr−1 between 1960 and 1988, at which time it increased abruptly by −0.88 (−0.77 to −1.04) Pg C yr−1 to a new relatively constant mean of −1.15 Pg C yr−1 between 1989 and 2003/7 (the sign convention is negative out of the atmosphere). This result is detectable at the 99% level using a t-test. The land use source (LU) is relatively constant over this entire time interval. While the LU estimate is highly uncertain, this does imply that most of the change in the net land carbon sink must be due to an abrupt increase in the land sink, LS = NLS – LU, in response to some as yet unknown combination of biogeochemical and climate forcing. A regional synthesis and assessment of the land carbon sources and sinks over the post 1988/1989 period reveals broad agreement that the Northern Hemisphere land is a major sink of atmospheric CO2, but there remain major discrepancies with regard to the sign and magnitude of the net flux to and from tropical land.ISSN:1726-4170ISSN:1726-417

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The present work aims to show how the hermeneutics of nihilistic Gianni Vattimo using his criticism of the ontological hermeneutic of Gadamer retrieves the figure of Walter Benjamin and the associated with the project of Heidegger. This leads to the present work, in the first place, describe which are the criticisms that Vattimo you performed to Gadamer; and, secondly, show how it is possible combine the philosophy of Heidegger with the critical thinking of Benjamin. Finally, it is indicated by the consistency of these authors as is possible the construction of a subject post-metaphysical</p

Leandro Catoggio

The historic disease of hermeneutics and its dialectical transformation. The weak thought between Gadamer and Benjamin.

We show here an updated estimate of the net land carbon sink (NLS) as a function of time from 1960 to 2007 calculated from the difference between fossil fuel emissions, the observed atmospheric growth rate, and the ocean uptake obtained by recent ocean model simulations forced with reanalysis wind stress and heat and water fluxes. Except for interannual variability, the net land carbon sink appears to have been relatively constant at a mean value of ?0.27 Pg C yr?1 between 1960 and 1988, at which time it increased abruptly by ?0.88 (?0.77 to ?1.04) Pg C yr?1 to a new relatively constant mean of ?1.15 Pg C yr?1 between 1989 and 2003/7 (the sign convention is negative out of the atmosphere). This result is detectable at the 99% level using a t-test. The land use source (LU) is relatively constant over this entire time interval. While the LU estimate is highly uncertain, this does imply that most of the change in the net land carbon sink must be due to an abrupt increase in the land sink, LS = NLS – LU, in response to some as yet unknown combination of biogeochemical and climate forcing. A regional synthesis and assessment of the land carbon sources and sinks over the post 1988/1989 period reveals broad agreement that the Northern Hemisphere land is a major sink of atmospheric CO2, but there remain major discrepancies with regard to the sign and magnitude of the net flux to and from tropical land

Sarmiento, J.L.

Gloor, M.

Gruber, N.

Beaulieu, C.

Jacobson, A.R.

Mikaloff Fletcher, S.E.

Pacala, S.

Rodgers, K.

Southampton (e-Prints Soton)

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