John Conway e o seu Jogo da Vida

Apresenta-se uma biografia sucinta de John Horton Conway, matemático nascido em 1937 em Liverpool. Conway tornou-se bem conhecido após a sua invenção do Jogo da Vida, o qual é um exemplo de auto-organização e interessante para biólogos, matemáticos, economistas, filósofos e público em geral.

The constitution, congress, and the courts : speech of Hon. David J. Lewis, of Maryland, in the House of Representatives, Monday, March 8, 1937.

"(Not printed at government expense.)"

John Adams,

Added t.-p., engraved for series.

John Quincy Adams,

Mode of access: Internet.

Los buscavidas: nómadas del capitalismo

Esta investigación se propone describir los rasgos esenciales de un tipo de personajes que hemos denominado, a efectos de generalización teórica, como “buscavidas”, peregrinos antihéroes del sistema laboral contemporáneo, deficientemente integrados a los valores del capitalismo e irreductibles a sus principios disciplinarios, que podemos hallar en la novelística del s. XX. He escogido a título de ejemplo cuatro novelas emblemáticas: Viaje al fin de la noche (1932), de Louis-Ferdinand Celine (1894-1961); La Conjura de los Necios (1980), de John Kennedy Toole (1937-1969); Factotum (1975), de Charles Bukowski (1920-1994) y Los Hermanos Tanner (1907), de Robert Walser (1878-1956). Asimismo, en el tercer capítulo de esta investigación, tendremos en cuenta la novela El Desaparecido (1927), de Franz Kafka (1883-1924), como un contrapunto iluminador que contribuye a analizar el tejido problemático de las dinámicas laborales en el pasado siglo. Karl Rossman, “el desaparecido”, no pertenece a la categoría de los buscavidas, porque a diferencia de estos, aspira a progresar en su carrera, pero sufre los golpes bajos de un sistema que tiene reservado a su condición de emigrante la misma suerte ingrata.

Surface exposure ages of samples obtained from Reedy Glacier, Antarctica

Fresh deposits above the margins of Reedy Glacier show that maximum ice levels during the last glaciation were several hundred meters above present near the glacier mouth and converged to less than 60 m above the present-day surface at the head of the glacier. Exposure ages of samples from five sites along its margin show that Reedy Glacier and its tributaries thickened asynchronously between 17 and 7 kyr BP At the Quartz Hills, located midway along the glacier, maximum ice levels were reached during the period 17-14 kyr BP. Farther up-glacier the ice surface reached its maximum elevation more recently: 14.7-10.2 kyr BP at the Caloplaca Hills; 9.1-7.7 kyr BP at Mims Spur; and around 7 kyr BP at Hatcher Bluffs. We attribute this time-transgressive behavior to two different processes: At the glacier mouth, growth of grounded ice and subsequent deglaciation in the Ross Sea embayment caused a wave of thickening and then thinning to propagate up-glacier. During the Lateglacial and Holocene, increased snow accumulation on the East Antarctic Ice Sheet caused transient thickening at the head of the glacier. An important result of this work is that moraines deposited along Reedy Glacier during the last ice age cannot be correlated to reconstruct a single glacial maximum longitudinal profile. The profile steepened during deglaciation of the Ross Sea, thinning at the Quartz Hills after 13 kyr BP while thickening upstream. Near its confluence with Mercer Ice Stream, rapid thinning beginning prior to 7-8 kyr BP reduced the level of Reedy Glacier to close to its present level. Thinning over the past 1000 years has lowered the glacier by less than 20 m.

Beryllium ages, sedimentology and weathering characteristics of Reedy Glacier deposits

Deposits corresponding to multiple periods of glaciation are preserved in ice-free areas adjacent to Reedy Glacier, southern Transantarctic Mountains. Glacial geologic mapping, supported by 10Be surface-exposure dating, shows that Reedy Glacier was significantly thicker than today multiple times during the mid-to-late Cenozoic. Longitudinal-surface profiles reconstructed from the upper limits of deposits indicate greater thickening at the glacier mouth than at the head during these episodes, indicating that Reedy Glacier responded primarily to changes in the thickness of the West Antarctic Ice Sheet. Surface-exposure ages suggest this relationship has been in place since at least 5 Ma. The last period of thickening of Reedy Glacier occurred during Marine Isotope Stage 2, at which time the glacier surface near its confluence with the West Antarctic Ice Sheet was at least 500 m higher than today.