933 research outputs found
China and the Spanish Empire
Editada en la Fundación Empresa PúblicaEn este artículo argumentamos que Ming China desempeñó un papel fundamental en el auge y decadencia del Imperio español. La demanda china de plata permitió elevados beneficios hasta 1640. El descenso de estos beneficios llevó a la reducción de la producción y la Monarquía se enfrentó a una grave crisis financiera. La consecuencia fue una presión fiscal creciente con objeto de compensar la pérdida de los ingresos externos procedentes de América.In this article we argue that Ming China had a fundamental impact on the rise and decline of the Spanish Empire. China's demand for silver was of such magnitude that private mining profits in the Spanish Empire remained high until about 1640. The decline of these profits led to abandon production. Spain faced a deepening financial crisis due to the fall of silver's value. The loss of purchasing power from the Crown's American enterprise was inevitable and the state's relentless pressure for increased taxation within Castile and elsewhere was mandatory in order to compensate for lost external purchasing power.Publicad
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Jurassic to Paleogene: Part 2: Paleogene geochronology and chronostratigraphy
We present a revised Paleogene geochronology based upon a best fit to selected high temperature radiometric dates on a number of identified magnetic polarity chrons (within the late Cretaceous, Paleogene and Neogene) which minimizes apparent accelerations in sea-floor spreading. An assessment of first order correlations of calcareous plankton biostratigraphic datum events to magnetic polarity stratigraphy yields the following estimated magnetobiochronology of major chronostratigraphic boundaries: Cretaceous-Tertiary boundary (Chron C29R), 66.4 Ma; Paleocene-Eocene (Chron C24R), 57.8 Ma; Eocene-Oligocene (Chron C13R), 36.6 Ma; Oligocene-Miocene (Chron C6CN), 23.7 Ma. The Eocene is seen to have expanded chronologically (~ 21 m.y.) at the expense of the Paleocene (~ 9 m.y.) and is indeed the longest of the Cenozoic epochs. In addition, magnetobiostratigraphic correlations require adjustments in apparent correlations with standard marine stage boundaries in some cases (particularly in the Oligocene). Finally, we present a correlation between standard Paleogene marine and terrestrial stratigraphies
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