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Las fluctuaciones en la oxigenación atmosférica del Precámbrico registradas por los isótopos de cromo
Robert Frei1, Claudio Gaucher, Simon W Poulton
1Institute of Geography and Geology and Nordic Center for Earth Evolution (NordCEE), University of Copenhagen, Øster Voldgade 10, 1350 Copenhagen, Denmark.
Nature
|September 11, 2009
Resumen
Tierra temprana de la Tierra temprana.
Área de la Ciencia:
- La geoquímica es la geoquímica.
- Paleoclimatología Paleoclimatología
- La geoquímica de los isótopos es la geoquímica de los isótopos.
Sus antecedentes:
- La atmósfera y los océanos de la Tierra sufrieron importantes eventos de oxigenación.
- El Gran Evento de Oxidación (GOE) hace alrededor de 2.45-2.2 Gyr marcó un gran aumento en el oxígeno.
- La evolución de los niveles de oxígeno del Precámbrico, particularmente antes y después del GOE, sigue siendo objeto de debate.
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