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1.
Gen Dent ; 56(7): 629-34, 2008.
Artículo en Inglés | MEDLINE | ID: mdl-19014021
2.
Science ; 321(5891): 949-52, 2008 Aug 15.
Artículo en Inglés | MEDLINE | ID: mdl-18635761

RESUMEN

Earth's surface chemical environment has evolved from an early anoxic condition to the oxic state we have today. Transitional between an earlier Proterozoic world with widespread deep-water anoxia and a Phanerozoic world with large oxygen-utilizing animals, the Neoproterozoic Era [1000 to 542 million years ago (Ma)] plays a key role in this history. The details of Neoproterozoic Earth surface oxygenation, however, remain unclear. We report that through much of the later Neoproterozoic (<742 +/- 6 Ma), anoxia remained widespread beneath the mixed layer of the oceans; deeper water masses were sometimes sulfidic but were mainly Fe2+-enriched. These ferruginous conditions marked a return to ocean chemistry not seen for more than one billion years of Earth history.


Asunto(s)
Sedimentos Geológicos/química , Hierro/análisis , Oxígeno/análisis , Agua de Mar/química , Animales , Atmósfera , Cubierta de Hielo , Océanos y Mares , Oxidación-Reducción , Sulfatos/análisis , Sulfuros/análisis , Tiempo
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