论文信息 - Ironing Out Biosphere Oxidation

Ironing Out Biosphere Oxidation

Various lines of evidence now indicate that the atmosphere became oxygen-rich about 2.3 billion years ago. In his perspective, [Kump][1] describes work by [Rouxel and colleagues][2] who used the stable isotopic composition of iron minerals to explore the environmental context of this monumental global change. [1]: http://www.sciencemag.org/cgi/content/full/307/5712/1058 [2]: http://www.sciencemag.org/cgi/content/short/307/5712/1088

L. Kump

[1] A. Bekker,et al. Iron Isotope Constraints on the Archean and Paleoproterozoic Ocean Redox State , 2004, Science.

[2] D. Abbott,et al. Plume‐related mafic volcanism and the deposition of banded iron formation , 1999 .

[3] D. Canfield. A new model for Proterozoic ocean chemistry , 1998, Nature.

[4] H. H. Anderson,et al. A Comparison of the Abundance Ratios of the Isotopes of Terrestrial and of Meteoritic Iron1 , 1947 .

[5] B. Sageman,et al. Marine Shales: Depositional Mechanisms and Environments of Ancient Deposits , 1994 .

[6] M. Gaffey,et al. The Chemical Evolution of the Atmosphere and Oceans , 1984 .