Preservation of iron(II) by carbon-rich matrices in a hydrothermal plume-Reference-Cited by-同舟云学术

Preservation of iron(II) by carbon-rich matrices in a hydrothermal plume

Published:2009-02-08 Issue:3 Volume:2 Page:197-201
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Toner Brandy M.,Fakra Sirine C.,Manganini Steven J.,Santelli Cara M.,Marcus Matthew A.,Moffett James W.,Rouxel Olivier,German Christopher R.,Edwards Katrina J.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo433.pdf

Reference33 articles.

1. German, C. R. & von Damm, K. L. Hydrothermal processes. Treatise Geochem. 6, 181–222 (2004).

2. Elderfield, H. & Schultz, A. Mid-ocean ridge hydrothermal fluxes and the chemical composition of the ocean. Annu. Rev. Earth Planet. Sci. 24, 191–224 (1996).

3. SCOR Working Group.SCOR GEOTRACES— An international study of the global marine biogeochemical cycles of trace elements and their isotopes. Chem. der Erde 67, 85–131 (2007).

4. Bennett, S. A. et al. The distribution and stabilisation of dissolved Fe in deep-sea hydrothermal plumes. Earth Planet. Sci. Lett. 270, 157–167 (2008).

5. Sander, S. G. et al. Organic complexation of copper in deep-sea hydrothermal vent systems. Environ. Chem. 4, 81–89 (2007).

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