Dissolved iron and iron isotopes in the southeastern Pacific Ocean
The Southeast Pacific Ocean is a severely understudied yet dynamic region for trace metals such as iron, since it experiences steep redox and productivity gradients in upper waters and strong hydrothermal iron inputs to deep waters. In this study, we report the dissolved iron (dFe) distribution from...
Main Authors: | Conway, Tim M., Thyng, Kristen M., John, Seth G., Fitzsimmons, Jessica Nicole, Lee, Jong-Mi, Kayser, Richard A, Boyle, Edward A |
---|---|
Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
Format: | Article |
Language: | en_US |
Published: |
American Geophysical Union (AGU)
2017
|
Online Access: | http://hdl.handle.net/1721.1/110777 https://orcid.org/0000-0002-6394-1866 |
Similar Items
-
Distal transport of dissolved hydrothermal iron in the deep South Pacific Ocean
by: Jenkins, William J., et al.
Published: (2015) -
The marine biogeochemistry of dissolved and colloidal iron
by: Fitzsimmons, Jessica Nicole
Published: (2014) -
Thorium isotopes tracing the iron cycle at the Hawaii Ocean Time-series Station ALOHA
by: Anderson, Robert F., et al.
Published: (2017) -
Siderophore-based microbial adaptations to iron scarcity across the eastern Pacific Ocean
by: Mende, Daniel R., et al.
Published: (2017) -
The marine geochemistry of iron and iron isotopes
by: Bergquist, Bridget A., 1973-
Published: (2010)