Cargando…
Tracing and constraining anthropogenic aerosol iron fluxes to the North Atlantic Ocean using iron isotopes
Atmospheric dust is an important source of the micronutrient Fe to the oceans. Although relatively insoluble mineral Fe is assumed to be the most important component of dust, a relatively small yet highly soluble anthropogenic component may also be significant. However, quantifying the importance of...
Autores principales: | Conway, Tim M., Hamilton, Douglas S., Shelley, Rachel U., Aguilar-Islas, Ana M., Landing, William M., Mahowald, Natalie M., John, Seth G. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6570766/ https://www.ncbi.nlm.nih.gov/pubmed/31201307 http://dx.doi.org/10.1038/s41467-019-10457-w |
Ejemplares similares
-
Surface Ocean Biogeochemistry Regulates the Impact of Anthropogenic Aerosol Fe Deposition on the Cycling of Iron and Iron Isotopes in the North Pacific
por: König, D., et al.
Publicado: (2022) -
Particle-Size Variability of Aerosol Iron and Impact on Iron Solubility and Dry Deposition Fluxes to the Arctic Ocean
por: Gao, Yuan, et al.
Publicado: (2019) -
Constraints on soluble aerosol iron flux to the Southern Ocean at the Last Glacial Maximum
por: Conway, T.M., et al.
Publicado: (2015) -
Pyrogenic iron: The missing link to high iron solubility in aerosols
por: Ito, Akinori, et al.
Publicado: (2019) -
The interplay between regeneration and scavenging fluxes drives ocean iron cycling
por: Tagliabue, Alessandro, et al.
Publicado: (2019)