EconPapers    
Economics at your fingertips  
 

Quantification of dissolved iron sources to the North Atlantic Ocean

Tim M. Conway () and Seth G. John
Additional contact information
Tim M. Conway: University of South Carolina, Columbia, South Carolina 29208, USA
Seth G. John: University of South Carolina, Columbia, South Carolina 29208, USA

Nature, 2014, vol. 511, issue 7508, 212-215

Abstract: A high-resolution oceanic section of dissolved iron stable isotope ratios reveals that the primary source of dissolved iron to the North Atlantic is atmospheric dust, while seafloor sediments and submarine volcanic vents also contribute significantly.

Date: 2014
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/nature13482 Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:511:y:2014:i:7508:d:10.1038_nature13482

Ordering information: This journal article can be ordered from
https://www.nature.com/

DOI: 10.1038/nature13482

Access Statistics for this article

Nature is currently edited by Magdalena Skipper

More articles in Nature from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().

 
Page updated 2025-03-19
Handle: RePEc:nat:nature:v:511:y:2014:i:7508:d:10.1038_nature13482