Iron persistence in a distal hydrothermal plume supported by dissolved–particulate exchange
Year: 2017
Type: article
Source: Nature Geoscience
DOI: 10.1038/ngeo2900
Institutions: Rutgers, The State University of New Jersey, Texas A&M University, University of Southern California, University of South Carolina, Skidaway Institute of Oceanography, University of Georgia, University of Minnesota, Ollscoil na Gaillimhe – University of Galway, Woods Hole Oceanographic Institution
Language: English
Subfield: Geochemistry and Petrology
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: green
Awards: Collaborative Research: Suspended particle geochemistry along the US GEOTRACES Eastern Pacific Zonal Transect, from high productivity ocean margin to deep sea hydrothermal plume, G1286251239, GEOTRACES Pacific section: Dissolved Fe, Cd, and Zn isotopes, Collaborative Research: Experimental constraints on marine Fe isotope effects - Biology, ligands, and particles, Collaborative Research: GEOTRACES Pacific Section: The Geochemistry of Size-fractionated Suspended Particles Collected by In-situ Filtration, G969889393, Collaborative Research: Suspended particle geochemistry along the US GEOTRACES Eastern Pacific Zonal Transect, from high productivity ocean margin to deep sea hydrothermal plume
OpenAlex ID: W2589524191