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Iron persistence in a distal hydrothermal plume supported by dissolved–particulate exchange

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Fitzsimmons, Jessica N., John, Seth G., Marsay, Christopher M., Hoffman, Colleen L., Nicholas, Sarah L., Toner, Brandy M., German, Christopher R., Sherrell, Robert M.·2017·Nature Geoscience

DOI 10.1038/ngeo2900

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“Succeeding studies have also confirmed that the vast majority of that dissolved Fe precipitates rapidly, as polymetallic sulfide and oxyhydroxide minerals that can be deposited much closer to the vent source (Findlay et al., 2019; Fitzsimmons et al., 2017; Hoffman et al., 2018; Yücel et al., 2021).”
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“…it seems reasonable to postulate that regardless of the magnitude of the atmospheric Fe input ﬂ ux, its interaction with in situ biogenic Fe-L (i.e., EPS and other Fe-speci ﬁ c ligands such as side-rophores) determines the fate of Fe in surface waters, similar to hydrothermal Fe inputs 62 .”
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“Data collected along GP16 have revealed the strong impact of hydrothermal plumes on the distribution of numerous inorganic trace elements and isotopic species (TEIs)–see, for example, Resing et al. (2015); Fitzsimmons et al. (2017); Moffett and German (2018) and references therein.”
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“Dissolved Fe in the hydrothermal plume mostly consists of colloidal species, whereas Mn is predominately soluble (Fitzsimmons et al., 2017).”
Background
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“Zone_01 Mar14 was previously published in Fitzsimmons et al. (2017 fall somewhere in between, with measurements collected by the beamline staff with guidance from the users.”
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“The resulting hydrothermal plumes can be traced over tens to thousands of kilometers using tracers, such as dMn, dFe, particulates, and isotopes such as (3)He [12, 13].”
BackgroundMethod
A hydrothermal plume on the Southwest Indian Ridge revealed by a multi-proxy approach: Impact on iron and manganese distributions (GEOTRACES GS02)
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“While iron particles were composed mainly of oxidized Fe (III) even directly above the ridge axis, Mn particles were reported to contain both Mn(II) and Mn (IV), depending on the distance from the source (Fitzsimmons et al., 2017; Lee et al., 2021).”
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Global oceanic iron distribution estimated by dynamic interpolationPreprint
Doi, T., Osafune, S., Masuda, S., Obata, H., Misumi, K., Achterberg, E. P., Bowie, A. R., & Nishioka, J. (2020) · doi:10.1002/essoar.10503738.1
“500 A supply of dFe from the East Pacific Rise (Fitzsimmons et al., 2017; Resing et al., 2015) 501 was not included in this estimation due to the hydrothermal supply.”
Background
Concentrations of soluble and dissolved iron (Fe) and iron isotope ratios from the U.S. GEOTRACES EPZT cruise (GP16, TN303) on R/V Thomas G. Thompson in the tropical Pacific during November & December 2013
Fitzsimmons, J. N., Steffen, J., Conway, T. M., & Sherrell, R. M. (2020) · Open Access Server of the Woods Hole Scientific Community (Woods Hole Scientific Community) · doi:10.26008/1912/bco-dmo.818707.1
Reply on RC1 on behalf of all co-authors
Forsch, K. (2021) · Biogeosciences · doi:10.5194/bg-2021-79-ac1
Replies on RC1 and RC2 (acp-2021-460)
Kurisu, M. (2021) · Atmospheric chemistry and physics · doi:10.5194/acp-2021-460-ac1
Comment on acp-2021-460
(2021) · Atmospheric chemistry and physics · doi:10.5194/acp-2021-460-rc1
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Saito, M. A. (2021) · Biogeosciences · doi:10.5194/bg-2021-96-ac1
Comment on bg-2021-79
(2021) · Biogeosciences · doi:10.5194/bg-2021-79-rc2
“The digestion method employed is described in Planquette and Sherrell (2013) and is widely used in the GEOTRACES program (Cutter and Bruland, 2012; Fitzsimmons et al., 2017) .”
Comment on bg-2022-73
(2022) · Biogeosciences · doi:10.5194/bg-2022-73-rc1
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Forsch, K. (2021) · Biogeosciences · doi:10.5194/bg-2021-79-ac2
Reviewer Comments: "How does glacier discharge affect marine biogeochemistry and primary production in the Arctic?” by Mark J. Hopwood et al
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Saito, M. A. (2021) · Biogeosciences · doi:10.5194/bg-2021-96-ac3
Comment on bg-2021-96
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Authors: Fitzsimmons, J. N., John, S. G., Marsay, C. M., Hoffman, C. L., Nicholas, S. L., Toner, B. M., German, C. R., & Sherrell, R. M.
Affiliations: Rutgers, The State University of New Jersey (US)
University of Southern California (US)
University of Minnesota (US)
Woods Hole Oceanographic Institution (US)
Corresponding author: Fitzsimmons, Jessica N.
ORCID: Fitzsimmons, Jessica N.
John, Seth G.
Marsay, Christopher M.
Hoffman, Colleen L.
Nicholas, Sarah L.
Toner, Brandy M.
German, Christopher R.
Sherrell, Robert M.
Venue: Nature Geoscience
Publisher: Springer Science and Business Media LLC
Published: 2017-02-20
Volume: 10
Issue: 3
Pages: 195-201
ISSN: 1752-0894 (ISSN-L)
1752-0908
DOI: 10.1038/ngeo2900
OpenAlex: W2589524191
Cited by: 318
References: 57
Citations by year: 2026: 27 · 2025: 36 · 2024: 32 · 2023: 24 · 2022: 34 · 2021: 52 · 2020: 34 · 2019: 26 · 2018: 28 · 2017: 25
FWCI: 27.30
Type: journal article
Language: en
Open access: green
hdl.handle.net
Licence: cc-by-nc-nd
www.springer.com/tdm (tdm)
Locations: Nature Geoscience (publishedVersion)
Arrow@dit (Dublin Institute of Technology) (submittedVersion)
ARAN (University of Galway Research Repository) (Ollscoil na Gaillimhe – University of Galway) (submittedVersion, cc-by-nc-nd)
Open Access Server of the Woods Hole Scientific Community (Woods Hole Scientific Community) (submittedVersion)
Topics: Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords: hydrothermal plumes, dissolved iron, particulate iron, iron oxyhydroxide, iron speciation, iron isotopes, Southern East Pacific Rise, GEOTRACES

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