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Iron persistence in a distal hydrothermal plume supported by dissolved–particulate exchange
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“it has been demonstrated that, even in the modern ocean, particulate and dissolved iron can be transported more than 2000 km from the ridge axis in seafloorhydrothermal settings (Fitzsimmons et al., 2017)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Fitzsimmons et al., 2017
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Niedermiller, J., & Baskaran, M. (2019) · Journal of Environmental Radioactivity · doi:10.1016/j.jenvrad.2018.12.016 · Cited by 22
Long‐Range Lateral Transport of Dissolved Manganese and Iron in the Subarctic Pacific
Wong, K. H., Nishioka, J., Kim, T., & Obata, H. (2022) · Journal of Geophysical Research Oceans · doi:10.1029/2021jc017652 · Cited by 21
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Prakash, L. S., Ray, D., Nagender Nath, B., Satyanarayanan, M., Kamesh Raju, K. A., Kurian, P. J., Dileep Kumar, M., & Srinivas Rao, A. (2020) · Chemical Geology · doi:10.1016/j.chemgeo.2020.119679 · Cited by 21
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Microbial manganese redox cycling drives co-removal of nitrate and ammonium
Wang, X., Liu, T.-C., Wang, X., Dang, C.-C., Tan, X., Lü, Y., Liu, B.-F., Xing, D., Ren, N., & Xie, G.-J. (2025) · Journal of Environmental Management · doi:10.1016/j.jenvman.2025.124095 · Cited by 20
Iron Isotope Biogeochemical Cycling in the Western Arctic Ocean
Zhang, R., Jensen, L. T., Fitzsimmons, J. N., Sherrell, R. M., Lam, P. J., Xiang, Y., & John, S. G. (2021) · Global Biogeochemical Cycles · doi:10.1029/2021gb006977 · Cited by 20
Trace Metal Dynamics in Shallow Hydrothermal Plumes at the Kermadec Arc
Kleint, C., Zitoun, R., Neuholz, R., Walter, M., Schnetger, B., Klose, L., Chiswell, S. M., Middag, R., Laan, P., Sander, S. G., et al. (2022) · Frontiers in Marine Science · doi:10.3389/fmars.2021.782734 · Cited by 20
Ho, P., Resing, J. A., & Shiller, A. M. (2019) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2019.04.009 · Cited by 20
Distribution and Cycling of Nickel and Nickel Isotopes in the Pacific Ocean
Bian, X., Yang, S., Raad, R. J., Odendahl, C. E., Lanning, N. T., Sieber, M., Huang, K., Fitzsimmons, J. N., Conway, T. M., & John, S. G. (2024) · Geophysical Research Letters · doi:10.1029/2024gl111115 · Cited by 19
“But much of the primary hydrothermal Ni can be scavenged onto Fe and Mn oxides in dilute plumes (Fitzsimmons et al., 2017; Fleischmann et al., 2023; Gueguen et al., It is also unclear whether hydrothermal vents are sources of isotopically light or isotopically heavy Ni to the oceans, since δ 60 Ni…”
The U.S.GEOTRACES Eastern Tropical Pacific Transect (GP16)
Moffett, J. W., & German, C. R. (2017) · Marine Chemistry · doi:10.1016/j.marchem.2017.12.001 · Cited by 19
Chen, T., Li, W., Guo, B. J., Liu, R., Li, G., Zhao, L., & Ji, J. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.119342 · Cited by 19
Li, J., Yang, J., Sun, M., Su, L., Wang, H., Gao, J., & Bai, S. (2020) · Frontiers in Marine Science · doi:10.3389/fmars.2020.581381 · Cited by 19
Pelagic clays as archives of marine iron isotope chemistry
Dunlea, A. G., Tegler, L. A., Peucker‐Ehrenbrink, B., Anbar, A. D., Romaniello, S. J., & Horner, T. J. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120201 · Cited by 19
Konn, C., Donval, J., Guyader, V., Germain, Y., Alix, A., Roussel, E. G., & Rouxel, O. J. (2021) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2021.103630 · Cited by 22
Speculations on the Paleozoic legacy of Gondwana amalgamation
Murphy, J. B., Nance, R. D., Johnston, S. T., Casas, J. M., Cawood, P. A., Matheson, E. J., Pufahl, P. K., Dan, W., Álvaro, J. J., Heron, P. J., et al. (2023) · Gondwana Research · doi:10.1016/j.gr.2023.12.002 · Cited by 19
Liao, J., Chen, J., Sun, X., Deng, Y., Wang, Y., Wang, D., Hong, G., Klose, L., & Koschinsky, A. (2024) · Geochemistry Geophysics Geosystems · doi:10.1029/2023gc011111 · Cited by 19
“Highly active volcanic and hydrothermal activities are found here, whose hydro-thermal plumes have been reported to spread westward leading to the precipitation of metalliferous materials in the Tiki Basin (Barrett et al., 1987; Fitzsimmons et al., 2017; Resing et al., 2015).”
BackgroundGardner, W. D., Mishonov, A. V., & Richardson, M. J. (2017) · Geophysical Research Letters · doi:10.1002/2017gl076571 · Cited by 19
“Some of these vents have been sampled in the GEOTRACES program (Fitzsimmons et al., 2017; Hayes et al., 2015; Lam et al., 2015) and intensive sampling along mid-ocean ridges (e.g., Thurnherr et al., 2008), but we have not encountered signals we could clearly identify as vents in our sections, which…”
BackgroundGrenne, T., & Slack, J. F. (2018) · Mineralium Deposita · doi:10.1007/s00126-018-0840-2 · Cited by 19
“…modern VMS systems, leads to rapid oxidation of iron to form ferric oxyhydroxide particles that may precipitate as much as 4000 km from vent sites (Fitzsimmons et al. 2017); in ancient systems with silica-rich seawater, the ferric oxyhydroxides combine with amorphous silica and may precipitate to…”
BackgroundLin, Y., Lui, H., Lee, J., Chen, C. A., Burr, G. S., Chou, W., & Kuo, F. (2019) · Marine Chemistry · doi:10.1016/j.marchem.2019.02.002 · Cited by 19
Using Excess 3He to Estimate Southern Ocean Upwelling Time Scales
Jenkins, W. J. (2020) · Geophysical Research Letters · doi:10.1029/2020gl087266 · Cited by 19
“…and manganese in the abyssal South Pacific suggest that ocean ridge crest hydrothermal activity produces a significant flux of a dissolved phase for these metals that persists for many thousands of kilometers away from their injection sites (Fitzsimmons et al., 2014, 2017; Resing et al., 2015).”
BackgroundAntarctic glaciers export carbon-stabilised iron(II)-rich particles to the surface Southern Ocean
Jones, R., Hawkings, J. R., Meredith, M. P., Lohan, M. C., Moore, O., Sherrell, R. M., Fitzsimmons, J. N., Abyaneh, M. K., Araki, T., Kaulich, B., et al. (2025) · Nature Communications · doi:10.1038/s41467-025-59981-y · Cited by 18
Detection, dispersal and biogeochemical contribution of hydrothermal iron in the ocean
Holmes, T. M., Chase, Z., van der Merwe, P. C., Townsend, A. T., & Bowie, A. R. (2017) · Marine and Freshwater Research · doi:10.1071/mf16335 · Cited by 18
Chemical Fluxes From a Recently Erupted Shallow Submarine Volcano on the Mariana Arc
Buck, N. J., Resing, J. A., Baker, E. T., & Lupton, J. E. (2018) · Geochemistry Geophysics Geosystems · doi:10.1029/2018gc007470 · Cited by 18
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Lough, A. J. M., Tagliabue, A., Demasy, C., Resing, J. A., Mellett, T., Wyatt, N. J., & Lohan, M. C. (2023) · Biogeosciences · doi:10.5194/bg-20-405-2023 · Cited by 18
“In order to examine the hydrothermal flux of Fe to the deep ocean, changes in Fe concentration are frequently compared to excess helium (xs3He), derived from δ3He, which is an inert tracer of hydrothermal activity (Lupton and Craig, 1981; Wu et al., 2011; Saito et al., 2013; Resing et al., 2015; Fitzsimmons et al., 20…”
BackgroundMethodInfluentialKadko, D., Aguilar‐Islas, A. M., Buck, C. S., Fitzsimmons, J. N., Landing, W. M., Shiller, A. M., Till, C. P., Bruland, K. W., Boyle, E. A., & Anderson, R. F. (2020) · Marine Chemistry · doi:10.1016/j.marchem.2020.103781 · Cited by 18
Oliveira, M. L. S., Neckel, A., Silva, L. F. O., Dotto, G. L., & Maculan, L. S. (2020) · Chemosphere · doi:10.1016/j.chemosphere.2020.129119 · Cited by 17
Submarine Shallow-Water Fluid Emissions and Their Geomicrobiological Imprint: A Global Overview
Caramanna, G., Sievert, S. M., & Bühring, S. I. (2021) · Frontiers in Marine Science · doi:10.3389/fmars.2021.727199 · Cited by 17
“, thousands of km from deep-sea hydrothermal vents, even reaching the photic zone, due to dissolved-particulate exchange processes (Fitzsimmons et al., 2017).”
BackgroundTagliabue, A., Bowie, A. R., Holmes, T. M., Latour, P. M. A., van der Merwe, P. C., Gault‐Ringold, M., Wuttig, K., & Resing, J. A. (2022) · Frontiers in Marine Science · doi:10.3389/fmars.2022.754517 · Cited by 17
Nielsen, S. G. (2020) · Cambridge University Press eBooks · doi:10.1017/9781108863438 · Cited by 41
Jiang, K., Wang, J., Kusky, T., Polat, A., Huang, B., Wang, L., Li, S., Deng, H., & Peng, Y. (2024) · Earth-Science Reviews · doi:10.1016/j.earscirev.2024.104710 · Cited by 18
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Deep-sea rare earth element-rich sediments: A review of distribution, carriers and petrogenesis
Fu, Y., Li, Z., Chew, D., Hollings, P., Peng, J., Chen, J., Tan, B., He, G., Yongjia, L., Huang, F., et al. (2025) · Global and Planetary Change · doi:10.1016/j.gloplacha.2025.104870 · Cited by 16
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Hansen, C. T., Kleint, C., Böhnke, S., Klose, L., Adam-Beyer, N., Saß, K., Zitoun, R., Sander, S. G., Indenbirken, D., Dittmar, T., et al. (2022) · Scientific Reports · doi:10.1038/s41598-022-25320-0 · Cited by 16
Optical observation of particles and responses to particle composition in the GEOTRACES GP16 section
Ohnemus, D. C., Lam, P. J., & Twining, B. S. (2017) · Marine Chemistry · doi:10.1016/j.marchem.2017.09.004 · Cited by 16
Tian, H.-A., van Manen, M., Bunnell, Z. B., Jung, J., Lee, S. H., Kim, T., Reichart, G., Conway, T. M., & Middag, R. (2023) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2023.10.029 · Cited by 15
Geochemical impacts of hydrothermal activity on surface deposits at the Southwest Indian Ridge
Pan, A., Yang, Q., Zhou, H., Ji, F., Wang, H., & Pancost, R. D. (2018) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2018.05.009 · Cited by 15
Wang, H., Resing, J. A., Yan, Q., Buck, N. J., Michael, S. M., Zhou, H., Liu, M., Walker, S. L., Yang, Q., & Ji, F. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.09.016 · Cited by 15
Nasemann, P., Gault‐Ringold, M., Stirling, C. H., Koschinsky, A., & Sander, S. G. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2017.11.005 · Cited by 15
Liao, J., Wang, D., Sun, X., Hong, G., Deng, Y., Yao, W., Manceau, A., & Koschinsky, A. (2025) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2025.119658 · Cited by 14
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Basak, C., Wu, Y., Haley, B. A., Muratli, J. M., Pena, L. D., Bolge, L., Fitzsimmons, J. N., Sherrell, R. M., & Goldstein, S. L. (2024) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2024.118692 · Cited by 14
Processes affecting dissolved iron across the Subtropical North Atlantic: a model study
Pagnone, A., Völker, C., & Ye, Y. (2019) · Ocean Dynamics · doi:10.1007/s10236-019-01288-w · Cited by 14
Grasse, P., Closset, I., Jones, J. L., Geilert, S., & Brzezinski, M. A. (2020) · Global Biogeochemical Cycles · doi:10.1029/2020gb006538 · Cited by 14
“However, such hydrothermal share calculations do not take abiotic processes into account, such as the formation of Fe(III) oxyhydroxides in the water column (Fitzsimmons et al., 2017) and the potential adsorption of DSi onto those particles.”
BackgroundHoffman, C., Schladweiler, C. S., Seaton, N. C. A., Nicholas, S. L., Fitzsimmons, J. N., Sherrell, R. M., German, C. R., Lam, P. J., & Toner, B. M. (2020) · ACS Earth and Space Chemistry · doi:10.1021/acsearthspacechem.0c00067 · Cited by 14
Neuholz, R., Kleint, C., Schnetger, B., Koschinsky, A., Laan, P., Middag, R., Sander, S. G., Thal, J., Türke, A., Walter, M., et al. (2020) · Minerals · doi:10.3390/min10110969 · Cited by 14
“Manganese does not form sulfide particles and is also not known to be stabilized by organic ligands in the open ocean [8,89], which would explain the constant decrease of Mn concentration with time and distance from the vent source.”
BackgroundWang, H., Wang, W., Liu, M., Zhou, H., Ellwood, M. J., Butterfield, D. A., Buck, N. J., & Resing, J. A. (2022) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2022.09.026 · Cited by 14
Sun, Z., Cao, H., Yin, X., Zhang, X., Dong, A., Liu, L., & Geng, W. (2018) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2018.06.014 · Cited by 14
Metal stable isotopes in the marine realm
Little, S., de Souza, G. F., & Xie, R. C. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00019-x · Cited by 16
Pathways and timescales of Southern Ocean hydrothermal iron and manganese transport
Birchill, A. J., Baker, C., Wyatt, N. J., Pabortsava, K., Venables, H. J., Moore, C. M., Turnbull, I., Milne, A., Ussher, S. J., Oliver, S., et al. (2024) · Communications Earth & Environment · doi:10.1038/s43247-024-01564-8 · Cited by 13
Microbial strong organic-ligand production is tightly coupled to iron in hydrothermal plumes
Hoffman, C., Monreal, P. J., Albers, J. B., Lough, A., Santoro, A. E., Mellett, T., Buck, K. N., Tagliabue, A., Lohan, M. C., Resing, J. A., et al. (2024) · Biogeosciences · doi:10.5194/bg-21-5233-2024 · Cited by 13
Ménèz, B., Pasini, V., Guyot, F., Benzerara, K., Bernard, S., & Brunelli, D. (2018) · Lithos · doi:10.1016/j.lithos.2018.07.022 · Cited by 13
“been shown to be transported to the non-buoyant hydrothermal plume and across oceans as complexes stabilized with organic ligands (Fitzsimmons et al., 2017; Resing et al., 2015; Sander et al., 2007).”
BackgroundA multi-modal approach to measuring particulate iron speciation in buoyant hydrothermal plumes
Stewart, B. D., Sorensen, J. V., Wendt, K. A., Sylvan, J. B., German, C. R., Anantharaman, K., Dick, G. J., Breier, J. A., & Toner, B. M. (2020) · Chemical Geology · doi:10.1016/j.chemgeo.2020.120018 · Cited by 12
Sindol, G. P., Babechuk, M. G., Conliffe, J., Slack, J. F., Rosca, C., & Schoenberg, R. (2022) · Precambrian Research · doi:10.1016/j.precamres.2022.106750 · Cited by 12
Annual variability of dissolved manganese in Northeast Pacific along Line-P: 2010–2013
Sim, N., & Orians, K. J. (2019) · Marine Chemistry · doi:10.1016/j.marchem.2019.103702 · Cited by 12
Nepheloid layer generation by gas eruption: unexpected experimental results
Zhu, C., Li, S., Chen, J., Wang, D., Song, X., Li, Z., Chen, B., Shan, H., & Jia, Y. (2023) · Journal of Oceanology and Limnology · doi:10.1007/s00343-022-2108-z · Cited by 11
“The striking lateral transport of the dissolved iron and manganese plumes over more than 4 000 km from their hydrothermal sources along the US GEOTRACES East Pacific Zonal Transect (Resing et al., 2015; Fitzsimmons et al., 2017) challenged our understanding of the element cycles.”
BackgroundWang, W., Lough, A., Goring-Harford, H. J., Flanagan, O., González-Santana, D., Resing, J. A., Connelly, D. P., Lohan, M. C., Tagliabue, A., & James, R. H. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2023.118468 · Cited by 11
An Ocean of Particles Characterization of Particulate Trace Elements by the GEOTRACES Program
Twining, B. S. (2024) · Oceanography · doi:10.5670/oceanog.2024.407 · Cited by 11
“This is notably evident in the neutrally buoy-ant hydrothermal plume west of 113°W. Micro-analytical images of plume particles revealed Fe(III) oxyhydroxide particles >2 μm associated with organic carbon matrices (Fitzsimmons et al., 2017), which should be collected by both bottles and pumps.”
BackgroundGEOTRACES: Ironing Out the Details of the Oceanic Iron Sources?
Conway, T. M., Middag, R., & Reiner Schlitzer, E. (2024) · Oceanography · doi:10.5670/oceanog.2024.416 · Cited by 11
“…where a small fraction of dFe from high-Fe vent fluids, stabilized by organic-ligands or as microparticles, or from particulate-dissolved exchange, can persist over great distances throughout the ocean (Toner et al., 2012; Fitzsimmons et al., 2017; Fitzsimmons and Steffen, 2024, in this issue).”
BackgroundFukami, Y., Kashiwabara, T., Amakawa, H., Shibuya, T., Usui, A., & Suzuki, K. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.12.005 · Cited by 11
Evans, G., Seyfried, W., & Tan, C. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2022.117943 · Cited by 11
Zhu, K., Achterberg, E. P., Bates, N. R., Gerringa, L. J. A., Middag, R., Hopwood, M. J., & Gledhill, M. (2023) · Global Biogeochemical Cycles · doi:10.1029/2022gb007617 · Cited by 10
“We omitted dFe profiles that were strongly influenced by source signatures from for example, hydrothermal vents, atmospheric dust and suboxic sediment inputs in both ocean basins (Fitzsimmons et al., 2017; Resing et al., 2015; Rijkenberg et al., 2014) (Table S2 in Supporting Information S1).”
MethodÁlvaro, J. J., & Mills, A. J. (2023) · Sedimentology · doi:10.1111/sed.13172 · Cited by 10
“A modern analogue of well-ventilated seawater has been reported in the Pacific Ocean, where it is characterized by transport of dissolved and particulate Fe 3 + - oxyhydroxides over long distances (Fitzsimmons et al ., 2017).”
BackgroundDeciphering the source of banded iron formations in the North China Craton
Wang, C., Xie, S., Zhang, X., Tong, X., Bai, Y., Peng, Z., Dong, Z., Zhang, L., & Wan, B. (2024) · Precambrian Research · doi:10.1016/j.precamres.2024.107298 · Cited by 12
Zhang, G., Bai, J., Zhao, M., Wang, P., Zhu, Y., Cao, J., Wu, H., Xu, R., He, G., Wei, G., et al. (2025) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2025.11.015 · Cited by 10
German, C. R., Lang, S. Q., & Fitzsimmons, J. N. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00048-6 · Cited by 15
Advances in Understanding the Marine Nitrogen Cycle in the GEOTRACES Era
Casciotti, K. L., Marshall, T. A., Fawcett, S. E., & Knapp, A. N. (2024) · Oceanography · doi:10.5670/oceanog.2024.406 · Cited by 10
“…being recognized as quantitatively important (Tagliabue et al., 2010, 2022; Conway and John, 2014; Rijkenberg et al., 2014; Resing et al., 2015; Fitzsimmons et al., 2017; Jenkins et al., 2020; Homoky et al., 2021; Fitzsimmons and Conway, 2023), including for alleviating regional diazotroph…”
BackgroundFitzsimmons, J. N., & Steffen, J. (2024) · Oceanography · doi:10.5670/oceanog.2024.421 · Cited by 10
“Additionally, under different conditions and assumptions, an isotopically heavy plume δ 56 Fe signature has been employed to identify and/or quantify the persistence of organically chelated dFe species within distal hydrothermal plumes (Fitzsimmons et al., 2016, 2017; Sieber et al., 2021).”
BackgroundMethodInfluentialPham, A. L. D., & Ito, T. (2021) · Journal of Geophysical Research Oceans · doi:10.1029/2020jc016475 · Cited by 10
Zhu, K., Birchill, A. J., Milne, A., Ussher, S. J., Humphreys, M. P., Carr, N., Mahaffey, C., Lohan, M. C., Achterberg, E. P., & Gledhill, M. (2021) · Marine Chemistry · doi:10.1016/j.marchem.2021.104038 · Cited by 10
Slack, J. F., McAleer, R. J., Shanks, W. C., & Dumoulin, J. A. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120568 · Cited by 11
Wang, W., Lough, A. J. M., Lohan, M. C., Connelly, D. P., Cooper, M. J., Milton, J. A., Chavagnac, V., Castillo, A., & James, R. H. (2021) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2021.117200 · Cited by 10
Liao, W., Planquette, H. F., Moriceau, B., Christophe Lambert, B., de Gésincourt, F. D., Laurenceau‐Cornec, E. C., Sarthou, G., & Gorguès, T. (2023) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2023.04.014 · Cited by 12
Cullen, J. T., & Coogan, L. A. (2017) · Geophysical Research Letters · doi:10.1002/2017gl074609 · Cited by 9
Wang, H., Yan, Q., Yang, Q., Ji, F., Wong, K. H., & Zhou, H. (2019) · Journal of Geophysical Research Oceans · doi:10.1029/2018jc014713 · Cited by 9
González-Santana, D., Lough, A., Planquette, H. F., Sarthou, G., Tagliabue, A., & Lohan, M. C. (2022) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2022.161179 · Cited by 9
Co‐acquisition of mineral‐bound iron and phosphorus by natural Trichodesmium colonies
Shaked, Y., de Beer, D., Wang, S., Zhang, F., Visser, A., Eichner, M. J., & Basu, S. (2023) · Limnology and Oceanography · doi:10.1002/lno.12329 · Cited by 10
Meridional distribution of dissolved manganese in the tropical and equatorial Pacific
Chen, G., & Wu, J. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.06.048 · Cited by 9
Lyu, J., Auer, G., Bialik, O. M., Christensen, B. A., Yamaoka, R., & Vleeschouwer, D. D. (2023) · Paleoceanography and Paleoclimatology · doi:10.1029/2023pa004761 · Cited by 8
Particulate Cadmium Accumulation in the Mesopelagic Ocean
Laubach, A., Lee, J., Sieber, M., Lanning, N. T., Fitzsimmons, J. N., Conway, T. M., & Lam, P. J. (2025) · Global Biogeochemical Cycles · doi:10.1029/2024gb008281 · Cited by 8
“…GP16, analysis was limited to the upper 1,800 m to avoid the potential influence of a known hydrothermal plume from the southern East Pacific Rise (Fitzsimmons et al., 2017; Resing et al., 2015), which may act to add or remove trace elements to ocean waters, decoupling trace elements from…”
刘, 全., 朱, 东., 孟, 庆., 刘, 佳., 吴, 小., 周, 冰., Qi, F., & 金, 之. (2018) · SCIENTIA SINICA Terrae · doi:10.1360/n072018-00086 · Cited by 7
Differential Behavior of Metal Sulfides in Hydrothermal Plumes and Diffuse Flows
Estes, E. R., Berti, D., Findlay, A., Hochella, M. F., Shaw, T. J., Yücel, M., Carlo, E. H. D., & Luther, G. W. (2022) · ACS Earth and Space Chemistry · doi:10.1021/acsearthspacechem.1c00377 · Cited by 8
A mining industry overview of cobalt in Finland: exploration, deposits and utilization
Konnunaho, J., Eilu, P., Törmänen, T., Karinen, T., Ranta, J.-P., Rasilainen, K., Nykänen, V. M., Pokki, J., & Dehaine, Q. (2023) · Geoenergy · doi:10.1144/geoenergy2023-016 · Cited by 8
Cotte, L., Chavagnac, V., Pelleter, E., Laës, A., Cathalot, C., Dulaquais, G., Riso, R. D., Sarradin, P., & Waeles, M. (2019) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2019.103204 · Cited by 8
Fassbender, A. J., Palevsky, H. I., Martz, T. R., Ingalls, A. E., Gledhill, M., Fawcett, S. E., Brandes, J. A., & Aluwihare, L. I. (2017) · Marine Chemistry · doi:10.1016/j.marchem.2017.09.002 · Cited by 8
Iron Isotopes reveal volcanogenic input during Oceanic Anoxic Event 2 (OAE 2 ∼ 94 Ma)
Yobo, L. N., Williams, H. M., Brandon, A. D., Holmden, C. E., Lau, K., Bergman, S. C., Eldrett, J. S., & Minisini, D. (2024) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2024.10.023 · Cited by 7
Colombo, M., LaRoche, J., Desai, D., Li, J., & Maldonado, M. T. (2023) · Limnology and Oceanography · doi:10.1002/lno.12407 · Cited by 7
“…al. 2011; Colombo et al. 2019 a ), reductive supply from suboxic or anoxic sediments (Vieira et al. 2019; Jensen et al. 2020), atmospheric deposition (Mahowald et al. 2018), sea ice melt (Marsay et al. 2018; Rogalla et al. 2022), and hydrothermal vents (Middag et al. 2011; Fitzsimmons et al. 2017).”
BackgroundInfluentialZhang, J., Ni, Z. T., Ren, J., Yu, F., Diao, X. Y., Wang, Y., Zhang, S. J., Su, H. T., Cong, S. L., Lu, Z., et al. (2024) · Progress In Oceanography · doi:10.1016/j.pocean.2024.103212 · Cited by 7
Anderson, R. L. (2024) · Oceanography · doi:10.5670/oceanog.2024.405 · Cited by 7
“…constitute about half of the operationally defined dissolved Fe in seawater (e.g., Nishioka et al., 2001; Wu et al., 2001; Bergquist et al., 2007; Boye et al., 2010; Fitzsimmons et al., 2017; Kunde et al., 2019; Lough et al., 2019; Homoky et al., 2021; Jensen et al., 2021; Tagliabue et al., 2022).”
BackgroundEvolution of the South Pacific's Iron Cycle Over the Cenozoic
Tegler, L. A., Horner, T. J., Nielsen, S. G., Heard, A. W., Squires, K., Severmann, S., Peucker‐Ehrenbrink, B., Blusztajn, J., & Dunlea, A. G. (2025) · Paleoceanography and Paleoclimatology · doi:10.1029/2025pa005149 · Cited by 6
“Indeed, the presence of Fe of hydrothermal origin has been observed several thousands of kilometers away from known vent sites (Fitzsimmons et al., 2017; Resing et al., 2015).”
InfluentialSiderite precipitation in Paleoarchean oceans during hydrothermal venting
Rasmussen, B., Muhling, J. R., & Tosca, N. J. (2025) · Science Advances · doi:10.1126/sciadv.ady6851 · Cited by 6
Linsy, P., Prakash, L. S., Roy, P., Shuhail, M., & Kurian, P. J. (2023) · Minerals · doi:10.3390/min13020209 · Cited by 6
“This result is consistent with previous studies, which found that most of the Fe in hydrothermal plumes consists of Fe oxyhydroxides [60,61].”
ResultHu, Q., Shi, X., Bi, D., Yu, M., Huang, M., Li, J., Liu, J., Zhou, T., Song, Z., Li, C., et al. (2024) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2024.106294 · Cited by 6
Ray, D., Sreenivas, B., Prakash, L. S., Mazumdar, A., Peketi, A., Paropkari, A. L., & Balu, G. (2021) · Marine Chemistry · doi:10.1016/j.marchem.2021.103929 · Cited by 6
Perspectives on premetamorphic stratabound tourmalinites
Slack, J. F. (2022) · Journal of Geosciences · doi:10.3190/jgeosci.349 · Cited by 6
“However, in seafloor environments, limited data suggest there is a general affinity of B with Mn, as for sediments on the East Pacific Rise that contain 300 to 800 μg/g B (carbonate-free basis) associated with Al-poor Fe-Mn sediments (Boström and Peterson 1969).”
Background
Metadata
- 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
- Venue
- Nature Geoscience
- Published
- 2017-02-20
- Volume
- 10
- Issue
- 3
- Pages
- 195-201
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- 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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