Authigenic mineral phases as a driver of the upper-ocean iron cycle.
Journal
Nature
ISSN: 1476-4687
Titre abrégé: Nature
Pays: England
ID NLM: 0410462
Informations de publication
Date de publication:
Aug 2023
Aug 2023
Historique:
received:
18
11
2022
accepted:
12
05
2023
medline:
4
8
2023
pubmed:
3
8
2023
entrez:
2
8
2023
Statut:
ppublish
Résumé
Iron is important in regulating the ocean carbon cycle
Identifiants
pubmed: 37532817
doi: 10.1038/s41586-023-06210-5
pii: 10.1038/s41586-023-06210-5
doi:
Substances chimiques
Iron
E1UOL152H7
Ligands
0
Minerals
0
Solutions
0
Types de publication
Journal Article
Langues
eng
Sous-ensembles de citation
IM
Pagination
104-109Informations de copyright
© 2023. The Author(s), under exclusive licence to Springer Nature Limited.
Références
Tagliabue, A. et al. The integral role of iron in ocean biogeochemistry. Nature 543, 51–59 (2017).
pubmed: 28252066
doi: 10.1038/nature21058
Gledhill, M. & Buck, K. N. The organic complexation of iron in the marine environment: a review. Front. Microbiol. 3, 69 (2012).
pubmed: 22403574
pmcid: 3289268
doi: 10.3389/fmicb.2012.00069
Johnson, K. S., Gordon, R. M. & Coale, K. H. What controls dissolved iron concentrations in the world ocean? Mar. Chem. 57, 137–161 (1997).
doi: 10.1016/S0304-4203(97)00043-1
Lauderdale, J. M., Braakman, R., Forget, G., Dutkiewicz, S. & Follows, M. J. Microbial feedbacks optimize ocean iron availability. Proc. Natl Acad. Sci. 117, 4842–4849 (2020).
pubmed: 32071221
pmcid: 7060696
doi: 10.1073/pnas.1917277117
Parekh, P., Follows, M. J. & Boyle, E. A. Decoupling of iron and phosphate in the global ocean. Glob. Biogeochem. Cycles 19, GB2020 (2005).
doi: 10.1029/2004GB002280
Whitby, H. et al. A call for refining the role of humic-like substances in the oceanic iron cycle. Sci. Rep. 10, 6144 (2020).
pubmed: 32273548
pmcid: 7145848
doi: 10.1038/s41598-020-62266-7
Boyd, P. W., Ellwood, M. J., Tagliabue, A. & Twining, B. S. Biotic and abiotic retention, recycling and remineralization of metals in the ocean. Nat. Geosci. 10, 167–173 (2017).
doi: 10.1038/ngeo2876
Frew, R. D. et al. Particulate iron dynamics during FeCycle in subantarctic waters southeast of New Zealand. Glob. Biogeochem. Cycles 20, GB1S93 (2006).
doi: 10.1029/2005GB002558
Ohnemus, D. C., Torrie, R. & Twining, B. S. Exposing the distributions and elemental associations of scavenged particulate phases in the ocean using basin‐scale multi‐element data sets. Glob. Biogeochem. Cycles 33, 725–748 (2019).
doi: 10.1029/2018GB006145
Tagliabue, A. et al. The interplay between regeneration and scavenging fluxes drives ocean iron cycling. Nat. Commun. 10, 4960 (2019).
pubmed: 31673108
pmcid: 6823497
doi: 10.1038/s41467-019-12775-5
Cullen, J. T., Bergquist, B. A. & Moffett, J. W. Thermodynamic characterization of the partitioning of iron between soluble and colloidal species in the Atlantic Ocean. Mar. Chem. 98, 295–303 (2006).
doi: 10.1016/j.marchem.2005.10.007
Fitzsimmons, J. N., Bundy, R. M., Al-Subiai, S. N., Barbeau, K. A. & Boyle, E. A. The composition of dissolved iron in the dusty surface ocean: an exploration using size-fractionated iron-binding ligands. Mar. Chem. 173, 125–135 (2015).
doi: 10.1016/j.marchem.2014.09.002
Tagliabue, A. et al. How well do global ocean biogeochemistry models simulate dissolved iron distributions? Glob. Biogeochem. Cycles 30, 149–174 (2016).
doi: 10.1002/2015GB005289
Somes, C. J. et al. Constraining global marine iron sources and ligand‐mediated scavenging fluxes with GEOTRACES dissolved iron measurements in an ocean biogeochemical model. Glob. Biogeochem. Cycles 35, e2021GB006948 (2021).
doi: 10.1029/2021GB006948
Sedwick, P. N. et al. Dissolved iron in the Bermuda region of the subtropical North Atlantic Ocean: seasonal dynamics, mesoscale variability, and physicochemical speciation. Mar. Chem. 219, 103748 (2020).
doi: 10.1016/j.marchem.2019.103748
Martinez-Garcia, A. et al. Iron fertilization of the Subantarctic Ocean during the last ice age. Science 343, 1347–1350 (2014).
pubmed: 24653031
doi: 10.1126/science.1246848
Raven, J. A., Evans, M. C. W. & Korb, R. E. The role of trace metals in photosynthetic electron transport in O
doi: 10.1023/A:1006282714942
Wade, J., Byrne, D. J., Ballentine, C. J. & Drakesmith, H. Temporal variation of planetary iron as a driver of evolution. Proc. Natl Acad. Sci. 118, e2109865118 (2021).
pubmed: 34873026
pmcid: 8713747
doi: 10.1073/pnas.2109865118
Tagliabue, A., Aumont, O. & Bopp, L. The impact of different external sources of iron on the global carbon cycle. Geophys. Res. Lett. 41, 920–926 (2014).
doi: 10.1002/2013GL059059
Buck, K. N., Sedwick, P. N., Sohst, B. & Carlson, C. A. Organic complexation of iron in the eastern tropical South Pacific: results from US GEOTRACES Eastern Pacific Zonal Transect (GEOTRACES cruise GP16). Mar. Chem. 201, 229–241 (2018).
doi: 10.1016/j.marchem.2017.11.007
Buck, K. N., Sohst, B. & Sedwick, P. N. The organic complexation of dissolved iron along the U.S. GEOTRACES (GA03) North Atlantic Section. Deep Sea Res. II Top. Stud. Oceanogr. 116, 152–165 (2015).
doi: 10.1016/j.dsr2.2014.11.016
Gerringa, L. J. A., Rijkenberg, M. J. A., Schoemann, V., Laan, P. & de Baar, H. J. W. Organic complexation of iron in the West Atlantic Ocean. Mar. Chem. 177, 434–446 (2015).
doi: 10.1016/j.marchem.2015.04.007
Bressac, M. et al. Resupply of mesopelagic dissolved iron controlled by particulate iron composition. Nat. Geosci. 12, 995–1000 (2019).
doi: 10.1038/s41561-019-0476-6
Lamborg, C. H. et al. The flux of bio- and lithogenic material associated with sinking particles in the mesopelagic “twilight zone” of the northwest and North Central Pacific Ocean. Deep Sea Res. II Top. Stud. Oceanogr. 55, 1540–1563 (2008).
doi: 10.1016/j.dsr2.2008.04.011
Twining, B. S. et al. Differential remineralization of major and trace elements in sinking diatoms. Limnol. Oceanogr. 59, 689–704 (2014).
doi: 10.4319/lo.2014.59.3.0689
Tagliabue, A. et al. Persistent uncertainties in ocean net primary production climate change projections at regional scales raise challenges for assessing impacts on ecosystem services. Front. Clim. 3, 738224 (2021).
doi: 10.3389/fclim.2021.738224
Gunnars, A., Blomqvist, S., Johansson, P. & Andersson, C. Formation of Fe(III) oxyhydroxide colloids in freshwater and brackish seawater, with incorporation of phosphate and calcium. Geochim. Cosmochim. Acta 66, 745–758 (2002).
doi: 10.1016/S0016-7037(01)00818-3
Feely, R. A., Trefry, J. H., Massoth, G. J. & Metz, S. A comparison of the scavenging of phosphorus and arsenic from seawater by hydrothermal iron oxyhydroxides in the Atlantic and Pacific Oceans. Deep Sea Res. A Oceanogr. Res. Pap. 38, 617–623 (1991).
doi: 10.1016/0198-0149(91)90001-V
Homoky, W. B. et al. Iron colloids dominate sedimentary supply to the ocean interior. Proc. Natl Acad. Sci. 118, e2016078118 (2021).
pubmed: 33771922
doi: 10.1073/pnas.2016078118
Homoky, W. B. et al. Iron and manganese diagenesis in deep sea volcanogenic sediments and the origins of pore water colloids. Geochim. Cosmochim. Acta 75, 5032–5048 (2011).
doi: 10.1016/j.gca.2011.06.019
Fitzsimmons, J. N. & Boyle, E. A. Both soluble and colloidal iron phases control dissolved iron variability in the tropical North Atlantic Ocean. Geochim. Cosmochim. Acta 125, 539–550 (2014).
doi: 10.1016/j.gca.2013.10.032
Kunde, K. et al. Iron distribution in the subtropical North Atlantic: the pivotal role of colloidal iron. Glob. Biogeochem. Cycles 33, 1532–1547 (2019).
doi: 10.1029/2019GB006326
Marsay, C. M., Barrett, P. M., McGillicuddy, D. J. & Sedwick, P. N. Distributions, sources, and transformations of dissolved and particulate iron on the Ross Sea continental shelf during summer. J. Geophys. Res. Oceans 122, 6371–6393 (2017).
doi: 10.1002/2017JC013068
Conway, T. M. et al. Tracing and constraining anthropogenic aerosol iron fluxes to the North Atlantic Ocean using iron isotopes. Nat. Commun. 10, 2628 (2019).
pubmed: 31201307
pmcid: 6570766
doi: 10.1038/s41467-019-10457-w
Tang, W. et al. Widespread phytoplankton blooms triggered by 2019–2020 Australian wildfires. Nature 597, 370–375 (2021).
pubmed: 34526706
doi: 10.1038/s41586-021-03805-8
Boyd, P. W., Mackie, D. S. & Hunter, K. A. Aerosol iron deposition to the surface ocean – modes of iron supply and biological responses. Mar. Chem. 120, 128–143 (2010).
doi: 10.1016/j.marchem.2009.01.008
Bowie, A. R. et al. Biogeochemical iron budgets of the Southern Ocean south of Australia: decoupling of iron and nutrient cycles in the subantarctic zone by the summertime supply. Glob. Biogeochem. Cycles 23, GB4034 (2009).
doi: 10.1029/2009GB003500
Wu, J. & Boyle, E. Iron in the Sargasso Sea: implications for the processes controlling dissolved Fe distribution in the ocean. Glob. Biogeochem. Cycles 16, 33-1–33-8 (2002).
doi: 10.1029/2001GB001453
Rijkenberg, M. J. et al. The distribution of dissolved iron in the West Atlantic Ocean. PLoS One 9, e101323 (2014).
pubmed: 24978190
pmcid: 4076309
doi: 10.1371/journal.pone.0101323
Black, E. E. et al. Ironing out Fe residence time in the dynamic upper ocean. Glob. Biogeochem. Cycles 34, e2020GB006592 (2020).
doi: 10.1029/2020GB006592
Wagener, T., Guieu, C. & Leblond, N. Effects of dust deposition on iron cycle in the surface Mediterranean Sea: results from a mesocosm seeding experiment. Biogeosciences 7, 3769–3781 (2010).
doi: 10.5194/bg-7-3769-2010
Honeyman, B. D. & Santschi, P. H. A Brownian-pumping model for oceanic trace metal scavenging: evidence from Th isotopes. J. Mar. Res. 47, 951–992 (1989).
doi: 10.1357/002224089785076091
Wu, J., Boyle, E., Sunda, W. & Wen, L. S. Soluble and colloidal iron in the oligotrophic North Atlantic and North Pacific. Science 293, 847–849 (2001).
pubmed: 11486084
doi: 10.1126/science.1059251
Völker, C. & Tagliabue, A. Modeling organic iron-binding ligands in a three-dimensional biogeochemical ocean model. Mar. Chem. 173, 67–77 (2015).
doi: 10.1016/j.marchem.2014.11.008
Misumi, K. et al. Slowly sinking particles underlie dissolved iron transport across the Pacific Ocean. Glob. Biogeochem. Cycles 35, e2020GB006823 (2021).
doi: 10.1029/2020GB006823
Seferian, R. et al. Tracking improvement in simulated marine biogeochemistry between CMIP5 and CMIP6. Curr. Clim. Change Rep. 6, 95–119 (2020).
pubmed: 32837849
pmcid: 7431553
doi: 10.1007/s40641-020-00160-0
Raiswell, R., Benning, L. G., Tranter, M. & Tulaczyk, S. Bioavailable iron in the Southern Ocean: the significance of the iceberg conveyor belt. Geochem. Trans. 9, 7 (2008).
pubmed: 18513396
pmcid: 2440735
doi: 10.1186/1467-4866-9-7
von der Heyden, B. P., Roychoudhury, A. N., Mtshali, T. N., Tyliszczak, T. & Myneni, S. C. Chemically and geographically distinct solid-phase iron pools in the Southern Ocean. Science 338, 1199–1201 (2012).
pubmed: 23197531
doi: 10.1126/science.1227504
Curti, L. et al. Carboxyl-richness controls organic carbon preservation during coprecipitation with iron (oxyhydr)oxides in the natural environment. Commun. Earth Environ. 2, 229 (2021).
doi: 10.1038/s43247-021-00301-9
Rauschenberg, S. & Twining, B. S. Evaluation of approaches to estimate biogenic particulate trace metals in the ocean. Mar. Chem. 171, 67–77 (2015).
doi: 10.1016/j.marchem.2015.01.004
Twining, B. S. et al. Taxonomic and nutrient controls on phytoplankton iron quotas in the ocean. Limnol. Oceanogr. Lett. 6, 96–106 (2021).
doi: 10.1002/lol2.10179
Rudnick, R. L. & Gao, S. in Treatise on Geochemistry, Vol. 3 (eds Holland, H. D. & Turekian, K. K.) 1–64 (Elsevier, 2003).
Shelley, R. U., Morton, P. L. & Landing, W. M. Elemental ratios and enrichment factors in aerosols from the US-GEOTRACES North Atlantic transects. Deep Sea Res. II Top. Stud. Oceanogr. 116, 262–272 (2015).
doi: 10.1016/j.dsr2.2014.12.005
GEOTRACES Intermediate Data Product Group. The GEOTRACES Intermediate Data Product 2021 (IDP2021). https://doi.org/10.5285/cf2d9ba9-d51d-3b7c-e053-8486abc0f5fd (NERC EDS British Oceanographic Data Centre NOC, 2021).
Kwiatkowski, L., Aumont, O., Bopp, L. & Ciais, P. The impact of variable phytoplankton stoichiometry on projections of primary production, food quality, and carbon uptake in the global ocean. Glob. Biogeochem. Cycles 32, 516–528 (2018).
doi: 10.1002/2017GB005799
Ye, Y. & Völker, C. On the role of dust-deposited lithogenic particles for iron cycling in the tropical and subtropical Atlantic. Glob. Biogeochem. Cycles 31, 1543–1558 (2017).
doi: 10.1002/2017GB005663
Aumont, O., Ethé, C., Tagliabue, A., Bopp, L. & Gehlen, M. PISCES-v2: an ocean biogeochemical model for carbon and ecosystem studies. Geosci. Model Dev. 8, 2465–2513 (2015).
doi: 10.5194/gmd-8-2465-2015
Hamilton, D. S. et al. Recent (1980 to 2015) trends and variability in daily‐to‐interannual soluble iron deposition from dust, fire, and anthropogenic sources. Geophys. Res. Lett. 47, e2020GL089688 (2020).
doi: 10.1029/2020GL089688
Liu, X. & Millero, F. J. The solubility of iron in seawater. Mar. Chem. 77, 43–54 (2002).
doi: 10.1016/S0304-4203(01)00074-3