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Status: Bibliographieeintrag

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Verfasst von:Corkill, Matthew [VerfasserIn]   i
 Meiners, Klaus Martin [VerfasserIn]   i
 Wongpan, Pat [VerfasserIn]   i
 van der Merwe, Pier [VerfasserIn]   i
 Creac'h, Layla [VerfasserIn]   i
 Feig, Sandrin [VerfasserIn]   i
 Nelson, Talitha [VerfasserIn]   i
 Smith, Abigail Jessica Rose [VerfasserIn]   i
 Townsend, Ashley T. [VerfasserIn]   i
 Twiname, Samantha [VerfasserIn]   i
 Lannuzel, Delphine [VerfasserIn]   i
Titel:Dissolved iron release by sediment and dust particles in Antarctic seawater greater than glacial flour and sea-ice particles
Verf.angabe:Matthew Corkill, Klaus Martin Meiners, Pat Wongpan, Pier van der Merwe, Layla Creac'h, Sandrin Feig, Talitha Nelson, Abigail Jessica Rose Smith, Ashley T. Townsend, Samantha Twiname, Delphine Lannuzel
E-Jahr:2025
Jahr:May 2025
Umfang:14 S.
Illustrationen:Illustrationen
Fussnoten:Online verfügbar 21 February 2025, Version des Artikels 28 February 2025 ; Gesehen am 23.07.2025
Titel Quelle:Enthalten in: Marine chemistry
Ort Quelle:Amsterdam [u.a.] : Elsevier Science, 1972
Jahr Quelle:2025
Band/Heft Quelle:270(2025) vom: Mai, Artikel-ID 104509, Seite 1-14
ISSN Quelle:0304-4203
Abstract:Primary productivity by phytoplankton in the Southern Ocean can be limited by low iron concentrations. Iron limitation in the surface ocean around Antarctica may be alleviated by particle dissolution of dust from exposed rock, glacial flour, resuspended marine sediment, and sea ice. Ligands, which are ubiquitous in seawater, chelate some metals and keep them in solution. Ligands are thereby thought to increase metal solubility, including iron. Leaching studies of Antarctic particles from various sources are rare but important due to observed and predicted changes occurring around Antarctica, e.g., changes in sea ice and ice-free areas on the continent. Here, we quantified the solubility of iron in different particle types using vertical flow-through leaching experiments that simulated sinking through the water column and ran for 78 min of flow at 4 °C under trace metal-clean conditions. Both unaltered and ultraviolet-irradiated seawater leaching solution treatments were used to test the effect of organic ligands on iron dissolution, which was found to be non-significant. Sediment and dust released the most dissolved iron to seawater, followed by glacial flour, and then sea-ice particles (9.00 ± 9.92 × 10−2 and 3.18 ± 3.79 × 10−2, 1.97 ± 1.79 × 10−4, 1.37 ± 0.90 × 10−9 g DFe/100 g material, respectively). We discuss these laboratory results in relation to particle availability and how this may affect the supply of dissolved iron to Antarctic surface waters.
DOI:doi:10.1016/j.marchem.2025.104509
URL:Bitte beachten Sie: Dies ist ein Bibliographieeintrag. Ein Volltextzugriff für Mitglieder der Universität besteht hier nur, falls für die entsprechende Zeitschrift/den entsprechenden Sammelband ein Abonnement besteht oder es sich um einen OpenAccess-Titel handelt.

kostenfrei: Volltext: https://doi.org/10.1016/j.marchem.2025.104509
 kostenfrei: Volltext: https://www.sciencedirect.com/science/article/pii/S0304420325000246
 DOI: https://doi.org/10.1016/j.marchem.2025.104509
Datenträger:Online-Ressource
Sprache:eng
Sach-SW:Fe
 Leach
 Ligands
 Southern Ocean
K10plus-PPN:1931587671
Verknüpfungen:→ Zeitschrift

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