Iron speciation in aerosol dust influences iron bioavailability over glacial-interglacial timescales
Autor: | Cristiano Varin, Paul Vallelonga, Natalie Kehrwald, Piero Zennaro, Carlo Barbante, Jacopo Gabrieli, Claude F. Boutron, Andrea Spolaor, G. Cozzi |
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Rok vydání: | 2013 |
Předmět: |
Carbon dioxide in Earth's atmosphere
010504 meteorology & atmospheric sciences media_common.quotation_subject Last Glacial Maximum 010501 environmental sciences 01 natural sciences Speciation Geophysics Deposition (aerosol physics) Oceanography Ice core 13. Climate action Environmental chemistry Phytoplankton Interglacial General Earth and Planetary Sciences 14. Life underwater Glacial period Geology 0105 earth and related environmental sciences media_common |
Zdroj: | Geophysical Research Letters. 40:1618-1623 |
ISSN: | 0094-8276 |
DOI: | 10.1002/grl.50296 |
Popis: | [1] Iron deposition influences primary production and oceanic sequestration of atmospheric carbon dioxide (CO2). Iron has two oxidation states, Fe(II) and Fe(III), with Fe(II) being more soluble and available for oceanic phytoplankton uptake. The past proportions of soluble iron in aerosol dust remain unknown. Here we present iron speciation (Fe2+ and Fe3+) in the Antarctic Talos Dome ice core over millennial time scales. We demonstrate that iron speciation over the last 55 kyr is linked to increasing quantities of fine dust (FD) (0.7–5 µm) and intensified long-range dust transport. We propose that Fe(II) and Fe2+ production is principally enhanced in FD by photoreduction, although pH and organic complexation may also contribute to the speciation dynamics. During the Last Glacial Maximum, Fe2+ concentrations in dust increased by up to seven times more than interglacial levels, while Fe3+ only doubled. Cold and dusty climatic periods may increase the percentage of biologically available Fe(II) and Fe2+ deposited in the nutrient-limited Southern Ocean, allowing greater phytoplankton uptake and perhaps increased CO2 drawdown. |
Databáze: | OpenAIRE |
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