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Iron isotope fractionation in a sulfide-bearing subterranean estuary and its potential influence on oceanic Fe isotope flux

Moutusi Roy 1, 2, * Olivier Rouxel 3, 4, 5 Jonathan Martin 1 Jaye Cable 6
* Corresponding author
1 UF|Geological - Department of Geological Sciences [Gainesville]
2 College of Oceanic and Atmospheric Sciences [Corvallis]
3 LDO - Domaines Océaniques
4 GM - Unité de recherche Géosciences Marines (Ifremer)
5 WHOI - Woods Hole Oceanographic Institution
6 Department of Marine Sciences
Abstract : We trace pathways of Fe reactions in the Indian River Lagoon (Florida, USA) subterranean estuary using Fe isotopes to provide new constraints on Fe-isotopic fractionation in a sulfide-bearing subterranean estuary. Porewater δ 56Fe values increase from -1.16‰ at 115cm depth to +0.2‰ at 7cm depth due to isotope fractionation in three distinct lithostratigraphic zones. The deepest zone contains orange sands with elevated Fe-oxide contents (0.2wt.%) that dissolve through diagenetic Fe-oxide reduction and elevate Fe concentrations in porewaters (100 to 300μM/l). This reaction causes porewater δ 56Fe values to be ~1‰ lighter than the sediment δ 56Fe values. An intermediate zone contains white Fe-poor sands, with Fe-oxide contents <0.1wt.% and dissolved Fe concentrations <20μM/l. This zone is a sink for dissolved Fe through adsorption of isotopically heavy dissolved Fe(II) onto mineral surfaces. This adsorption results in porewater δ 56Fe values that are as much as 1.8‰ lighter than sediment δ 56Fe values. The uppermost zone contains organic carbon and Fe-sulfide rich black sediments with low dissolved Fe (<1μM/l) and elevated porewater sulfide (up to 600μM/l) concentrations. Precipitation of isotopically light Fe-sulfides increases the porewater δ 56Fe values as much as 0.68‰ more than corresponding sediment δ 56Fe values. The near-surface Fe-sulfide precipitation delivers to the lagoon dissolved Fe with slightly positive δ 56Fe values, averaging about +0.24‰, via submarine groundwater discharge (SGD). Iron-sulfide precipitation in sulfide-containing subterranean estuaries thus may result in a previously unidentified source of isotopically heavy Fe to the coastal oceans.
Keywords : Coastal sediments Indian River Lagoon Iron diagenesis Iron isotopes Submarine groundwater discharge (SGD) Subterranean estuary
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Submitted on : Tuesday, March 27, 2012 - 4:10:51 PM
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Moutusi Roy, Olivier Rouxel, Jonathan Martin, Jaye Cable. Iron isotope fractionation in a sulfide-bearing subterranean estuary and its potential influence on oceanic Fe isotope flux. Chemical Geology, Elsevier, 2012, 300-301, pp.133-142. ⟨10.1016/j.chemgeo.2012.01.022⟩. ⟨insu-00683059⟩

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