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dc.contributor.authorRouxel, Olivier J.  Concept link
dc.contributor.authorSholkovitz, Edward R.  Concept link
dc.contributor.authorCharette, Matthew A.  Concept link
dc.contributor.authorEdwards, Katrina J.  Concept link
dc.date.accessioned2008-08-25T13:15:43Z
dc.date.available2008-08-25T13:15:43Z
dc.date.issued2008-04-25
dc.identifier.urihttps://hdl.handle.net/1912/2352
dc.descriptionAuthor Posting. © Elsevier B.V., 2008. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Geochimica et Cosmochimica Acta 72 (2008): 3413-3430, doi:10.1016/j.gca.2008.05.001.en
dc.description.abstractDissolved Fe concentrations in subterranean estuaries, like their river-seawater counterparts, are strongly controlled by non-conservative behavior during mixing of groundwater and seawater in coastal aquifers. Previous studies at a subterranean estuary of Waquoit Bay on Cape Cod, USA demonstrate extensive precipitation of groundwater-borne dissolved ferrous iron and subsequent accumulation of iron oxides onto subsurface sands. Waquoit Bay is thus an excellent natural laboratory to assess the mechanisms of Fe-isotope fractionation in redoxstratified environments and determine potential Fe-isotope signatures of groundwater sources to coastal seawater. Here, we report Fe isotope compositions of iron-coated sands and porewaters beneath the intertidal zone of Waquoit Bay. The distribution of pore water Fe shows two distinct sources of Fe: one residing in the upward rising plume of Fe-rich groundwater and the second in the salt-wedge zone of pore water. The groundwater source has high Fe(II) concentration consistent with anoxic conditions and yield δ56Fe values between 0.3 and –1.3‰. In contrast, sediment porewaters occurring in the mixing zone of the subterranean estuary have very low δ56Fe values down to –5‰. These low δ56Fe values reflect Fe-redox cycling and result from the preferential retention of heavy Fe-isotopes onto newly formed Fe-oxyhydroxides. Analysis of Feoxides precipitated onto subsurface sands in two cores from the subterranean estuary revealed strong δ56Fe and Fe concentration gradients over less than 2m, yielding an overall range of δ56Fe values between –2 and 1.5‰. The relationship between Fe concentration and δ56Fe of Fe-rich sands can be modeled by the progressive precipitation of Fe-oxides along fluid flow through the subterranean estuary. These results demonstrate that large-scale Fe isotope fractionation (up to 5‰) can occur in subterranean estuaries, which could lead to coastal seawater characterized by very low δ56Fe values relative to river values.en
dc.description.sponsorshipThis study was supported by the National Science Foundation (OCE 0550066) to OR and ES , (OCE 0095384) to MC and ES and NASA Astrobiology Institute - Cycle 3 CAN-02-OSS-02 to KJE.en
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen
dc.relation.urihttps://doi.org/10.1016/j.gca.2008.05.001
dc.titleIron isotope fractionation in subterranean estuariesen
dc.typePreprinten


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