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Sedimentary mechanisms of a modern banded iron formation on Milos Island, Greece
Stockholms universitet, Naturvetenskapliga fakulteten, Institutionen för geologiska vetenskaper. Cardiff University, UK.
Stockholms universitet, Naturvetenskapliga fakulteten, Institutionen för geologiska vetenskaper.
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Antal upphovsmän: 82018 (Engelska)Ingår i: Solid Earth, ISSN 1869-9510, E-ISSN 1869-9529, Vol. 9, nr 3, s. 573-598Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

An early Quaternary shallow submarine hydrothermal iron formation (IF) in the Cape Vani sedimentary basin (CVSB) on Milos Island, Greece, displays banded rhythmicity similar to Precambrian banded iron formation (BIF). Field-wide stratigraphic and biogeochemical reconstructions show two temporal and spatially isolated iron deposits in the CVSB with distinct sedimentological character. Petrographic screening suggests the presence of a photoferrotrophic-like microfossil-rich IF (MFIF), accumulated on a basement consisting of andesites in a similar to 150 m wide basin in the SW margin of the basin. A banded nonfossiliferous IF (NFIF) sits on top of the Mn-rich sandstones at the transition to the renowned Mn-rich formation, capping the NFIF unit. Geochemical data relate the origin of the NFIF to periodic submarine volcanism and water column oxidation of released Fe(II) in conditions predominated by anoxia, similar to the MFIF. Raman spectroscopy pairs hematite-rich grains in the NFIF with relics of a carbonaceous material carrying an average delta C-13 org signature of similar to-25%0. A similar delta C-13 org signature in the MFIF could not be directly coupled to hematite by mineralogy. The NFIF, which postdates large-scale Mn deposition in the CVSB, is composed primarily of amorphous Si (opal-SiO2 center dot nH(2)O) while crystalline quartz (SiO2) predominates the MFIF. An intricate interaction between tectonic processes, changing redox, biological activity, and abiotic Si precipitation are proposed to have collectively formed the unmetamorphosed BIF-type deposits in a shallow submarine volcanic center. Despite the differences in Precambrian ocean-atmosphere chemistry and the present geologic time, these formation mechanisms coincide with those believed to have formed Algoma-type BIFs proximal to active seafloor volcanic centers.

Ort, förlag, år, upplaga, sidor
2018. Vol. 9, nr 3, s. 573-598
Nationell ämneskategori
Geovetenskap och miljövetenskap
Identifikatorer
URN: urn:nbn:se:su:diva-156805DOI: 10.5194/se-9-573-2018ISI: 000431413300001OAI: oai:DiVA.org:su-156805DiVA, id: diva2:1210821
Tillgänglig från: 2018-05-29 Skapad: 2018-05-29 Senast uppdaterad: 2018-11-19Bibliografiskt granskad

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Chi Fru, ErnestRattray, Jayne E.Broman, Curt
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Institutionen för geologiska vetenskaper
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Solid Earth
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