Hydrothermal nontronite formation at Eolo Seamount (Aeolian volcanic arc, Tyrrhenian Sea). - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Chemical Geology Année : 2007

Hydrothermal nontronite formation at Eolo Seamount (Aeolian volcanic arc, Tyrrhenian Sea).

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Vesselin M. Dekov
  • Fonction : Auteur
George D. Kamenov
  • Fonction : Auteur
Jens Stummeyer
  • Fonction : Auteur
Médard Thiry
Carlo Savelli
  • Fonction : Auteur
Wayne C. Shanks
  • Fonction : Auteur
Danielle Fortin
  • Fonction : Auteur
Erno Kuzmann
  • Fonction : Auteur
Attila Vertes
  • Fonction : Auteur

Résumé

A sediment core containing a yellowish-green clay bed was recovered from an area of extensive hydrothermal deposition at the SE slope of the Eolo Seamount, Tyrrhenian Sea. The clay bed is composed of pure nontronite (described for the first time in the Tyrrhenian Sea), which appears to be the most aluminous nontronite ever found among the seafloor hydrothermal deposits. The high Al content suggests precipitation from Al-containing hydrothermal solutions. The REE distribution of the Eolo nontronite has a V-shape pattern. The heavy REE enrichment is in part due to their preferential partitioning in the nontronite structure. This enrichment was possibly further enhanced by the HREE preferential sorption on bacterial cell walls. The light REE enrichment is the result of scavenging uptake by one of the nontronite precursors, i.e., poorly-ordered Fe-oxyhydroxides, from the hydrothermal fluids. Oxygen isotopic composition of the nontronite yields a formation temperature of 30 °C, consistent with a low-temperature hydrothermal origin. The relatively radiogenicNd isotopic signature of the nontronite compared to the present-dayMediterranean seawater indicates that approximately half of Nd, and presumably the rest of the LREE, are derived from local volcanic sources. On the other hand, 87Sr/86Sr is dominated by present-day seawater Sr. Scanning electron microscopy investigation revealed that the nontronite is composed of aggregates of lepispheres and tube-like filaments, which are indicative of bacteria assisted precipitation. Bacteria inhabiting this hydrothermal site likely acted as reactive geochemical surfaces on which poorly-ordered hydrothermal Fe-oxyhydroxides and silica precipitated. Upon aging, the interactions of these primary hydrothermal precipitates coating bacterial filaments and cell walls likely led to the formation of nontronite. Finally, the well-balanced interlayer and layer charges of the crystal lattice of seafloor hydrothermal nontronite decrease its sorption capacity to zero.

Dates et versions

hal-00647193 , version 1 (01-12-2011)

Identifiants

Citer

Vesselin M. Dekov, George D. Kamenov, Jens Stummeyer, Médard Thiry, Carlo Savelli, et al.. Hydrothermal nontronite formation at Eolo Seamount (Aeolian volcanic arc, Tyrrhenian Sea).. Chemical Geology, 2007, 245, pp.103-119. ⟨10.1016/j.chemgeo.2007.08.006⟩. ⟨hal-00647193⟩
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