Geochemistry of hydrothermal sediments from ODP sites 834 and 835 in the Lau Basin, southwest Pacific

Geochemical investigations have been carried out on hydrothermally enriched metalliferous sediments collected at ODP Sites 834 and 835 in the Lau Basin. Enhanced hydrothermal inputs of both Mn and Fe occur in an acid-reducible oxide phase, unlike mid-ocean ridge sediments where Fe is mainly present in more resistant HCl soluble phases. Barium, V, Co, Ni, Cu, Zn, Pb and REEs mainly follow Mn and Fe in their behaviour and associations and are thought to be largely scavenged from seawater by Mn- and Fe-rich plume particulates, although there is a significant HCl soluble non-hydrothermal component of Ba present. Compositional differences between Eastern Lau Spreading Centre and Central Lau Spreading Centre hydrothermal sediments, and between them and hydrothermal sediments on mid-ocean ridges, are thought to be due to a combination of factors including temporal and areal variation in the composition of hydrothermal solutions, variation in hydrothermal flux to the sediments related to their proximity to propagator or spreading centre, and variable containment of the Lau Basin hydrothermal plume consequent on changing basin morphology through time. Our results are consistent with published models for the evolution of the Lau Basin and confirm that a time lag occurs between propagator passage and maximum hydrothermal flux to associated sediments. (C) 1997 Elsevier Science B.V.