Fluxes to sediments underlying the Rainbow hydrothermal plume at 36°14′N on the Mid-Atlantic Ridge
- 21 March 2002
- journal article
- Published by Elsevier
- Vol. 66 (11) , 1905-1923
- https://doi.org/10.1016/s0016-7037(02)00823-2
Abstract
No abstract availableKeywords
This publication has 71 references indexed in Scilit:
- The rainbow vent fluids (36°14′N, MAR): the influence of ultramafic rocks and phase separation on trace metal content in Mid-Atlantic Ridge hydrothermal fluidsPublished by Elsevier ,2002
- Hydrography and high‐temperature heat flux of the Rainbow hydrothermal site (36°14′N, Mid‐Atlantic Ridge)Journal of Geophysical Research: Oceans, 2001
- Constraints on the energy and chemical balances of the modern TAG and ancient Cyprus seafloor sulfide depositsJournal of Geophysical Research, 2000
- Detection of mineral dust over the North Atlantic Ocean and Africa with the Nimbus 7 TOMSJournal of Geophysical Research: Atmospheres, 1999
- Phosphorus accumulation in marine sediments and the oceanic phosphorus cycleGlobal Biogeochemical Cycles, 1998
- Air‐borne dust fluxes to a deep water sediment trap in the Sargasso SeaGlobal Biogeochemical Cycles, 1998
- The Rainbow Hydrothermal Plume, 36°15′N, MARGeophysical Research Letters, 1996
- Modern and Last Glacial Maximum eolian sedimentation patterns in the Atlantic Ocean interpreted from sediment iron oxide contentPaleoceanography and Paleoclimatology, 1995
- The geochemical evolution of the continental crustReviews of Geophysics, 1995
- Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the HolocenePaleoceanography and Paleoclimatology, 1988