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Title: History and geochemistry of a metalliferous sediment core from the Mid-Atlantic Ridge at 26 degree N

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
;  [1];  [2]
  1. Florida Institute of Technology, Melbourne (USA)
  2. NOAA-AOML-OCD, Miami, FL (USA)

Fourteen thousand years of hydrothermal deposition are recorded in a metalliferous sediment core recovered from the Trans-Atlantic Geotraverse (TAG) Hydrothermal Field on the Mid-Atlantic Ridge at 26{degree}N. An estimated 26 to > 96% of the sediment at this core site is hydrothermally derived as determined from the CaCO{sub 3}, Al and Fe data. Layers of essentially pure vent precipitates contain < 3% CaCO{sub 3} and < 0.5% Al, with high concentrations of Fe (43%), Cu (4.1%), Zn (1.2%), Mn (1.1%), V (480 ppm), Pb (175 ppm), Cd (32 ppm) and Hg (3.8 ppm). Sediment accumulation rates vary from {approximately}1 to > 30 g/cm{sup 2}/1,000 y throughout the core, a function of the intensity of hydrothermal inputs. Distinct hydrothermal events are recorded at 6,000 and 8,500 y B.P. in layers containing > 90% vent-derived material. Vertical metal profiles and interelement relationships in the core result from variable deposition of oxides and sulfides, oxidation and dissolution of sulfide phases and scavenging of metals from seawater.

OSTI ID:
5231398
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Vol. 52:10; ISSN 0016-7037
Country of Publication:
United States
Language:
English