Open AccessIs methane venting at the seafloor recorded by δ 13 C of benthic foraminifera shells?
Author(s) -
Torres M. E.,
Mix A. C.,
Kinports K.,
Haley B.,
Klinkhammer G. P.,
McManus J.,
de Angelis M. A.
Publication year - 2003
Publication title -
paleoceanography
Language(s) - English
Resource type - Journals
eISSN - 1944-9186
pISSN - 0883-8305
DOI - 10.1029/2002pa000824
Subject(s) - foraminifera , geology , benthic zone , calcite , anaerobic oxidation of methane , chemosynthesis , methane , carbonate , cold seep , seawater , oceanography , authigenic , geochemistry , mineralogy , diagenesis , paleontology , chemistry , hydrothermal vent , hydrothermal circulation , organic chemistry
The isotopic composition of the dissolved inorganic carbon (DIC) collected at sites of active methane discharge on Hydrate Ridge, Oregon, reveals anaerobic methane oxidation mediated by bacteria, with δ 13 C DIC reaching values as low as −48‰ in the upper 4 cm of the sediment. In spite of the high sulfide levels in the discharging fluids, living specimens of the benthic foraminifera Uvigerina peregrina are abundant in the vents, probably owing to the rich bacterial food source. Although pore water δ 13 C DIC is extremely low (−6 to −48‰), the δ 13 C values of living (Rose Bengal stained) foraminifera shells collected from active methane seeps are not significantly lower than those observed in nonventing pelagic sediments, and are within the range expected from local organic matter decomposition (0 to −4‰). The apparent δ 13 C disequilibrium between biogenic calcite and DIC suggests that at seep localities, foraminifera calcify mostly during periods when there is little methane discharge or during intermittent episodes of seawater flow into the sediments. The isotopic composition and Mg/Ca ratios of fossil (unstained) foraminifera recovered at carbonate‐rich sites on the northern Hydrate Ridge reveals overprinting of the biogenic record by inorganic calcite with high Mg/Ca and anomalously low δ 13 C values. Thus overprinting of the original isotopic composition of foraminifera by overgrowths or recrystallization at or below the sediment surface, rather than primary calcification in contact with 13 C depleted DIC, can explain extreme 13 C depletion observed in fossil foraminifera recovered from sites of active methane discharge.