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| Titel |
Oxygen penetration deep into the sediment of the South Pacific gyre |
| VerfasserIn |
J. P. Fischer, T. G. Ferdelman, S. D'Hondt, H. Røy, F. Wenzhöfer |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1726-4170
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| Digitales Dokument |
URL |
| Erschienen |
In: Biogeosciences ; 6, no. 8 ; Nr. 6, no. 8 (2009-08-07), S.1467-1478 |
| Datensatznummer |
250003941
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| Publikation (Nr.) |
 copernicus.org/bg-6-1467-2009.pdf |
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| Zusammenfassung |
| Sediment oxygen concentration profiles and benthic microbial oxygen
consumption rates were investigated during an IODP site survey in the South
Pacific Gyre. Primary production, particle fluxes and sedimentation rates are
extremely low in this ultra-oligotrophic oceanic region. We derived O2
consumption rates from vertical oxygen profiles in sediments obtained on
different spatial scales ex situ (in piston cores and multi cores), and in
situ (using a benthic lander equipped with a microelectrode profiler). Along
a transect in the area 24 to 46° S and 165 to 117° W, cores
from 10 out of 11 sites were oxygenated over their entire length (as much as
8 m below seafloor), with deep O2 concentrations
>150 μmol L−1. This represents the deepest oxygen penetration
ever measured in marine sediments. High-resolution microprofiles from the
surface sediment layer revealed a diffusive oxygen uptake between 0.1 and
1.3 mmol m−2 d−1, equal to a carbon mineralization rate of
~0.4–4.5 gC m−2 yr−1. This is in the lower range of
previously reported fluxes for oligotrophic sediments but corresponds well to
the low surface water primary production. Half of the pool of reactive
organic matter was consumed in the top 1.5–6 mm of the sediment. Because of
the inert nature of the deeper sediment, oxygen that is not consumed within
the top centimeters diffuses downward to much greater depth. In deeper zones,
a small O2 flux between 0.05 and 0.3 μmol m−2 d−1 was
still present. This flux was nearly constant with depth, indicating extremely
low O2 consumption rates. Modeling of the oxygen profiles suggests that
the sediment is probably oxygenated down to the basalt, suggesting an oxygen
flux from the sediment into the basaltic basement. |
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