RARE EARTH ELEMENT CYCLING IN THE PORE WATERS OF THE BERING SEA SLOPE (IODP EXP. 323)
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Title
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RARE EARTH ELEMENT CYCLING IN THE PORE WATERS OF THE BERING SEA SLOPE (IODP EXP. 323)
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Other Titles
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배링해 퇴적물 공극수 회토류 원소 지화학 성질 연구
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Authors
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Huh, Youngsook
Tseren-Ochir, Soyol-Erdene
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Keywords
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REE; diagenesis; fractionation
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Issue Date
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2012
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Citation
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Huh, Youngsook, Tseren-Ochir, Soyol-Erdene. 2012. RARE EARTH ELEMENT CYCLING IN THE PORE WATERS OF THE BERING SEA SLOPE (IODP EXP. 323). KOPRI. KOPRI. 2012.11.26~.
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Abstract
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We studied the diagenetic behavior of rare earth elements in a highly productive passive margin
setting of the Bering Sea Slope. Pore water concentrations of fourteen REEs were determined to a
depth of ~140 meters below seafloor (mbsf). Site U1345 was drilled during the Integrated Ocean
Drilling program (IODP) Expedition 323 at a water depth of 1008 m presently in the center of an
oxygen minimum zone. The concentrations of REEs were enriched in the pore water relative to deep
seawater indicating that there is significant liberation from sediment during diagenesis. There
was a peak at ~ 10 mbsf, which was more pronounced for the HREE, whose depth coincided with those
of dissolved iron and manganese and below the sulfate-methane transition zone (~6.3 mbsf). In the
upper 1 mbsf, there is a minor peak in HREE. Below ~40 mbsf, the concentration profiles were
relatively constant. The positive Ce anomaly was relatively constant (average shale-normalized
Ce/Ce*=1.1±0.2) throughout the depth profile indicating that Ce depletion in seawater is
completely regenerated and maintained. HREE-enrichment is observed for the entire 140 mbsf except
for the upper ~1 mbsf where there is MREE-bulge. REE release in the shallow depths (upper ~1 m) is
attributed to preferential release of LREEs and MREEs during organoclastic reduction of Fe, Mn
hydroxides in anoxic sediments. The high HREE concentrations observed Site U1345 was drilled during the Integrated Ocean
Drilling program (IODP) Expedition 323 at a water depth of 1008 m presently in the center of an
oxygen minimum zone. The concentrations of REEs were enriched in the pore water relative to deep
seawater indicating that there is significant liberation from sediment during diagenesis. There
was a peak at ~ 10 mbsf, which was more pronounced for the HREE, whose depth coincided with those
of dissolved iron and manganese and below the sulfate-methane transition zone (~6.3 mbsf). In the
upper 1 mbs
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URI
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https://repository.kopri.re.kr/handle/201206/8392
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Conference Name
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KOPRI
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Conference Place
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KOPRI
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Conference Date
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2012.11.26~
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Type
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Proceeding
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Indexed
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Pro(초록)국외
- Appears in Collections
- 2012-2012, Variations in atmospheric platinum group elements in Dome C (East Antarctica) over the last 800 Millenium years (12-12) / Tseren-Ochir Soyol-Erdene (PE12270)
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