Temporal variability of Δ14C, δ13C, and C/N in sinking particulate organic matter at a deep time series station in the northeast Pacific Ocean
A 6‐year time series of Δ14C, δ13C, and C/N measurements in deep sinking particulate organic matter (POM) is presented for an abyssal site, Station M in the northeast Pacific Ocean. The Δ14C values revealed that sinking POM at 3450 m depth (650 m above bottom) contained old carbon despite its presum...
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Veröffentlicht in: | Global biogeochemical cycles 2004-12, Vol.18 (4), p.GB4015.1-n/a |
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