Upper Ocean Carbon Export and the Biological Pump¶
Ducklow, Steinberg, & Buesseler. (2001). Upper Ocean Carbon Export and the Biological Pump.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Marine Snow
- The resulting export flux, measured in mg C m⁻² d⁻¹ at reference depths (typically 100–200 m), closes the column budget connecting surface primary production, deep-water oxygen consumption, and the sequestration of carbon in sediments on millennial timescales.
This sourceThe biological pump's particle export out of the surface layer as measured by sediment traps, tracking the large-scale rate of new production.
Supported in partVerified against the work's full text
“that the flux of particles out of the surface layer, as measured by sediment traps, generally approximated the large-scale rate of new production.”
- The resulting export flux, measured in mg C m⁻² d⁻¹ at reference depths (typically 100–200 m), closes the column budget connecting surface primary production, deep-water oxygen consumption, and the sequestration of carbon in sediments on millennial timescales.
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Registry ID ref:aa7a380a4fe0 · see in the full table