Organic carbon flux and organic carbon to calcite flux ratio recorded in deep-sea carbonates: Demonstration and a new proxy

Using rare earth elements to constrain particulate organic carbon flux in the East China Sea

Fluxes of particulate organic carbon (POC) in the East China Sea (ECS) have been reported to decrease from the inner continental shelf towards the outer continental shelf. Recent research has shown that POC fluxes in the ECS may be overestimated due to active sediment resuspension. To better characterize the effect of sediment resuspension on particle fluxes in the ECS, rare earth elements (REE...

Corrigendum: Using rare earth elements to constrain particulate organic carbon flux in the East China Sea

Fluxes of particulate organic carbon (POC) in the East China Sea (ECS) have been reported to decrease from the inner continental shelf towards the outer continental shelf. Recent research has shown that POC fluxes in the ECS may be overestimated due to active sediment resuspension. To better characterize the effect of sediment resuspension on particle fluxes in the ECS, rare earth elements (REE...

Seasonal organic carbon flux in the Fraser River

Introduction Conclusions References

Global Distribution and Magnitude of Deep Particulate Organic Carbon Fluxes Estimated by Benthic Flux Measurements

What controls the mixed-layer depth in deep-sea sediments? The importance of particulate organic carbon flux

Smith and Rabouille (2002; hereafter SR02) have examined the relationships between the mixed-layer depth in deep-sea sediments, L, as based on 210Pb and 14C profiles, and a set of environmental variables that include particulate organic carbon (POC) flux, oxygen penetration depth, and oceanographic depth. They have established the existence of a strong nonlinear correlation between their operat...