Towards a Better Understanding of Coastal Carbon Cycling and Sequestration: Quantifying Sinking Carbon in the Bedford Basin and Beyond
Abstract:
Here, we quantify seasonal changes in carbon export in Bedford Basin, an estuary on the Scotian Shelf off Eastern Canada during the 2019 spring bloom. We use the deficit of naturally occurring, particle reactive thorium-234 with respect to its conservative parent uranium-238 to quantify sinking carbon fluxes. While this method is well established for quantifying seasonal changes in the open ocean’s biological carbon pump, it’s use in complex coastal regimes is still rare.
In order to test the feasibility of quantifying carbon fluxes via the thorium-234/uranium-238 disequilibrium method, we measured thorium-234 and carbon in the water column, sinking particulates and the top most sediment in central Bedford Basin. Under steady state conditions, carbon fluxes determined from the water column deficit should match those derived from thorium-234 excess in the topmost sediments. If confirmed, this will open up the possibility of an alternative method for measuring carbon fluxes and deposition in coastal settings on time-scales of weeks to months, which could significantly aid our understanding of common environmental concerns, such as hypoxia, in these vulnerable regions. Preliminary results indicate a good agreement between water column and sediment fluxes of thorium-234 throughout the spring and summer 2019.